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HomeMy WebLinkAboutLUA16-000963_Report 1Parametrix
ENGINEERING. PLANNING. ENVIRONMENTAL SCIENCES
'JI/II/I fif;w»rs .......
719 21\D i'WE:.NUE, $Lill E 200 I SE.AHLI:, WA 98104 ! P 206.394.3700
MEMORANDUM
DATE:
TO:
FROM:
SUBJECT:
CC:
December 6, 2016
Mathew Herrera
Katheryn Seckel
Steep Slope Exemption Request/ Changed Shoreline Mitigation Strategy Proposal
Jason Rich, King County Parks
Jenny Bailey, Parametrix
PROJECT NUMBER: 554-1521-084
PROJECT NAME: Lake to Sound Trail Segment A
This memorandum addresses two remaining elements for the City of Renton's approval regarding the Lake to
Sound Trail Project: 1) a Critical Areas Exemption for protected slope, and 2) approval for relocation of mitigation
that was previously approved by the hearings examiner (Shoreline Substantial Development Permit, Shoreline
Conditional Use Permit and Shoreline Variance, file number LUA15-000257 ECF, SSDP, S-CUP, S-V). Attachment A
includes a list of items submitted on behalf of the previous permit submittal -for purposes of this request, the
City of Renton waived the requirement to resubmit the permit materials listed. The following discusses each of
these permit approval items individually.
Critical Areas Exemption (for protected slope)
It was requested by the City of Renton that we file the attached (Attachment B) Critical Areas Exemption Short
Form to comply with the Hearing's Examiners conditions for the above referenced shoreline permit. And because
we already submitted a comprehensive package with the original permit application, it was requested that in lieu
of resubmitting the entire permit package, we instead provide a detailed narrative of the work that would occur
in the steep slope and identify where in the Geotechnical Report the bridge foundation is analyzed in order to
expedite the exemption. The following is a detailed narrative of the work to be performed in the protected slope.
For your reference, we have provided the final Geotechnical Report with this memorandum.
A prefabricated steel girder pedestrian bridge, approximately 110 feet long and 12feet wide, will be installed to
allow trail users to cross the Black River separately from vehicle traffic. The bridge wi/1 be located about 150 feet
east of the existing Monster Road bridge. The contractor will construct the foundation system, then hoist the
bridge with a crane to place it on the foundation. The crane will operate from the level area above the bank crest.
As described in Sections 3.3 and 4 of the Geotechnical Report, substrates in the vicinity of the bridge are relatively
deep, liquefiable soils that are prone to settlement and lateral spreading during a seismic event. Based on these
soils and the results of the slope stability analysis presented in Section 4.2 of the Geotechnical Report, ground
improvements wi/1 be necessary to improve seismic stability and to prevent undue lateral pressure on the bridge
foundation. The method to be employed is wet soil mixing, also known as the deep mixing method. This ground
improvement technique improves weak soils by mechanically mixing them with cementitious binder slurry. A
powerful drill constructs columns of stable soil by advancing an auger with radial mixing paddles located near the
bottom of the drill string. The binder slurry is pumped to the tool as it advances; additional soil mixing is achieved
as the tool is withdrawn.
December 6, 2016
Page 2 of 7
The deep mixing method creates columns of stabilized soil upon which the bridge foundations can be constructed.
A total of approximately 63 soil columns will be created in this manner, stabilizing an approximately 16-foot by
37-foot area on the south side of the river and an approximately 16-foot by 30-foot area on the north side of the
river. Each column will be approximately 4 feet in diameter and will extend 30 to 40 feet below existing grade.
Construction machinery that will be used includes trucks, backhoes, a trackhoe, compressors, pumps, a drill rig
(for wet soil mixing), and a crane for bridge placement. All above-ground elements of the bridge will be situated
upslope of the ordinary high water mark (OHWM}.
Mitigation Relocation
The project design has progressed since the 60-percent plans were submitted with the shoreline permit
applications. During that process, the proposed location of several Buffer Vegetation Conservation Areas (BVCAs)
have changed due to property and access constraints (see Attachment C). Specifically:
• King County cannot construct and maintain the BVCA originally envisioned within the property owned
by a railroad company (BCV2; Station 8+00 to 11+00). The railroad will allow only an easement for the
trail itself.
• The County also cannot construct or maintain a portion of a BCVA that would obstruct the existing
access road to the King County-operated pump station (BCVl; Station 105+00 to 107+00).
These two areas total approximately 15,125 square feet. It is important to note that King County has identified
equivalent areas in which to construct and maintain BCV As that are in the vicinity of the originally proposed areas.
The areas from east to west:
• East and west of the proposed pedestrian bridge (Station 17+00), the banks on both sides of the Black
River, which we are referring to as BVC4.
• East of the proposed pedestrian bridge, which we are referring to as BVC3.
• North of the Black River between the pump station access road and the river, within BCV2.
Under the approved permit, we proposed 42,741 square feet of BVCA. We are now proposing slightly more BVCA
for a total of 43,050 square feet. The new areas of proposed mitigation are commensurate, if not of higher value
to the area we removed under BVC2. We thank you for your consideration of these remaining permitting
requirements. Please Jenny Bailey, Parametrix, at (206) 394-3656 if you have questions.
'
Attachment A
Previous Permit Submittal List
Renton
Lake to Sound Regional Trail -Segment
Proposal Submittal Requirements
Item# Item
1. Pre-Application Meeting Summary:
2. Waiver Form:
3. Plat Certificate or Title Report: (Submitted on CD)
4. Land Use Permit Master Application Form:
5. Environmental Checklist:
6. Project Narrative:
Conditional Use Permit Justification:
Variance Justification
None Draft Legal Documents:
7. Construction Mitigation Description:
Fees:
Waiver Density Worksheet:
8. Full Size 60% Plan Set
Neighborhood Detail Map: (Part of Color Maps)
Site Plan: (Part of Color Maps)
Grading Plan, Conceptual: (Part of 60% Plan set, Sheets
9-17):
Landscape Plan, Conceptual: (Part of Color Maps):
Waiver Architectural Elevations:
Waiver Floor Plans:
Topography Map (Part of Color Maps):
Tree Cutting/Land Clearing (Tree Inventory) Plan: (Part
of 60% Plan set, Sheets 9-17, trees with Note 14)
9. Tree Retention Worksheet:
10. Wetland Assessment (Critical Area Report):
11. Standard Stream or Lake Study:
12. Habitat Data Report (Veg & Wildlife}:
Flood Hazard Data (Part of TIR):
Utilities Plan, Generalized {sewer, water, stormwater,
transportation improvements} (Part of 60% Plan Set):
13. Geotechnical Report (Draft}:
Drainage Control Plan (Part of 60% Plan Set):
14. Drainage Report (TIR):
Traffic Study: Include Parking Analysis (Included in #6.
Project Narrative Section 2.6.1)
Waived Urban Design Regulation Analysis
Photographs of Property
15. Plan Reductions: II W' 1111" (11 x 17) legible reduction of
each full size plan sheet
16. Colored Maps for Display
# of Copies
Submittal
5
5
3
12
12
12
None
5
$8,240
Waiver
12
Waiver
Waiver
4
2
12
12
12
5
4
4
Waived
Optional
1
1
Attachment B
Critical Exemption Form
CRITICAL AREAS EXEMPTION
Applicant Name
King County Parks, Jason
Rich
Parcel Number
(FOR SEPA EXEMPT ACTIVITIES)
Planning Division
1055 South Grady Way-Renton, WA 98057
Phone: 425-430-7200 Fax: 425-430-7231
Project Name
Lake to Sound Trail Segment A
Project Address
Phone Number
(206) 477-4582
722950-0281,377920-0090 The pedestrian bridge crossing of the Black River, for
which this critical area exemption pertains, is at 550
Monster Rd SW.
Brief Description of Project
King County, together with the cities of Renton and Tukwila, the Washington State Department of
Transportation (WSDOT), and the Federal Highway Administration (FHWA), is proposing to develop a
1.2-mile segment of what will ultimately be the 16-mlle Lake to Sound Trail. The 1.2-mlle segment is
referred to as Segment A of the Lake to Sound Trail, and is also commonly referred to as the Two
Rivers Trail. Segment A extends from Naches Avenue SW, parallel to the railroad tracks north of the
Black River Riparian Forest, across the Black River on a new non-motorized bridge and under two
railroad bridges to the Green River Trail at the north end of the Starfire Sports Complex In Fort Dent
Park.
Type of Critical Area t8) Work Occurs in D Work Occurs in Protected Slope Critical Area Buffer
PURPOSE: Exempt activities provided with a letter of exemption from the Development Services
Administrator may intrude into a critical area or required buffer (Subject to any conditions or
requirements provided by the Administrator).
APPLICABILITY OF EXEMPTIONS: The following is a general list of activities that may be exempt from the
critical areas regulations. More specific descriptions of the activities are contained in the Critical Areas
Regulations. Some of the listed activities may not be exempt in certain critical areas. The Planning
Division will evaluate you request according to the City of Renton Critical Areas Regulations in RMC 4-3-
050C, J, L, and N.
I AM REQUESTING A CRmCAL AREAS EXEMPTION FOR ONE OR MORE OF THE FOLLOWING ACTIVITIES:
D Conservation, Enhancement, and Related Activities:
• Conservation or preservation of soil, water, vegetation, fish, and other wildlife
• Enhancement activities as defined in chapter 4-11 RMC D;
• Any critical area, buffer restoration, or other mitigation activities that have been approved
by the City
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CUP\Rentpn\CrttiulAreasE11;t?mpl20ltS\AttachA_CAExemptShortFrm.dooc
D Research and Site Investigation:
• Nondestructive education and research
• Site investigative work necessary for land use application submlttals such as surveys, soil
logs, etc.
0 Agricultural, Harvesting, and Vegetation Management:
• Harvesting wild foods
• Existing/Ongoing agricultural activities 1
• Removal of dead, terminally diseased, damaged, or dangerous ground cover or hazardous
trees which have been certified as such by a forester, registered landscape architect, or
certified arborist
D Surface Water Alteration:
• New surface water discharges provided the discharge meets the requirements of the
Storm and Surface Water Drainage Regulations '2 3
• New or modified regional storm water facilities 1 2 3
• Flood hazard reduction 1 3 4 6
[gj Roads, Parks, Public and Private Utilities:
• Relocation of Existing Utilities out of Critical Area and Buffer
• Maintenance, operation, and repair of existing parks, trails, roads, facilities, and utilities 1 2
• Installation, construction, replacement, or operation of utilities, traffic control, and
walkways within existing improved right.if-way or easement 1 2
• Modification of existing utilities and streets by 10% or less 12 s
• Management and essential tree removal for public or private utilities, roads and public
parks 1
D Wetland Disturbance, Modification, and Removal:
• Any activity in small Category 3 wetlands ' 2 3 • s
• Temporary disturbances of a wetland due to construction activities that do not include
permanent filling 1 2 3 s
D Maintenance and Construction for Existing Uses and Facilities:
• Remodeling, replacing, or removing existing structures 1 2
• Normal and routine maintenance and repair of any existing public or private uses and
facilities where no alteration ofthe critical area and required buffer or additional fill
materials will be placed 1 2
• Construction activity connected with an existing single family residence or garage,
provided that no portion of the new work occurs closer to the critical area or required
buffers than the existing structure and/or the developed area of the site 1 2
• Existing activities which have not been changed, expanded or altered provided they
comply with the applicable requirements of chapter 4-10 RMC 1
D Emergency Activities:
• Removal of trees or ground cover by a City department, agency, public, or private utility in
an emergency situation
U:\PSO\Projeru\Oieot>\1S2l·kin1Co\5~-1S21-{)84 L2Sl'\02W8S\PH·A 2 Rlver,\Sh0<eline
CUP\Renton\Crttlc.ilAreasbempt2016\AttKhA_CAEJ:emptShortFrm,doo:
• Public interest emergency use, storage, and handling of hazardous materials by
governmental organizations in an Aquifer Protection Area
ADDITIONAL PERMITS: Additional permits from other agencies may be required. It is the applicant's
responsibility to obtain these other approvals. Information regarding these other requirements may be
found at http://apps.ecy.wa.gov/opas/
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D Exemption Granted
C.E. "Chip" Vincent, Planning Director
Planning Division
Conditions of Approval:
'Exemption does not apply in Aquifer Protection Areos
'Exemption does not apply In Flood Hozard Areas
'Exemption does not apply in Geologic Hozard Areas
4 Exemption does not apply in Habilal Conservation Areas
'Exemption does not apply In Streams and Lakes: Class 2 to 4
'Exemption does not apply in Wetlands
U:\PSO\Pro}ects\Oients.\l52l·K1ngCo\SS4-lS21-084 l..2Sl\02WBS\PH~A 2 Rivtts\Shoreline
CUP\Renton\CnticalAreasbemptl016\Attic:hA_C6,£xempt5hortfrm.docx
D Exemption Denied
Date
Attachment C
Mitigation Plan Changes
0
**
GREEN RNER .-----01-1~------
/.,,,,,--------------------0 *
j 1
~/-i **oO * ~ 0 0 * O * ~ 0
0 .: * * 0 * ~ \ f \~ GREEN RIVER TRIJL
1
~ . i!
CONSTRUCTION NOTES :
8 PLANTING AREA CLEARING AND GRUBBING STAKE OR FLAG
PROPOSED PLANTNG AREA LIMITS FOR >PPROVAL OF
PROJEC T REPRESENTATM: PRIOR TO STARTING CLEARING
WORK. CLEAR AND GRUB ROOTS AN D RE MOVE: ANO
DISPOSE or ALL UNWANTED VEGETATION IN THIS PLANTING
Afl.EA LEAVE SOIL IN PLACE. SEE SPECIFICATION FOR
UST or UNWANTED VEGETATION.
lo\ COUPOST. PLACE 3· LAYER COMPOST OVER THE ENTIRE
\_V SURFACE OF THIS PLANTING AREA.
0 WOOD CHIP MULCH. PLACE 3" LAYER WOOD CHIP MULCH.
GENERAL NOTES:
1. SEE SHEET MP6 AND FOR PLANTING DETAJLS AN D
REQUIREME NTS.
2. LOOSEN m Y SOILS IN PLANTNG AREAS COMPACTED
BY CONSTRUCTION ACTMTI ES BY RIPPING OR TILLING
THE AREA TO A DEPTH or 2~" '\.; ~ ,.,
, ·, '-""'-. ,w
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,~ """ "' I w '•" ' ~ "' '"o' '--~--w -~ -......___ ~ c-----<:-z ·-~ --' ,-
----~ -~-LINE ~--'
TREE REPLACEMENT CALCULATION FOR
3. PLANTING Afl.EA LIMITS ANO INTERPLANTING LOCATIONS
SHALL BE STAKED IN THE FIELD m o APPROVED BY
PROJECT REPRESENTATM: PRIOR TO PLANTING.
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SIGNIFICANT TREES
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PLAN ®
SCALE IN FEET ~ FORT DENT PARK
DIAUETER' or TREE
NUMBER or RE MOVED ('MEASURED
AT HEIGHT or 4 .5 FEET REPLACEMENT
FR OM THE GROUND) TREES REQU IRED
4-6 INCHES (SINGLE TRUNK);
2 INCHES (ANY TRUN K or A 3
MULTI -TRUNK TREE)
OVER 6-8 INCHES 4
OVER 8 -20 INCHES 6
OVER 20 INCHES 8
TOTAL
0 20 40
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FORT DENT PARK
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NUMBER or
TREES REM OVED
1
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10
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DAT£ leY I CESI CN(O
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~----1------------+---+---------,
ORA.wt.
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CH£CKED I I I OVEOKUTA J I 0. Kl
AP P!<
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' ------I -l' ___________ _ --------~
~"'°' II p •~"'"'" SW
SCA --• LANDs~.f~rsIRcHITECT . I R IVER TRA IL TO NACHES AVE <O @>Ii:/'@ " "'" ,~ .... ,,:;,c,,-.1 A,, N 656 O:W:'-C "; , ,,.,.~, ""' ::::~;:::.:.:~
~u
ENGINEERING PLANNING ENVIRONMENTAL K IE NCES
LAKE TO SOUND TRAIL
SEGMENT A
PROJECT NAME
NUM BER or
TRE ES TO
REPLACE ONSITE
3
8
30
, 6
57
~. ALL PLANTS TO BE SAVED mo PROTECTED WITHIN
CLEARING AND GRUBBING Afl.EAS WILL BE FLAGG ED BY
PROJECT RE PRESENTATIVE. NOTIF'I' ENGINEER 5 DAYS
PRIOR TO START or CLEARING ACTMTY. USE ON LY
HAND TOOLS AND METHODS WHEN WORKING INSIDE
THE ORIPLINE AREA or EXISTING TREES AND SHRUBS
5 . PLANT DEBRIS FROM REMOVAL OF INVASM: PLANTS
OR PRUN ING SHALL BE RE MOVED FROM THE SITE AN O
DISPOSED or PROPERLY.
LEGEND:
--------URBm CONSERVANCY BUFFER
WETLAND BOUNDARY
-------ORDINARY HIGH WATERLINE
• ~-----· DESIRABLE VEGETATION EDGE
EXISTING TREES
~x·~~--, ' ' . EXISTING TREES TO BE REMOVED
' . -' '
HABITAT LOG . SEE SHEET MP-6
* BRUSHPILE. SEE SHEET MP-6
TILL />REA 10 24" DEPTH
PLANTING QUANTITY TAB
-THIS SHEET ONLY-
.:, 1Mi;.vl ITE M I OUANTIT)'
TREE REPLACEMENT PLANTNG I
~~ NATM: CONIFER TR EES -SPACE 15 0.C .
LA: ~II'( I 10
41" W N I 14
oll KA ,, o U~t I 10
1' ~ NATIVE DECIDUOUS TREES -SPACE 15 0 .C.
"lv-LtAt MReo I 14
I'<. J
... m:r.hl N ASH 9
95% REVIEW SUB MITT AL
NOT FOR CONS TRUCT IO N
CRA'll1NC N O
48 OF 59
MITIGATION PLAN
ABBREVIATIONS:
ACP ASPHN.T CONCRCTE PAVEMENT PC
BOC BACK OF CURS PT
BOW BACK OF SIDEWALK P/L
BP BEGIN PROFILE PRC
BVCE BEGIN VERTICAL CURVE ELEVATION PUD
BVCS BEGIN VERTICAL CURVE STATION PV1
CB CATCH BAS IN R
C&G CURB AND GUTTER RT
C/L CENTERLINE ROW o r R/W
CONC CONCRCTE SD
CONST CONSTRUCTION SDMH
CMP CORRUGATED METAL PIPE ss
COR CITY OF RENTON STA
CP CONCRETE PIPE TOA
CSTC CRUSHED SURFACING TO P COURSE TEL
DIA DIAMETER TESC
DI, DIP DUCTILE IRON PIPE lYP
E EAST, EASTING VC
EOA EDGE OF ASPHALT VERT
EOG EDGE OF GRAVEL w
EOP
"' EDGE OF PAVEMENT ws
~ EP END PRO Fll£ WSDOT
;;;
] EVCE END VERTICAL CURB ELEVATION
t EVCS EN D VERTICAL CURB STATION ~
" EX, EXIST EXISTING i FOC FACE OF CURB li :
"'
FL FLANGE, FLOWUNE
~ G GAS
D
GB GRADE BREAK D
1
t HMA HOT MIX ASPHALT
~ HORIZ HORIZONTAL
0 ,t ID INDENTI FICATION
IE INVERT ELEVATION
1 KC KING COUNTY
~ LF LINEAR FEET
ii LP LOW POINT
'.;, LT LEFT "' j ME MATCH EXISTING
~ MIN MINIMUM 8 < ~ MON MONUMENT y
~ N NORTH, NORTHING
C
~ N.I.C. NOT IN CONTRACT
~ NO. NUMBER 0 I
~ NST NOT STEEPER THAN j OHWM ORDINARY HIGH WATER MARK
1 ¥
:j
~
j
0
" i
!
;; CITY OF RENTON LUA 15-00257 SSDP, S-CUP, AND S-V
!1£ /:::, I RE\15'0NS lo•TE l•v I D(S,f'b°VORAJ< < ..
DRAWN
M. MILLER
Oi[O<W
0 . KIKUTA
APPROVED
POINT OF CURVE
POINT OF TANGENT
PROPERlY LIN E
POINT OF REVERSE CURVATURE
PUBLI C UTILllY DISTRICT
POINT OF VERTICAL INTERSECTION
RADIU S
RIGKT
RIGKT-OF-WAY
STORM DRAIN
STOR MWATER MANHOLE
SANITARY SEWER
STATION
THRESHOLD DISCHARGE AREA
TELEPHONE
TEIAPORARY EROSION AND SEDIMENT CONTROL
lYPICAL
VERTICAL CURVE
VERTICAL
WATER
WATER SERVICE
WASHINGTON STATE
DEPARTMENT OF TRANSPORTATION
O N E INCH AT F U L L SCAL E .
IF N OT, SCALE ACCORDING L Y
03
--INDEX TO DRAWINGS
DWGNO. SHTNO. SHEET TITLE
GENERAL
1 G1 COVER SHEET
2 G2 ABBREVIATIONS AND SH EET UST
3 G3 LEGEND
4 G4 SURVEY CONTROL PLAN
5 G5 SURVEY CONTROL PLAN
6 G6 A-LINE CONSTRUCTI ON BASELINE CONTIROL
7 G7 C-UNE CONSTRUCTION BASELIN E CONTROL
8 G8 B-LINE CONSTRUCTION BASELINE CONTROL
SITE PREPARATION
9 TESCl CLEARING, GRADING AND TESC PLAN
10 TESC2 CLEARING, GRADING AND TESC PLAN
11 TESC 3 CLEARING. GRADING AND TESC PLAN
12 TESC 4 CLEARING, GRADING AN D TESC PLAN
13 TESC5 CLEARING, GRADING AND TESC PLAN
14 TESC6 CLEARING, GRADING AN D TESC PLAN
15 TESC7 CLEARING. GRADING AND TESC PLAN
16 TESC8 CLEAR ING , GRADING AND TESC PLAN
17 TESC9 CLEARING , GRADING AND TESC PLAN
TYPICAL SECTIONS
18 CS 1 TYP ICAL CROSS SECTIONS
PLAN & PROFILE
19 Cl PLAN AND PROFll£
20 C2 PLAN AND PROFll£
21 C3 PLAN AND PROFlLE
22 C4 PLAN AND PROFll£
23 C5 INTERSECTION PLAN
24 C6 PLAN AND PR0Fl l£
25 C7 PLAN AND PROFILE
26 CB PLAN AND PROFll£
27 C9 PLAN AND PROFll£
28 c,o PLAN AND PROFll£
29 C11 PLAN AND PROFIUE
30 C12 PLAN AND PROFILE
31 C13 PLAN AND PROFILE
32 Cl 4 PLAN AND PROFll£
33 C15 SIGN SCHEDUUE AND GRADING DETAI L
34 C16 GRADING PLAN
STORM DRAINAGE
35 SDl CULVERT DETAILS
WALL PROFILES
36 WP1 GRAVllY BLOCK WALL PROFlUES
DETAILS
37 0 1 DETAILS
38 02 DETAILS
39 D3 DETAILS
40 D4 DETAILS
SIGNALIZATION
41 TSl SIGNAL PLAN
42 TS2 SIGNAL WIRING DIAGRAM
43 TS3 SIGNAL POL£ SCHEDUUE AND DETAI LS
STRUCTURAL
44 S1 BRIDGE PLAN ANO ELEVATION
45 S2 BRIDGE FOUNDATION LAYOUT
46 S3 PEDESTRIAN BRIDGE PIERS 1 AND 2
47 S4 BAIRLIST
MITIGATION
48 MPl MITIGATION PLAN
49 MP2 MITIGATION PLAN
50 MP 3 MITIGATION PLAN
51 MP4 MITIGATION PLAN
52 MPS MITIGATION PLAN
53 MP 6 MITIGATION PLAN
54 MP7 MITIGATION PLANTING DETAILS
55 MPB MITIGATION NOTES
TEMPORARY TRAFFIIC
CONTROL
56 TC1 TRAIFFIC CONTROL PLAN
57 TC2 TRAIFFJC CONTROL PLAN
58 TC3 TRAmc CONTIROL PLAN
59 TC4 TRAIFFIC CONTROL PLAN
RIGHT-OF-WAY
60 RW 1 RIGKT OF WAY PLAN
61 RW2 RIGKT OF WAY PLAN
62 RW3 RIGKT OF WAY PLAN
63 RW4 RIGHT OF WAY PLAN
64 RW5 RIGKT OF WAY PLAN
65 RW6 RIGHT OF WAY PLAN
PRO...CCT NAME
ENGIHEE "-ING. Pl.ANNING . EN IIIMONMENTAL 5(:IEHCll!:S
LAKE TO SOUND TRAIL
SEGMENT A
GREEN RIVER TRA IL TO N ACHES AVE SVV
100% REVIEW SUBMITTAL FOR RENTON
NOT FOR CONS TRUCTION
ABBREVIATIONS AND
SHEET LIST
OR AWl"IG NO.
