HomeMy WebLinkAboutLUA-06-020_MiscKennydale Cafe
PRELIMINARY SURFACE WATER
TECHNICAL INFORMATION REpORT
January 19,2006
I8'JlRES J2 . z,? 0 e,,!
Prepared by:
LPD Engineering, PLLC
7936 Seward Park Avenue South
Seattle, WA 98118
Contact: JeffLarnoureux
(206) 725-1211
Prepared for:
Pool Brothers Construction
POBox 3023
Renton, W A 98056
Contact: Matt Pool
(253) 405-3475
•
TABLE OF CONTENTS
SECTION I-PROJECT OVERVIEW ................................................................................................................................ .
SECTION 2 -PRELIMINARY CONDITIONS SUMMARy ............................................................................................. .
SECTION 3-OFF-SITE ANALySIS ................................................................................................................................... .
SECTION 4-FLOWCONTROLAND WATER QUALITY FACILITY ANALYSIS AND DESIGN ........................... .
SECTION 5 -CONVEYANCE SYSTEMS ANALYSIS AND DESIGN ......................................................... .
SECTION 6 -SPECIAL REPORTS AND STUDIES ....................................................................................... ..
SECTION 7 -OTHER PERMITS ....................................................................................................... .
SECTION 8 -ESC ANALYSIS AND DESIGN ................................................................................ .
SECTION 9 -BOND QUANTITIES/FACILITY SUMMARIEs/ DECLARATION OF COVENANT ..... .
SECTION 10-OPERATIONS AND MAINTENANCE MANUAL ................................................................ .
FIGURES
D Figure I (a. b, c) TIR Worksheet ............................................................................................................................ .
D Figure 2a Vicinity Map................. ....................................................................................... . .......................... .
n Figure 2b Parcel Map.................... ........ ... ... . .................................................................................................... .
U Figure 2c Existing Conditions Map ....................................................................................................................... .
D Figure 3a Drainage Basin Map...... . ...................................................................................................... .
IJ Figure 3b Developed Conditions Drainage System Map ..................................................................................... ..
n Figure 4 (a. b) Soils Map and Legend .................................................................................................................. ..
D Figure 5a OjfSite Analysis Drainage System Table................................................... .. ........................... ..
D Figure 5 (b, c) OjfSite Downstream Drainage Map ............................................................................................ ..
D Figure 6 (a, b) Stormwater Facility Summary Sheet .............................................................................................. ..
D Figure 7 (a, b, c) Conveyance System Analysis and Sizing Table .......................................................... ..
D
• Appendix A Design Drawings ...... .. .................. . • Appendix B Geotechnical Report. .. ........... .. • Appendix C Design Calculations and Supporting Information
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Page 1 of 2
King County Building and Land Development Division
TECHNICAL INFORMATION REPORT (TIR) WORKSHEET
Address -+:p.---'-:Ll;!'x"~..2$;L£.<....;:l'-r:-'4-"!:.li-"-'-'r-"'CJ"
Phone __ ~~~~~Z-~2-~~ ______ _
Project Engineer .. ~~tf:. __ Jd,~<u'.JL~:.2:'-----_
com~y~L~~~~~~~~~ __ ~
Address Phone -'S-,-=""""-:-',-=-,,,?=.:,,::-~::-'--o~o--.
PART 2 PROJECT LOCATION
AND DESCRIPTION
Project Name tr J1 Ii 1 ,/c... Ie-
Location t
Township '2--?/J
Range GG
Sadlon ~~5L-____ __
Project Size 12 ( '18 AC ,.pr---
Upstream Drainage Basin Size ---''f-\C---AC
PART 3 TYPE OF PERMIT APPLICATION PART 4 OTHER PERMITS
D Subdivision .
o Short Subdivision
D Grading
~ Commercial o Other _____________ _
D DOF/GHPA
D COE404
D DOE Dam Safety
D FEMA Floodplain
D COE Wetlands
PART 5 SITE COMMUNITY AND DRAINAGE BASIN
Community
Drainage Basin t c<. t. (, tJ,f( ~;, ;: ... ' : ! ~ /1 £ .
PART 6 SITE CHARACTERISTICS
-&1 ---
Shoreline Management
Rockery f~ f~ .... '7
Structurai Vaults
Other
HPA
DRiver ________________________ _ D Floodplain _____________________ _
D Stream ____________________ _
o Critical Stream Reach
o DepressionslSwales
D Lake -__ -;-__ -,--,---,---,-__
~ Steep Slopes d>k f/;" h· j .J/of~
o LakesidelErosion Hazard £: " ,f "'A I' f' 0 rJ
PART7 SOILS
Slopes ,'7
U-JIJ "'It' 4-r/ I ,'7
7
o Additional Sheets Attatched
D Wetlands --____________________ _
D SeepslSprings
'0 High Groundwater Table
D Groundwater Recharge
D Other
Erosion Potential Erosive Velocities
1/90
[, '1 rI/e i Page 2 of 2
King County Building and Land Development Division
TECHNICAL INFORMATION REPORT (TIR) WORKSHEET
PART 8 DEVELOPMENT LIMITATIONS
REFERENCE LIMITATION/SITE CONSTRAINT
J:Zf Ch. 4 -Downstream Analysis
D
D
D
D
D
D AdditiorIaJ Sheets Attatched
PART 9 ESC REQUIREMENTS
MINIMLfv1. ESC REQUIREMENTS
DURIN~ CONSTRUCTION
Sedimell)tation Facilijies
Stabiliz.id Construction Entrance
Per·im"ter Runoff Control
Cle,arh,d .ind Grading Restrictions
Other
D Tank
~Vault
N la
MINIMUM ESC REQUIREMENTS
FOLLOWING CONSTRUCTION
Stabilize Exposed Surface
Remove and Restore Temporary ESC Facilities
Clean and Remove All Silt and Debris
Ensure Operation of Permanent Facilijies
Rag Umils of NGPES
Other
Method of Analysis
513 v 1-1
D Energy Dissapator
D Wetland
D InfiHration
D Depression
D Flow Dispersal
D Waiver
CornpensationIMiligation
of Eliminated Site Storage
D Stream
Brief Descripti(jIn of System Operation
rl/U "a!. uI~ .. /-
C'" -1 (,:
D Regional Detention
h-,<;/, ,It '1<-$'151,..""
Facility Relate!:! Site Umilations
Reference . Facility Umijation D Additional Sheets Attatched
PART 11 STilUCTURAL ANALYSIS
(May require ,p"cial structural review)
D Cast in Place Vault D Other
r3' RetainingiWall
D Rockery>4'High
D Structural On Steep Slope
PART 14 SIGNATURE OF PROFESSIONAL ENGINEER
PART 12 EASEMENTSrrRACTS
D Drainage Easement
D Access Easement
D Native Growth Protection Easement
D Tract
D Other
I or a civil anglneer under my supervision have visited the site. Actual CJ' ./
Site conditions as observed were incorpor_ into this worksheet and the . J ....
attatchments. ·To the best of my knowledge the information provided -;...d:~~~~~~~~~~
here is accurate. ~
1 KV\
SECTION 1
This Storm Drainage Report addresses the eight core and five special requirements of the King County Surface
Water Design Manual, 1990 (KCSWDM). A Level I downstream aualysis is also included, Note that this
Storm Drainage Report is a conceptual preliminary report. The report will be finalized after site design has
been finalized and prior to site development pennit
Overview
The proposed development is the construction of a multi-use 3 story mixed use building with associated
parking, Given the topography of the existing site, a number of structural retaining walls will be included in the
proposed design, To minimize the impact to the steeper portion of the site to the west, proposed improvements
are located as far to the east of the property as is feasible, The building has been sited fronting the street as
encouraged by land use to facilitate pedestrian access and enhance the aesthetic of the street
Existing site
The existing site slopes up from a low point along Lake Washington Blvd westerly towards the 1405 right of
way. The slopes vary from 15% up to 40% and greater (Please note that a protected slope exemption has been
granted for this project). The eastern portion of the site has an average slope of 17%. The site is in an Aquifer
Protection Zone 2.