2 OF 65
G2
Puget
Soun d
,-
' Lake
Washington
-... ~~
J,
PORTION OF SECTIONS 13, 14, 23, AND 24 TOWNSHIP 23 NORTH, RANGE 4 EAST&.
Lake to Sound Trail
Segment A
Green River Trail to Naches Avenue SW
King County, Washington
Contract No. C01119C17
Federal Aid No . CM-2017(110)
4f iJ'1"i UNIN.CORPORATED ', I ~ l I KING ' St,i,,
l/~~. ~OUNTY / {a/11 '\~ I . Sf.
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LOCATION MAP
NOT TO SCALE
CITY OF RENTON LUA15-00257 SSDP , S-CUP, AND S-V
6 1 REYIS<OOS BY OCSICNEO
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NOT TO SCALE
PRO...CCT NAM[
LAKE TO SO UND TRAIL
E.NGiNEEllt!NG.PLJINHINC.fNWONMfNlAlSCIENCH I I SEGMENT A
GREEN RIVER TRAIL TO NACHES AVE SW
JI
CONTACT INFORMATION :
APPLI CANT: KING COUNTY PARKS AND RECREATION
201 S. JACKS ON , 7TH FLOOR
SEATTLE, WA 98104
ATTN : JASON RIC H
(206) 427-8576
ENGINEER: PARAMETRIX, INC .
719 2ND AVENUE , SUITE 200
SEAffiE, WA 98104
ATTN : JENNIFER DVORAK
(253) 604-67 50
SURVEYOR: PARAMETRIX, INC.
719 2ND AVENUE. SUITE 200
SEATTLE, WA 98 10 4
ATTN: BOB PUSEY
(360 ) 850-5342
~
100% REVIEW SUBMITTAL FOR RENTON
NOT FOR CONSTRUCTION
COVER SHEET
OR..._'NI NG NO.
1 OF 65
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ELV=35.01 Q ~ BEGIN C-LINE FOUND I.ION IN CASE I ...I
STA201+00.00 SW13-23-04 IW
"-SE 14-23-04
KC p""[l NO 002 \en BEGIN PROJECT """""° N•1764n.49 _ -r STA 1+00 .00A-l.lNE "-I I 0 ':.,_,"",;:'° I E-1290501 99 --------lli I ~ : ,LCss!l-"""~---/ ELV=34.95 -------Cl) ,c N !()l <O 11195003(,<) , , _ --,-• --' ---l.0&11< ---· -+ I
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: ElV=27.80 "-~ ~,"' '··----N=176395.57 "'-I '--. FOUND 1-W BRASS DISK , "-...... ~-[=1290884.66 \ /
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SUR VEY NOTES:
1. HORIZONTAL DATUM, BASIS OF MERIDIAN .
GRID NORTH , WA SHINGTON COORDINATE SYSTEM,
NORTH ZO NE, NAD83(9 1) HELD CITY OF REN TON
MONU MENTS: HORI ZONTAL AND STATIONS 1333
AND 1854
2 . VERTICAL DATU M: NAVO 88 HELD CITY OF RE NTON
BENCH MARKS B M#1 333 AND BM # 18 5 4
3. THIS MAP CORRECTLY REPRESENTS COND ITIONS
AND FEATU RES E XISTING AT THE TIME OF THI S
TOPOGRAPHY IN OCTOBER, 20 1 0 .
4. CONVENTIONAL AND GP S SURVEY EQU IP MENT WAS
USED IN THE PERFORMANCE OF TH IS SURVEY .
ALL EQU IPMENT IS MAI NTA INED IN CONFO RMANC E
WITH CURRENT STATE STATUTE.
,; ,
'}
u CITY OF RE N TON LUA15-00257 SSDP, S-CU P . AND S-V
100% REVIEW SUBMITTAL FOR RENTON
NOT FOR CONSTRUCT ION
~ 6 REVISIONS OA TE BY O(SJG~[O i i ~ J. DVORAK
OR.A \toN
K. BRAATE N
0 CrECKED G05
~ 0. KIKUTA
PRO...CCT NAME
EHGINl!:ffUNC, PLANNING . f.Nl/lft.ONW:NTA L $C~NC[$
LAKE TO SOUND TRAIL
SEGMENT A
~ APPRQ\l[Q ==~ -w--I GRE EN RIVER TRAIL TO NACHES AVE SW I
SURVEY CONTROL PLAN
DRl.."'1<.lG NO
4 OF 65
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LEGE ND
DESCRIPTION
RaN LINE
RAILROAD C/L
PROPERTY LINE
CITY BOUNDARY LINE
EASEt.lE NT LINE
FOUND MONUMENTS
REBAR & CAP
HUB & TACK
PK NAIL
PROPERTY CORNER
STREAM BUFFER
STREAM
EDGE OF WATER
WETLAND FLAG
ORDINARY HIGH WATER t.l/\RK
I 00-YEAR FLOODPLAIN BOUNDARY
SURFACE FLOW DIRECTION
DITCH LINE
STORM DRAIN LINE
CULVERT
QUAR RY SPALL
CATCH BASIN, TYPE 1
CATCH BASIN, TYPE 2
INLET PROTECTION
SANITARY SEWER LINE
SANITARY SEWER MN-IHOLE
SANITARY SEWER VAULT
CL£AN OUT
CONTOURS MAJOR
CONTOURS MINOR
FlL TER FABRIC FENCE
HIGH VISl81UTY FENCE
Cl.EARING AND GRUBBING LIMITS
Fll..L LINE
CUT LINE
SAWCUT LINE
ASPHALT EDGE
CONCRffi LINE
CURB ANO GUTTER LINE
EDGE OF PATCH
EDGE OF GRAVEL
JURISDICTIONAL DITCH
ROCKERY
CONCRETE BARRIER
PROPOSED
~
•
(a)
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-----2-----
-0 -0 -0 -0 -0-
--0--00-00-oa --
-----r-----r-----r -----r-
-----c-----c -----c-----c-
I I I I I I I I I
CITY OF RENTON LUA15-00257 SSDP, S-CUP, AND S-V
~
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___ RAILROAD C/L_
______ ELh_ _____ _
-··-··-··-··-
•
•
___ _JlliW.J!_
~ 6 R[\11S:QNS DA 1[ B'r' OCSICNEO
o.. J. DVORAK ONE INCH AT F U LL SCALE.
DRAWN IF N OT, SCALE ACCORD INGLY
n M. MILLER
O CHECKED
" 0. KIKUTA
LEGEND
DESCR IPT ION
SPLIT RAIL FENCE LINE
BARBWIRE FENCE LINE
CHAIN LINK FENCE LINE
HOG WIRE FENCE LINE
WOOO GUARDRAIL
GUY ANCHOR
POWER POLE WITH LICHT
FLOOD LIGHT
UTILITY POLE
PP W/ UG DROP
PP W/ UG DROP & XMFR
OVERHEAD POWER
POWER
POWER VAULT
POWER TRAN SFORMER
POWER MN-IHOLE
POWER HANDHOLE
POWER CABINET
POWER RISER
POWER METER
SOLID LID J-BOX
LUMINARE
TELEPHONE VAULT
TELEPHONE RISER
TE1£PHONE MANHOLE
TELEPHONE
TV RISER
TV
FlBER OPTIC
GAS VALVE
GAS
WATER LINE
FIRE HYDRANT
WATER METER
WATER VN..\/f.
WATER BLOW OFF VALl/f.
WATER POST INDICATOR
SPRINKLER HEAD RC T~90
IRRIGATION CONTROL VALVE
PROPOS ED ~
--11---11---11--
a a a a o o u
+--)(
....
PRO.,CCT NAM[
[HGIHf!l'UNG. "l.ANN!NG f NVlll;OHMf:NT.ll $Cll!NCf S
LEGE ND
DESCRIPT ION
TRAFFIC SICNAI. POLE W / LAMP
TRAFF1C SIGNAL POLE
TRAFFlC CONTROL LOOP (SO)
TRAFFlC CONTROL CABINET
PEDESTRIAN POLE
MONITORING WELL
SURFACE POST
SIGN
SKIP LANE LINE
SOLID LANE LI NE
FOG LINE
LEFT ARROW
STRAIGHT ARROW
RIGHT ARROW
MAJLBOX
TREES
~ffiAND SYMBOL
WET\AND BOUNDARY
1/f.GETATION
RETAINING WALL
RIP RAP
ROCKERY
HANDICAPPED SYMBOL
WHEELCHAIR RAMP
BUILDING LINE
CONCRETE STAIR LINE
WOOD STIJRWAY
ASPHALT PATH
CEMENT CONCRETE SIOEWIJLK
ENGINEERED SOIL MIX
LANDSCAPE AREA
RAMP OIETECTABLE WARNI NG
RESTORATION PLANTING AREA
TEST PIT OR BORE HOLE
LAKE TO SOUND TRAIL
SEG MENT A
~ APPRO,~O -~-,-I I GREEN RIVER TRAIL TO NACHES AVE SW I I
PRO POSED ~
.
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NOT FOR CONSTRUCTION
I
C>R.A.WNC NO.
3 OF 65
LEGEND
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·---"'" ----------------WETIA -----'-------------------------------
/
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"-,
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'"-,
'"-,,
"-,,
"-,
'"-,
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SCALE IN FE IT
0 20 40
STATE OF
wCi ~~~sG[8N
O N E INCH AT F ULL SCALE.
IF N O T , SCALE ACCOR.DINGL Y
,u
r ~ 6 REIIISIONS OAT( EY DESIGNED I I J . SWENSON
LANDSCAPE ARCHITECT
ORA'Nf',.I
J . SWEN SON
CHEg"E~IKUTA I ~a=~·••w ,cn •v'-W~~m, I
AF=PN QV[Q
---------
was on area
dedicated to pump
station access .
~l,.-w cJ,
---------~ -----------------------.
Vegetation
Conservation
Areas (BVC3 and
BVC2)
---------
Total BVCA area proposed at 60% design = 42,741 SF
Revised total BVCA area = 43,050 SF
f:PK.IN EEll!N G ~LANNrNQ ENVIRONMENTAL SC IENCES
PRQJ[Ci NAM[
LAKE TO SOUND TRAIL
S EGMENT A
GREEN RIVER TRAIL TO NACHES AVE SW
CONSTRUCTION NOTES:
(,\ MITIGATION Ci.£ARING AND GRUBBING. STAKE OR fl.AG
\..:_,J PROPOSED PLANTING Ml.EA LIMITS FOR APPROVAL OF
PROJ ECT REPRESENTATIVE PRIOR TO STARTING CLJEARI NG
WORK. CL.EAR AND GRUB ROOTS AND REMOVE AN D
DISPOSE OF All UNWAN TED VEGETATION IN THIS PlANTING
AAEA LEAVE SOIL IN PLACE. SEE SPECIFICATION FOR
UST OF UN WANTED VEGETATION.
r;;\ COMPOST PLAC E 3• LAYER COMPOST OVER THE ENTIRE \::.J SURFACE or THIS PLANTING AAEA.
f,\ WOOD CHIP MULCH. PLACE J" LAYER WOOD CHIP MULCH
\.::.) OVER THE ENTIRE SURFACE OF THIS PLANTING AAEA.
GENERAL NOTES:
1. SEE SHEET MP6 AND FOR PLANTING OETIJLS AND
REOUIR[M[NTS.
2. LOOSEN ANY SOILS IN PLANTING Afl.EAS COMPACTED
BY CONSTRUCTION ACTlVTTIES BY RIPPING OR TILLING
THE AREA TO A DEPTH OF 24 •
3. PLANTING AREA LIM ITS AND INTERPLANTING LOCATIONS
SHALL BE STAKED IN THE FIELD AND APPROVED BY
PROJECI RlPRESENlATIVE PRIOR TO PLANTING .
4 ALL PLANTS TO BE SAVED AND PROTECTED WITHIN
CLEARING AND GRUBBING Afl.EAS WILL BE fl.AGGED BY
PROJEC T REPRESENTATIVE. NOTIFY ENGINEER 5 DAYS
PRIOR TO STAA T Of CLEARING ACTMTY. USE ONLY
HAND TOOLS AND METHODS WH EN WORKING INSIDE
THE ORIPLJNE AAEA Of EXISTING TREES AND SHRUBS .
5 PLANT DEBRIS FROM REM OVAL OF INVASIVE PLIJNTS
OR PRUN ING SKALL BE REMOVED FROM THE SITE AN O
DISPOSED OF PROPERLY.
LEGEND:
--------URBAN CONSERVANCY BUFFER
WETLAND 80\JNDAfl.Y
------OROI NAAY HIGH WATERLINE
• ------· DESIRABLE VEGETATION EDGE
EXISTING TREES
..-¥· "-7.. EXISTING TREES TO BE REMOVE D ~'?\, z'.
\,. HABITAl LOG , SEE SHEET MP-6 * BRUSHPILE , SEE SHEET ~P-6
TILL Ml.EA TO 2•. DEPTH
c ::::;::c;:::::;:1c::;::cJ STRAW WATTLE
PLANTING QUANTITY TAB
· THIS SHEET ONLY·
QUANTITY
BVC2
18 ,496 SF
OUANTITY
11,~}\F
14
H
14
95% REVIEW SUB MITT AL
NOT FOR CONSTRUCTION
MITIGATION PLAN
DRAWll'\C r,w
51 OF 59
MP4
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Vegetation
Conservation
Planting Areas for
ass in BVC1 and
BVC2.
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ORAW'-1
J . SWENSON ~ CHE CKEO ~ 0. KIKUTA ~ APPRO\'£D
:'i
<'.
' '
ONe INC H AT ~ULL SCA.Le:.
IF N O T , SCALE ACCORDINOL Y
'~ --
~11!!"~-
PLAN ®
SCALE I N FEET N
0 20 40
•
STATE OF W6~~~fl8N "iii:""
" + ' ~ -----...
ENOINU:RIN G . P'I.ANN ING ENVIRONMENTAL SCIENCE$
PROXC1 NAM (
LAKE TO SOU ND TRAIL
SEGMENT A
GREEN RIVER TRAIL TO NACHES AVE SW
CONSTRUCTION NOTES:
r,\ MITIGATION CL£AR1NG AND GRUBBING. STAI<[ OR FlAG
\_:J PROPOSED PLANTING AREA LIMITS FOR APPROVAL Of
PROJECT REPRESENTATM PRIOR TO STARTING CLEARING
WORK. CLEAR AND GRUB ROOTS AND REMOVE AND
DISPOSE OF AU. UNWANTED VEGETATION IN THIS PLANTING
AREi\. L£AVE SOIL IN PLACE. SEE SPECIFICATION FOR
UST OF UNWANTf:D VEGETATION.
(';\ COMPOST. PLACE J" LAYER COMPOST O'IER THE ENTIRE
\:.) SURFACE OF THIS PLANTING AREA
(';\ WOOD CHIP MULCH. PlACE 3• LAYER WOOD CH IP MULCH
\.:::,) OVER THE ENTIRE SURFACE OF THIS PLANTING AREA.
GENERAL NOTES :
I . SEE SHEET MP6 AND FOR PLANTING DETAILS AND
REOUlREMENTS.
2 . LOOSEN ANY SOILS IN PLANTING AREAS COMPACTED
BY CONSTRU CTION ACTMTIES BY RIPPING OR TIWNG
THE AREA TO A DEPTH or 24".
3. PLANTING AREA LIMITS AND INTERPLANTING LOCATIONS
SHALL BE STAKED IN THE FIELD AND APPROVED BY
PROJECT REPRESENTATIVE PRIOR TO Pl.ANTING.
4 . ALL PLANTS TO BE SAVED AND PROTECTED WITHIN
CLEARING AND GRUBBING AREAS WILL BE FLAGGED BY
PROJECT REPRESENTATIVE. NOTIFY ENGINEER 5 DAYS
PRIOR TO START OF CLEARING ACTMTY. USE ONLY
HAND TOOLS AND METH ODS WHEN WORKING INSIDE
THE DRIPUNE AREA or EXISTING TREES AND SHRUBS.
5. PLANT DEBRIS FROM REMOVAL OF INVASM PLANTS
OR PRUNING SHAU BE REMOVED FROM THE SITT: AND
DISPOSED OF PROPERLY.
LEGEND :
"-
¥®
*
URBAN CONSERVANCY BUfHR
WETLAND BOUNDARY
ORDINARY HIGH WATERLINE
DESIRABLE VEGETATION EDGE
EXISTING TREES
EXISTING TREES TO BE REMOVED
HABITAT LOG. SU SHEET MP-6
8RUSHPIL£. SEE SHEET MP-6
TILL AREA TO 24. DEPTH
======· STRAW WATTlE
PLANTING QUANTITY TAB
• THIS SHEET ONLY • ---_QUANTITY
Ml I M2
95% REVIEW SUBMITTAL
NOT FOR CONSTRUCTION
MITIGATION PLAN
ORA.WING NO
50 OF 59
MP3
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'Vj
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----/~ ~f:._4-;::_-::_--:,::;
11,719 square feet
of the Buffer
Vegetation
Conservation Area
( BVC 1 ) proposed
in the 60% design
level was on
railroad-owned
property , and will
instead be
relocated to new
areas along the
river east of
Monster Road .
I
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PLAN
SCALE IN FEIT
0 20
f'/...___--\BLACK RIVER_ ------... ......._-------' ----
1-·· --·
\ V v, ~-/
,-J ' /
~:..~"~ o, ( ----(
!:: -----...... _ --
/
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\/~
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:t ~_::.___ r--'
% ________ .,_ __ t~ ~ . '
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UI ---------' -~--~-in r -----,,_ ', -~ --~~--"'\---, ,,, , r--=---.. ~ --
> '--,.:~-' ----,=,-····· ,. ,-7'----_ ----c,,;cc,. · '-A 0' / / J'----.Le..---,-_7_7_-:_-=~--------'--.., -< ,.. , -----c' "'' /, /,..,.-;
\
, -----<-----c, / '/ , ----C ''y.._C... /~
/ --/ , / ' / ' /
' \ I PLAN ~
SCALE IN FEIT N
0 20 40
"\
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'y~ ---, +04-1 --:;:-
_3S'~ ~ ~~ <"o,'.'Oo,
0-f() ~~
-----1:/1,_::__ ~~ ---~
'
-~
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BLACK RIVER
--/ _____ _
~
----------ii7ir
LICENSED i!: LANDSC APE ARCHITECT PflOJE CT r-i.:.ME
STRUCTION NOTES:
8 MITIGATION CLEARIN G AND GRUBBING. STAKE OR FLAG
PROPOSED PLANTING AREA LIMITS FOR APPROVAL OF
PROJECT REPRESENTATM: PRIOR TO STARTING CLEARING
WORK. CLEAR AND GRUB ROOTS AND REl.4 0VE AND
DISPOSE OF All UNWANTED VEGETATION IN THIS PLANTING
AREA LEAVE SOIL IN PLACE. SEE SPECl flCATION FOR
LIST OF UNWANTED VEGETATION.
0 COMPOST. PLACE 3-LAYER COMPOST OVER THE ENTIRE
SURFACE Of THIS PLANTING AREA.
I,\ WOOD CHIP I.IULCH. PLAC E 3• LAYER WOOD CHIP MULCH
\:.) OVER THE ENTIRE SURFACE OF THIS PLANTIN G AR'fA.
GENERAL NOTES :
1. SEE SHEET MP6 AND FOR PLANTING DETAILS AND
REQUIREMENTS.
2. LOOSEN Al{'( SOILS IN PLANTING AREAS COf.lPAC TEO
BY CONSTRUCTION ACTMTIES BY RIPPING OR TILLING
THE AREA TO A DEPTH OF 2~"
3. PtANTING AREA LIMITS AND INTERPLANTING LOCATKlNS
SHAll BE STAKED IN THE FIELD AN D APPROVED BY
PROJECT REPRESENTATM: PRKlR TO PLANTING.
4. All PLANTS TO BE SAVED AND PROTECTED WITHIN
CLEARING AND GRUBBING AREAS WILL BE FLAGGED BY
PROJECT REPRESENTATM:. NOTlf'Y ENGINEER 5 DAYS
PRIOR TO START OF CLEARING ACTMTY. USE ONLY
HAND TOOLS AN O l.4ETHODS WHEN WORKING INSIDE
THE DRIPUNE AREA OF EXISTING TREES AN D SHRUBS.
5. PtANT DEBRIS FROM REMOVAL OF INVASM: PLANTS
OR PRUNING SHALL BE REt.10\/EO FROM THE SITE AND
DISPOSED OF PROPERLY.
LEGEND:
--------URBAN CONSERVANCY BUFFER
WETLAND BOUNDARY
-------ORDINARY HIGH WATERLINE
· ~-----• DESIRABLE VEGETATION EDGE
X• I x·'· ~ ", '.
, ~-
' '
\-
*
EXISTING TREES
EXI STING TREES TO BE REf.lOVED
HABITAT LOG, SEE SHEET MP-6
SRUSHPILE. SEE SHEET l.4P-6
TILL AREA TO 24. DEPTH
c:=====· STRAW WATTLE
PLANTING QUANTITY TAB
-THIS SHEET ONLY -
Q\/ANTITY
SEE SHEET 1.4 PJ FOR MORE
INFORMATION
95% REVIEW SUB MITT AL
NOT FOR CONSTRUCTION
•
W~g~1~8bN
t l::, R(VSIOSS DATE BY
0
"'}"'~WENSON LAKE TO SOUND TRAIL
~ DRA.7-" SWENSON AJ~·,: ... ,. ...... PLAN.iNO .EN~RONM<N"CSCIENCU SEGMENT A I MITIGATION PLAN I I
'i CHECKED " I M P2
'-0. KIKU TA GREEN R IVER TRAI L TO NACHES AVE SW I -~-----~
ORA Wl'IG NO
49 OF 59
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40
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TREE REPLACEMENT CALCULATION FOR
SIGNIFICANT TREES
DIAMETER• OF TREE I :~~rMrtT I NUMBER OF I N¥:E~~R TgF REMOVED (•MEASURED
AT HEIGHT OF 4.5 FEET TREES REQU IRED TREES REMOVED REPLACE ONSITE FROM THE GROUNO )
4 -6 INCHES (SINGLE TRUNK);
2 INCHES (ANY TRUNK OF A 3 1 3
MULTI-TRUNK TREE )
OVER 6 -8 INCHES 4 2 8
OVER 8-20 INCHES 6 5 30
OVER 20 INCHES 8 2 16
TOTAL 10 5 7
O 20 ,
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-----------~-----~--------------I PLAN----------------------------------------------i ---' FORT DENT PARK
----~~~-----~~-~iiiiiiSilCALE~~INiiiiiiFEiET~~. ®-_ ""' , -----
0 20
CONSTRUCTION NOTES :
8 PLANTING AREA CLEARING AND GRUBBING. STAK E OR flAG
PROPOSED PLANTING AREA LIMITS FOR APPROVAL o r
PROJECT REPRESENTATM PRIOR TO STARTING CLEARING
WORK. CLEAR AND GRUB ROOTS ANO REMOVE AND
DISPOSE OF ALL UNWANTED VEGETATION IN THIS PLANTING
AREA. LEAVE SOIL IN PLACE. SEE SPECIFlCATION FOR
LIST Of UNWANTED VEGETATION.
0
0
COMPOST. PLACE 3-LAYER COMPOST OVER THE ENTIRE
SURFACE OF THIS PLANTING AREA.
WOOO CHIP MULCH . PLACE 3• LAYER WOOO CHIP MULC H.
GENERAL NOTES :
1. SEE SHEET MP6 ANO roR PLANTING DETAILS AND
REQUIREMENTS.
2. LOOSEN ANY SOILS IN PLANTING AREAS COMPACTED
BY CONSTRUCTION ACTMTlES BY RIPPING OR TIWNG
THE AREA TO A OEPTH OF 24 ".
3. PLANTING AREA LIMITS AND INTERPLANTING LOCATIONS
SHALL BE STAKED IN ,HE FlElO AND APPROVED BY
PROJECT REPR ESENTATM: PRIOR TO PLANTING.
4. ALL PtANTS TO BE SAVEO AND PROTECTED WITHIN
CLEARING ANO GRUBBING AREAS WILL BE FLAGGED BY
PROJECT REPRESENTATM:. NOTIFY ENGINEER 5 OAYS
PRIOR TO START OF CLEARING ACTM1Y. USE ONLY
HANO TOOLS AND METHODS WHEN WORKING INSIDE
THE ORIPLINE AREA OF EXISTING TREES ANO SHRUBS .
5. PLANT OEBRIS FROM REMOVAL OF INVASIVE PLANTS
OR PRUNING SHALL BE REMOVED FROM THE SITE AND
OISPOSEO or PROPERLY.
LEGEND :
--------URBAN CONSERVANCY BUFFER
WETLAND BOUNDARY
-------OROIN.ARY HIGH WATERLINE
• ------· OES1RA8LE VEGETATION EDGE
EXISTING TREES
~~® EXISTING TREES TO BE REMOVED
HABITAT LOG, SEE SHEET MP-6
BRUSHPILE. SEE SHEET MP-6
TILL AREA TO 24. OEPTH
t
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PLANTING QUANTITY TAB
-THIS SHEET ONLY·
QUANTITY
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NOT FOR CONSTRUCTION
tiA.Tr lay I OES1CNE£.,NS0N ~l 6l·"''"M 1--1 m v,,
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PROJECT NAME DRAWING NO
48 OF 59
40
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PLAN
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ONE INCH AT FULL SCALE.
IF N Oi, SCALE ACCORDINGLY
WASHINGTON
LICENSED
LANDSCAPE AR CHITECT
•
STATE OF
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(lty or RENTON
KC PARCEL HO. 1323049020
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(llY or RENTON
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'>,,--. KC PARCU NO. 13230<9012
CllY or REIIION
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WETLAN01/2
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ENGINEEl'I.ING PU NNING l!NVl~MENTAL SClfN<::fS
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GREEN RIVER TRAIL TO NACHES AVE SW
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JCTION NOTES:
MITIGATION CLEARING ANO GRUBBIN G. STAKE OR FLAG
PROPOSED PL.ANTING AREA LIMITS FOR APPROVAL OF
PROJECf REPRESENTATrvE PRIOR TO STARTING CLEARING
WORK. CLEAR AND GRUB ROOTS AN D REMOVE AND
DISPOSE OF ALL UNWANTED VEGETATION IN THIS PLANTING
AREA LEAVE SOIL IN PL.ACE. SE( SPECln CATION FOR
LIST OF UNWANTED VEGETATION.
COMPOST. PL.ACE 3" LAYER CO MPOST OVER THE ENTIRE
SURFACE OF THIS PL.ANTNG AREA .
WOOD CHIP MULCH. PL.ACE 3" LAYER WOOD CHIP MULCH
OVER THE ENTIRE SURFACE OF THIS PLANTING AREA.
SITE ACCESS. RESTORE AREA AITTR CONSTRUCTION PER
THE REDUIREMENTS or NOTE #9 OF THE PLANTING NOTIES
ON SHEET MP-6.
GENERAL NOTES:
1. SEE SHEET MP6 AN D FOR PLANTING DETAILS ANO
REQUIREMENTS.
2. LOOSEN ANY SOILS IN PL.ANTNG AREAS COMPACTED
BY CONSTRUCTION ACTIVITIES BY RIPPING OR TILLING
THE AREA TO A DEPTH or 2C
3. PLANTING AREA LIMITS AND INTERPLANTING LOCATIONS
SHALL BE STAK ED IN THE nELD AN D APPROVED BY
PROJECT REPRESENTATIVE PRIOR TO PLANTING.
4. ALL PL.ANTS TO BE SAVED AND PROTECTIED WITHIN
CLEARING AN D GRUBBING AREAS WILL BE FLAGGED BY
PROJECT REPRESENTATIVE. NOTIFY ENGINEER 5 DAYS
PRIOR TO START or CLEARING ACTIV1TY. USE ONLY
HANO TOOLS AN O l.lETHOOS WHEN WORKING INSIDE
THE DRIPUNE AREA or EXISTING TREES AND SHRUBS
5. PL.ANT DEBRIS FROM REMOVAL OF INVASNE PLANTS
OR PRU NING SHALL SE REMOVED FROM THE SITE ANO
DISPOSED OF PROPERLY.
LEGEND:
J
>!-~ ~ ·~-
*
URBAN CONSERVANCY BUFFER
WETLAND BOUNDARY
ORDINARY HIGH WATERLINE
DESIRABLE VEGETATION EDGE
EXISTING TREES
EXISTING TREES TO BE REMOVED
HABITAT LOG, SEE SHEET MP-6
BRUSHPILE. SE£ SHEET MP-6
PLANTING QUANTITY TAB
-TH IS SHEET ONLY -
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CURRANT
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6 2 2
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CONSTRUCTION NOTES:
-, 0 ~:~~~ ~~g :~ G~~~~1%t::J:AL n: ~ PROJECT REPR ESENTATM: PRIOR TO STARTI NG CLEARING ( l,_ WORK . CLEAR ANO GRUB ROOTS ANO REMOVE ANO '· ) I DISPOSE OF ALL UNWANTED VEGETATION IN THIS PLANTING
• ·. AREA. LEAVE SOI L IN PLACE . SEE SPECIFICATION FOR
....
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0
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COMPOST. PLACE 3" LAYER COMPOST OVER THE ENTIRE
SURFACE OF THIS PLANTING AREA.
WOOD CHIP MULCH. PLACE 3" LAYER WOOD CHIP MULCH
OVER THE ENTIRE SURFACE OF THIS PLANTING AREA .
SITE ACCESS. RESTORE AREA AFTER CONSTRUCTION PER
THE REQUIREMENTS OF NOTE #9 OF THE PLANTING NOTES
ON SHEET MP-6.
GENERAL NOTES :
1. SEE SHEET MP 6 ANO FOR PLANTING DETAI LS ANO
REQ UIREMENTS
2. LOOSEN ANY SOILS IN PLANTING ARf.J,S COMPACTED
BY CONSTRUCTION ACTMTIES BY RIPPING OR TILLING
THE AREA TO A DEPTH OF 24".
3. PLANTING AR EA LIMITS AND INTERPLANTING LOCATIONS
SHAU. BE STAKED IN THE FIELD AND APPROVED BY
PROJECT REPRESENTATM: PRIOR TO PLANTING.
4. ALL PLANTS TO BE SAVED AN D PROTECTED WITHIN
CLEARING AND GRUBBING ARW WILL BE FLAGGED BY
PROJECT REPRESENTATIV£. NOTIFY ENGIN EER 5 DAYS
PRIOR TO START OF CLEARING ACTMTY. USE ONLY
HANO TOOLS AND METHODS WHEN WORKING INSIDE
THE DRIPLINE AREA OF El11STING TREES ANO SHRUBS .
5. PLANT DEBRIS FROM REMOVAL OF INVASM: PLANTS
OR PRU NING SHALL BE REMOVED FROM THE SITE AN D
DISPOSED OF PROPERLY .
LEGEND :
.:JI "'
*,,J ~~
/ {
V t
*
URBAN CONSERVAN CY BUFFER
WETl.AND BOUNDARY
ORDINARY HIGH WATERLINE
DESIRABLE VEGETATION EDGE
EXISTING TREES
EXISTING TR EES TO BE REMOVED
HABITAT LOG. SEE SHEET MP-6
8RUSHPILE. SEE SHEET MP -6
I I (' I I
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-I KC P/ORCO.
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<= ~--~ LANDSCAPE ARCHITECT < OAT[ BY O(SICNED ~
Q. 6 RE\
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Sl0NS J. SWENSON ONE INC H AT FULL S CALE.
OR.:.WN IF N OT, SCALE ACCORDINGLY
FRO..CCT NAME DR.6.~NG NO
52 OF 59
~ J . SWEN SON ll <a'~~~2 1084PAT01200C-MP 656 "''"""'""-""' "-"'""" MPS a. CHEOC(D N BEu..E\\lE. WASr ,-.;:,ra,,. 1J1600,1
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LAKE TO SOUND TRAIL
SEGMENT A MITIGATION PLAN E NGINEEltlNG . PUNNING . ENVIRONMENTAL SCIENCES
~ APPR Ov!:D OAT~OVE MBER 2016 :.
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1 MITIGATION GOALS, OBJECTIVES, AND PERFORMANCE STANDARDS
THE OVERAll GOAL OF THE MITIGATION IS TO REPLACE TH[ HABITATS AN O FUNCTIONS LOST AS A RESULT OF TH[
PROJECT. TH[ PROPOSED MITIGATION WOULO ACCOMPLISH THI S BY ENHANCING 0.4 9 ACRE OF WETLAND BUFf[R
ANO 0.60 ACRE or STREAM BUFFER ANO 0.60 ACRE STREAM BUFFER AT MITIGATION SITES I ANO 2. SPEClnc
GOALS AN D OBJECTIVES FORMULATED TO ACHl(VE THIS RESULT AR[ PRESENTED BELOW.
MITIGATION GOAL
GOAL· ENHANCE 0.49 ACRE OF WETLAND BUffER AN D 0.60 ACRE OF STREAM BUFFER TO NATrvE FORESTED
UPLAND.
ACHIMMENT OF THIS GOAL IS EXPECTED TO INCREASE THE PRODUCTION OF ORGANIC MATTER BY PLANTI NG
TREES AND SHRUBS IN THE ENHANCED BUFFER; INCREASE WILOLIFE HABITAT: AND IM PROVE BIOLOGICAL DIVERSITY
BY PLANTING WITH A VARIETY OF NATIVE RIPARIAN PLANT SPECIES.
MITIGATION OBJECTIVES AND PERFORMANCE STANDARDS
OBJ[CTrvE 1: ESTABLISH A MIN IMUM OF O 49 ACRE OF FORESTED WETLAND BUff[R ANO 0.60 ACRE OF
FORESTED STREAM BUFFER BY PLANTING NATrvE TREES ANO SHRUBS.
PERFORMANCE STANDARD:
YEAR 1 SURVIVAL OF PLANTED WOODY SPECIES IN ENHANCED WETLAND BUFFER ANO STREAM BUFFER AREAS
\\1LL BE AT LEAST 80 PERCENT.
YEAR 3 NATIVE WOODY SPECIES WILL ACH IM A MINIMUM OF 35 PERCENT AREAL COVER IN THE ENHANCED
WETLAND BUFFER ANO STREAM BUFFER AREAS.
YEAR 5 NATIVE WOODY SPECIES \\1LL ACH IM A MINIMUM OF 60 PERCENT AREAL COVER IN THE ENHANCED
WETLAND BUFFER AND STREAM BUFFER AREAS.
OBJECTM: 2: LIMIT INVASM: NON-NATM: SPECIES THROUGHOUT TH[ MITIGATION SITE PLANTING AREAS .
PERFORMANCE STANDARD:
YEARS 1-5 HIMALAYAN BLACKBERRY, CUTLEAF BLACKBERRY (RUBUS LACINVITUS), SCOTCH BROOM (CYTISUS
SCOPARIUS), BUTTERFLY BUSH (BUODL[JA SP.), POISON HEMLOCK (CONIU M MACULATUM). CANV\DA
THISTLE (CIRSIUM ARVENSE), BULL THISTLE (CIRSIUM VULGAR£), ANO REED CANV\RYGRASS Will NOT
EXCEED 20 PERCENT AREAL COVER IN AU PLANTING AREAS .
OBJECTM: 3 . PROVIDE UPLAND WILOUFE HABITAT.
PERFORMANCE STANDARD:
INCREASE IN AREAL COVER or NATIVE WOODY SPECIES IN TH [ PLANTED BUFFER. AS MEASURED IN
OBJECTrvE 1 TO BE USED AS A SURROGATE TO INDICATE INCREASING flABITAT FUNCTIONS
OBJ[CTM: 4: PROTECT THE MITIGATION SITE FROM ANTHROPOGENIC DISTURBANCE.
PERFORMANCE STANDARD,
YEARS 1-5 CONDUCT YEARLY OUALITATM: MONITORING TO ASSESS TH[ STATUS OF TH[ SITES DURING TH
5-YEAR MONITORING PERIOD FOR HUMAN DISTURBANCE. INCLUDING BUT NOT LIM ITED TO FI LLI NG, TRASH, AN O
VANDALISM.
2 MONITORING AND MAINTENANCE
2.1 MONITORING
THE MITIGATION AREAS WOULD BE MONITORED DURING ANO AFTER CONSTRUCTION. DURING CONSTRUCTION,
MONITORING WOULD ENSURE THAT TH[ BIJPS ARE OBSERVED TO MINIMIZE IMPACTS. ANO THE ON-SIT[
CONSTRUCTION WORK (INCLUDING EARTHWORK AND PLANTING) WOU LD BE COORDINATED TO ENSURE THAT TH[
SITE IS CONSTRUCTED AS DESIGNED.
AFTER CONSTRUCTION IS COMPLETED. AN "AS-BUILT' MITIGATION REPORT WOULD BE SUBMITIED TO TH[ CITIES OF
RENITON ANO TUKWILA WITHIN 1 MONTH OF MITIGATION INSTALLATION. POST-CONSTRUCTI ON MONITORING OF TH[
MITIGATION AREAS WOULD BE PERFORMED OVER A 5-YEAR PERIOD BY QUALIFIED BIOLOGISTS. THE CITY Of
RENTON SHALL HAVE TH[ AUTHORITY TO EXTEND TH[ MONITORING PERIOD TO 10-YEA,qS AS CONDITIONED BY THE
HEX DECISION . MONJTORING WOULO B[ PERFORMED OUART[RLY THE FIRST YEAR AN D ANN UALLY FOR SUBSEQUENT
YEARS TO ENSURE THAT TH[ GOALS ANO OBJECTM:S OF THE MITIGATION AR[ BEING MET. A COMBINATION OF
QUALITATIVE AND OUANTITATM: MONITORING ACTIVITIES WOULO BE USED TO ASSESS THE MANAGEMENT OBJECTIVES
ANO ASSOCVITED PERFORMANCE STANDARDS OCSCRIBED IN THIS MITIGATION PROPOSAL. ACTMTIES WOU LD INCLUDE
CONDUCTING SITE VISITS TO MONITOR UNNATURAL SITE DISTURBANCE, TAKING PHOTOGRAPHS TO DOCUMENT SITE
D(V[LOPMENT, AN O COLLECTING DATA FOR TH[ QUANTITATIVE (VAL UATION OF PERFORMANCE STANDARDS. TH
RESULTS or THE MONITORING \\1 ll BE SUBMITTED TO THE CITIES OF RENTON ANO TUKWILA FOLLOWING EACH
MONITORING MNT.
APPROPRIATE CONTINGENCY MEASURES Will 6[ DEVELOPED, AS NEEDED, BY A QUALIFIED PROFESSIONAL TO
ENSURE THAT TH[ SITES OCV[LOP HEALTHY VEGETATIO N THAT MEETS THE OBLIGATIONS OCSCRIB[D IN THIS
MITIGATION PLAN AND TH[ ASSOC IATE D PERMITS.
DESIGNEO
J. $111:N SON
R[VISIONS OAT( av
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ONE INC H A T F ULL SCALE.
IF NOT, S CALE ACCORDINGLY
APPROVED
2.1 .1 QUANTITATIVE MONITORING
THE f0LLOl\1NG BULLETED IT[MS DESCRIBE TH[ METHODS TO 3[ USED FOR TH[ QUANTITATIVE MONITORING,
MONITORING SCHEDULE, ANO R[PCRT OEADUN[S.
• THE MITIGATION SIT[$ WILL BE ASSESSED BY AN APPROPRLI.TE QUANTITATIVE VEGETATM: COVER Fl[LO
ASSESS MENT METHODOLOGY. TH[ LINE INTERCEPT METHOD Will BE USED FOR DITTRMINING PERCENT AREAL
COVER FOR WOODY AN D INVASrvE SPECIES.
• QUANTITATIVE VEGETATION ASSESS MENITS Will FOLLOW TH [ SAME METHOD IN EACH CONSECUTrvE MONJTORING
YEAR.
• QUANTITATIVE VEGETATION ASSESSMENTS Will BE P[RFORMW BETWEEN JUN[ 15 AND SEPTEMBER 15 OF
EACH MONITOR ING YEAR .
• MONITORING RE PORTS WILL BE S[NIT TO AGENCIES REQUIRING MONITORING REPORTS 8Y FEBRUARY 15 OF
TH[ FOLLOWING YEAR.
• QUANTITATIVE MONITORING Will INCLUDE PHOTOGRAPHIC DCC UMENTATION OF THE SITES FROM PERMANENT
PHOTOGRAPH STATIONS.
2.1.2 QUANTITATIVE MONITORING
OUAUITATM: ASSESSMENT Will BE PERFORMED YEARLY TO VISUALLY ASSESS THE HEALTH or PLANTS ANO
IDENTIFY AREAS THAT MAY NEED CONTROL OF NON-NATM: INVASM: SPECIES OR OTHE R MAJ NTENANC[ ACTMTl[S
ADDITIONALLY. DURING YEARS 1, 2, AND 3 THE SCR[[NING PLANTINGS (SP-I) Will ALSO BE OUAUITATM:LY
MONITORED TO VISUALLY ASSESS THE HEAL TH OF TH[ PLANTS ANO IDENTIFY AREAS THAT MAY NEED CONTROL OF
NON -NATIVE INVASIVE SPECIES OR OTHER MAJNTENANC[ ACTM11ES.
2.2 MAINTENANCE
TH[ PROPOSED MITIGATION IS INTENDED TO ACH l(V[ THE PERFORMANCE STANDARDS WITH MINIMAL ONGOING
MAJNTENANCE. PLANTED VEGETATION SPECIES SHOULD BE ADAPTED TO VARYING Sil[ CONDITIONS IN TH[ PUGET
SOUND LOWLAND; HOWEVER, SUPPLEMENTAL IRRIGATION MIGHT 8[ NEEDED DURING THE FIRST TWO GROWING
SEASONS AFT ER INSTALLATION TO ENSURE TH[ LONG-TERM SURVIVAL OF THE PLANTS. THE NEED FOR IRRIGATION
WOULD BE (VALUATED BASED ON TH E CONDITIONS OBSERVED DURING TH[ [STABUSHM[NIT PERIOD.
TO ENSURE RAPID ESTABLISH MENT OF THE PLANT COMMUNITY. TREES AND SHRUBS WOULD BE PLANTED CLOSER
TOGETHER THAN WOULD GENERAllY OCCUR IN NATURAL MATURE STANDS. SOM[ NATURAL MORTALITY IS EXPECTED
TO OCCUR DURING TH E MONITORING PERIOD. All DEAD AN D DOWN ED WOODY MATERV\L WOULO BE LEFT IN PLACE
TO PROVIDE MI CROHABITATS FOR WILDLIFE PLANTS WOUUD BE REPLACED AS NEEDED TO MEET PERFORMANCE
STANDARDS
MAINTENANCE TO CONTROL NUISANCE SPECIES IN TH[ MITIGATION AREAS MAY B[ NECESSARY. DURING THE
MONITORING PERIOD. If IT BECOMES E'.1DENT THAT INVASM: SPECIES AR[ IM PEDING ESTABUSHMENT OF DESIRABLE
NATI\/[ PLANTS, MEASURES WOULO BE IMPLEMENTED TO CONTROL NU ISANCE SP ECI ES. A PROGR[SSM:LY
AGGRESSIVE APPROACH WOULD BE USED TO CONTROL NUISANCE SPECIES. CONTROL MEA,~URES WOULD FIRST
INCLUDE HAND CUTTING AN D/OR GRUBBING AND REMOVAL: IF THIS FAJLS, AN ENVIRONMENTALLY SENSITIVE
HERBICIDE (RODEO' OR EQUIVALENT) MAY BE APPLIED.
2.3 CONTINGENCY MEASURES
IF MONITORING IN~CAT[S THAT THE SITES AR[ NOT MEETING ViRFOR MANCE STANDARDS, CONTINGENCY MEASURES
WOULD BE IMPLEMENTED (TABLE 2-1 ). SITE CONDITIONS WOULO BE (VALUATED TO DETERMINE TH[ CAUSE OF
TH[ PROBLEM AN D THE MOST APPROPRLI.T[ COUNTER MEASURES.
IN FOR MATION FROM TH[ ANN UAL MONITORING PROGRAM WILL BE USED TO IDENTIFY ANY MAJNT[NANC[ AND/OR
CORRECTM: ACT IONS. IF PROBLEMS ARE IDENTI FIED IN MONITORING. KI NG COUNTY BIOLOGISTS \\1ll DETERMINE
TH[ CAUSE OF THE PROBLEM AND IMPLEMENT PROPER MAINTEHANC[ OR CORR[CTM: ACTIVITIES. THESE ACTIVITI ES
Will BE DISCUSSED IN THE ANNUAL MONITORING REPORT.
TABLE 2-1. CONTINGENCY MEASURE S FOR THE MITIGATION SITES
PROBLEM cONTINGENCY MEASURE
LESS THAN 80!>: OF PLANTED WOODY I KING COUNTY BIO_OGISTS (OR OTHER OUALIFIED BIOLOGIST)
SPECIES SURVIVE IN YEAR I WOULO ASSESS THE SITE TO DETERMINE v.iHAT CONDITIONS
AR E PR[V[NTING THE PLANTS FROM THRMNG . APPROP RIATE
MEASURES WOULD BE TAKEN TO CORRECT ANY CONDITIONS
THAT AR E LI MITING GROWTH. LOST PLANTS WOULD BE
REPLACED WITH A>'PROPRVIT[ NATrvE SPEC IES UNLESS
APPROPRV\T[ NATIVE WOODY SPECIES AR[ VOLUNTEERING AT
A RATE SUFFICIENT TO REPLACE THEM. ADDn lONAL
MEASURES (SUCH AS PROVIDING ADDITIONAL PROTECTION)
WOULO BE CONSIOERED IF NECESSARY. ADDITIONAL
PROTECTION COUUD INCLUOC TH[ USE OF AN HERBIVORE
REPELLENT (PLAN;SKYDO OR EQUIVALENT)
PERCENT COVER FOR WOODY SPECIES NOT I KING COUNTY BIOLOGISTS (OR OTHER QUALIFIED BIOLOGIST)
MET IN YEAR 3 OR 5 WOULD ASSESS TH[ SITES TO DITTRMIN[ WHAT CONDITIONS
AR [ PRCV[NTING TH[ PLANTS FROM THRMNG. APPROPRLI.TE
MEASURES WOULD 8[ TAKEN TO CORRECT ANY CONDITIONS
THAT AR[ LIMITING GROWTH.
INVASIVE SP[Cl[S EXCEED PERC[NIT
COVER THRESHOLD
PERFORMANCE STANDARDS NOT MET
AT YEAR 5
WA SHINGTON
LICENSED
IMPLEMENT/RCVISE INVASM: SPECIES CONTROL PLAN.
CONTINUE TH[ MONITORING REGIME FOR I ADDITIONAL YEAR.
TH[ SITES WOULD CONTINUE TO BE (VALUATED (V[RY YEAR
UNTIL THEY IIEET THE STATED PERFORMANCE STANDARDS
ASSOCIATED 111TH Mv\NAG[M[NT OBJECTM:S. OTHER
CONTINGENCY MEASURES MAY BE IMPLEMENTED DURING TH IS
PERIOD.
•
STATE OF
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ENG4NEERIHG . Pl.ANNING . li:NVlROH""-EHlAL $CIENCU
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SEGMENT A
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PLACE J" DEPTH WOOD CH IP
t.lULCH OVER ENTIRE PLANTED
AREA. KEEP MULCH Off OF STEMS
BACKflU WITH NATI\/£ SOILS.
WATER THOROUGHLY TO
REMOVE AJR POCKETS
I PLANTING HOLE TO BE I
2 X DIA. OF ROOTBALL
SHRUB AND SMALL TREE PLANTING
DETAIL ffi
NO SCALE
6 , cf TR EE
12
00 ·
flNISHED GRAOE
COMPOST
\------EXISTING SOIL
lOI~
.llifil;
PLANT SHRUBS IN SINGLE
SPECIES GROUPS or 7 TO
12 PLANTS EACH PLANT
TREES IN SINGLE SPECIES
GROUPS OF I TO 5 PLANTS
EACH.
4 '
~06
~"'"'"=
RE Vl~ON S
TYPICAL TREE AND SHRUB SPACING
DETAIL ffi
NO SC ALE
DAT[ BY
EDGE OF PLANTI NG AJREA
OESICNED
J. SWEN SON
TREE STAKING "ARBOR TIE"
·eve· HEMLOCK/nR STAKE,
2" DIA (1 PER TREE)
DRMN MO UNDISTURBED
SUBSOIL MIN 2 4" DEPTH
flNISHED GRADE
BACKFILL WrTH NATI\/£ SOILS.