The existing site is currently undeveloped. lbe site is vegetated with some large matnre trees, primarily 8" to
12", The site appears to be second growth with an under story of blackberry and other invasive vegetation. The
site soils are brown, gravelly sand which appears to allow some infiltration; a soils investigation has not yet
been done for the project, but will be prior to pennirting.
Based on the surveyed topography and site observations, the existing site appears to drain via surface mnoff
across Lake Washington Blvd. The roadway is super-elevated fronting the site and there is no ditch along the
east side of the road.
Proposed site
The proposed development will construct approx. 12,000 sf of impervious area subject to vehicular use.
Parking lot mnoff will be collected in catch basins and routed through a water quality treatment facility.
Discharge from the water quality facility will join the tightlined drainage from the building downspouts and be
routed to the existing storm drain which is located in the unimproved Morgan Ave. (NE lOth ST) right of way
just north of the property.
(See Figure 2-Vicinity Map).
Based upon the King County Soil Survey maps the site soils are Alderwood and Kitsap soils (AKF) (See
Figure 3a & 3b -Soils Map.
Stormwater Improvements
Per the City of Renton, the project is subject to the requirements of the 1990 King County Surface Water
Design Manual with City of Renton Amendments. The project is located within a Zone 2 Aquifer Protection
Zone, Based on these requirements, the project will provide a water quality treatment facility for mnoff from
impervious areas subject to vehicular use. The project will create a negligible increase in peak rate mnoff so
detention will not be required. See Section 2 and Section 4 below.
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~ 7936 SEWARD PARK AVENUE S. ~1:S:E~ATT~L~E~W~A:SH~'N~GT:O:N'~9~81~18~~~ __ ~ ______________________________________________ -L __________ __ ~ LH' 206.725,1211 FAX, 206.725,1211
IS part of
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Scale 1 :24 000
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U. S. DEPARTMENT OF AGRICULTURE
SOil CONSERVATION SERVICE
SOIL LEGENO
The fint (op;lol leller 15 the ..,irial one of Ihe soil nomoi!!. A SltcOl"ld capital lett~,
A. 5, C, D, E, 0( F, indIcates t~ class of slope. Symbols without a slope letler
ore r!,os<!' of nearly l",v .. 1 !'.ods.
SYUBOL
AgB
AgC
AgO "F AmB
A",C
Ao
BeC
BoD
SoF
Bh
S'
Bu
Cb
loA
10C
10D
<pS
KpC
KpD
K.C
Mo
NO<:
Ng N' No
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RoC
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NAME
Alderwood gravelly sandy loam. 0 to 6 po. ... c .. nt slopes
AJder ..... ood grovelly sa",qy iOgm, 6 10 15 p!!'fce",r sJopo!s
Alderwood grovelly SQndy loom. 15 fo 30 perce'" ,Jopes
Alder .... ood and I(i.sop soils, ~ .. ry Meep
Ar .. "'~. Ald .......... ood mater;",., 0'06 percenl slope ...
Arenr~, Ald" ........ <><>d mo1erool, 6 to !::. percent "10,,,",5 *
Ar ... ,,'s. E v ..... " m(lr ..... 'oJ-
8 .. ou,,, .. gravelly sandy loom, 6 to 15 perc.nt :s.l~s
BeQ<Jsite graveUy .. GOd.,. loam, 15 to 30 percent 'Slopes
Beausi ... gravelly !:Qndy loom, 40 to 75 percent slopes
3ell'I"l<Jham sd. loam
3,,~car ~d, loam
Buckl .. ~ sil, IOQrn
Coaslal Beaches
Eadmon. sill loam
Edgew'ck f,n .. sandy l()CIm
E".,.rert gra"ell~ s<;Indy loom, 0 fa 5 p.ei'c...,.t slopes
E .... er" " 9ra" .. lly sandy l()CIm, 510 15 ~c_1 $IO~5
E .... ~r .. tI gro ...... ll y s'lody IOQm, 15 r~ 30 perce-nt sloP<ts
E"",e,.-Aldecwood g,ovelly sandy looms, 6 to 15 percent slapes
Ind,onolo loomy f,ne $Clnd, 0 to./l pe-rcent SlClf.>Oi!5
Ind'onolCl loamy fine-sand, 41015 percent S/Clp$'S
Indionola 100my f'ne sand, 15,030 percent slopes
Kinop silt loam, 2 to 8 f.>Oi!rcent slOjlO!ls
Kils"p sil. I<XIm, 8 10 15 percent slopes
K"SOP sill IOQm, 1510 30 percen' $loP<ts
Klaus gra"elly loamy sand, 610 15 piir'cer>t slClPGs
Mix .. d alluvial rand
NeilTon .... ery grayelly loomy SClnd, 2 to 15 perCent slopes
N<.wberg sd, loam
Nooksack silt 1000m
NOI"mQ sandy lcom
Orcas pea.
Or-idia sib loam
Ovoll grovelly loom, 0 to 15 percent slopes
Oval/gravelly loom, 15 to 25 percen' slopes
Ova/! gravelly loom, ./10 to 75 percenr slopes
Pile huck loamy fine sand
P·"ehuck fin.,. sandy 10000m
Puge. s.if.y day loam
Pvyo/Jup fine SQ'ldy loom
RClgnQr fine sandy loam, 6 to 15 pMcenr slapes
Rogno, fine sQndy loom, 151025 perc,",' slopes
RagnQr-IndionalQ QSSOCiCltOon, sloping.
Regnor-lndianalQ OSSOclOlion, mode-rotely STeep-
R.nton S; I. I C>om
Riyer-osh
Solol sill 1000m
SommrJmish silr lOam
SeQrtle mlJCk
Sm ShoJcOT mv.::J.
Sn Si s >It IOQm
So. Snohom'sh sil. loom
Sr SnohomIsh slit iOQm, t"iel<: surfac:e .... orlOnl
Su Sullon silt loom
Tu Tukwila muc:k
Ur Urban rond
Wo Woodinvdl .. silT 10000m
• The compos,hon of tht\fs,", ,m"~
SECTION 2
Conditions and Requirements Summary
This section addresses the requirements set forth by the King County SUlface Water Management Design
Manual (KCSWDM), 1998 Edition, Core and Special Requirements listed io Chapter I.
I. Discharge at natural location (1.2.1): All flows from this project site will remaio io the natural draioage
patterns withio a quarter mile downstream of the project. See the off site investigation included in Section
3 of this report.
2. Off-site Analysis (1.2.2): An off site investigation was preformed for this project and is included io
Section 3 of this report.
3. Runoff Control (1.2.3): The project is within the Lake Washington E draioage sub basin and is not subject
to special runoff volume controls. The proposed project site post-developed peak runoff rate for the 100
year, 24 hour duration design storm event is calculated to be less than 0.5 cfs more than the peak runoff
rate for the existing site conditions so on-site nmoff control will not be required for the proposed project.
The calculated peak runoff rate for the 100 year 24 hour duration design storm events are as follows:
Existing 100 year peak ~ 0.38 cfs
Post-Developed 100 year peak ~ 0.46 cfs
Net change in 100 year peak rate ~ 0.08 cis
The proposed project will result in surface water runoff from more than five thousand (5,000) square feet
of impervious surface subject to vehicular use. Per COR code 4-6-030 E.3.b this impervious nmoff sbalI
be treated prior to discharge with biofiltration measures. A biofiltration swale design was evaluated, but
we are requesting that the City of Renton consider an alternative method of treatroent. See Section 4 of this
report for additional information and justification.
4. Conveyance Facilities (1.2.4): The project includes a tight line conveyance system in the proposed
parkiog lot that will collect onsite drainage and route it through the stormwater treatroent facility. Per City
of Renton Code 4-6-030 E.3.g., any open channel may require a liner to prevent groundwater
contamination. A complete conveyance analysis will be included in the fmal TIR.
5. Erosion/Sedimentation Control Plan (1.2.5): A full TESC plan will be included with the permit submittal
and wilI be in accordance with the 1990 KCSWDM requirements. These plans will be considered the
miuirnum for anticipated site conditions. The Contractor will be responsible for implementing the all
TESC measures and upgrading as necessary. The TESC facilities in place prior to any clearing, grubbing
or construction.
6. Maintenance and Operation (1.2.6): The final TIR will include maintenance and operations guidelines for
all of the proposed draioage facilities, including the water quality treatroent facility and the conveyance
system.
7. Financial Guarantees and Liability (1.2.7): This Core requirement is specifically required for a project
constructed and permitted in King County and is not applicable for the City of Renton. City of Renton
requires bonding for all street and drainage improvements. The Owner will post a bond equal to 120% of
the estimated value of improvements~ prior to construction frontage improvements. An engineer's estimate
of probable cost will be included in the permit submittal TIR.
Special Requirements
I. Critical Drainage Areas -Project is not within a designated critical drainage area.
2. Compliance With An Existing Master Drainage Plan -Project is not withio an area covered by an
approved Master Draioage Plan.
3. Conditions Requiring A Master Drainage Plan -Project is not a Master Planned Development, a
Planned Unit Development, a subdivision with at will bave more thao 100 lots, a commercial
development that will construct more than 50 acres of impervious surface, or will not clear more thao
500 acres withio a draioage sub-basin so a Master Draioage Plan is not required.
4. Adopted Basin Or Community Plan -Project is not withio an area with an adopted plan.
5. Special Water Quality Controls -The project proposes discbarge to a conveyance system that
eventually outfalls to a stream that runs through Gene Coulon Beach Park and discbarges to Lake
Washington. See Section 3 Off Site Analysis. Water quality treatment for impervious area subject to
vehicular use will be required as indicated by City of Renton codified amendments to the KCSWDM
as noted above.
6. Coalescing Plat DillWater Separators -"lbe project will not construct more than 5 acres of
impervious surface.
7. Closed Depressions -Proposed project ""ill not discharge runoff to an existing closed depression.
8. Use of Lakes, Wetlands or Closed Depressions for Peak Rate Runoff Control -The project will not
use a lake, wetland or closed depression for peak rate runoff control.
9. Delineation of 100 Year Floodplain -The Proposed project site does not contain or abut a stream,
lake, wetland or closed depression.
10. Flood Protection facilities for Type 1 and 2 Streams -The proposed project does not contain or abut
a Class 1 or 2 that bas a flood protection facility.
11. Geotechnical Analysis and Report -A geotechnical analysis should not be required for the
construction of the stormwater facilities, however a geotechnical study will be performed for the site
and the Engineer will include information regarding draioage recommendations. A copy of the
geotechnical study will be included in the fmal TIR.
12. Soils Analysis And Report -The soils analysis will be included in the geotechnical report noted above
and the information will be included in the final TIR.
SECTION 3
Off-site Analysis
The following is the preliminary Level I downstream analysis. 1ms downstream analysis is based upon the
following:
• LPD Engineering, PLLC site investigation January 17, 2005 -The site was visited on a partly sunny
day which followed a period of nearly 30 consecutive days of record amounts of rainfall.
• Meeting with Arneta Heuninger, City of Renton Engineering Specialist, 10126/05 and 11/23/04.
• Review of City of Renton as-built records including Pinnacle at the Bluffs Grading and Drainage,
Grading and Drainage, as built drawings (1/30/02).
• Review of Project topographic survey by SadlerlBarnard.
Existing condition
The subject property is currently undeveloped. There is an existing abandon building foundation on the site.
The site is vegetated with what appears to be second growth with an under story of blackberry and other
invasive vegetation.
The site is bounded to the east by Interstate Highway 405 right of way, to the north by unimproved SE IlOth St
(Morgan St) right of way on the west by Lake Washington Blvd right of way and on the south by a privately
owned parcel that is currently being used for vehicle storage and an espresso stand.
The existing site slopes up from a low point along Lake Washington Blvd westerly towards the 1405 right of
way. The slopes vary from 15% up to 40% and greater (Please note that a protected slope exemption has been
granted for this project). The eastern portion of the site has an average slope of 17%. The site is in an Aquifer
Protection Zone 2.
Developed condition
The proposed discharge point for runoff from tbe site is an existing storm drainage CB located in the
unimproved Morgan St right of way inunediately north of the proposed development. The path of drainage
from there is described as follows (See Figure 4a -Off Site Analysis Drainage System Table, Figure 4b Off-
site Drainage Map):
• From the Existing type 2 drainage catcbbasin the flow is conveyed west across the Lake Washington
Blvd right of way in an approx. 70' 15" PVC pipe.
• The 15" pipe outfalls west of the Lake Washington Blvd right of way to a rip rap lined channel that
conveys the flow south along the railroad tracks. The channel is armored with 4" to 6" spalls. Channel
is approximately 2' -3' wide, 18" deep, with 3:1 side slopes. The channel is approximately 120 If.
• Flow in the Channel flows into a 24" CMP culvert which conveys the water west under the railroad
tracks, through a catcbbasin, into another 24" CMP pipe to an outfall to "John's Creek".
• John's Creek is a stream reach that flows through Coulon Beach Park to discharge into Lake
Washington.
Existing and Predicted Problems
The downstream conveyance system within 'I, mile of the proposed development property is in good condition
with no indications of drainage problems observed.
OFF·SITE ANALYSIS DRAINAGE SYSTEM TABLE
, Surface Water Design Manual, Core Requirement #2
Basin: b Subbasin Name: Subbasin Number:
c.t, C</i/i<: (
L1Table.doo 1112/92
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:l 1936 SEWARD PARK AVENUE s. g l ;s:~:n~LE~~wA~SH~'N~GI~ON:9:8~"~8 ~~ __ ~ ________________________________________ L-________ ~ i!! LH' 206.725.1211 FAX, 106.))5.1211
SECTION 4
Detention and Water Quality
Analysis and Design
Preliminary drainage drawings are included in Appendix A.