WATER THOROUGHLY TO
REMOVE AJ R POCKETS PLANTI NG HOLE TO BE
2 X DIA. OF ROOTBALL
NOTE:
STAKE All TREES 3' AND TALLER.
PLANT so THAT TOP or ROOT
BALL IS [V[N WITH THE flNISHED
GRADE
PLACE 3" DEPTH WOOD CHIP
MULCH OVER ENTIRt: PLANTED
AREA OR IN 5' DIA. t.l ULCH
RINGS WHERE TREES ARE
INflLL PLANTED. KEEP MULCH
OFF OF STEMS
COMPOST
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2
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PLANTING HOLE
TO BE
2 X DIA.
OF ROOTBALL
NOTE:
STAKE ALL TRt:ES 1 • CALIPER ANO GREATER.
TREE STAK ING "ARBOR TIE"
HARDWOOD STAKES
PLANT so THAT TOP or ROOT
BALL IS [V[N WITH THE flNISHED
GRAOE
PLACE 3· DEPTH WOOD CHIP
MULCH OVER ENTIRE PLANTED
AREA OR IN 5' OIA. MULCH
RINGS WH ERE TREES ARE
INFlLL PLANTED. KEEP t.l ULCH
Off or STEMS
flNISHED GRAOE
COt.l POST
BACKflLL WITH NATN[ SOILS .
WATER THOROUGHLY TO
RE MOVE AIR POCKETS
EX ISTING SUBGRAOE
PLANTING NOTES:
1. CONTRACTOR SHAU ARRANGE TO MEET ON SITE WITH PROJECT
REPR ESENTATIVE TO DISCUSS LIMITS or WORK ANO METHODS. CONSTRUCTION
ACTIVITIES SHALL NOT COMMENCE UNTIL ACCESS. LIMITS or WORK. AND
METHODS ARE APPROVED.
2. MITIGATION PLANTING PlANS Rt:PRESENT A CONCEPTUAL PLANT LAYOUT. flNAL
PLANT LOCATIONS SHALL BE AJPPROVEO BY PROJECT REPRESENTATM PRIOR
TO PLANTING.
3. USE ONLY HANO TOOLS TO CLEAR ANO CULTNATE SOIL UNDER TH E CANOPY
(WITHIN ANO 5' OUTSIDE THE DRIPUNE) OF EXISTING TREES.
4. ALL PLANTS SHALL BE NURSERY GROWN A MINIMUt.l or ONE YEAR. PLANT
t.lATERW. IS TO BE SUPPLIED BY COM MERCIAL NURSERIES THAT SPECIALIZE IN
PLANTS NATI\/£ TO TH E PAClnc NORTHWEST. PLANT SUBSTlTUTlONS ARE
SUBJECT TO AJPPROVAL BY PROJECT REPRESENTATM. PLANTS SHAU MEET
THE REQUIREMENTS OF THE LATEST ADDITION OF TH[ At.lERICAN STANDARD
FOR NURSERY STOCK.
5. MITIGATION PLANTING SHALL TAKE PLACE DURING THE OORt.lANT SEASON
(OCTOBER 1ST TO MARCH 1ST). PLANTING t.lAY BE ALLOWED AT OTHER TIMES
AFTER REVIEW AND WRITTEN APPROVAL BY PROJECT REPRESENTATIVE.
6. THE CONTRACTOR SHALL BE RESPONSIBLE FOR DISPOSING or ALL DEBRIS ANO
EXCESS SOIL OCCASIONED BY THIS PROJECT.
7. CONTRACTOR SHAU VERIFY THE LOCATION Of All UTILITIES PRIOR TO
EX CAVATION.
8. ALL DIMENSIONS FOR LISTED HEIGHT, LENGTH ANO CONTAJNER SIZE ARE
MINIMUt.l REQUIREM ENTS.
9. EXISTI NG AREAS DISTURBED BY CONSTRUCTION ACTMTIES ANO NOT SHOWN TO
BE RE-VEGETATED ON THESE PLANS SHAU BE RESTORED AND SEEDED. THE
CONTRACTOR SHALL REPLANT ANY NATM WOODY VEGETATKlN DISTURBED
DURING CONSTRUCTION WITH SPECIES PROVIDED IN THE PLANT t.lATERW.S UST
AT 1:1.
CONIFEROUS TREE PLANTING
DETAIL ffi
DECIDUOUS TREE PLANTING DETAIL
DETAIL ffi
I 0. DISCREPANCIES BETWEEN THE PLANS AN D SITE CONDITIONS SHAU BE
BROUGHT TO TH E AfilNTION OF TH E PROJECT REPRESENTAT II/£ PRIOR TO
PROCE[DING WITH AF FECTED WORK.
11 . CONTRACTOR SHALL BE Rt:SPONSIBLE FOR WATERING PLANTS FOR THE FIRST
YEAR AFTER ACC EPTAN CE OF COMPLETION or PLANTING FOR THE PROJECT.
COUNTY WIU t.lAKE PROVISIONS FOR WATERING AS NEEDED FOR TH E
REMANOER or THE ESTABLISHMENT PERIOD AFTER THE nRST YEAR.
AMENDED
NATIVE SO ILffi._/\
SEE DETAIL ~
NO SCALE
.... ......
.... ;:.
LIVE STAKE INSTALLATION
DETAIL ffi
NO SCALE
I
FINISH GRADE
NO SC ALE
SEE SPECIAL PROVISIONS
FOR MATERIAL REOUIREMENTS
;,,
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;,., ' 0~--,-"/i~~-·1 8 ' , 8' I i~
BRUSH PILE
DETAIL ffi
NO SCALE
12" TO 18" DIA. LOGS. STAK E LOCATION
OF LOG PLACEMENT WHERE INDICATED
IN PLAJNS. ENGINEER SHALL APPROVE
LOC ATIONS BEFORE LOG PLACEMENT
EXISTING GRADE
L-15' TO 25' .tiQlE.;.
LOGS SHALL BE SALVAGED
FROM TREES FLAGGED BY
ENGIN EER FROM ONSITE
WITHIN PROJECT CLEARING
LIMITS.
LICENSED
LANDSCAPE AJRCHIT ECT
HABITAT LOG
DETAIL
NO SCALE
ffi
PROJEC T NAME
PLANT MATERIAL LIST
BOTANICAL NAME
Elli
59 ACER CIRCINATUM '
9 4 ACER MACROPHYLLUM •
16 BETULA PAYRIF[RA •
9 FRAXINUS LATIFOLIA •
69 PICEA SITCHENSIS '
4 6 POPULUS BALSAMIFERA •
178 PSEUOOTSUGA MENZIESII •
52 SALIX LUCIOA •
56 SALIX SITCH ENSIS '
136 THUJA PLICATA '
~
266 CORNUS SERICEA
220 CORYLUS CORNUITA
247 CRATAEGUS OOUGLASII
357 HOLOOISCUS DISCOLOR
481 OEMLERL's CERAS1f0RMIS
469 MYRICA CALIFORNICA
270 RISES SANGUINEM
805 ROSA Nl/Tl<ANA
252 RUBUS PARVIFlORUS
831 SYMPHORICARPOS ALBUS
..tlQIE;
12 . PLANT TREES NO CLOSER THAN I 0-FEET ANO SHRUBS NO CLOSER THAN
8 -FEET FROM EDGE or ROADS. TRAJL WALLS OR SIGNS.
CO MMON NAME MIN SIZE / CONDITION NOTES/ SPACING
VINE t.lAP LE 1 • CAL. / CONT. OR 8&8
BIGLEAF t.lAPLE 1 • CAL. / CONT. OR 8&8
PAJPER BIRCH 1 • CAL. / CONT. OR 8&8 STAKE PROPOSED TREE
LOCATKlNS IN OPEN
OREGON ASH 3· HT. / CONT. OR B&B INnLL AREAS WITHIN
SITKA SPRUCE 3' HT. / CONT. OR B&B
PLANTING AREAS. PLACE
WILLOWS CLOSER TO TH[
BLACK COTIONWOOO 1 • CAL. / CONT. OR B&B RMR EDGE.
DOUGLAS FIR J' HT. / CONT. OR 8&8
PACIFIC WILLOW 1 • X 3· LIi/£ STAKE CUTIING
SITKA WILLOW 1 • X 3' LIVE STAKE CUTTING
WESTERN RED CEDAR 3' HT. / CONT. OR B&B
RED -TWIG DOGWOOD 1 GAL CONT.
BEAK ED HA2ELNUIT 1 GAL CONT. STAKE PROPOSED
BLACK HAWT HORN 1 GAL CONT. SHRUB LOCATIONS IN
OPEN INFlU AREAS
OCEANSPRAY 1 GAL CONT. WITHIN PLANTING
INOIAN PLU M 1 GAL CONT. AREAS
CALl'ORNIA WAX MYRTLE 1 GAL CONT.
FLOWERING RED CURRANT 1 GAL CONT.
NOOTKA ROS E 1 GAL CONT.
THlt.lBLEBERRY 1 GAL CONT.
COMMON SNOWB ERRY 1 GAL CONT.
• REPLACEMENT TREES. DECIDUOUS TREES ARE 1" CALIPER AN D CONIFEROUS TREES AT 3· HEIGHT ARE COUNTED />S EOUWALENT
FOR I. OF CALIPER REPLACEMENT FOR TREES REMOVED BY PROJECT.
95% REVIEW SU~MITT AL
NOT FOR CONSTRUCTION
DRA'MNC NO.
54 OF 59 O N E INCH A T ,..ULL SCALE.
IF N O T . SCA.LE A C C O RDINGLY : I I I I I:::~(;::;; I· _oL•~«vo•r~•v•L~v-Mrl
~ APPROVED
•
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AJ!: ENG!Nff lUNG !"LANNING f NVtftONMf:NTAL SCIENCE&
LAKE TO SOUND TRAIL
SEGMENT A
GREEN RIVE R TRA IL TO NACHES AVE SW
MITIGATION PLANTING DETAILS
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FINAL GEOTECHNICAL REPORT
Lake to Sound Trail
Segment A -Black River Bridge
Renton, Washington
HWA Project No. 2010-100-21 Task 200
Prepared for
Parametrix, Inc.
um HWA GEOSCIENCES INC.
• (;Ctl!Cd111icll} f11s_1l1CCrtll__(:.
• J l,rifro.i,::.eoloiy
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ff1m:I uua, HWA GEOSCIENCES INC.
October 3, 2016
HWA Project No. 2010-100-21 Task 200
Parametrix, Inc.
719 2nd A venue, Suite 200
Seattle, Washington 98104
Attention:
Subject:
Dear Jenny:
Ms. Jenny Bailey
FINAL GEOTECHNICAL REPORT
LAKE TO SOUND TRAIL
SEGMENT A -BLACK RivER BRIDGE
RENTON,\VASHINGTON
Enclosed is the final geotechnical report for the proposed Black River Bridge on Segment A of
the Lake to Sound Trail in Renton, Washington. To stabilize the river banks during a design
earthquake event per AASHTO LRFD bridge design specifications, ground improvement
treatment is recommended. In particular, we recommend the Deep Mixing Method for ground
improvement. The bridge could then be supported on shallow foundations.
We appreciate the opportunity of providing geotechnical services on this project. Should you
have any questions please do not hesitate to call.
Sincerely,
H\V A GEOSCIENCES INC.
Sa H. Hong, P .E.
Principal Geotechnical Engineer
'
21312 30th Drive SE
Suite 110
Bothell, WA 98021.7010
Tel: 425.774.0106
Fax: 425.774.2714
www.hwageo.com
TABLE OF CONTENTS
Page
I. INTRODUCTION ............................................................................................................. 1
1.1. PROJECT DESCRIPTION .................................................................................. 1
1.2. SCOPE OF SERVICES AND AUTHORIZATION .................................................... 1
2. FIELD AND LABORATORY INVESTIGATIONS ................................................................... 2
2.1. FIELD EXPLORATJONS .................................................................................... 2
2.2. LABORATORY TESTJNG .................................................................................. 2
3. SITE CONDITIONS ......................................................................................................... 2
3.1. SURFACE CONDffIONS ................................................................................... 2
3.2. GENERAL GEOLOGIC CONIJITIONS ................................................................. 2
3.3. SUBSURFACE CONDITJONS ............................................................................. 3
3.3.1. Soil Stratigraphy ............................................................................ 3
3.3.2. Ground Water ................................................................................ 5
4. CONCLUSIONS AND RFCOMMENDATIONS ...................................................................... 5
4.1. SEISMIC DESIGN ............................................................................................ 5
4.1.1. General .......................................................................................... 5
4.1.2. Regional Seismicity ....................................................................... 5
4.1.3. Seismic Considerations ................................................................. 6
4.1.4. Soil Liquefaction ........................................................................... 7
4.1.5. Ground Fault Hazard ..................................................................... 7
4.2. SLOPE STABILITY EVALUATIONS ................................................................... 7
4.2.1. Static Slope Stability Analyses ...................................................... 8
4.2.2. Pseudo-Static Slope Stability Analyses ......................................... 8
4.2.3. Post-Liquefaction Slope Stability Analyses .................................. 8
4.2.4. Lateral Spreading and Sliding ....................................................... 9
4.2.5. Global Stability after Ground Improvement.. ................................ 9
4.2.5.1. Static Slope Stability Analyses ................................................... 9
4.2.5.2. Pseudo-Static Slope Stability Analyses ....................................... 10
4.3. GROUND IMPROVEMENT TECHNIQUES (GIT) ................................................. I I
4.3.1. Deep Mixing Method .................................................................... 11
4.3.2. Stone Columns .............................................................................. 14
4.3.3. Ground Improvement Verification Tests ....................................... 15
4.4. SJ !ALLOW FOUNDATIONS ............................................................................... 15
4.4.1. Spread Footing Bearing Capacity for Bridge Support ................... 15
4.4.2. Sliding Resistance on Existing Fill for Cast-In-Place Concrete
Footings ......................................................................................... 15
4.4.3. Passive Earth Pressure Component of Sliding Resistance for ClP
Concrete Footings .......................................................................... 15
4.5. BRIDGE ABUTMENTS, FOOTINGS AND WING WALLS ..................................... 16
4.5.1. Static Lateral Earth Pressures ........................................................ 16
October 3, 2016
HWA Project No. 20 I 0-100-21 Task 200
4.5.2. Seismic Lateral Earth Pressures .................................................... 16
4.6. GRAVITY BLOCK WALLS DESIGN .................................................................. 17
4.7. RESISTANCE FACTORS FOR WALLDESIGN ..................................................... 17
4.8. WALL BACKFILL ............................................................................................ 17
4.9. EMBANKMENT SLOPES .................................................................................. 18
4.10. STRUCTURAL FILL MATERIALS AND COMPACTION ...................................... 18
4.11. SITE DRAfNAGE AND EROSlON .................................................................... 19
4.11.1. Surface Water Control.. ............................................................... 19
4.11.2. Erosion Control ........................................................................... 19
4.12. WET WEATHER EARTHWORK ...................................................................... 19
5. CONDITIONS AND LIMITATIONS .................................................................................... 20
6. REFERENCES ................................................................................................................. 23
LIST OFT ABLES
Table I
Table 2
Table 3
Table 4
Seismic Coefficients for Evaluation Using AASHTO Specifications ........... 7
Global Stability Analyses Results without GIT ............................................. 9
Global Stability Analyses Results after GIT .................................................. 11
Recommended Design Parameters for Gravity Block and Str. E. Walls ....... 17
LIST OF FIGURES (FOLLOWING TEXT)
Figure 1
Figure 2
Figure 3
Figure 4
APPENDICES
Vicinity Map
Site and Exploration Plan
Cross Section A-A'
Proposed Ground Improvement Areas
Appendix A: Field Exploration
Figure A-1
Figures A-2 -A-3
Legend of Terms and Symbols Used on Exploration Logs
Logs of Boreholes BH-1 and BH-2
Appendix B: Laboratory Testing
Figures B-1 -B-4 Particle Size Distribution Test Results
Appendix C: Slope Stability Analyses Results
Figures C-1 -C-14 Slope Stability Analyses
20 IO. J 00 T200 FR 2 HWA GEOSCIENCES INC.
FINAL GEOTECHNICAL REPORT
LAKE TO SOUND TRAIL
SEGMENT A -BLACK RIVER BRIDGE
RENTON, WASHINGTON
1. INTRODUCTION
1.1. PROJECT DESCRIPTION
HWA GeoSciences Inc. (HWA) performed a geotechnical study for the proposed Lake to Sound
Trail Segment A, Black River Bridge in Renton, Washington. The location of the site and the
general project layout are shown on the Vicinity Map (Figure I) and the Site and Exploration Plan
(Figure 2), respectively. The purpose of this geotechnical study was to explore and evaluate
surface and subsurface conditions at the site and provide recommendations for the geotechnical
aspects of the project.
The new trail pedestrian bridge will consist of a single-span steel or concrete girder structure
over the Black River with a minimum span of approximately 114 feet. The new bridge is being
designed in accordance with AASHTO Load and Resistance Factor Design (LRFD)
methodology.
We understand construction impacts will need to be mitigated to protect the wetland located
north of the trail alignment, as well as the Black River channel.
1.2. SCOPE OF SERVICES AND AUTHORIZATION
Geotcchnical engineering services were authorized in a subconsultant agreement dated
November 7, 20 I 4 and two subsequent amendments. Our scope of work included collecting and
reviewing available geotechnical and geologic information in the vicinity of the project site, and
performing subsurface explorations at the proposed ends of the bridge span to determine soil and
ground water conditions. Our work also included coordinating the field activities with the
project team; performing laboratory testing and engineering analyses to develop geotechnical
recommendations for the proposed improvements; and preparing draft and final geotechnical
reports. The need for additional work was identified during the investigation, in which
seismically liquefiable soils were encountered in the borings (unlike the prior borings for the
adjacent Monster Road Bridge) and therefore the need for additional analyses to address lateral
spreading of the river banks, which would adversely affect the proposed bridge.
October 3, 2016
HWA Project No. 2010-100-21 Task 200
2. FIELD AND LABORATORY INVESTIGATIONS
2.1. FIELD EXPLORATIONS
Two exploratory borings were drilled on November 10, 2014 and January 6, 2015. Borehole
BH-1 was drilled on the north side of the river to a depth of 61 feet, and BH-2 was drilled on the
south side to a depth of 86.5 feet. Both borings were drilled utilizing hollow-stem auger
methods. The explorations were supervised and logged by a geologist from HWA, who observed
the exploratory work on a full time basis. A detailed discussion of the field exploration
methodologies and the equipment used is presented in Appendix A, along with the borehole logs
and a legend of terms and symbols used on the logs. The exploration locations are shown on
Figures 2 and 3.
2.2. LABORATORY TESTING
Laboratory tests were performed on selected samples obtained from the borings to characterize
relevant engineering and index properties of the site soils. Laboratory tests included
determination of in-situ moisture content, and grain size characteristics. The tests were
conducted in general accordance with appropriate American Society of Testing and Materials
(ASTM) standards. The test results and a discussion of laboratory test methodologies are
presented in Appendix B, and/or displayed on the exploration logs in Appendix A, as
appropriate.
3. SITE CONDITIONS
3.1. SURFACE CONDITIONS
The proposed bridge alignment is located approximately 80 feet (south end) to 230 feet (north
end) east of Monster Road Bridge in the City of Renton. The river banks in this area are inclined
at approximately 2H: IV. We understand the bridge approaches will be slightly above the
original ground surface on the embankments. Both banks are armored with rip-rap rock having
maximum diameters ranging from approximately 12 to 24 inches.
3.2. GENERAL GEOLOGIC CONDITIONS
The geology of the Puget Sound region includes a thick sequence of glacial and non-glacial soils
overlying bedrock. Glacial deposits were formed by ice originating in the mountains of British
Columbia (Cordilleran Ice Sheet) and from alpine glaciers which descended from the Olympic
and Cascade Mountains. These ice sheets invaded the Puget Lowland at least four times during
the early to late Pleistocene Epoch (approximately 150,000 to I 0,000 years before present). The
southern extent of these glacial advances was near Olympia, Washington. During periods
between these glacial advances and after the last glaciation, portions of the Puget Lowland filled
2010-IOOTIOOFR 2 HWA GEOSCIENCES INC.
October 3, 2016
HWA Project No. 20 I 0-100-21 Task 200
with alluvial sediments deposited by rivers draining the western slopes of the Cascades and the
eastern slopes of the Olympics. The most recent glacial advance, the Fraser Glaciation, included
the Vashon Stade, during which the Puget Lobe of the Cordilleran Ice Sheet advanced and
retreated through the Puget Sound Basin. Existing topography, surficial geology and
hydrogeology in the project area were heavily influenced by the advance and retreat of the ice
sheet.
Surficial geological information for the site area was obtained partly from the published maps,
"Geologic Map of the Renton Quadrangle, King County, Washington"' (Mullineaux, 1965) and
"Geologic Map of'the Des Moines Quadrangle, King County. Washington"' (Booth and Waldron,
2004 ). The maps indicate that the uplands to the southwest and immediate north consist of
Tertiary igneous bedrock predominantly mantled by Pleistocene Vashon till, while the valley
floor is covered by alluvial deposits.
The bedrock consists of highly jointed and faulted andesite. The till was deposited as a
discontinuous mantle of ground moraine beneath glacial ice on the eroded surface of older
deposits. Soils defined as Vashon till consist of an unsorted, non-stratified mass of silt, gravel,
and sand in varied proportions. The till is of high density/strength due to glacial
over-consolidation, and typically has low permeability.
The 1965 map, which includes the subject site, indicates the valley floor is covered by alluvium
deposited by the White River and Green River, prior to historical diversion of the White River
south into the Puyallup in 1906. According to the map this alluvium consists of silt and fine sand
at the surface, becoming medium to coarse sand with depth. Black volcanic sand is typical of
White River deposits in the valley. The Black River formerly was the outlet for Lake
Washington, prior to completion of the Lake Washington Ship Canal in 1917. Very little
sediment would be expected to exit the lake; therefore, Black River deposits would consist
primarily of reworked sediment of the Cedar River and White River.
3.3. SUBSURFACE CONDITIONS
3.3.1. Soil Stratigraphy
Our interpretations of subsurface conditions were based on the results of field explorations, our
review of available geologic and geotechnical data, and our general experience in similar
geologic settings. It should be noted that in-situ tests performed during drilling, e.g. Standard
Penetration Tests represented by N values, identified liquefiable fine sandy silt layers within both
borings. For reference, the blow count values recorded during tests are included on the boring
logs and are plotted on the penetration resistance chart on each log. Soil density descriptions on
the boring logs are based on our observations of soil granularity vs. cohesiveness in addition to
the recorded penetration values.
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In general, the area of the proposed bridge site is underlain by a sequence of layers of recent silty
and sandy alluvium deposited by the historical White River and Black River. This alluvium is
underlain by glacial till. Bedrock was encountered below the till in BH-1. Suitable bearing
material for bridge foundations was encountered at a depth of approximately 45 feet on the north
bank (glacial till, over bedrock in BH-1) and at 67 feet at the south bank (glacial till in BH-2).
The soil units encountered in the borings are described separately and in more detail below. The
conditions are also summarized in Figure 3. Appendix A contains detailed summary logs of
subsurface conditions encountered at the individual exploration locations.
• Fill-Both borings encountered fill at the ground surface to depths of7.5 feet in BH-1 and
approximately 25 feet in BH-2. The fill consisted of medium dense to dense, gravelly silty
sand in the upper 4 to 7 feet, then medium dense to loose sandy silt to silty sand with
variable gravel content. In BH-2 this latter material had the appearance of alluvium with
fine bedding below 17.5 feet; however, a chunk of rubber in the sampler obtained from the
sample taken at 20 feet indicated the material was fill to approximately 25 feet. Based on
this depth of fill, we speculate that it originated as dredge tailings fill from channel
modifications to the Black River. The protective surficial layer of fill on both banks of the
river consisted ofloosely placed riprap rocks.
• Loose Alluvium -Recent alluvial deposits were encountered beneath the existing fill in
both borings. The upper portion of alluvium in BH-1 consisted of fine sandy silt and silty
sand. It was typically very loose with N values ranging from Oto 10 and extended from
approximately 7.5 to 30 feet deep. In BH-2, loose alluvium consisting of slightly silty sand
and sandy gravel was encountered from 25 to 40 feet deep.
• Medium Dense to Dense Alluvium -Gravelly, silty sand was encountered below the loose
alluvium in BH-1 from approximately 30 to 40 feet. In BH-2, medium dense, clean to
slightly silty sand was encountered from approximately 40 to 67 feet, with the upper 5 feet
consisting of dense sandy gravel.