Detention
As noted in the core requirements section of this report, the project is subject to the negligible increase in peak
rate runoff exemption and detention is not required for the project. See the attached preliminary drainage
calculations.
Water Quality Treatment
As noted in the core requirements section of this report, water quality treatment is required to treat the runoff
from the impervious areas subject to vehicular use. LPD Engineering wrote a letter to the City of Renton
(10/27/06) requesting a drainage requirement adjustment to aliow an alternative method of treatment. A copy
of the letter is attached and a summary of the key issues is included below.
In coordination with City planners the Owner and Architect have arrived at a preliminary design that sites the
building near Lake Washington Blvd. The building location was chosen to minimize the impact to the steep
slopes on the eastern portion of the site and to facilitate pedestrian access and enhance the aesthetic of the
street. The Architect is proposing a landscaped plaza area with outdoor seating multiple access points to the
sidewalk along Lake Washington Blvd.
The most feasible location for a biofiltration swale is in the space proposed for the plaza area. Siting the swale
here would create restrictions and possibly safety issues for pedestrians in area that intends to encourage
pedestrian activity. A prelirninary biofiltration swale design was performed to verify that if required, a swale
could be constructed in front of the building.
We request an adjustment of the drainage be granted to allow an underground water quality treatment facility in
lieu of a biofiltration swale on this site. Options include a wet vault or the Stormwater Managemen~ Inc.'s
Stomtfilter treatment system
Our preferred method is the Stomtfilter treatment system based on its performance and long term maintenance
advantages. Washington State Department of Ecology has approved use of the proposed Stomtfilter Treatment
System as a basic stormwater treatment practice for total suspended solids (TSS) removal and King County has
approved the System for basic water quality treatment.
The proposed Stomtfilter will be maintained by the Owner under a long term maintenance agreement with the
manufacturer. A water quality vault would also be maintained by the Owner as required by the City.
SECTION 8
TESC Analysis and Design
Project plans include a Preliminary Temporary Erosion and Sedimentation Control (TESC) design (See
Preliminary Design Documents Appendix A). Included in that design is the TESC measures to be utilized
include the following:
• Construction Access Pads
• Perimeter Siltation Control Measures
• Temporary interceptor Swales
• Temporary Sediment Pond -Sediment Pond sizing calculations are included in Appendix C.
The implementation of the TESC plan and construction maintenance, replacement and upgrading of the TESC
facilities sball be the responsibility of the contractor per the contract documents. The TESC facilities will be
construction prior to and in conjunction with all clearing and grading activity and is a manner which sediment
or sediment laden water does not leave the project site, enter the drainage system or violate applicable water
standards. The TESC measures shown on the plan are considered the mininrum requirements for anticipated
conditions. During construction the contractor sball be responsible for upgrading these facilities as necessary.
APPENDIXA
Preliminary Design Documents
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Surveyor
S\DlEFHWi'NMD &: ASSOC. N:.
12714 VALLEY OC E. SUITE B
SIJI,INElt "" g8l9O
(253) 82&--8135
COHT,I.CT: WICE LUNA
Site Benchmark
R{R SPIKE SET IN POWER POLf
AT SOUTHWEST CORNER Of SITE
Ei._SI.60
Legal Description
Vertical Datum
mY Of REIfTON BENCHIIAA1( '2177
J.5" BRISS IXSK AT "TH£ NW COiHR
OF CON:. ~E OF SlGNN.. BRIlGE
AT 1HE R/R C!IOSSIm A1 lItE
NORTH OOIW«:E OF CClU.0tI PARk
EL= J7.~ fEET ~ 88
Basis of Bearing
RECORD {f SU1i\{Y IS RECORDED
UIf[£R RECORDIHG NUIIBER
9901159OOJ. R[COR(lS or THE
kING COlI~ AIJOO"CfI (ROS)
NORTH 75 rn OF LOTS 312 THROLCH 315 OF THE PlAT Of r:tl HII..U.1AH's
LJ.KE WASHINGTON GAAOCN or EDEN, tMSION NO.5, RECQWED IN VOl.IJI.IE
11, ~ 8J RECORDS OF KING COUNl'(, WASHINGTON. TOGETHfR WITH l}£
SOUTHERIJ 30 FITT OF MORGAN AVE. (TO BE Wu,lED)
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Construction Sequence
T. BEfORE ~ CONS1RUCllON M DEVELOPNEIfI AC'rMJY, -. PRECONSffiUCTlOH MEETlNG t.lUST BE HaD BElWEEN
1HE CITY Of RENTON, THE AI'f'I.I:mT AND 1HE N'Pl.Jc.wIS CO"'5'1RlIC"J"O; REPRESENTATh'[.
2. \ofRIfY \£RTIC.I,L Nl) tlORllOlIUL LOCAlJONS OF .IJ.L EXISTING UNDERGROUND ununES. CONTACT AU lfTlJTY
CI)I,IPJ,NIES THAT w.Y BE EffEClED EI'I' THE PROPOSED OONSTRUCTKlN. THE 0Nf: CALL NUIoIBER IS
1-1300-424-5555.
3. IIlAINTAIN AI...!. EXlSTNJ tml/lY SERIIICES DURING COHSTRucnoo.
VERIFY CRADES PR(JR TO~. f'"l--'G CI.£AR1NG Lt.IllS,
5. INSTALl. STAIIIL1Zfl) CONS1RUC1!ON ENTRANCE.
6, mTAlJ. nrrm FNlRIC FEHC:E: AS tlllIO,ITD ON PlAN
7. INSTAll. 0FfS/J[ ~TCH BASIl PRoTEci1ON
8. CLEAR a: GRUB AREAS OF 111: SIT[ 1ll BE ROJGH GfWlEO Of flUID.
9. CO!€lRIJ:T SEDIMO/T IImRW"lOR SWN.£S AND CHECIC D.+.IIS.
10. IIDIO\'[ Ut/SUrT.I&.E B£ARIHG WiJERW. AS REQIJIRfll
11. GRADE Ah'!l PlACE AlXU'TAIlf FIJ. '5 REc,uRED ANO COMPACT ACCESS DRIVE SUB-GfWlE AS IIOCATED ctj
1HE D~. IHSTAU. S1t:m1 COtM'!'AtICE SYSTOI. DIRECT ill SURfACE WATER TO THE PROf'OS(D CATCH
BASIN. t.() I./NCCJIlln.LID SURfACE ~TER S~ BE IUOWED TO l£A\IE THE SITE AT mt DIE DUR!HG TI£
GRAtMNG OPERKIIONS. USE Cl.TCH BASIN SEDlWENT fllITRS TO CAPTURE SEDIWEN'T PRIOR TO ascHAAG[
12. INSTAll. N£W lJIlJIlES PER THE WIrIIGS .
A. WET TN'S TO THE cr.y OF RENTON WATER S'I'STEN StIAU. BE w.oE BY A CITY APf'RO'I{D S~.
a THE em OF ROlT(ltj SKAu IISTAU. Tt£ OOMES11C WATER WfJERS.
13. fljlS/1 GRID[ SITE AND CONS1JK.ICT ASPIW.T PAYING AREAS. ACtESS ORMS SlDEWJiKS, CURBS AND c;JJTlERS.
14. COII'UTE STABIlIZATION .. ACaJRlWI! IiTTH lANOSCIPE PLANS .
15. REIOJE EXCiSS EXCAVATED 1MlD!W.S, TRo\SH (lEBR5, AND WASTE: UATEllWS .+.ND DISPOSE Of IN HI
AUTHORIZED LOC.I.TION A1 t.W) COST TO M OWNER.
16. CLfAH SlORt.I OIIAINItGE SYSlDI or AI..L SEDIWlI HID DEa'iIS.
17. RD/O'v'[ TDIF'ORAI!Y E~ CONJROL fACIUTIES WHEN sm: IS COiolPlETEl.Y ST,lBUZED.
Erosion Control Notes
I. BEFORE »1'1 CXWiTRUCTION (JII:EVELOf'I,IOO A::TMTY OCC~, A PRf-CONSTRVCOCW IIEETlHG IoIUST !£
tHO WITH THE CfIY !)<" ~ DEPAIm.!DiT 0'" PU~C '/KIRIG. D£SIG~ E~GINE£~.
All. UI,(f!S or CLEARING .'.NO A~Eo\S OF VEGETATION PRESDNATIOU IS PRESCRIBED 011 THE PlAN SHALL BE
Cl.£\RLY FlAGGED IN THf FlELC AND OBSEfN[D DURING CDNSTRUC'TK>N.
3. ALL R[QUIREO SEDiIiENTATION"~ROSI~ CONTROL F,lCIl.IT]ES MUST BE CONSTRUCTED .'.NO IN Of'ERATlON PRIOR
TO I)NIJ ClfARlNG ~DjOR OTHER COOSTRUCTION TO INSURE TI\I.T sm~ENT w)EN WATER DOES NOT ENiER
THE AATURN. IJRAlNAGE SYSTEIi. AU EROSKlN AND SEDII.tENT FACIUTlES SWil BE ),!AlmA/NED IN A
SATISfACTORY COtlDl1lON UNTil SUCH TIlliE THAT CLEARING mojOR CONSTRUCTION IS cOl.tPlITED mD
POTEIiTW. FOR OH-SITE ffiGS/ON fIAS PASSED. THE Ir.rPLfljENWW, w.rNTHW,lCE, REPlACEUENT AND
AOOITIDNS TO £ROSj()NjSEDlIoiENTATI<W CONTROL SYSTEi6 SHAll. B[ "THE RESPCNSIBlliTY or THE PERIITl!E.
04. "THE EROSION oW) SEDIllOOATIlN CONTRa. 5YSTEI.IS D£Pl'TEO ON THIS DRAWING AAf. IKTEHOCD 10 BE
IINlMUIi REQIJIREWOOS 10 IftIT Ho'OCIPATED SITE ~ IS CONSJROC"TKlN PROGRESSES oW)
U~ OR SE.IS01W. CXlItlIIIOHS OO"ATE, "THE PfR!.IffIII SIIAL.L HffiCIPATE THAJ t.l)RE EROSDH oW)
SEDlilfNTAlK:'t1 CCM1!Cl f.-lClJT(S WILL HE NECESSARY TO INSUIE 00II1'l.ETE SIL1A"OON CQIlJR(t ON 11£
PROPOSED SITE. MN> THE COURSE Of ~, IT S/WJ. HE TI£ 0Bl.lGIJ00 AI() ~
Of THE PERM11TII m ,I£l()f!fSS Mrr NEW ~ ffil.T w.y BE CREATED BY HIS ACTMTIS NIO 10
PROIIDE ADOITIOtW. fACll.lJ1(5, OIlER HID ABO'I'E II,"IIUI R[QUIREIoIOOS, AS w.y IJ[ h'E£OED TO PROTECT
A£l...W:8oIf PROPERTIES JHI WNER OUIUJY or THE REC£MNG OR.I.I'i'oGE SYSTEII.
5. APPRWAI. or lHS f'lNI IS ~ EROSKlN/SEIlIIOOA~ CONTROL ~Y. IT DOES NOT CONSTITlJIE NI
Ii'PRWAL OF S"r0Rl0l DRAtW?E [(SIGN, SIZE hOR I.DCATIOtoI or PIPES, RESTRlCTORS, CKlHNELS, OR
R~f~.
6. DlRING THE TIllE P£ROO OF III1vnIBER I THRQ\X;H WrRCH 31. AU PROJECT DmlJRBED SOIL AREAS
GREATER "fI-Wj 5,000 SIlUARE FEEf, THIIT ARE TO BE LffT l.IIffIOOI(£D fOR IIORE nWI "!WEl.\IE (12) I{lURS,
SIWl. B£ CO'.{RED BY !.IULeii, S()()()I,I,t, DR PlASOC CCJl.'E1i'1NG.
7. IN JoH( KO WHICH HAS 8EEH SfRiPf'EQ Of Y£GflATICIN HlD Wf/ERE NO FURTHER M;)RK IS ANOOPATED FOR
A PER100 Of 30 !».YS OR WORE. All IlISIURBED ARfAS IoIUST BE IIIMID!ATELY STABJJ.JmI wrrn I.tIl.CHING,
GRASS PI.JHfN> OR OTHER o\."PROYED EROSK»I CONTRa.. TREi\n.ENT APPl.ICABlE TO "THE TIllE Of \'IN! N
QI.JESTIOH. GRASS SUOII«; AU»£ WIU.. BE ACCEPrf&E ONLY DlRING THE t.IONTHS Of N'RIl lHRO..IGH
SEPIDIBER 1NQUSiV£. SEEDIIIG /MY PROCEED, HCtfEVER, Wl£N&R IT IS N THE INTERESI Of THE
PERN1TTrE, BUT IoItIST BE AI.IGI.ENTID \WTH "UlCItNG. NElTING, OR OTHER lREATWENT N'PRO.£D B'!' THE
CITY or RfNTOH. OUTSIDE THJ:: SPECIF[!) TillE PERIOD.
8. fOR AU EROSOI,/SEOO£NTA1D1 tcmRO!. PONDS WHERE THE DEIJl STI:)f!N;E DEPTH EXCEEDS 6 INCHES, A
FOCE, II WINMUII Of 3 FIEf IIIlH IS REQIIftD, WIIH :3:1 SlOE Sl.CPE.S
A"''''.'''' BE
Uo:I\Il£'
CONSJ"WCTION EHlRANCE, 2-4' X 50' X 8" Dr +-10 6-INCH 0IJN!R't SPN..l.S SIW..L
Of IIEH(:UI..AR lNt1iESS HID EGRESS TO THE CONSTRUCTION 511£.