• Glacial Till -Glacial Till was encountered below the alluvium in both borings, and
consisted of unsorted, non-stratified dense to very dense, sandy, gravelly silt to silty,
gravelly sand.
• Bedrock -Bedrock was encountered at a depth of approximately 55 feet in borehole BH-1
at the north bank, but was not encountered within BH-2 at the south bank. This is also a
pile foundation bearing strata at the site. The bedrock consisted of fractured basalt,
becoming less weathered and stronger with depth.
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3.3.2. Ground Water
Ground water was observed during drilling in both borings, at depths of approximately 13.5 and
19 feet below the existing ground surface at BH-1 and BH-2, respectively. Because of relatively
high permeability of the fill soils and silty sand, it is expected that ground water levels will be
reflective of river level. The observed ground water levels during drilling are indicated on the
boring logs and on Figure 3. The ground water conditions reported on the exploration logs are
for the specific dates and locations indicated and, therefore, may not necessarily be indicative of
other times and/or locations. Furthermore, it is anticipated that ground water conditions will vary
in response to other factors such as rainfall, time of year, local subsurface conditions, and other
factors.
4. CONCLUSIONS AND RECOMMENDATIONS
The possibility of lateral spreading of the riverbanks due to soil liquefaction during a design
seismic event became evident after completion of the subsurface exploration program. This was
in contradiction to conditions observed by others in borings conducted for the adjacent Monster
Road Bridge (Golder, 1995). The alluvium encountered in our borings was very loose to
medium dense, as opposed to medium dense to dense as encountered in the Monster Road Bridge
borings. Our analyses indicate the looser soils will liquefy during a design-level earthquake,
resulting in lateral spreading of the riverbanks. Therefore, we recommend the bridge abutment
areas be stabilized through Ground Improvement Techniques (GIT).
Geotechnical recommendations are provided below for bridge seismic design, ground
improvement to minimize potential liquefaction and lateral spreading damage, slope stability,
bridge foundations, bridge abutments and earthwork, and site drainage.
4.1. SEISMIC DESIGN
4.1.1. General
Based on the LRFD Bridge Design Specifications, 7th Edition (AASHTO, 2014 ), potential
secondary effects of earthquakes on the proposed bridge include soil liquefaction, lateral
spreading, seismically-induced settlement, and ground faulting. The following sections provide
additional discussions and recommendations pertaining to these seismic issues for use in design
of the bridge.
4.1.2. Regional Seismicity
The seismicity of northwest Washington is not as well understood as other areas of western
North America. Reasons for this include: (I) incomplete historical earthquake records; (2) deep
and relatively young glacial deposits and dense vegetation which obscure surface expression of
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faults (Hall and Othberg, 1974); and (3) the distribution of recorded seismic epicenters is
scattered and does not define map-able fault zones (Gower, et al., 1985). Historical records exist,
however, of strong earthquakes with local Modified Mercalli Intensities up to VIII (indicative of
structural damage such as cracked walls and fallen chimneys).
Since the l 850's, 28 earthquakes of Magnitude 5 (Richter Scale) and greater have reportedly
occurred in the eastern Puget Sound and north-central Cascades region. Five events may have
exceeded Magnitude 6.0. Researchers consider the North Cascades earthquake of 1872, centered
near Lake Chelan, the strongest (Magnitude 7.4) historical earthquake in the region. Earthquakes
of Magnitude 7.2 occurred in central Vancouver Island in 1918 and 1946. The most significant
recent event, the Nisqually Earthquake, occurred on February 28, 2001, near Olympia and had a
magnitude of 6.8. Other significant historical earthquakes in the region include a 1949 event
near Olympia (Magnitude 7 .2), and a 1965 event centered between Seattle and Tacoma
(Magnitude 6.5). These latter three were intraplate Benioff Zone earthquakes, occurring at a
depth of about 30 miles within the descending subducted oceanic plate.
Potential sources of earthquakes that may be significant to the site include: (I) the Cascadia
subduction zone, along which the Juan de Fuca oceanic plate is being thrust under the North
American plate; and (2) shallow crustal faults that may generate earthquakes in the site vicinity
(McCrumb et al., 1989). The latest subduction zone earthquake in the Pacific Northwest had
been determined from Japanese tsunami records to have occurred in 1700, and recent offshore
sedimentological research has indicated that the entire length of the subduction zone slipped at
once, which would result in an earthquake of around Magnitude 9.0.
4.1.3. Seismic Considerations
Earthquake loading for the proposed Black River bridge structure was developed in accordance
with Section 3.4 of the AASHTO Guide Specifications for LRFD Bridge Design, 2014. For
seismic analysis, the Site Class is required to be established and is determined based on the
average soil properties in the upper I 00 feet below the ground surface. Based on our
explorations and understanding of site geology, it is our opinion that the proposed alignment is
underlain by soils classifying as Site Class D. Table I presents recommended seismic
coefficients for use with the general procedure described in the guide (AASHTO, 2014), which is
based upon a design event with a 7 percent probability of exceedance in 75 years (equal to a
return period of 1,033 years). Ground motions for the site are based on probabilistic earthquake
hazard mapping efforts including those conducted by the United States Geological Survey.
Accordingly, a Seismic Design Category D, as given by the guide (AASHTO, 2014) should be
used.
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T bl 1 S . . C ffi . a e e1sm1c oe 1c1ents i E or va uatmn U. AASHTOS "fi sm2 ,pec1 1catmns
Peak Spectral Spectral Site Amplification
Site Ground Bedrock Bedrock Coefficients Design Acceleration
Class Acceleration Acceleration Acceleration Coefficient
at 0.2 sec at 1.0 sec As, (g) PGA,(g)
S..(g) s,.(g) F,,. Fa F.
D 0.446 0.993 0.331 1.05 I. I 1.74 0.470
4.1.4. Soil Liquefaction
Liquefaction occurs when saturated and relatively cohesionless soil deposits such as silts, sands,
and fine gravels temporarily lose strength as a result of earthquake shaking. Primary factors
controlling the development of liquefaction include intensity and duration of strong ground
motion, characteristics of subsurface soils, in-situ stress conditions and the depth to ground
water. Potential effects of soil liquefaction include temporary loss of bearing capacity and lateral
soil resistance, and liquefaction-induced settlement and deformations, with concomitant potential
impacts on the proposed bridge and embankment fills.
Based on the saturated, loose nature of the alluvium noted below fill in BH-1 and BH-2,
liquefaction will be a design consideration for this project.
Based on the methods by Seed and Idriss ( I 971) and Ishihara and Yoshimine ( I 992), liquefaction
of the loose alluvium/fill layer, 20 feet thick, below the upper medium dense fill will liquefy
during an earthquake with PGA=0.446g and Mw=7.5.
4.1.5. Ground Fault Hazard
The Seattle and Tacoma Faults are probably the most serious earthquake threat to the populous
Seattle-Tacoma area. The Black River Bridge site is located between these faults. A study in
2005 (EERl and Washington Military Dept.) of bridge vulnerability estimated that a magnitude
6.7 earthquake on the Seattle Fault would damage approximately 80 bridges in the Seattle-
Tacoma area, whereas a magnitude 9.0 subduction event would damage only around 87 bridges
in all ofwestem Washington. The same study also found that with failure of just six bridges (the
minimum damage from a Benioff M 6.5 event) there could be at least $3 billion lost in business
revenue alone. Seismic retrofitting would likely reduce damage to key bridges.
4.2. SLOPE STABILITY EVALUATIONS
The proposed pedestrian bridge abutments are to be constructed above the top of the river bank
slopes. The stability of these slopes was evaluated using limit-equilibrium methods utilizing the
computer program SLIDE 5.0 (Rocscience, 2013). Limit equilibrium methods consider force (or
moment) equilibrium along potential failure surfaces. Results are provided in terms of a factor of
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safety, which is computed as the ratio of the summation of the resisting forces to the summation
of the driving forces. Where the factor of safety is less than 1.0, instability is predicted. With
limit equilibrium, the shear strength available is assumed to mobilize at the same rate at all points
along the failure surface. As a result, the factor of safety is constant over the entire failure
surface.
4.2.1. Static Slope Stability Analyses
The static factors of safety calculated along Cross Section A-A', Figure 3, was evaluated with
Spencer's method, Janbu's Simplified method, and Bishop's Simplified method with the
observed site conditions.
The factor of safety of the slope at the southern abutment, under static loading, is
approximately 1.26 and for the northern abutment is approximately 1.1, as shown on Figures C-1
and C-4 of Appendix C, respectively. These analyses indicate that the factor of safety is slightly
greater than 1, which means that the slopes are marginally stable under the static condition with
the current condition of the slopes.
4.2.2. Pseudo-Static Slope Stability Analyses
Cross Section A-A' was evaluated using pseudo-static methods to evaluate the response of the
slope under earthquake loading prior to the onset of liquefaction. Spencer's, Janbu's Simplified,
and Bishop's Simplified methods were used in this evaluation. Pseudo-static slope stability
analyses model the anticipated earthquake loading as a constant horizontal force applied to the
soil mass. For our analyses, we used a horizontal seismic coefficient of 0.235g, which is one-
half of the design acceleration coefficient (As, in Table I). Pre-liquefaction strengths were used
for all materials in this analysis.
The results of these analyses indicate a factor of safety of approximately 0.65 and 0.62, for the
southern and northern abutments, respectively, as shown in Figures C-2 and C-5 of Appendix C.
These analyses indicate that slope instability is likely to occur during the design seismic event,
prior to the onset of liquefaction. As a factor of safety less than 1.0 was calculated, we expect the
existing slopes to undergo lateral spreading upon the onset of liquefaction.
4.2.3. Post-Liquefaction Slope Stability Analyses
Additional stability analyses were completed for the slopes depicted in Cross Section A-A' to
determine the response of the slopes after the onset of liquefaction. The post-liquefaction
residual shear strengths for the liquefiable soils were used to model the anticipated loss of shear
strength during a seismic event. The results of these analyses indicate a factor of safety of
approximately 0.31 and 0.19, for the southern and northern abutments, respectively, as shown in
Figures C-3 and C-6 of Appendix C, respectively. As a factor of safety less than 1.0 was
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calculated, we expect the existing slopes to undergo large lateral spreading upon the onset of
liquefaction.
A summary of the anticipated factor of safety for global stability at the abutments are provided
below in Table 2.
T able 2. Global Stability Analyses Results Without GI T
Factor of Safety
South Side North Side
Static 1.26 I. I 0
Pseudo-Static 0.65 0.62
Post Liquefaction 0.31 0.19
4.2.4. Lateral Spreading and Sliding
Lateral spreading occurs cyclically when the horizontal ground accelerations combine with
gravity to create driving forces which temporarily exceed the available strength of the soil mass.
This is a type of failure known as cyclic mobility. The result of a lateral spreading failure is
horizontal movement of the partially liquefied soils and any overlying crust of non-liquefied
soils. We would expect displacements associated with lateral spreading to be very large at this
site.
Bartlett and Youd ( 1992) used a large data base of lateral spreading case histories and developed
an empirical formula. According to the research, we calculated a yield acceleration (ay=0.2g) by
means of a trial and error method for the existing bank slope (2H: IV) and Newmark's sliding
block slope stability analyses. When an earthquake magnitude Mw=7 occurs, the estimated
lateral spreading ranges from about 24 to 134 inches depending upon assumed epicenter
distances, 60 km (Tacoma Fault) and 6 km (Seattle Fault) away, respectively. Although the
results vary widely, the analyses demonstrate that large lateral spreading is likely during a
significant seismic event.
To mitigate these liquefiable soil conditions and lateral spreading, we recommend that the
strength of the slopes be increased by in-situ ground improvement techniques (GIT). See Section
4.3 for a discussion of GIT methods: Deep soil mixing method (DMM) and Stone column
treatment (SC).
4.2.5. Global Stability after Ground Improvement
4.2.5.1. Static Slope Stability Analyses
The static factors of safety calculated along Cross Section A-A' were evaluated with Spencer's
method, Janbu's Simplified method, and Bishop's Simplified method assuming ground
improvement was performed per Section 4.3.
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The factor of safety of the slope at the southern abutment, under static loading assuming stone
columns as GIT, is approximately 1.30 and for the northern abutment is approximately 1.24, as
shown on Figures C-7 and C-8 of Appendix C. These analyses indicate that the factor of safety
increases slightly after the application of stone columns as GIT. These factor of safety
magnitudes confirm that the composite shear strength properties achieved from the utilization of
stone columns as GIT are not adequate for the stabilization of the slope.
The factor of safety of the slope at the southern abutment, under static loading assuming deep
soil mixing (DMM) as GIT, is approximately 3.5 and for the northern abutment is
approximately 2.5, as shown on Figures C-9 and C-10 of Appendix C. These analyses indicate
that the factor of safety increases significantly after the application of deep soil mixing (DMM)
and that global slope instability is not likely to occur under static loading conditions.
4.2.5.2. Pseudo-Static Slope Stability Analyses
Cross Section A-A' was evaluated using pseudo-static methods to evaluate the response of the
slope under earthquake loading prior to the onset of liquefaction, after the application of GIT.
Spencer's, Janbu's Simplified, and Bishop's Simplified methods were used in this evaluation.
Pseudo-static slope stability analysis model the anticipated earthquake loading as a constant
horizontal force applied to the soil mass. For our analyses, we used a horizontal seismic
coefficient of0.235g, which is one-half of the design acceleration coefficient (As). Pre-
liquefaction strengths were used for all materials in this analysis.
The results of these analyses assuming stone columns as GIT indicate a factor of safety of
approximately 0.77 for the southern abutment and 0.68 for the northern abutment, as shown in
Figures C-11 and C-12 of Appendix C. This indicates that slope instability is likely during a
seismic event, prior to the onset of liquefaction. As a factor of safety less than 1.0 was
calculated, we expect the SC-treated slopes to undergo minor lateral spreading (non-catastrophic)
upon the onset of liquefaction. These factor of safety magnitudes confirm that the composite
shear strength properties achieved from the utilization of stone columns as GIT are not adequate
for the stabilization of the slope.
The results of these analyses assuming deep soil mixing (DMM) as GIT indicate a factor of
safety of approximately 1.6 for the southern abutment and l .2 for the northern abutment, as
shown in Figures C-13 and C-14 of Appendix C. The results shown in Figures C-13 and C-14
are for a sliding surface passing beneath the deep soil mixing depth. Additional to these
analyses, we evaluated potential sliding surfaces that pass through the deep mixed zone and
shallow sliding surfaces as is recommended by FHW A design manual for deep soil mixing
(FHW A, 2013). These analyses indicate that global slope instability is not likely during the
design seismic event.
The summary of the stability analyses is summarized in Table 3, below.
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Table 3. Global Stabilit Analvses Results after GIT
Factor of Safety
South Side North Side
SC DMM SC DMM
Static After GIT 1.3 3.5 1.2 2.5
Pseudo-Static After GIT 0.77 1.6 0.68 1.2
4.3. GROUND IMPROVEMENT TECHNIQUES (GIT)
The bridge foundations should be designed to withstand liquefaction-induced lateral and down-
drag loading as well as liquefaction-induced lateral spreading. To mitigate liquefaction
conditions and densify the loose sand/silt layer noted below the fill, we recommend ground
improvement techniques (GIT) be applied. Based on our analyses, we recommend the deep
mixing method (DMM). Slope stability analyses of modeled conditions post-application of
DMM present factors of safety greater than 1.0 for static and pseudo-static conditions for both
abutments. Additionally, the deep mixing method reduces the potential of adverse construction
impacts to the river, in comparison to stone columns. The particular methods are described in
Sections 4.3.1 and 4.3.2 below. The section on stone columns is included for comparison, but
we recommend against using stone columns due to inadequate factors of safety against static
slope instability and lateral spreading, and greater (and partly unmitigatable) construction
impacts to the river and adjacent wetland.
4.3.1. Deep Mixing Method
The deep mixing method (DMM) is an in-situ method in which the physical properties of weak
soils are improved by mechanically mixing in wet or dry cement. Specialized augers and mixing
paddles are used to mix the soil in a column. DMM is achieved by a rotating motion with no
vibration applied, such that accidental slope failure during DMM construction will not be likely.
We recommend 4-foot diameter columns. Rows of overlapping soil mixed columns oriented in
the direction of the possible soil movement (perpendicular to river) would resist sliding and
lateral spreading. As a result of DMM, the treated rows will behave like shear walls at the bridge
abutments to resist lateral movement. The rows of overlapping columns should be spaced with a
2-foot gap in between rows (6 feet center to center). The DMM treatment area should begin
above the Ordinary High Water Mark (OHWM) and extend to 4 feet behind ( opposite the river
from) each abutment. The width of treatment area should be 16 feet, making 3 rows of
overlapping columns (see Figure 4). The columns should overlap at least 1 foot along each row.
The ground improvements should be conducted in the dry summer months to take advantage of
lower water levels. The treatment depths should extend to EL -2 and EL -14 at the north and
south banks, respectively. The loose alluvium to be treated is about 15 to 23 feet thick,
extending to depths of approximately 32 feet below ground surface on the north side and 42 feet
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below ground surface on the south side. These depths include a 2-foot penetration into the
medium dense sand layer.
Installation of the first columns should begin just above OHWM and progress away from the
river. A temporary three-sided sheet pile containment wall would be necessary for each
abutment area, along OHWM and perpendicular to the bank along the sides of the GIT areas as
shown on Figure 4. The sole purpose of the containment wall is to prevent any wet spoils
generated from the GIT operations from entering the river. This wall should be designed by the
contractor who will be performing the GIT. We anticipate the sheet pile wall would be
embedded approximately IO feet with a stickup of about 7 feet. We recommend a 5-foot setback
distance from the sheet pile wall to the DMM columns.
We recommend that DMM replacement ratio per volume be on the order of 40 percent. The
cemented soil columns provide high shear strength to resist lateral movements. Typical DMM
unconfined compressive strength (qam. spec) within columns ranges from I 00 to 300 psi depending
upon the sand/silt contents. We recommend a 28-day unconfined compressive strength (UCS) of
qu= 150 psi be achieved by the contractor for 90% of all cores obtained and tested after DMM
completion and wet samples taken during DMM. The specialty contractor should obtain wet
samples at every 5 feet in selected columns (at least one per day) and the samples should be
tested at 7, 14, 28 and 56 days. The specialty contractor should provide drilled core samples at
two DMM columns each at the south and north abutment per the owner's designation. The
specialty contractor should submit laboratory cement slurry mix-design with the unconfined
compressive strength.
Medium dense to dense fill soils were encountered from the surface to depths of 7.5 feet to 17
feet, at the north and south bank, respectively. We recommend that this surface crust (Fill) be
predrilled for each DMM column in order to facilitate the deep mixing method. The existing
river banks are armored with riprap stones which should be removed prior to pre-drilling. The
cost associated with predrilling, removal and restoration ofriprap on the slopes should be
included for estimating the cost of the project. Riprap restoration is still needed after DMM
because untreated areas between DMM will be vulnerable to erosion.
DMM will bring up wet, silty and cementitious spoils to the surface from the mixing process.
This will tend to flow towards the river and will need to be contained by means of a short sheet
pile wall and lined with erosion mats and geotextile fencing. For the extent of ground
improvement proposed, a local specialty contractor estimated about 1,500 cubic yards of soil-
cement spoils would need to be hauled off for disposal. However, this amount shall be re-
evaluated by each contractor based on their equipment and experience for their actual bidding.
We recommend that shallow spread footings resting on the deep soil mixed columns be used to
support the bridge (see Section 4.4).
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DMM Construction Considerations
The existing rip-rap will be an impediment to driving sheet piles for the temporary containment
wall, as well as to drilling for deep soil mixing. The uncertainty of rip-rap size and thickness,
and therefore the relative difficulty of driving/ drilling vs. excavating out the rip rap, poses a
significant cost risk to the project. The risk can be greatly reduced by evaluating the rip-rap size
and thickness in advance, so that the cost of removing the rip-rap can be estimated for budgeting,
and contractors can bid for rip-rap removal on an even basis. All rip-rap within the proposed
treatment areas would need to be removed, as selective removal for each DMM shaft would
remove most of the rip-rap anyway but at greater effort than removing all. The rip-rap size and
thickness should be investigated during design with a trackhoe having at least a 30-foot reach.
The contract should state that rip-rap should be removed prior to driving sheets and drilling for
deep soil mixing. It will need to be done in such a way as to avoid increasing the turbidity of the
river. Assuming removal of rip-rap will be from OHWM and up, the work should not be done
during high tides, e.g. a buffer between the excavation work and river level should be
maintained.
The depth limitation of DMM is about 130 feet. The intended ground improvement depths, in
the range of 30 to 40 feet, are well within the range of maximum depth.
The abutment work space needs to be large enough to accommodate a large crane, other auxiliary
equipment, concrete truck, and pump truck. Adjacent property ownership and land use (wetland,
river and narrow foot print of embankment) constrain the available work areas. The north side
work area is particularly constrained to a narrow width at the proposed bridge site, but in our
opinion and based on conversations with a ground improvement contractor, there is adequate
room for construction. The crane would operate from the level area above the bank crest. Based
on the presence of medium dense granular fill at the surface to a depth of 7 feet, it does not
appear that the north side would require ground mitigation for crane support. However, timber
crane mats may be desirable. The contractor should provide a submittal regarding equipment
type and size, support, and slope stability evaluations, as well as general staging procedures.
Potential turbidity impacts to the river include siltation from removing rip-rap close to the water
line, and runoff from spoils with cement from wet-mixing. These can be mitigated by installing
a sheet pile wall on each river bank just above OHW, lined with visquene, to catch loosened soils
and cement and allow for removal with heavy equipment for disposal off site. The walls would
need to be embedded IO feet and stickup approximately 7 feet. The purpose of the sheet pile
walls is to contain drilling spoils and stonnwater runoff only; it would not stabilize the slope.
Even with predrilling of the columns through the medium dense upper soils, spoils consisting of
excess soil and cement slurry will come to the ground surface and need to be contained and
disposed of continuously as DMM progresses. The volume of material could potentially be up
to, or greater than, the cement replacement volume, e.g. 40 percent of shaft volume.
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Assuming a 4-foot diameter for DMM columns, the lowermost columns would need to be at least
5 feet from the sheet pile wall to prevent destabilization of the wall. By standard procedure,
adjacent column rows would not be installed on the same day, to allow for curing of the cement
before installation of adjacent rows. Constraints to installation sequencing should be provided to
bidders, who will need to provide submittals regarding means and methods including sequencing.
After all DMM columns are installed and rip-rap reestablished on the banks, the sheet pile walls
would be removed. Installation and removal of the sheet pile walls would be conducted with a
crane-suspended vibratory hammer, such that the piles can be installed on a slope distant from
where equipment actually sits.
We recommend that the wet rotary method be specified, and the wet jet method prohibited. With
the wet jet method, which utilizes high-pressure water during drilling and injection of cement
slurry, there is a higher risk of turbid water eruption at the ground surface or within the river.
Also, slope stability could be compromised during installation of the lower columns.
We do not anticipate impacts to ground water flow from DMM. Alkalinity increases will be
temporary during cement treatment and curing of soil columns.
4.3.2. Stone Columns
The stone column (SC) method is a method by which vertical columns are made of compacted
aggregate extending through a deposit of loose soil, and result in increased shear resistance of the
slope and relief of pore-water pressure during the design earthquake event. Using the dry
method, SCs are installed with a vibratory probe and a deep stone feed tube, forcing the
aggregate radially into the loose soil zones, compacting the stone as well as any granular zones
formed in the surrounding soil. Typical diameters of stone columns are 2 to 4 feet. Stone
columns provide dissipation of excess pore pressure during strong shaking and the treated soil
layer will not liquefy.
As indicated in the previous sections of slope stability analyses, SC would not completely
eliminate the slope instability problem during the design earthquake event, but it would prevent
liquefaction of the loose alluvium layer, and thereby reduce lateral spreading (Bohn and Lambert,
2013).
The wet, top-feed method can create "geysers" of silty water coming up from the ground in
random, unwanted locations. If constructed in an improper order, e.g. progressing toward the
river instead of away, then vibrations may cause local liquefaction and accidental embankment
failure.
Based on the higher risks of slope instability as well as turbidity impacts to the river and adjacent
wetlands, we recommend against using the SC method.