VG\l!l1": -..........,."'"-'"~.~--
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APPENDIXB
Design Calculations and Supporting
Information
~Q!mwate~6~ Size and Cost Estimate
Kennydale Cafe -Stormwater Treatment System
Renton, WA
Information provided:
• Total contributing area = 0.61 acre
• Impervious area = 0.43 acre
• Water quality flow, Qwq (60% of 2-yr) = 0.126 cfs
• Peak hydraulic flow rate, Qpeak = 0.46 cfs
• Presiding agency = City of Renton,WA
Assumptions:
• Media = ZPG cartridges
• Per cartridge flow rate = 15 gpm
• Drop required from RIM to outlet = 2.3' minimum
Size and cost estimates:
The Storm Filter is a flow-based system, and therefore, is sized by calculating the peak water quality flow rate
associated with the design storm. The water quality flow rate was calculated by using KCRTS and provided to
Stormwater360.
The StormFilter for this site was sized based on treatment flow rate of 0.126 cfs. To accommodate this
treatment flow rate. Stormwater360 recommends using a steel four-cartridge CatchBasin StormFilter (see
attached detail). The estimated cost of this size system is $13,900, complete and delivered to the jobsite. The
contractor is responsible for setting the CatchBasin Storm Filter and all external plumbing. The steel
CatchBasin StormFilter has an internal bypass capacity of 1.0 cfs, which does not exceed the peak flows from
this site.
The leaders in the storm water industry, Stormwater Managemen~ Inc. and Vortechnics. Inc .. have unN.ed as Stormwater360 n• -the comprehensive provider of stormwater solutions. With
an unparalfe/ed product Ifne and unma/c;hed customer support team under one umbrella, Stormwater360 has the treatment option to meet your water quality goals.
@Z005 Stormwater360
11/17/2005 lIellgdon
www.stormwater360.com
12021-6 NE Airport Way, Portland OR 97220
Toll-free: 800.548.4667 Fax: 800.561.1271
OUTLET STUB
(SEE NOTES 405)
10" ~~~~~~_WE~I~R~WTA~LL~~~~~~~--~-L--~~ ____ ~~~ OVE~F
G"
INLET STUB
(OPTIONAL)
(SEE NOTE5 405)
4-CARTRIDGE CATCHBASIN -PLAN VIEW
INLET GRATE
OUTLET STUB
REINFORCING BARS
(SEE NOTE G)
ED
~ Ei~~~~~(5.E.E.N.O.TE~5~4~'~5~)~~~~~~~~~ ...... ~~~~~ 2 1/2"
<02005 Stonnwater360
CLEANOUT
ACCE55 PLUG
ON WEIR WALL
3'-8" 2'-8' 3'-8"
1-----IN5IDE -----I-~INSIDE ---I-----IN5IDE ~~--I
10'-1 "
OUTSIDE
4-CARTRIDGE CATCHBASIN -SECTION VIEW
CONCRETE COLLAR
(SEE NOTE G)
5 TORM FI LTER
CARTRI DGE (TYP)
(5EE NOTE 2)
UNDERDRAIN
MANIFOLD
THE 5TORMWATER. MANAGEMENT
5tormFII,er®
U.s. PATENT No. 5,322,629,
No. 5,707,527, No. 10,027,1039
1>.10. b,G49,048, No. 5,1;24,5710,
AND OTHER U.5. AND FOREIGN
PATEN75 fENDING
§ STEEL CATCHBASIN STORMFILTER DRAWING
~!.mwater36a ~-=".,..,..,------,_P_LA_N_A.,.-N_D_S_E_CT_IO_N_V_I_EW_S----,. __ ..----,--,,1~, roc STANDARD DETAIL - 4 CARTRIDGE UNIT
www.atonnlljafllr38G,com DATE: 11101105 SCALE: NONE FILE NAME: CBSF4-S-DTl DRAWN: MJW CHECKED: ARG
C200S Stormwat<r360
PER.MANE~' POOL
ELEVATION
VARIES
2'-3 5/B" MAX.
~[-
INLET STUB 7
(OPTIONAL)
(5EE NOTE5 4;' 5)
2'
IN51DE
2'-0 1/2"
f--OUTSIDE-I
OUTLET 5TUB
(5EE NOTE5 4;' 5)
2"0 OUTLET PIPE
FROM UNDERDRAIN
4-CARTRIDGE CATCHBASIN -SECTION VIEW
3'-9'
1'-';" CAR,RIDGE
5UPcORT (TYP)
L--__ '-__ ...J ...1
LlPTING EYE
(TYP OF 4)
ELEVATION
4-CARTRIDGE CATCHBASIN -SECTION VIEW
THE 5TORMWATER MANAGEMENT
StormF'lter®
U.S. PATENT No. 5,322,G29,
No. 5,707,527, No, G,027,G39
No. G,G49,048, No. 5,G24,57G,
AND OTHER U.s. AND FOREIGN
PATENTS FENDING
~.!.mwate~§) STEEL CATCHBASIN STORMFIL TER
SECTION VIEWS
STANDARD DETAIL - 4 CARTRIDGE UNIT
DRAWING
2
www.Atoi •• lW.ter3lO.com ~~~~~~~~ __ -,~~~~~~ ______ -,~~~~~~~m~
DATE: 111{11105 SCALE: NONE FILE NAME: CBSF4-S-DTL DRAWN: MJW CHECKED: ARG
GENERAL NOTES
I) STORM FILTER BY STORMWATER3GO; WEST, PORTLAND, OREGON (800) 548-4GG7; EAST, 5CARBOROUGH, ME (877)
907-8G7G; MID-ATLANTIC ELKRIDGE, MD (8GG) 740-3318.
2) FILTERS TO BE 51 PHON-ACTUATED AND 5ELF-CLEANING.
3) 5TEEL 5TRUCTURE TO BE MANUFACTURED OF ! /4 INCH STEEL PLATE.
4) 5TORMFILTER REQUIRES 2.3 FEET OF DROP FROM RIM TO OUTLET. INLET 5HOULD NOT BE LOWER THAN OUTLET. INLET (IF
APPLICABLE) AND OUTLET PIPING TO BE SPECIFIED BY ENGINEER AND PROVIDED BY CONTRACTOR.
5) CBSF EQUIPPED WITH 4 INCH (APPROXIMATE) LONG STUBS FOR INLET (IF APPLICABLE) AND OUTLET PIPING. STANDARD OUTLET
STUB 15 8 INCHES IN DIAMETER. MAXIMUM OUTLET STUB IS 15 INCHE5 IN DIAMETER. CONNECTION TO COLLECTION PIPING CAN
BE MADE USING FLEXIBLE COUPLING BY CONTRACTOR.
G) FOR H-20 LOAD RATING, CONCRETE COLLAR IS REQUIRED. CONCRETE COLLAR WITH QUANTITY (2) #4 REINFORCING BARS TO BE
PROVIDED BY CONTRACTOR.
7) ALL 5TORMFILTERS REQUIRE REGULAR MAINTENANCE. REFER TO OPERATION AND MAINTENANCE GUIDElINES FOR MORE
INFORMATION.
4-CARTRI DGE CATCHBASI N
STORMFILTER DATA
STRUCTURE I D XXX
WATER QUALITY FLOW RATE (ds) XXX
PEAK FLOW RATE « I ds) XXX
RETURN PERIOD OF PEAK FLOW ( cs) XXX
CARTRIDGE FLOW RATE ( I 5 OR 7.5 qpm) XX
MEDIA TYPE (CSF, PERLITE, ZPG) XXXXX
RIM ELEVATION XXX.XX'
PIPE DATA, I.E. DIAMETER
INLET STUB XXX.XX' XX"
OUTLET STUB XXX.XX' XX"
CONFIGURATION
OUTLET
1001:1001
INLET
SLOPED LID YE5INO
SOLID COVER YES\NO
NOTES/SPECIAL REQUIREMENTS,
ACCESS COVE~ --...