20 I 0-100 T200 FR 14 HWA GEOSC!ENCES INC.
October 3, 2016
HWA Project No. 2010-100-21 Task 200
4.3.3. Ground Improvement Verification Tests
DMM Verification Tests
After DMM treatment, two borings should be made at each abutment site with core samples
retrieved for unconfined compressive strength tests. The average strength should be
approximately 150 psi and the minimum strength 75 psi. The geotechnical engineer ofrecord
should evaluate the DMM strength improvement. The boreholes should be backfilled with grout
after coring.
4.4. SHALLOW FOUNDATIONS
Shallow strip and square footings, as recommended below, can be used to support the bridge
structure after DMM treatment is implemented.
4.4.1. Spread Footing Bearing Capacity for Bridge Support
Shallow strip and square footings supporting the bridge abutment and bridge approach retaining
walls on level ground that has been treated with DMM per the strength improvement
recommendations specified above can be designed with a net bearing capacity ( qn) of 12,000 psf
and on sloping ground (2H: l V) 5,000 psfwith a 2-foot minimum width. A resistance factor, <pb
= 0.5, should be applied for the design. All footing areas should be treated with DMM. Total
settlement under the load will be one inch or less. The depths of the footings should not be less
than 18 inches below ground surface for frost protection. Footings located on slopes should have
a minimum embedment depth of 36 inches. The resistance factor for the extreme and service
cases should be 1.0. While earthwork and concrete work for the footings can begin as soon as
the next day after completion of ground improvement, we recommend that 14 days be allowed
for curing of the DMM columns before installation of the bridge superstructure.
4.4.2. Sliding Resistance on Existing Fill for Cast-In-Place Concrete Footings
The friction coefficient at the base of footings should be 0.4. Resistance Factor <p, =0.8 should
be used. The resistance factor for the extreme and service cases is 1.0.
4.4.3. Passive Earth Pressure Component of Sliding Resistance for CIP Concrete Footings
The passive earth pressures for static and dynamic cases shall be estimated per Sections 4.5.1 and
4.5.2, respectively.
2010-100 T200 FR 15 HWA GEOSCIENCES INC.
October 3, 2016
HWA Project No. 20 I 0-100-21 Task 200
4.5. BRIDGE ABUTMENTS, FOOTINGS AND WING WALLS
4.5.1. Static Lateral Earth Pressures
Lateral at-rest earth pressures used for design of bridge abutments under static loading conditions
should be equivalent to that generated by a fluid weighing 55 pcf, assuming the tops of the
abutments are restrained from lateral movement. An equivalent fluid unit weight of 35 pcf
should be utilized if the tops are free to rotate (i.e. active case). The above recommendations
assume a level backslope behind the wall, and that properly compacted, well-drained granular fill
is placed as backfill behind the abutment walls. Traffic surcharge loads should also be included
in the abutment design. The traffic surcharge should be multiplied by the active earth pressure
coefficient (ka) of0.27 for a wall free to rotate, or the at-rest earth pressure coefficient (ko) equal
to 0.43 for a wall restrained from movement at its top.
Lateral loads at bridge abutments can be resisted by passive resistance of buried structural
elements. Passive resistance may be evaluated using an equivalent fluid density of 300 pcf for
structural elements cast neat against the wall on the levelled ground surface. The upper two feet
should be ignored for passive resistance. The soil in front of the wall must also be level for a
distance of at least twice the depth of embedment below the ground surface. If the slope
geometry does not meet these requirements, we recommend the passive resistance be ignored
when evaluating lateral restraint.
In addition, structural elements will need to be able to move sufficiently to generate the full
passive resistance. The lateral movement required to generate 100 percent of the passive
pressure is a function of the type of soil bearing against the footing and the thickness of the
footing. We estimate structural elements founded against undisturbed structural fill would need
to move laterally a distance of0.02H, to generate 100 percent of the passive pressure, where H
represents the height of the structural element. The AASHTO LRFD Bridge Design
Specifications state that surveys of the performance of bridges indicate that horizontal abutment
movement less than 1.5 inches can usually be tolerated by bridge superstructures without
significant damage. It appears therefore that, for abutments with heights not exceeding 6.25 feet,
full passive resistance can be mobilized by allowing the abutment to move laterally a distance
equal to 0.02H.
4.5.2. Seismic Lateral Earth Pressures
During a seismic event, seismic earth pressures acting on bridge abutments should be equivalent
to that generated by a fluid weighing 55 pcf, assuming the tops of the abutments are able to
deflect at least 1 to 2 inches during seismic loading. To determine the lateral earth pressure
under seismic loading, the Mononobe-Okabe analysis was utilized, as formulated by Richards
and Elms (I 992). For computation of the lateral seismic earth pressure a seismic horizontal
coefficient (kh) of0.235 was used. This fluid pressure should be used in place of the earth
20JQ.JOOT200 FR 16 HWA GEOSCJENCES INC.
October 3, 2016
HWA Project No. 20 l 0-100-2 l Task 200
pressure recommended for use under static loading. Note that the current AASHTO code
recommends the resultant of the seismic earth pressures to be applied at l/3*h.
4.6. GRAVITY BLOCK WALLS DESIGN
We understand that portions of the trail will be supported by either gravity block walls or
structural earth walls (SEWs). We assume that the gravity block and SEW walls will conform to
one of the current WSDOT pre-approved systems. and that the wall suppliers will design the
walls for internal stability. The retaining walls should be designed in accordance with AASHTO
Standard Specifications for Highway Bridges. We recommend that each of the walls be designed
using the parameters presented in Table 4.
Table 4.
Recommended Desi2n Parameters for Gravity Block Walls and Structural Earth Walls
Soil Properties Wall Backfill Retained Soil Foundation Soil
Unit Weight (pct) 140 140 140
Friction Angle (deg) 36 36 36
Cohesion (pst) 0 0 0
AASHTOLoad AASHTO Load Group
Group I VII (EP+EQ)
(EP+LL)
Ultimate Bearing Capacity (pst) 5,000 5,000
Acceleration Coefficient (g) NIA 0.47
4. 7. RESISTANCE FACTORS FOR WALL DESIGN
The resistance factors for the Strength Limit State should be obtained from Table 11.5.7-1 of the
AASHTO LRFD Bridge Design Specifications (AASHTO, 2014) for the appropriate wall type.
Resistance factors for the Extreme Event Limit State are provided in Section 11.5.8 also in the
LRFD Bridge Design Specifications.
4.8. WALL BACKFILL
Abutment wall design and construction should be in accordance with applicable WSDOT
Standards. Wall backfill materials should consist of Gravel Backfill for Walls (WSDOT 9-
03.12(2)), or Gravel Borrow (WSDOT 9-03.14), as described in the WSDOT Standard
Specifications (WSDOT, 2014). Placement and compaction of fill behind walls shall be in
accordance with WSDOT 2-09.3( I) E, with the exception that the compaction standard
referenced in Section 2-03.3(14) D should be Modified Proctor, per ASTM D 1557.
2010-100 T200 FR 17 HWA GEOSC!ENCES ]NC.
October 3, 2016
HWA Project No. 2010-100-21 Task 200
Wall drainage systems should also be designed and constructed in accordance with the WSDOT
Standard Specifications. Provisions for permanent control of subsurface water should at a
minimum consist of a perforated drain pipe behind and at the base of the wall, embedded in
clean, free-draining sand and gravel. The base of the drain pipe should be a minimum of 12
inches below the base of the adjacent ground surface at the toe of the wall. The drain pipe should
be graded to direct water away from backfill and subgrade soils and to a suitable outlet.
4.9. EMBANKMENT SLOPES
We recommend that the planned compacted fill slopes or bank slopes be constructed/restored no
steeper than 2H: IV (Horizontal:Vertical). For fill slopes constructed at 2H: IV or flatter, and
comprised of fill soils placed and compacted as structural fill as described above, we anticipate
that adequate factors of safety against global failure will be maintained. Measures should be
taken to prevent surficial instability and/or erosion of embankment material. This can be
accomplished by conscientious compaction of the embankment fills all the way out to the slope
face, by maintaining adequate drainage, and planting the disturbed slope face with vegetation as
soon as possible after construction. To achieve the specified relative compaction at the slope
face, it may be necessary to overbuild the slopes several feet, and then trim back to finish grade.
In our experience, compaction of.slope faces by "track-walking" is generally ineffective and is,
therefore, not recommended.
Even after ground improvement treatment, riprap rocks should be installed on the banks from the
toe level of the slopes to the design flood level of the river. The riprap rocks removed from the
slopes can be re-used. Riprap rocks ( 18" minus in diameter) meeting WSDOT 9-13 and 9-
13.4(2) should be underlain by a 12-inch layer of 4-inch minus Quarry Spalls, per WSDOT 9-
03.6. If rip-rap is not allowed by the agencies, bioengineered erosion protection should be
incorporated into the slope restoration, the design of which is beyond our current scope of work.
4.10. STRUCTURAL FILL MATERIALS AND COMPACTION
In our opinion, the existing fill on site will not be suitable for use as structural fill. Imported
structural fill should consist of relatively clean, free draining, sand and gravel conforming to the
Gravel Borrow specification, Section 9-03.14 (Gravel Borrow) of the 2014 WSDOT Standard
Specifications. If earthwork is performed during extended periods of wet weather or in wet
conditions, the structural fill should conform to the recommendations provided below in Section
4.9, Wet Weather Earthwork.
In general, the backfill should be placed in horizontal lifts and compacted to a dense and
unyielding condition, and at least 95 percent of its maximum dry density, per test method
ASTM D 1557. The thickness of loose lifts should not exceed 8 inches for heavy equipment
compactors and 4 inches for hand operated compactors.
2010-100T200 FR 18 HWA GEOSCIENCES INC.
October 3. 2016
HWA Project No. 2010-100-21 Task200
The procedure to achieve the specified minimum relative compaction depends on the size and
type of compaction equipment, the number of passes, thickness of the layer being compacted, and
on soil moisture-density properties. We recommend that the appropriate lift thickness, and the
adequacy of the subgrade preparation and materials compaction, be evaluated by a representative
of the geotechnical consultant during construction. A sufficient number of in-place density tests
should be performed as the fill is being placed to determine if the required compaction is being
achieved.
4.11. SITE DRAINAGE AND EROSION
4.11.1. Surface Water Control
Surface runoff can be controlled during construction by careful grading practices. Typically,
these include the construction of shallow, upgrade, perimeter ditches or low earthen berms and
the use of temporary sumps to collect runoff and prevent water from damaging exposed
subgrades. Also, measures should be taken to avoid ponding of surface water during
construction. The use of Ground Improvement Techniques will require the use of a sheetpile
containment wall for each treatment area during GIT construction.
Permanent control of surface water should be incorporated in the final grading design. Adequate
surface gradients and drainage systems should be incorporated into the design such that surface
runoff is directed away from structures and pavements and into swales or other controlled
drainage devices.
4.11.2. Erosion Control
In our opinion, erosion at the site during construction can be minimized by implementing the
recommendations presented in Wet Weather Earthwork, Section 4. I 2, and by judicious use of
straw bales, silt fences and plastic sheets. The erosion control devices should be in place and
remain in place throughout site preparation and construction. Potential problems associated with
erosion may also be minimized by establishing vegetation within disturbed areas immediately
following grading operations. Vegetation with deep penetrating roots is the preferred choice,
since the roots tend to maintain the surficial stability of slopes by mechanical effects and
contribute to the drying of slopes by evapotranspiration.
4.12. WET WEATHER EARTHWORK
The on-site fill is considered moderately moisture sensitive and may be difficult to traverse with
construction equipment during periods of wet weather or wet conditions. Furthermore, the near-
surface soils may be difficult to compact if their moisture content significantly exceeds the
optimum. General recommendations relative to earthwork performed in wet weather or in wet
conditions are presented below.
20 I 0-100 T200 FR 19 HWA GEOSCIENCES INC.
October 3, 2016
HWA Project No. 20 I 0-100-21 Task 200
• Earthwork should be performed in small areas to minimize exposure to wet weather.
Excavation or the removal of unsuitable soil should be followed promptly by the
placement and compaction of clean structural fill. The size and type of construction
equipment used may have to be limited to prevent soil disturbance. Under some
circumstances, it may be necessary to excavate soils with a backhoe to minimize
subgrade disturbance that may be caused by equipment traffic.
• Material used as structural fill should consist of clean granular soil with less than 5
percent passing the U.S. Standard No. 200 sieve, based on wet sieving the fraction
passing the %-inch sieve. The fine-grained portion of the structural fill soils should
be non-plastic.
• The ground surface within the construction area should be graded to promote run-off
of surface water and to prevent the ponding of water.
• The ground surface within the construction area should be sealed by a smooth drum
vibratory roller, or equivalent, and under no circumstances should soil be left
uncompacted and exposed to moisture.
• Excavation and placement of structural fill material should be performed under the
full-time observation of a representative of the geotechnical engineer, to determine
that the work is being accomplished in accordance with the project specifications and
the recommendations contained herein.
• Bales of straw and/or geotextile silt fences should be strategically located to control
erosion and the movement of soil.
5. CONDITIONS AND LIMITATIONS
We have prepared this report for use by Parametrix, Inc. and King County in design of a portion
of this project. The report and any other applicable geotechnical data should be provided in its
entirety to prospective contractors for their bidding or estimating purposes, but our report,
conclusions and interpretations should not be construed as a warranty of the subsurface
conditions. Experience has shown that subsurface soil and ground water conditions can vary
significantly over small distances. Inconsistent conditions can occur between explorations and
may not be detected by a geotechnical study. If, during future site operations, subsurface
conditions are encountered which vary appreciably from those described herein, HWA should be
notified for review of the recommendations of this report, and revision of such if necessary. If
there is a substantial lapse of time between the submission of this report and the start of
construction, or if conditions have changed due to construction operations at or near the site, it is
2010-100T200 FR 20 HWA GEOSCJENCES INC.
October 3, 2016
HWA Project No. 2010-100-21 Task 200
recommended that this report be reviewed to determine the applicability of the conclusions and
recommendations considering the changed conditions and time lapse.
This report is issued with the understanding that the information and recommendations contained
herein will be brought to the attention of the appropriate design team personnel and incorporated
into the project plans and specifications, and the necessary steps will be taken to verify that the
contractor and subcontractors carry out such recommendations in the field.
Within the limitations of scope, schedule and budget, HWA attempted to execute these services in
accordance with generally accepted professional principles and practices in the fields of
geotechnical engineering and engineering geology in the area at the time the report was prepared.
No warranty, express or implied, is made. The scope of our work did not include environmental
assessments or evaluations regarding the presence or absence of wetlands, hazardous substances
in the soil, or surface water at this site.
This firm does not practice or consult in the field of safety engineering. We do not direct the
contractor's operations, and cannot be responsible for the safety of personnel other than our own
on the site. As such, the safety of others is the responsibility of the contractor. The contractor
should notify the owner if he considers any of the recommended actions presented herein unsafe.
---------0•0----
2010-100 T200 FR 21 HWA GEOSCIENCES INC.
October 3, 2016
HWA Project No. 20 I 0-100-21 Task 200
We appreciate the opportunity to provide geotechnical services on this project. Should you have
any questions or comments, please do not hesitate to call.
Sincerely,
HWA GEOSCIENCES INC.
BRADLEY W. C. THURBER
Brad W. Thurber, L.G, L.E.G.
Senior Engineering Geologist
2010-JOOT200 FR
Sa H. Hong, P.E.
Principal Geotechnical Engineer
22 HWA GEOSCIENCES INC.
6. REFERENCES
AASHTO, 2014, LRFD Bridge Design Specifications, 7th Edition.
Bartlett, S.F., Youd, T.L., 1992, Empirical analysis of horizontal ground displacement generated
by liquefaction-induced lateral spread, Tech report NCEER-92-0021.
Bohn Cecilia and Lambert Serge, 2013, Case Studies of Stone Columns Improvement in Seismic
Areas, 3rd Conference. Maghrebine en Engenierie Geotechnique.
Brandenberg et al, 2011, Recommended Design Practice for Pile Foundations in Laterally
Spreading Ground, Pacific Earthquake Engineering Research Center.
EERI and Washington Military Dept. -Emergency Management Division, 2005, Scenario.for a
Magnitude 6. 7 Earthquake on the Seattle Fault.
Ensoft, Inc (2002), Documentation of Computer Program LPILE.
Federal Highway Administration (FI-I WA), 2013. Deep Mixing for Embankment and Foundation
Support, Pub. No. FHWA-NRT-13-046, October 2013, McLean, VA.
Federal Highway Administration (FHW A), 1983, Design and Construction of Stone Columns
Volume I, Report No. FHW A/RD-83/026, December 1983, McLean, VA.
Golder Associates Inc., 1995, Geotechnical Engineering Study -Monster Road Bridge
Replacement, Renton, Washington. For INCA Engineers, Inc. dated January 23, 1995.
Gower, H. D., J.C. Yount and R.S. Crosson, 1985, Seismotectonic Map of the Puget Sound
Region, Washington. U. S. Geological Survey. Miscellaneous Investigations Series Map 1-
1613.
Hall, J.B. and K.L. Othberg, 1974, Thickness of Unconsolidated Sediments, Puget Lowland,
Washington, State of Washington, Department of Natural Resources, Division of Geology
and Earth Resources.
Idriss, I. M., and Boulanger, R. W., 2007, SPT and CPT based relationships for the residual shear
strength of liquefied soils, Earthquake Geotechnical Engineering, Proc., 4th International
Conf. on Earthq. Geotech. Engineering.
Ishihara, K. and Yoshimine, M., 1992, Evaluation of Settlements in Sand Deposits following
Liquefaction during Earthquakes, Soils and Foundations, Vol 15, No. I, pp 29-44.
23
McCrumb, D.R., et al., 1989, Tectonics, Seismicily, and Engineering Seismology in Washington,
Engineering Geology in Washington, Vol. I, Washington Division of Geology and Earth
Resources Bulletin 78, pp. 97-120.
Rocscience Inc., 2013, Slide, Version 5.044, Computer Software.
Seed, H.B., and Idriss, I. M. 1971, Simplified procedure for evaluating soil liquefaction potential,
J. Soil Mech. Found. Div.
Washington State Department of Transportation (WSDOT), 20 l l, Geotechnical Design Manual
(GDM), M 46-03.06.
Washington State Department of Transportation (WSDOT), 2014, Standard Specifications for
Road, Bridge and Municipal Construction.
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VICINITY MAP
BLACK RIVER BRIDGE
LAKE TO SOUND TRAIL
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,,. Black River R,p,
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FIGURE NO
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T200
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BLACK RIVER BRIDGE
LAKE TO SOUND TRAIL
RENTON, WASHINGTON
SITE AND
EXPLORATION
PLAN
' ' \ A•
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A South
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10
·I ALLUVIUM ?
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shook:! be considered approximate. Further, the cootact lines shown berween units are
Interpretive in nat\Jre and "lilY vary l.iterally or 'lerticaHv over r0atively !ihort distance,; on
site.
16+00
Black River
17+00
BLACK RIVER BRIDGE
LAKE TO SOUND TRAIL
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IMPROVEMENT AREAS i"'O'io-100
10.4.16 T
APPENDIX A
FIELD INVESTIGATION
APPENDIX A
FIELD INVESTIGATION
Two geotechnical borings were drilled for the proposed Black River Bridge, on November I 0,
2014 and January 6, 2015. These borings were designated BH-1 and BH-2, and were drilled at
the top of the river banks in the general centerline of the proposed bridge alignment. The
borings were drilled to maximum depths ranging from 61 to 86.5 feet below the existing ground
surface. The exploration locations were located in the field by taping distances from known site
features and plotted. The locations of the borings are indicated on Figures 2 and 3.
The borings were drilled by Holocene Drilling, Inc. of Puyallup, Washington, under subcontract
to HWA Geosciences Inc. The borings were advanced using a track-mounted, Diedrich D-50
drill rig equipped with hollow stem augers. Each of the explorations was completed under the
full-time supervision and observation of an HWA geologist.
Soil samples were collected at 2.5-to 5-foot intervals using Standard Penetration Test (SPT)
methods in general accordance with ASTM D-1586. SPT sampling consisted of using a 2-inch
outside diameter, split-spoon sampler driven with a I 40-pound drop hammer using a rope and
cathead. During the test, a sample is obtained by driving the sampler 18 inches into the soil with
the hammer free-falling 30 inches per blow. The number of blows required for each 6 inches of
penetration is recorded. The Standard Penetration Resistance ("N-value") of the soil is
calculated as the number of blows required for the final I 2 inches of penetration. This
resistance, or N-value, provides an indication of the relative density of granular soils and the
relative consistency of cohesive soils.
HWA personnel recorded pertinent information including soil sample depths, stratigraphy, soil
engineering characteristics, and ground water occurrence. Soils were classified in general
accordance with the classification system described in Figure A-1, which also provides a key to
the exploration log symbols. Representative soil samples were taken to our laboratory for
further examination. The summary logs of boreholes are presented on Figures A-2 and A-3.
The stratigraphic contacts shown on the individual logs represent the approximate boundaries
between soil types; actual transitions may be more gradual. Moreover, the soil and ground water
conditions depicted are only for the specific locations and dates reported and, therefore, are not
necessarily representative of other locations and times.
2.010-100T200FR A-I HWA GEOSC!ENCES INC.
RELATIVE DENSITY OR CONSISTENCY VERSUS SPT N-VALUE
COHESIONLESS SOILS COHESIVE SOILS
Approximate Approximate
Density N (blows/ft) Relative Density(%) Consistency N (blows/ft) Undrained Shear
Strength (psf)
Very Loose 0 lo 4 0 15 Very Soft 0 lo 2 <250
Loose 4 to 10 15 35 Soft 2 lo 4 250 500
Medium Dense 10 to 30 35 65 Medium Stiff 4 to 8 500 1000
Dense 30 lo 50 65 85 Stiff 8 lo 15 1000 2000
Very Dense over 50 85 100 Very Shff 15 to 30 2000 4000
"'"' over 30 >4000
uses SOIL CLASSIFICATION SYSTEM
MAJOR DIVISIONS GROUP DESCRIPTIONS ·-GW Gravel and Clean Gravel ·•· Well-graded GRAVEL
Coarse
Grained
Gravelly Soils (11!\le or r10 fines) -~Cs GP Poorly-gr<1ded GRAVEL
Soils
More than
50% of Coarse Gravel w,th
0 GM Silty GRAVEL
FracUon Retained Fines (appreciable
on No. 4 Sieve amount of fines) ~ GC Clayey GRAVEL
Sand and Clean Sand ... SW Well-graded SAND
More than
Sandy Soils (l1ttla or no fmes) Ii SP Poorly-graded SAND
50% Retained
50% or More ll on No. Sand with SM S111ySAND of Coarse
200 Sieve Fines (appreciable ~. So, Fraction Passing
amount of fines) SC Clayey SAND No. 4 S1e~e
ML SILT
Fine Sill
Grained aod Liquid Limit CL Less than 50% Lean CLAY
Soils Clay -~-OL Organic SILT/Organic CLAY -
C
MH Elastic SILT
Silt
50% or More Liquid Limit
Passing aod CH Fat CLAY
Clay 50% or More
No. 200 Sieve
S12e OH Organic Sil T/Organic CLAY
,,,,
Highly Organic Soils PT PEAT
J ,If
%F
AL
TEST SYMBOLS
Percent Fines
Atterberg Limits: PL = Plastic Limit
LL = Liquid Limit
CBR Cal1fom1a Bearing Ratio
CN Consolidation
DD Dry Density (pcf)
OS Direct Shear
GS Grain Size Distribution
K Permeability
MD Moisture/Density Relationship (Proctor)
MR
PIO
pp
Resilient Modulus
Photoionizat1on Device Reading
Pocket Penetrometer
Approx. Compressive Strength {!sf)
SG Specific Gravity
TC Triax1al Compression
TV Torvane
Approx. Shear Strength (tsf)
UC Unconfined Compression
~
I
B
0
~
LI
0
SAMPLE TYPE SYMBOLS
2.0" OD Split Spoon (SPT)
(140 lb. hammer with 30 1n. drop)
Shelby Tube
3-1/4" OD Split Spoon with Brass Rings
Small Bag Sample
Large Bag (Bulk) Sample
Core Run
Non-standard Penetration Test
(3.0" OD split spoon)
GROUNDWATER SYMBOLS
Groundwater Level {measured at
time of drilling)
Groundwater Level (measured in well or
open hole after water level stabilized)
COMPONENT DEFINITIONS COMPONENT PROPORTIONS
COMPONENT SIZE RANGE PROPORTION RANGE DESCRIPTIVE TERMS
Boulders Larger than 12 in
<5% Clean
Cobbles 3mto12in
Gravel 3 in to No 4 (4.5mm)
Coarse gravel Jin to 3/4 in
5-12% Slightly (Clayey, Silly, Sandy)
Fine gravel 314 1n to No 4 (4.5mm)
Sand No. 4 (4.5 mm) to No. 200 (0.074 mm)
12-30% Clayey, Silty, Sandy, Gravelly
Coarse sand No. 4 (4.5 mm) to No. 10 (2.0 mm)
Medium sand No. 10 (2.0 mm) to No. 40 (0.42 mm) 30-50% Very (Clayey, Silty, Sandy. Gravelly)
Fine sand No. 40 (0.42 mm) to No. 200 (0.074 mm)
Sill and Clay Smallerthan No. 200 (0.074mm) Components are arranged in order of increasing quantities
NOTES: Soil classifications presented on exploration logs are based on visual and laboratory observation.