(TYP) '\ ~ INLET GRATE
02005 Stonnwab:r360
""""f.~-''-'.''''''''''\'--'' .•••• :7";...-. ; .. -'-•. ' .~, ___ --./-... -.-::,-,-;.,-.... -"-'."--'-•• ·A~· -T'---;;-. ~-.--'-"---~.-~:'-'. '.-"--'" "0' .'--"';" ".' .. '\ . ~ .. ~'mX'" <~' ..• "';;:"""',:.,+-. I:::.~: I II~"~, INsf] I:~IM
II~ .' .. '
I ~· .".' : .... ;.-........ : .. < ... : ..... ,. ,..". ,. . ,'. , : .... '.'; -' :.. .' .:. '. . '~':. • .... ..., .. '.~,;" /'';; '~;" .... < •.. ~ .. '.-
4'
INSIDE RJM
2'-4"
INSIDE RIM
10'-5"
OUTSIDE RIM
4'
INSIDE RIM
4-CARTRIDGE CATCHBASIN -TOP VIEW THE 5TORMWATER MANAGEMENT
StormFllter®
U.s. PA.TENT No. 5,322,G2~,
No. 5.707,527. No. b.027,G3~
No. ':;,1049,045, No. 5,1024,5710,
AND OTHER U.s. AND FOREIGN
PATENTS PENDING
§) STEEL CATCHBASIN STORMFIL TER DRAWING
gpLmwater360 TOP VIEW, NOTES AND DATA ,3"
STANDARD DETAIL - 4 CARTRIDGE UNIT
~D~A=TE~,,~,ro~,-ro~5'1~:s~CA~L~E'~N=ON~E------~IF=IL~E~~-M-E-'C-B=SF~"'=-=DR~--------O=IIDAA--W-N-'M-Jw--I~c-H=EC=K~ED~'A~R~G~ www.storlnWlltw38O.com
, --._-'----------------------- ------------
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11/16/05 4 :41 :45 pm
Preliminary Storm Drainage
LPD Engineering, PLLC
Coughlin, Porter, Lundeen Inc.
Kennydale Cafe
Calcs
page 1
=====================================================================
BASIN ID: 100yrdev
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TyPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
ABSTRACTION COEFF:
TcReach -Sheet L:
TcReach -Channel L:
PEAK RATE: 0.46 cfs
BASIN ID: 100yrex
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TyPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
ABSTRACTION COEFF:
TcReach -Sheet L:
TcReach -Shallow L:
PEAK RATE: 0.38 cfs
BASIN ID: 10yrdev
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TyPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
ABSTRACTION COEFF:
TcReach -Sheet L:
TcReach -Channel L:
PEAK RATE: 0.33 cfs
BASIN SUMMARY
k./
NAME: Kennydale cafe -eJ(il!i~ilig
0.61 Acres
TYPE1A
3.90 inches
10.00 min
BASEFLOWS:
AREA .. :
CN .... :
TC .... :
0.00 cfs
PERV
0.18 Acres
89.00
5.37 min
0.20
100.00
350.00
VOL:
ns:0.2400 p2yr: 2.00
kC:42.00 s:0.1300
0.17 Ac-ft TIME:
s:0.5000
480 min
NAME: Kennydale cafe -existing
0.61 Acres BASEFLOWS: 0.00 cfs
TYPE1A PERV
3.90 inches AREA .. : 0.61 Acres
10.00
0.20
100.00
215.00
VOL:
min CN .... : 89.00
TC .... : 5.96 min
ns:0.2400 p2yr: 2.00
kS:8.00 s:0.2100
0.14 Ac-ft TIME:
s:0.5000
480 min
de...--
NAME: Kennydale cafe -exi:!!~i1I9
0.61 Acres BASEFLOWS: 0.00 cfs
TYPE1A PERV
2.90 inches AREA .. : 0.18 Acres
10.00
0.20
100.00
350.00
VOL:
min CN .... : 89.00
TC .... : 5.37 min
ns:0.2400 p2yr: 2.00
kc:42.00 s:0.1300
0.12 Ac-ft TIME:
s:0.5000
480 min
IMP
0.43 Acres
98.00
5.36 min
IMP
0.00 Acres
0.00
0.00 min
IMP
0.43 Acres
98.00
5.36 min
11/16/05 4 :41 :45 pm
Preliminary Storm Drainage
LPD Engineering, PLLC
Coughlin,
Kennydale
Calcs
Porter,
Cafe
Lundeen Inc. page 2
=====================================================================
BASIN ID: 10yrex
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TyPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
BASIN SUMMARY
NAME: Kennydale cafe -existing
0.61 Acres BASEFLOWS: 0.00 cfs
TYPEIA PERV
2.90 inches AREA .. : 0.61 Acres
10.00 min CN .... : 89.00
TC .... : 5.96 min
ABSTRACTION COEFF: 0.20
TcReach -Sheet L: 100.00
TcReach -Shallow L: 215.00
PEAK RATE: 0.25 cfs VOL:
s:0.5000 ns:0.2400 p2yr: 2.00
ks:8.00 s:0.2100
0.09 Ac-ft TIME: 480 min
de./'
eKistipg BASIN ID: 25yrdev
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TYPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
ABSTRACTION COEFF:
TcReach -Sheet
TcReach -Channel
PEAK RATE: 0.40
BAS IN ID: 25yrex
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TYPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
ABSTRACTION COEFF:
NAME: Kennydale cafe -
0.61 Acres
TYPEIA
3.40 inches
10.00 min
BASEFLOWS:
AREA .. :
CN .... :
TC .... :
0.00 cfs
PERV
0.18 Acres
89.00
5.37 min
0.20
L: 100.00
L: 350.00
cfs VOL:
ns:0.2400 p2yr: 2.00
kc:42.00 s:0.1300
0.15 Ac-ft TIME:
s:0.5000
480 min
NAME: Kennydale cafe -existing
0.61 Acres BASEFLOWS: 0.00 cfs
TYPE1A PERV
3.40 inches AREA .. : 0.61 Acres
10.00 min CN .... : 89.00
TC .... : 5.96 min
TcReach -Sheet L:
0.20
100.00
215.00
ns:0.2400 p2yr: 2.00
ks:8.00 s:0.2100
0.12 Ac-ft TIME:
s:0.5000
TcReach -Shallow L:
PEAK RATE: 0.32 cfs VOL: 480 min
IMP
0.00 Acres
0.00
0.00 min
IMP
0.43 Acres
98.00
5.36 min
IMP
0.00 Acres
0.00
0.00 min
11/16/05 4:41:45 pm
Preliminary Storm Drainage
LPD Engineering, PLLC
Coughlin,
Kennydale
Calcs
Porter, Lundeen Inc.