Soil descriptions are presented in the following general order-
Densitylconsistency, color, modifier (if any) GROUP NAME, additions to group name (if any), moisture
content. Proportion, gradation, and angularity of constituents, additional comments.
(GEOLOGIC INTERPRETATION)
Please refer to the discussion in the report text as well as the exploration logs for a more
complete description of subsurface conditions.
-HWAGEoSclENCES INC
Lake to Sound Trail
Black River Bridge
Renton, Washington
MOISTURE CONTENT
DRY
MOIST
WET
Absence of moisture, dusty,
dry to the touch.
Damp but no visible waler.
V1s1ble free water, usually
soil is below waler table.
LEGEND OF TERMS AND
SYMBOLS USED ON
EXPLORATION LOGS
PROJECTNO.c 2010-100-200 FIGURE:
LEGEND 2010-100-200.GPJ 2120115
A-1
DRILLING COMPANY: Holocene Drilling
DRILLING METHOD: Diedrich D-50 track rig with HSA
SAMPLING METHOD: SPT Autohammer
SURFACE ELEVATION: 26.50 :I: feet
"' "' :s
<.)
~
~ i5
:c 0 "' tz-"' "' "' <.) w fil >-"' ""-"' :, DESCRIPTION
0 -
·:::t::·1:i:
SM Medium dense, gray, silty to slightly silty, fine SAND, moist. -Blocky tei,:ture, light broNn at surface, trace organics and
-burnt VvOOd bits.
-'·' (FILL)
-ML Medium dense, dark grayish brown, sandy SILT, moist. -5
-ML Very loose to medium dense, gray, fine sandy SILT, moist to
wet. Trace organic bits and layers, some laminar bedding.
-(ALLUVIUM) 10
-
Blow counts are weight of hammer only.
Sample is wet at tip of sample. Ground water seepage was
15 -observed at 13.5 feet below ground surface.
Abundant organics in sample.
-
20 -
laminar layers or organics.
-
--------------------SM
25 -
Lots of heave encountered, 4-5 feet cleaned out of auger. -Loose, grayish brown, silty, fine SAND, wet.
:
-:_:-::. .:
-. '/:·
30
No recovery of sample .
.
-:_:--· . . -. ,._:-
-SM Medium dense, gray, silty, gravelly, fine to coarse SAND, 'Net. -·:· ::: ... Wood bits and organics observed. :_:· . (ALLWIUM)
35
. : ..
. -... -... · . .... :_.
40 -
a: w
w <.)
w m ~ U) "' 0. "' >-• >->-:, "'~ "' >-z -0 w
w w U) .!= >-
~ ~ ~ !,e a:
0. 0. ,d w
"' "' :c
" " ~e >-
"' "' 0
0s-1 6-9-10
0s-2 9-9-8 GS
0 S-3 4-S.5 GS
0$-4 2-2-3
0s-5 0-0-0 GS
0S-6 1-0-1
0S-7 0-0-0 GS
0s-a 1-1-1
0S-9 1-2-2 GS
~S-10 3-6-10
~S-11 6-10-10
For a proper understanding of the nature of subsurface conditions, this
exploration log should be read in conjunction with the text of the
oeotechnical report.
NOTE: ""rhis log of subsurface conditions applies only at the specified bcation and on the date indicated
and therefore may not necessarily be indicative of other times and/or locations.
-HWAGEoSCIENWINC
Lake to Sound Trail
Black River Bridge
Renton, Washington
LOCA _ : See Figure 2
DATE STARTED: 11/10/2014
DATE COMPLETED: 11/10/2014
LOGGED BY: D. Coltrane
a: w
~ :,:
0 z :,
0 a:
CJ 0
~
0
Standard Penetration Test
(140 lb. v.tJight, 30'' drop}
A Blows per foot
10 20 30
..
.. , ... ...
• .. ··•
...
20
.,
•
••
•••••
•
60
Water Content{%)
40
80
Plastic Limit I e I Liquid Limit
Natural Water Content
BORING:
BH-1
PAGE: 1 of 2
PROJECTNO.: 2010-100-200 FIGLJRE"
BORING 2010-100-200.GPJ 9112116
:c
Ii:"' wj
50 0-
0
5
10
15
20
25
30
35
40 100
A-2
DRILLING COMPANY: Holocene Drilling
DRILLING METHOD: Diedrich D-50 track rig with HSA
SAMPLING METHOD: SPT Autohammer
SURFACE ELEVATION: 26.50 :I: feet
J: >--CL -~!
40
45
50
55
60
65
70
75
80
"' "' '.I
l)
~
~ i5
0 "' "' "' :, l) >-"' "' ::,
SM
DESCRIPTION
Medium dense to very dense, ijght brown, gravelly, silty, fine
to coarse SAND, v.et. Angular gravel and sands, blocky
texture.
(GLACIAL TILL)
Bluish gray, moderately weak, highly v.eathered, fractured,
basalt. Speckled coloring.
{WEATHERED BEDROCK)
""""----1, Bluish gray, moderately strong, moderately weathered,
fractured, BASALT. Speckled coloring.
(TUKWILA FORMATION)
Boring was terminated at 61 feet below suriace in bedrock.
Ground water seepage was observed at 13.5 feet below
ground surface.
O'. w
w l)
"' 2-"' w " . CL :, >-• >->-::, "'~ "' >-2 -0 w oo .E >-w w Wm ~ ~ "' -. O'. CL CL w :, :, :i. ~ J:
" " w" >-
"' "' CL -0
~S-12 9-7-16 GS
~S-13 12-27-44
~S-14 26-13-15
~ S-15 12-10-25
[i<J S-16 50-50/2''
For a proper understanding of the nature of subsurface conditions, this
exploration log should be read in conjunction with the text of the
aeotechnical report.
NOTE: lhis log of subsurface conditions applies only at the specified location and on the date indicated
and therefore may not necessarily be indicative of other times and/or locations.
-HWAGEoSCIENCES INC
Lake to Sound Trail
Black River Bridge
Renton, Washington
LOCATION: See Figure 2
DATE STARTED: 11/10/2014
DATE COMPLETED: 11110/2014
LOGGED BY: D. Coltrane
O'. w >-~
0
2 ::,
0
O'.
"' 0
0
10
•
20
Standard Penetration Test
(140 lb. v.eight, 30" drop)
A Blows per foot
20 30 40
.....
•·
40 60 80
Water Content(%)
Plastic Limit I e I Liquid Limit
Natural Water Content
BORING:
BH-1
PAGE: 2 of 2
PROJECTNO.: 2010-100-200 FIGURE:
BORING 2010-100-200.GPJ 9112/16
50
45
50
55
60
65
70
75
80
100
A-2
DRILLING COMPANY: Holocene Drilling
DRILLING METHOD: Diedrich D-50 track rig with HSA
SAMPLING METHOD: SPT Autohammer
SURFACE ELEVATION: 29.00 t feet
"' 0: w
"' w u
'.'i w "' Z-"' " <( • u 0.. f-• f-__, ~ ::, "'~ "' z -u w __, 6 w w "'.!: f-
r 0 "' __, __, ~ i: "' f--"' "' 0.. 0.. •• w o..-" u " " Z O r ~:! :,. "' <( <( ~e f-
"' ::, DESCRIPTION "' "' 0
0 SP Grass at surface.
SM
~ S-1 20-18-19 Dense, light brov.in, slightly silty, slightly gravelly, SANO,
moist. Broken gravels and concrete.
5
(FILL)
~ S-2 9--12-15
ML ~ S-3 SM Medium dense, gray, slightly gravelly, very sandy SILT, moist. 4-5-7 GS
Wood bits observed.
10
~S-4 5-10-10
~ S-5 3-6-6
15 ~ S-6 5-7-8 GS
SM loose, gray and bro'Ml, interbedded fine to medium SAND ~ S-7 2-2-2
with SILT layers, moist to wet.
20
Ground \\later seepage observed at 19.0 feet during drilling.
SP Loose, gray, slightly silty SAND, wet. Initial 6-inch blow count ~ S-8 30-1-2
is from chunk of rubber in sampler.
25 GP Loose, gray, sandy, fine GRAVEL, wet.
(ALLUVIUM)
~ S-9 1-2-4
30
~S-10 3-3-3
35
~S-11 4-3-3
40
For a proper understanding of the nature of subsurface conditions, this
exploration log should be read in conjunction with the text of the
aeotechnical report.
NOTE: This log of subsurface conditions applies only at the specified location and on the date indicated
and therefore may not necessarily be indicative of other times and/or locations.
-HWAGEoSCIENCFS INC
Lake to Sound Trail
Black River Bridge
Renton, Washington
LOCA See Figure 2
DATE STARTED: 1/6/2015
DATE COMPLETED: 116/2015
LOGGED BY: D. Coltrane
0: w
i
" z ::,
0
"' co 0
~
0
Standard Penetration Test
(140 lb. weight, 30" drop)
A Blows per foot
10 20 30 40
••
•• • ••
••
• •
••
• •
• •
·••·
......
• •
20 40 60
Water Content(%)
Plastic Limit I e I Liquid Limit
Natural Water Content
BORING:
BH-2
PAGE: 1 of 3
PROJECTNO.• 2010-100-200 FIGURE·
BORING 2010-100-200.GPJ 9112116
r tc;:-
wfil
50 "~
0
5
10
15
20
25
30
35
40
A-3
DRILLING COMPANY: rlolocene Drilling
DRILLING METHOD: Diedrich 0-50 track rig with HSA
SAMPLING METHOD: SPT Autohammer
SURFACE ELEVATION: 29.00 :t feet
_,
I 0
Ii:= "' " ~! >-"' 40
45
50
55
60
"' "' '.'i u _,
i5
"' "' u
"' ::,
GP
SP
DESCRIPTION
Dense, gray, slightly silty, sandy GRAVEL, wet. Broken
gravels in sampler.
Medium dense, black, fine to medium SAND, wet. Bits of
w:xx:l noted in samples.
Medium dense, dark gray, slightly silty, fine to medium SAND,
wet. Shells observed.
O'. w
w u
Z-w "' "'. Q. " f-•
~ ::, "'~ z -u
w w Cl).!: w~ _, _,
O'. " Q. Q. •• " " z 0
;\ "' w-
"' a. e
·~s-12 6-16-19
.. ~S-13 4-8-11
~S-14 2-11-10
~S-15 7-10-11
~S-16 6-10-13
"' f-
"' w
f-
O'. w
I
f-
0
GS
GS
LOCATION: See Figure 2
DATE STARTED: 1/6/2015
DATE COMPLETED: 1/6/2015
LOGGED BY: D. Coltrane
O'. Standard Penetration Test w
a' (140 lb. weight. 30" drop)
" A Blows per foot 0 z ::,
0
O'.
CJ 0 10 20 30
. ..
•••
I
f--a.-~! 40 50
40
45
50
55
60
• •
70
75
BO
GM Drilling becomes gravelly.
Poor recovery; broken gravel.
Dense, gray, sandy, silty GR<\VEL, wet. Broken gravels in
sampler.
(GLACIAL TILL)
~S-17 6-20-19
~S-18 9-11-20 GS
For a proper understanding of the nature of subsurface conditions, this
exploration log should be read in conjunction with the text of the
oeotechnical report.
NOTE: ]his log of subsurface conditions applies only at the specified location and on the date indicated
and therefore may not necessarily be indicative of other times and/or locations.
-HWAGEoSCIENCES INC
Lake to Sound Trail
Black River Bridge
Renton, Washington
0 20 40 60 80
Water Content(%)
Plastic Limit I e I liquid Limit
Natural Water Content
BORING:
BH-2
PAGE: 2 of 3
PROJECT NO• 2010-100-200 FIQLJRE:
BORING 2010-100-200.GPJ 9112116
70
75
80
100
A-3
DRILLING COMPANY: Holocene Drilling
DRILLING METHOD: Diedrich D-50 track rig with HSA
SAMPLING METHOD: SPT Autohammer
SURFACE ELEVATION: 29.00 :i: feet
"' "' '.S
Ll
~
~ 5
J: 0 "' li::c <D <I)
" Ll ~! >-<I)
"' :, DESCRIPTION
80
Becomes medium dense, broken gravel in sampler.
85
"' w
w Ll
<D Z-w <( •
0. " t-• >-:, <I)~
t-z -0
w w U) .::
~ ~ Ww
0. 0. "' .,
" " •• Z a " " ~e "' "' 03-19 12-13-17
C:S.!Ll_-1., Very dense, gray, sandy, gravelly SILT, wet. rv1ost likely driven ZI S-20 50/4"
90
95
100
105
110
115
120
on boulder.
Boring terminated at 86.5 feet below ground surface due to
refusal. Ground water seepage was observed at 19 feet
below-ground surface during the exploration.
<I)
t-
<I) w
t-
"' w :c
t-
0
GS
For a proper understanding of the nature of subsurface ccnditions, this
exploration log should be read in conjunction with the text of the
qeotechnical report.
NOTE: lhis log of subsurface conditions applies only at the specified location and on the date indicated
and therefore may not necessarily be indicative of other times and/or locations.
-HWA.GEoSCIENCEs INC
Lake to Sound Trail
Black River Bridge
Renton, Washington
LOCA : See Figure 2
DATE STARTED: 1/6/2015
DATE COMPLETED: 1/6/2015
LOGGED BY: D. Coltrane
"' Standard Penetration Test w
i
Cl z :,
0
"' " 0
0
{140 lb. weight, 30" drop)
.&. Blows per foot
20 30 40
20 40 60 80
Water Content(%)
Plastic Limit I e I Uquid Limit
Natural Water Content
BORING:
BH-2
PAGE: 3 of 3
PROJECTNO., 2010-100-200 FIGURE:
BORING 2010-100-200.GPJ 9112116
J: li::c ~! 50
80
85
90
95
100
105
110
115
120
100
A-3
APPENDIXB
LABORATORY INVESTIGATION
APPENDIXB
LABORATORY TESTING
Laboratory tests were performed on selected samples obtained from the borings to characterize
relevant engineering and index properties of the site soils. Because of the predominantly coarse-
grained nature of the encountered soils, the collected and tested samples should not be
considered representative of the existing soils. For the same reason, only a limited number of
laboratory tests could be performed on the obtained soil samples.
HWA personnel performed laboratory tests in general accordance with appropriate ASTM test
methods. We tested selected soil samples to determine moisture content and grain-size
distribution. The test procedures and results are briefly discussed below.
Moisture Content
Laboratory tests were conducted to determine the moisture content of selected soil samples, in
general accordance with ASTM D-2216. Test results are indicated at the sampled intervals on
the appropriate boring logs in Appendix A.
Grain Size Analysis
The grain size distributions of selected soil samples were determined in general accordance with
ASTM D 422. Grain size distribution curves for the tested samples are presented on Figures B-1
through B-4.
2010-1001'200 FR B-1 HWA GEOSC!ENCES ]NC.
I GRAVEL I SAND
I Coarse Fine I Coarse Medium Fine
U.S. STANDARD SIEVE SIZES
314"
3" 1-1/2" I 5/8" 318"
100 ' : I I
I I
90
' I ' I
I I
BO
f-I I I ! I I g I 70 w I I ;;:
' ! ' I
>-60
"' I
O'. I
w 50 II z u: ,I
f-40 :1
z II I 11 w
0 I
O'. 30 .
w I
Q_
• I
20
I
I
10 .
I
II I I
0
50 10
SYMBOL SAMPLE DEPTH (ft)
• BH-1 S-2 5.0 -6.5
• BH-1 S-3 7.5-9.0
• BH-1 S-5 12.5-14.0
mm,
HWAGEOSCIENCES INC
HWAGRSZ 2010-100-200GPJ 2120115
#4 #10 #20 #40 •'!" #100 #200
-,,.-~ -] • I
I I
' " -"1 \ I
I
'I ' '\ I .\ I I 'I •
I I
' :1 ; : I
II I I "
I
' I
-, ,,
I •
I
I : : Ii
I
II I I I I " 1 05 0.1 0.05
GRAIN SIZE IN MILLIMETERS
CLASSIFICATION OF SOIL-ASTM 02487 Group Symbol and Name
(ML) Dark grayish brown, Sandy SILT
(ML) Dark grayish brown, SILT with sand
(ML) Gray, SILT with sand
Lake to Sound Trail
Black River Bridge
Renton, Washington
SILT CLAY
11
' '
i
! '
'
'
!
'
I I
I
I I
' I
I ' ' i !
0.01 0.005 0.001 0.0005
%MC[ LL PL Pl "Grovel Sand Fines ,, ,, ,,
16 i 1.7 40.4 57.9
i :1 0.7 21.7 77.6
15.0 85.0
PARTICLE-SIZE ANALYSIS
OF SOILS
METHOD ASTM D422
PROJEC7NO 2010-100-200 FIGURE B-1
I GRAVEL I SAND
I Coarse I Fine I Coarse I Medium I Fine l
U.S. STANDARD SIEVE SIZES 3/4"
3' 1-1/2" I 5;8" 3/8" #4 #10 #20 #40 #60 #100 #200
~
100
Ii ~ ~ .
I I I '11--i "' I I I I I 90 I' 11 I ~ jl I ~ I ,. I I I 1--I I I
80 " 1, f--I I I 11 I I (!) " 70 w I I 11 s: 1: 1! ! I
>-60 I I I co
0:: 1' w 50 I
z ,:
U: " f--40 11 II I z w ,:
()
0:: 30 I' I' ' w a.
20 " " '
" " . 10
!I ,: ,: . 0
50 10
~YMBOI SAMPLE DEPTH {ft)
• BH-1 S-7 17.5 -19.0
• BH-1 S-9 25.0 -26.5 .. BH-1 S-12 40.0-41.5
um
HWAGEoSclENcEs INC
isWAGRSl 2010-100-200GPJ 2120115
" ~ I I I I
I ! \ ! " I IC,-_ r+ ~ 1; I II
' I [\" I
I \ ~ I
I
' I I ~ I
I ,,
I
I I
I I
I ; ; I
I I
I 1! ' ' ' 1 0.5 0.1 0.05
GRAIN SIZE IN MILLIMETERS
CLASSIFICATION OF SOIL-ASTM 02487 Group Symbol and Name
(ML) Gray, SILT 'Mth sand and organics
(SM) Grayish brown, Silty SAND
(SM) Yellowish brown, Silty SAND with gravel
Lake to Sound Trail
Black River Bridge
Renton, Washington
SILT CLAY
0.01 0.005 0.001 0.0005
%MC LL PL Pl Gr:_vel s~,nd Fi~es
56 20.4 79.6
38 71.8 28.2
25 15.3 39.4 45.3
PARTICLE-SIZE ANALYSIS
OF SOILS
METHOD ASTM D422
PROJECT NO 201 Q-1 QQ-2QQ FIGURE: 8-2
GRAVEL SAND
Coarse Fine Coarse Medium Fine
U.S. STANDARD SIEVE SIZES
314'
3"
100
1 1/2" 5/8" 3/8"
>-I
Cl
w ;;:
90
BO
70
>-60
"' 0::
W 50 z u:
f-40 z w
~ 30
w c..
20
10
a
', I
I
I
I
I
I I
! ,!
'I 1,
I
,,
50
SYMBOL SAMPLE
• BH-2
• BH-2 .. BH-2
mm,
I
I
'
Ii i
I
II I
I
" I
I
,: I
I: I
I
Ii !
S-3
S-6
S-13
HWAGEoSCIENCES INC
HWAGRSZ 2010-100-200GPJ 2120115
I I I , I
i !
I
I I
I
DEPTH (fl}
7.5 -90
15.0-16.5
45.0 -46.5
#4 #10 #20 #40 #60 #100 #200
I i i ', ~ I I I I
~ ~ " ~, I I '" ! I
I ' Ki I
I ! I
j
I I I~ I I I ! I Ii !
1 I I I i
I I
I I
I I I
\ I I I
I i I I ,, II ' i i i I
I I I
I " i i I
" 'i I I
I I " !I i\ ' I I
i " " i ! '-I I
I I!, !I i !
I~. I
I
'
1 0.5 0.1 0.05
GRAIN SIZE IN MILLIMETERS
CLASSIFICATION OF SOIL-ASTM 02487 Group Symbol and Name
(ML) Dark grayish brown, sandy SILT
(ML) Dark grayish brown, sandy SILT
(SP) Black, Poorly graded SAND
Lake to Sound Trail
Black River Bridge
Renton, Washington
SILT CLAY
!
I
! '
i '
!
I
I
i '
i
!
I
0.01 0.005 0.001 0.0005
%MC LL PL Pl Gravel I Sand Fines
"' ' "' "'
19
18
29
1.2 46.8 52.0
3.2 44.2 52.7
5.7 89.9 4.3
PARTICLE-SIZE ANALYSIS
OF SOILS
METHOD ASTM D422
PROJECTNO.: 2Q1Q-10Q-2QQ FIGURE· B-3
GRAVEL SAND
Coarse Fine Coarse Medium Fine
U.S. STANDARD SIEVE SIZES
3'
100
90
60
314"
1-1/2" I 516" 318"
\ ~I I
\ti I
I
#4
I
I
r Ii
#10 #20 #40 #60 #100 #200 . .
~ I I I I I
I I I I I -I i i I
! ! I
f-
I
~ 70 Ii
~ ~~ 1: ;
I \ I I ~ I
I ! ! I
w ;;:
>-Ol
c:: w z u:
I;:
w
~ w a.
SYMBOL
• •
•
6-0
,,
50
40 "
3-0 I'
20
10 Ii
0 so
SAMPLE
BH-2
BH-2
BH-2
um
1: '
I! '
1: '
1: ;
Ii
S-16
5-18
S-20
HWAGEOSCIENCFS INC
H\l\'AGRSZ 201(>.100·200.G~J 2120115
10
DEPTH (ft)
60.0 -61.5
75.0 -76.5
86.0 -86.5
I I I I I
1! I I
~ ' I l : ~ I
I I
I I
I I
I \ I I
I I I
1: ' ' ' I I
I I I
1, ' i ' I
I i I
I j\ I
1! i ! N I
I I
,! I I I . '
5 1 0.5 0.1 0.05
GRAIN SIZE IN MILLIMETERS
CLASSIFICATION OF SOIL-ASTM 02487 Group Symbol and Name
(SP-SM) Dark gray, Poorly graded SAND with silt
(GM) Gray, Silty GRAVEL with sand
(Ml) Gray, Sil T with sand
Lake to Sound Trail
Black River Bridge
Renton, Washington
SILT CLAY
I
I
0.01 0.005 0.001 0.0005
%MC LL PL Pl Gravel Sand Fines
" '" •; .
23 0.9 92.0 7.1
21 27.7 22.7 49.6
21 12.3 23.5 64.2
PARTICLE-SIZE ANALYSIS
OF SOILS
METHOD ASTM 0422
PROJECT NO.: 2Q1Q-1QQ-2QQ FIGURE B-4
APPENDIXC
SLOPE STABILITY ANALYSES, COMPUTER
CALCULATION RESULTS
:5atety r•c"Cor
0 .000
~ 0 .500
1.000
1,500
~ 2.000
2.SOO
:!.000
3.SOO
~ '4,000
4.SOO
s.ooo
~ 5.SOO
(i,0001-
~
~
~
~
~ ....
Project Number . 20 10-100-21 Task·200
P,oject Name . 8'ack Rtver Bndge
lake lo Sound Tra il
Renlon . Washington
Analysis Methods use-d
Bishop simplified
Spence,
Janbu simplrfie<I
South Side· Static Analysis
•100
Material: Fill
Slrenglh Type: Mohr.Coulomb
Uno Weight 1 JO lb/Ill
Fr,c11on Angl e 36 degrees
T
•120
Material · Loose Sand
Strenglh Type : Mohr.Coulomb
Un< Weight 110 lb/113
Fnc11on Angle 28 degrees
Material: Medium Dense .4Jh.Mum
Strength Type Mohr-Coolomb
Unit Wetgln: 124 ll>'lll
Friction Angle: 35 degrees
Matenal: Glacial TiH
Strength Type. Mohr-Cou!omb
Und Weigh t· 134 lb/113
Fricti on Angle: 36 degree,
.,.., ., ... ~11D
STATIC STAB ILITY: SOUTH ABUTMENT
u~ I HWA GEOSCIENCES INC
BLACK RIVER BRIDGE
LAKE TO SO UND TRAIL
RENTON, WA
e,oo
PROJECT 00
2010-100-2 1
Sa.!ety F<?.c tor
0.000
! 0 .500
1 .0 0 0
1 .5(10
~ 2 .000
2.500
3 .000
! 3.500
4 .000
4 .5 00
5.000
~ 5.500
,.ooo +
~
~
~
~
§
.... ....
Pro1ec1 Number· 20 10-100-21 Tas k·200
PJ oiect Name. Black RN'E'1 Budge
lake to Sound T1a1I
Rerioo . W3shtnglon
Material: F1U
S11eng1h Type Mohr-Coulomb
Und W eight 130 1Wft3
Fu ct ion Angle. 36 deg1ees
·,.....-.!!.. _______ _
Analysis Methods used·
Bishop s1mptrfied
Spencer
Janbu s1mplrfied
Malena! l oose Sand
Strength Type· Mohr-Coulomb
Unit We;gt,1 110 11>i11 3
Fnctrnn Angle 28 degrees
Maten.al· Medium Dense Allwum
Strength Type . Moh1.Coulomb
Unn Weight 124 lblft3
F ricttOn Ang.e: 35 degr ees
Mateual. Qac1al Tin
St1ength Type Moh,.Coulomb
Unit Wei ght. 13d lt.'ft3
Fnct1on Angle : 36 degrees
1"------------------1·~·1----------------.,
e-100 et 0!00 <220 e,240, e2ao e,oo
SEIS MI C STABILITY: S OUTH ABUTMENT (DE SIGN EVENT)
u~, I HWAGEOSCIENCEs lN C.
B LACK R IVE R BRIDGE
LAKE T O SOUND T RAIL
RENTON, WA
PROJECT NO
2010-100-2 1
~ Sal~t v !'actor
0.000
0 .500
1 .(100
! 1.soo
2 .(100
2.500
~ 3.000
3 .500
4..000
4 .500
§ 5.000
5 .500
6.000+
~
~
~
~
§
....
P1oiec1 Number. 2010-100-21 Task:200
Pro.,ec1 Name . Black Rr.-er Sndge
lak.e to S ound Trail
R&nton. Washington
South SKl e: Post Liquefaction Anatysis
M.rteriaJ F~I
Strength Type . Mohr-Coul omb
Uno We~ht. 130 lblft3
Fuctton Angle : 36 di gree s
. , .. 0'20
M atenal· loose Sand
Strengt h Type : Mohr -Coolomb
Unil Weight 11 0 lb/113
FnC11on Angle· 5 degrees
~fatena1· Medium Dense AIILMum
Stre ngth Type. Moh r.Coulomb
Uni! Weighl 124 11>'!13
Frict ion Angle: 35 degees
Matenal: Glacial Til
St,engt h Type· Mol-.-Coulon-b
Unit Weight: 134 lb/113
Frid ion Angle. 36 degrees
..... e110
o~, I HWA GEosc,ENCES INC.
0200 <280
POST LIQUEFACTIO N STABILITY: SOUTH A BUTMENT (DES IGN EV ENT)
BLACK RIVER BR IDGE
LAKE TO SOUND TRAIL
RENTON .WA
PROJ ECT NO.
2010-100-21
Safety !'ac tc-::
' 0.000
o.soo
l .lJOO
1 .500
~ ,.ooo
;.500
).000
~ 3.500
4 .0(10
4.50('
~ 5 ,00{'1
s.soo
6,0(10 ,j,
~
~
~
~
~
e 120
Proiect Number. 2010-100-21 Tssk.200
Project Narne Black River Bridge
Lake to Sound Trai l
Rent on , Washington
North Side: S1auc. Anatys1s
Material. Medium Dense AJh.MUm
Strength Type· Mohr-Coulomb
Un< We,ghl 124 lblft3
Cohesion· 1 psf
Fnclion An9'e 34 degrees
.... 6110
Material Medium Dense Glac ial Till
Suength Type Mohr-Coulomb
Unrt We ight. 130 11>1ft 3
Cohesion· 1 psf
Fnctioo Angle. 36 degrees
::r~ I HWAGEOSCIENCES INC
Analysis Methods used
Bishop s,mphfied
Janbu simplified
Spencer
Mateual FiU
S1re1191h Type-M ohr-Coolomb
Un,t we,gt,1 130 lb/113
C hes1on: O psf
F 1ction Angle 36 degees
Material. Loose Sand
Strengih Type-Mohr-Coulomb
Umt We,ghl tlO 11>'!1 3
Cohesion· 1 psf
F nctionAngle . 28 degrees
M.tenal Bed Rock
S1rength Type · Mohr-C oulomb
Unrt Weight 145 lblft3
Cohesion 1 psf
Fuc:t1on Angle 45 deg,ees
STATIC STABILITY: NORTH ABUTMENT
BL AC K RIVER BRIDGE
LAKE TO SO UN D TRAIL
RENTON , WA
PROJECT NO
20 10-100-21
Safety f actor
! 0.000
0,500
1.000
! 1.SOO
2.000
2 .500
3.000
~ 3.500
,.ooc
4 ,500
~ 5,000
5.500
6 .(100+
~
~
~
~
~
0120 0140
Project Number. 20 10-100 -21 Ta sk.200
Projecl Name Black Aiyer Bridge
l ake to Sound Trail
Aen1on. Washington
Nor1h Side . Ps,udo ~ Static Analysis
Malerial. Medium Denn Alluvium
Strength T)'J)e. Mohr-Coulomb
Umt We,ght 124 lblft3
Cohesion· 1 psf
Friction Angle : 34 degrees
.... ~110
D&i1 I HWA GEOSCIENCES IN C.
Material: Medium Dense Glacial Till
Strength Type · Mohr-Coulomb
Unrt Weight: 134 ID!ft 3
Cohesion: 1 psf
frict ion Anfje . 36 degrees
0200
Matenal: Fill
Strength Type Mot.-Coulomb
Uno Weight: 130 tb/113
Cohes,on· 0 psi
Friction Angle 36 deg,ees
',,..~------..,::, __ ...;•
Mattrial· loose Sand
Strength Type. Mohr-Coulomb
unn Weight · 11 0 tb/113
CohesW>n· I psr
Friction AnfJ.e : 28 degree s
Matenal: Bed Rock
St,ength Type : Moh r-Coulomb
Un,t Weight. 145 lbtl3
Cohesion· 1 psf
Fnt11on Angle · 4 S degrees
L.'"'"'
F'"
. ...,
SEISMIC STABILITY: NORTH ABUTMENT (DES IGN EVENT)
BLACK RIVER BR IDGE
LAKE T O SOUND TRAIL
RENTON, WA
PROJECT NO
2010-100-21
~ Sduy Factor
0 .000
0.500
1.000
' 1.SOO
2.000
2.500
3 .000
~ 3. soo
4 ,000
4 • .500
~ s.ooo
5.500
,.oOO •
~
i
~
!
e120 ....
Project Number 201 0-100 -21 Ta sk 200
Pro1ect Name Black River Bndge
La~e to Sound Trail
Renton. W ashing1on
North Side. Post Liquefaction Analysis
Matenal· Med10m Den se All~um
Strength Type Mohr -Coulomb
Unrt Weight 124 lb/!1.3
Cohe sion 1 psf
Fricuon Angle 34 de91ees
Material: Medium Dense Glacial Ttll
Strength Type · Mohr-Coulomb
UM Weight · 134 lb/!13
Cohesion. 1 psf
Friction Angle: 36 degrees
e,eo 0180 ., ..
:r~, I HWAGEOSCIENCES INC
Mate nal Fri!
Strength Type . Mohr-Coulomb
Unn Weight 130 lb/!1.3
Cohesion· 0 psf
Friction Angle 36 degree•
Material Loose Sand
Strength Type. Mohr-Coulomb
UM Weight 110 lblft3
Cohes,on 1 psf
Friction Angle 5 deg,ees
Matenal Bed Rock
Strength Type : Mohr-Coulomb
Unn Weight 145 tbl!l.3
Cohesion · 1 psf
Friction Angle 45 degrees
... ..
P OST LI QUEFACTION STABILITY: NORTH A B UTM ENT (DESIGN EVENT)
BLAC K RIV ER BRI DGE
LAKE T O SOUND T RAIL
RENTON , W A
••
PROJECT NO
201 0-100 -2 1
Safety F•etcr
0 .000
¥
0 .500
1.000
l.SOO
2,000
~ 2,500
3 .000
3.SOO
! •• ooo
4..SOO
S.000
§ s.soo
6 .000+
~
~
~
~
~
.... 0020
Fill
Strengch Type . Mohr-Coulomb
Un,1 Weight 130 lb/113
CohOSl()l1 " 0 psi
Frit110n Angle · 36 deg:tes
Water Surface Water Table
Loos, Sand
Slrength Typo . Mohr-Coulomb
Unn Weight . 110 lblllJ
Cohesion: 1 psf
Fnchon Artg.e · 28 degrees
Water Surface Wate r Tabte
Medium Dense .A.Jh.Mu m
Strength Typo . Mohr-Coulomb
Unl Weight. 124 lblft3
Cohesion 1 psi
Fnclion Angle 35 degrees
Water Surface: Water Ta~e
.... 0000
n~, I HWA GEOSCIINCEs INC.
Projecl Numbe~ 2010-100-21 Task·200
Project Name . Black River Budge
Lake lo Sound Trail
Ren1on , Washington
South S,de : Stat«: Anelysis
After Ground lmprovemenls
(Stone Columns)
GJacial Till
Slrength Type . Moh r-Coulomb
Unn Weight . 134 lb'lJ
Cohesion· 1 psf
Fnction Angle · 36 degrees
Wmer Surlace: Water Table
lmproved Matenal
Strength Type: Mohr-Coulomb
Unit Weigh!. 115 lb/113
Coliesion . 1 psi
Friction Angl e 32 degrees
Wate r Surface· Water Table
eoso 15100 0120 ....
!Mediu m DenseAlllMum!
.... 15110 .. ..
STATIC STABI LITY AFTER GROUND IMPROVEMENTS :
STONE C OLUMNS -SOU T H ABUTMENT
BLACK R IVER BRIDGE
LAKE TO SOUND TRAIL
....
PROJECT NO
2010-100-21
....
Proj<cl Number 2010-100-2 1 Task ·200
Pio~cl Name· Blatk R.,,., Bridge
L.ake 10 Sound Tra,I
Renton . Wa shing1on
Nonh Stde S1a11c A.nalysis
Afte r Ground lmprcwemenl s
{Stone Columns)
Fill
Strength Type Mohl-Coulomb
Unrt W e,ghl 130 lb/113
Cohesion o psf
Friction Angle 36 degrees
Water Surface Water Table
Loose Sand
Strenglh Type. Mohl-Coulomb
Uno We,ght 110 lb/!13
Cohes,on 1 psf
Ftict1onAngle. 28 d&g,ees
Wate r Surface Water Table
Medium Dense AlllMum
Strengl h Type Mohr-Coulomb
Unn Weight 124 lb/113
Cohes,oo. 1 psf
F ri<;hon Angle 34 degrees
Water Surfsce . Water Table
•• ....
Glaci al HI
Strength Type Mohr-Coulomb
Unrt Wetght 134 lblft3
Cohesion · I p<f
FncttonAngle · 36 degrees
Water Surface · Water Ta bl e
Bed Roc k
Strength Type· Mohl-Coulomb
Unn Weight· 14 5 lblft3
Cohes oo 1 psf
Fnct1on Angle 45 degrees
Wal er Surface · Water Table
knproved Malena!
Strength Type · Mohr-Coulomb
Unrt Weight· 115 lblft3
Coheston 1 psf
Fnction Angle 32 degrees
W ater Surface Wal er Tabl e
....
Ir~ I HWA GEOSCIENCES lNC.
!Dense Glacral Tin!
Analysis ~1ethods used
Btshop simpldied
Janbu simplified
Spencer
1"<---------------i1:::::?1J---------------t
.,., . ... 0200 .,., e ,oo
STATIC STABI LIT Y AFTER GROUND IMPROVEMENTS :
STONE COLUMNS -NORTH ABUTMENT
BLACK RIVER BRIDGE
LAK E TO SOUND TRAIL
PROJECT NO
2010-100-21
!
'
!
§
S•!dy F•ct-or
..
0 .000
0 .500
1.000
1 .500
2 .000
2 ,500
3 .000
3 .500
4.000
-t .~oo
S.000
5.500
6 .000+
FIii
Strength Type · Mohr.Coulomb
Uni Weight · 130 lblft3
CohesK>fl· O psf
Fnctioo Angle. 36 dogrees
Wa1e1 Suri.le, Waler fable
Loose Sand
Sueogth Type Mohl-Coulomb
Un< Weigh! 110 lb/113
Cohesion. 1 psf
Fnction Angl e· 28 degree s
Wate r Sutface Wa1e1 Table
Medium Dense AJh.Mum
Strength Type · Mohr.Coulomb
Uni We;gt,1 124 lb/113
Cohes,on: 1 psf
Fnction Angle. 35 deg,ee'.I
Water Surface· Waler Tab(e
....
Project Number 2010-100-2 1 Task 200
Project Namt: 81ac.k Riwr Bndge
Lake 10 Sound Tral
Renton, Washington
SolJth &de· Pseudo.Static Analysis
Mer Ground lmpn1trement s
(0.ep S0<I Mixing)
Glaci8'T1II
Strength Type: Mohr-Coulomb
Unn Weight. 134 lb/113
Cohesion: 1 pst
Frie.Mn Angle 36 degrees
Water Suiface Wster Table
Improved Materi8'
Sllenglh Type. Mohr-Coulomb
Unn Weight 120 lb/11 3
Cohesion: 2000 ps1
Friction Angle . 32 degrees
Water Surface· Wal.er Ta bl e
... , o,oo .. ,.
::rw I HWAGmsc,E NCEs INC
. ... .... ~110
ST ATIC STABI LI TY AFTER GROUN D IM PROVEMENTS:
DEEP SOI L M IX IN G -SOUT H ABUTM ENT
BLACK RIVER BRIDG E
LAKE TO SOUND T RAIL
PROJECT NO
2010-1 0 0-21
!
!
~
§
~
Sa!ny r a c:t o i:
0 ,000
0.500
1.000
Pro,ect Number 2010-1 00-21 Task.200
P,ot9ct Nsme Black Rive, Sndge
1.5-00
2 .000
Lakt t o Sound Trail
Renton . Washington
,.soo
3.000
North SHie Pseudo·Stahc Analysis
M er Ground lmprovemems
{De ep So,I Moxing)
3.500
,.ooo
,.soo
S.O<IO
5 .SOO
6.000+
6 100
Fdl
Streng1h Type Mohr-Coulomb
Unn Weight· 130 lblft3
Coheston O ps f
FncllonAngle. 36 deg,ees
Water Sutface Water Table
l oose Sa~
Strt ngth Type M ohr-Coulomb
Unn We,ght 110 lb/113
Cohesion 1 psf
friction Angle 28 de,grees
Wa1a1 Sortace Waler Table
Medium Dense AlllMum
Strength T1'PO Moht.Coulomb
Unrt We;gt-< 124 lblllJ
Cohesion 1 psf
Fnc1ionA.n9'e 35 deg,ees
Wa1 er Surface Water Table
.. ,. ....
G1~1:alTill
Stiength Type Motu-Coolomb
Unn Wetgnt· 134 lb/ft)
Cohesion 1 psf
Fnct1on Angl e 36 deg,ees
Wa1e, Surtace Wmtr Tablt
S.d Roc k
Strength Type· M ohr.Coulorrib
Unn Weight 14S lblft3
Cohesion 1 psf
FnctionAngle 4S degrHs
W mer Surface Water Table
Improved Malena!
Strength Typo Mohl-Coulomb
Unn Weigh• 120 lblftJ
CoheslOI\ 2000 psf
Fnction Angle 32 degrees
Water Surtace Watu Tabl e
.... ~110
IJW I HWA GEOSCIENCES INC.
!De nse Glacial Ti!!
..,,.
An,tys,s: Methods used
B ishop simphfied
Janbu $1mpltfled
Spenctr
030
STATIC STABILITY AFTER GROUND IMPROVEMENTS:
DEEP SOIL MIXI NG -NORTH ABUTMENT
BLACK RIVER BRIDGE
LAKE TO SOUN D TRA IL
PROJECT NO
2010 -100-21
Sa.re~y fac'tOr
0.000
! o.soo
1.000
LSOO
! 2.000
2.soo
3.000
3.500
¥ ,.ooo
,.soo
S.000
§ S.500
6 .000+
!
~
~
~
§
Fill
Strength Type Mohr-C oulomb
Uno Weigh1 · 130 lb/113
Cohe&1on· O pst
Friction Angle 36 degrees
Water Surface· Water Table
loose Sand
Strength Type Mohr-Coulomb
Uno Weight · 110 lblll3
Cohesion: 1 ps:f
Friction Angie. 28 degrees
Water Surface· W3ter Table
Medium Dense Alluvium
StrengJh Type Mohr-Coulomb
Unn Wei9h1 : 124 lblft3
CoheSton. 1 psf
Friction Ang.e. 35 degrees
Water Surface. Water Table
.... ....
Projeet Number: 20 10-100-21 Task:200
Pro1ect Name Black Rive, Bridge
Lake to Sound Trail
Renton. Washington
So'"h Side Pseudo Static Analysis
After Ground lmp,OWtments
(Stone Columos)
Glacial Till
StrengJh Type. Mohr.Coulomb
Uno Weigh1: 134 lblll3
Cohe,i9n: 1 p,f
Friction Angle. 36 degree s
Wa!.tr Surface . Water Table
Improved Material
Strer,glh Type . Mohr-Coulomb
Unn Weigh1 . 11 5 lblll3
Cohes,on 1 psf
Fnchon Angle. 32 degree s
Water Surface Wa1 er Tabte
.... ., .. 01'0
n~, I HWA crnscrENCE s INC.
01<0 ., ..
!Medium Dense Allooum!
e.110 ....
PS EUD O STATI C STABI LI TY AFTER GROUND
IMPROVEMEN TS : STON E COL UM NS-SOUTH ABUTM ENT
BLAC K RIVER B RIDGE
LAK E T O SO UND T RAI L
..
PROJECT NO
2 010-100 -2 1
..
~
~
!
§
~
Sa!r:ty fa c t or
0.000
o.soo Project Numbet 2010-100-2 1 Task:200
Project Name · Bleck River Bndge
1.000 Lake to Sound Tr ail
Renton . Washingt on
1.500
2.000 Nonh Side Pseudo-5tattC Anatys1s
Afte, Ground lmiwovements
2.500 (Slone Columns )
3.000
3.500
L OOO
4. soo
S.000
s. soo
6 .MO+
0100
Fill
Streng1h Type Mohr-Coulomb
Urnt Weogt,, 1 JQ lblllJ
~sion Ops!
Friction Angle. 36 degrees
Wa1e1 Surface:. Water Table
loose Sand
S1teng1h Type · Mohr-Coulomb
Unit Weight 11 0 lb/113
Cohesion . 1 psf
Friction Art<}e 28 deg,ees
Water Surtac e Waltr Table
Me<fium Dense Alh.Mum
S1 reng1h Type : Moh,-Coulomb
Uni! W eight 124 lt.'113
Cohesion 1 psf
Frict ion ~e 35 degrees
Water Surface · W.Jt.er Tabl e
01'0 .....
Glaci al Till
S1reng1h Type Mohr-Coulomb
UM Weight· 134 11>'11 3
Coheo oOI\ I psf
Fncl1on Angle 36 degrees
Waler Surface Watef Tabte
Bed Rock
S1reng1h Type Mohr -Coul om b
Uno Weight · 145 lblll3
Cohe sion-1 psf
Fnct1on JJ,.rt<je· 45 degrees
Waler Surface Wal e, Table
lmp,oved Mal enal
S1reng1h Type . Moh1-Coulom b
Uno! Weight 115 lblll3
Cohesion. 1 psf
Friction Angle. 32 degrees
W aler Surfac e Water Table
o,eo e1 10
::r~, I HWAGEOSCIEN CES IN C.
I Loo se Sand I
!Den se Glacial nnj
.... 0210 0300
PSEUDO STATI C STABILITY AFTER GROUND
IMPROVEMENTS STONE COLUMNS-NORTH ABUT MENT
BLACK RIVER BRI DGE
LAKE TO SOUND T RAIL
PFIOJEC-NO
2010 -100-2 1
!! S•t'~ty F•ctor
0.000
0.500
1 .000
1 .SOO
2,000
'2 .500
3.000
3.SOO
(.000
•l.500
s.ooo
5.SOO
6.000+
~
~
~
~
~
0000 ....
Fil
St1ength Type: M-0111-Coulomb
Unn W191t 130 lblftJ
Cohesion . O psi
Fricuon Angl o· 36 degrees
Water Surface· Waler Table
Loose Sand
St1ength Type · Mohr.Coulomb
Uno Weight 110 lb/113
Cohesion 1 psf
Friction Angle 28 deg,ees
Water Surface Water Tabl e
Medium Oe nH Alluvium
Strength Type· Moh r.Coulomb
Un( Weight: 124 lblft 3
Cohesion 1 psi
Friction Angle· 35 degree s
Waler Sufface: Water Table
.... ....
Ir~ I HWA GEOSCIENCES INC.
P,oject Number: 20 10 -100-21 Task·200
P,oject Name Black River Bndge
Lake lo Soood Trail
Renlon . Was hington
Soulh Side: Pst-udo-Stat ic. Analysis
Aft er Ground lmprOYements
(Deep Soil Mixing)
Glacial Till
S1Jength Type : Mohl -Coulomb
Unrt Wei9h1 · 134 lb/113
Cohts,on· 1 psi
Friciioo Angle: 36 deg<•••
Wate1 Surface. Water Table
lmprowd Maenal
Strength Type· Mohr-Coulomb
U,,,t Weight. 120 lb/113
Cohesion· 2000 psf
Friction Angle · 32 degree s
Wttttt Sutface . Water Table
.... . , 0 120 ....
Midtum Dense Alll.Nium
.... eu o 0220
PSEUDO STATIC STAB I LITY AFTER G RO U ND
IMPR OVE MEN TS : DEEP SOI L M IXIN G. SOU TH A BUTMENT
BLAC K R IVER BRI DG E
LAKE TO SO UN D T RAIL
,
....
PROJECT NO
201 0-100 -21
•' .
••
Pro1ect Numbe, 2010-100-2 1 Task·200
Pro1ect Name Black RNer Bndge
Lake to Sound Trail
Renton W ashington
North Side Pseudo-Stahc Analys is
Aft er Gtound lmprovemenls
(Deep Soll Muong)
Fill
Srrengih T\1)0 Mohr-Coulomb
Unn we,ght 130 11>'113
Cohesion: 0 psf
Fnction A.ngle 36 degrees
Water Surlace· Water Table
Loose S.nd
Strength Type Moh<-Coufomb
Unrt We,ght t 10 lblft3
Cohesion t psi
Friction Angle 28 de9'ees
W ater Surface Water T;1bfe
Medium Dense AU\Mu m
Strenglh Type . Mohr-Coulomb
Unit Weight 124 lbffl)
Cohesroo 1 psf
Fnct1on Angle 35 degrees
Water Surface Water Table
0120 0 1'0
Glacial Till
St,ength Type Mohr-Coulomb
Unn We1gh1· 134 lblft3
Cohesion· 1 psf
f nct1onAng.e 36 degree,
Wate r Surface· Wate, Table
Bed Rock
Sl rengih Type Mohr-Coulomb
Unn Weight 145 11>'113
Cohe$10ff 1 psi
Fnclion Angle 45 degrees
Water Surface· Wal er Table
lmpor•;ed Material
Strength Type Mohr-Coulo mb
Unrt W.,ght. 120 11>'113
Cohesion 2000 psf
Fnclion Angle 32 degrees
Water Surface Water Ta bfe
0 100 e ,10
:r~, I HWA GEOSCI ENCES [NC.
0200
!Dense Glacial Till!
i.---------------~,t~l----------------..i
.,., 0 )00
PS EUDO STATIC STABILITY AFTER GRO UND
IMP ROV EM ENTS DEE P SOI L MIXING -NORTH ABUTME NT
BLAC K R IVER BRIDGE
LAKE TO SO UN D TRA IL
~om
PROJECT NO
2010-1 00-2 1