Cafe
page 3
=====================================================================
BASIN ID: 2yrdev
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TyPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
ABSTRACTION COEFF:
TcReach -Sheet L:
TcReach -Channel L:
PEAK RATE: 0.21 cfs
BASIN ID: 2yrex
SBUH METHODOLOGY
TOTAL AREA ....... :
RAINFALL TYPE .... :
PRECIPITATION .... :
TIME INTERVAL .... :
ABSTRACTION COEFF:
TcReach -Sheet L:
TcReach -Shallow L:
PEAK RATE: 0.14 cfs
BASIN SUMMARY
NAME: Kennydale cafe -
0.61 Acres
TYPE1A
2.00 inches
10.00 mln
BASEFLOWS:
AREA .. :
CN .... :
TC .... :
d-e ./
e7:iSLiIIg
0.00 cfs
PERV
0.18 Acres
89.00
5.37 min
0.20
100.00
350.00
VOL:
ns:0.2400 p2yr: 2.00
kC:42.00 s:0.1300
0.08 Ac-ft TIME:
s:0.5000
480 min
NAME: Kennydale cafe -existing
0.61 Acres BASEFLOWS: 0.00 cfs
TYPE1A PERV
2.00 inches AREA .. : 0.61 Acres
10.00 min CN .... : 89.00
TC .... : 5.96 min
0.20
100.00
215.00
ns:O.2400 p2yr: 2.00
ks:8.00 s:0.2100
0.05 Ac-ft TIME:
s:0.5000
VOL: 480 min
117 i-.)
IMP
0.43 Acres
98.00
5.36 min
IMP
0.00 Acres
0.00
0.00 min
Page I of I
Proposed Areas
Date: 11-15-2005 Time:11:13:13a
. ··QIUrlj~
Layer Description
impervious vehicle-use Asphalt Pavement
. . lIllpervlous Building
Basin Area: 26562 Sf (.61 Ac)
Pervious Area: 7883 Sf (.18 Ac) [29.68%]
Impervious Area: 18679 Sf (.43 Ac) [70.32%]
Layer Description
Layer Block Quantity
Imp DeJ?th Area Sf(Ac) Volume Volume
(sq.m.) (cu. ft.) (cu.yd.)
Yes 6 11938(.3) 5969.1 221.1
Yes I 6740(.2) 561.7 20.8
Length (ft.)
Description
Drawing performed on:Z:\LPD Engineering PLLCIProjects\Pool Brothers ConstructionlKennydale
Cafe Lake Washington CommerciallDesign IAreas\Lake _ Base.dwg By:Leland
Note: All information calculated from objects in drawing. Drawing must be draw accurately for
information to be reliable.
file:IIZ:\LPD Engineering PLLClProjectslPool Brothers ConstructionlKennydale Cafe La... 1111512005
.e
:0
;0
Permeability is moderatelY rapid in the surface
layer ,and subsoil ·and very slow in the substratum.
Roots penetrate easily to the consolidated substra-
tum. where they tend to mat on the surface. Some
roots enter the substratum through cracks. Water
moves on top of the substratum in winter. Available
water capacity is low. Runoff is slow to medium~
and the hazard of erosion is moderate.
This soil is used for timber, pasture, berries,
and row crops, and for urban development. Capability
unit IVe-2; woodland group 3d!.
Alderwood gravelly sandy loam, 0 to 6 percent
slopes (AgB).--This soil is nearly level and
undulating. It is similar to Alderwood gravelly
sandy loam, 6 to 15 percent Slopes, but in places
its surface layer is 2 to 3 inches thicker. Areas
are irregular in shape and range from 10 acres to
slightly more than 600 acres in size.
Some areas are as much as IS percent included
Norma, Bellingham, Tukwila, and Shalcar soils, all
of which are poorly drained; and some areas in the
Vicinity of Enumclaw are as much as 10 percent
Buckley soils.
Runoff is slow, and the erosion hazard is
slight.
This Alderwood soil is used for timber. pasture,
berries, and row crops, and for urban development.
Capability unit IVe-2; woodland group 3d2.
Alderwood avelly sandy loam, 15 to 30 ercent
slopes (AgD) .--Depth to the su stratum in this 5011
varies within short distances, but is commonly
about 40 inches. Areas are elongated and range
from 7 to about 250 acres in size.
Soils included with this soil in mapping make
up no more than 30 percent of the total acreage.
Some areas are up to 25 percent Everett soils that
have slopes of 15 to 30 percent, and some areas are
up to 2 percent Bellingham, Norma, and Seattle soils,
which are in depressions. Some areas, especially
on Squak Mountain, in Newcastle Hills, and north of
Tiger Mountain, are 25 percent Beausite and OVall
soils. Beausite soils are underlain by sandstone,
and Ovall soils by andesite. "
Runoff is medium, and the erosion hazard is
severe. The slippage potential is moderate.
This Alderwood soil is used mostly for timber.
Some areas on the lower parts of slopes are used
for pasture. Capability unit VIe-2; woodland group
7 -----
Alderwood and Kitsa~ soils~ very steep (AkF).--
This mapping unit is a out 50 percent Alderwood
gravelly sandy loam and 25 percent Kitsap silt
loam. Slopes are 25 to 70 percent. Distribution
of the soils varies greatly within short distances.
About 15 percent of some mapped areas is an
included, unnamed, very deep, moderately coarse
textured soil; and about 10 percent of some areas
is a very deep, coarse-textured Indianola soil.
Drai1l8.ge' and pomeability vary. Runoff is rap
to-YerJ"""rapid; and the erosion hazard is severe a
very severe. The slippage potential
These soils are used for timber.
unit VIle-I; woodland group 2dl.
10
Arents~ Alderwood Material
Arents, Alderwood material cons ists of Ale
soils that have been so disturbed through uri
ization that they no longer can be classifiet
the Alderwood series. These soils, however,
many similar features. The upper part of thl
to a depth of 20 to 40 inches, is brown to d
brown gravelly sandy loam. Below this is a
brown, consolidated and impervious substratw
Slopes generally range from 0 to 15 percent.
These soils are used for urban developrnen
Arents, Alderwood material, 0 to 6 perc en
(AmB). -In many areas this soil is level~ as
result of shaping during construction for ur
facilities. Areas are rectangular in shape
range from 5 acres to about 400 acres in siz
Representative profile of Arents, Alderwo
material, a to 6 percent slopes, in an urban
1,300 feet west and 350 feet south of the no
corner of sec. 23, T. 25 N.) R. 5 E.:
o to 26 inches, dark-brown (lOYR 4/3) gravel
sandy loam, pale brown (lOYR 6/3) dry;
massive; slightly hard, very friable,
sticky, nonplastic; many roots; mediun
abrupt, smooth boundary. 23 to 29 inc
thi ck.
26 to 60 inches, grayish-brown (2.5Y 5/2) lH
conSOlidated to strongly consolidated
till, light brownish gray (2.5Y 6/2) ,
common, medium, prominent mottles of ~
bro\m (lOYR 5/6) moist; massive; no r(
medium acid. Many feet thick.
The upper, very friable part of the soil
to a depth of 20 to 40 inches and ranges frc
grayish brown to dark yellowish brown.
Some areas are up to 30 percent included
that are similar to this soil material, but
shallower,or deeper over the compact substr
and some areas are 5 to 10 percent very gra
Everett soils and sandy Indianola soils.
This Arents, Alderwood soil is moderatel
drained. Permeability in the upper, distur
material is moderately rapid to moderately
depending on its compaction during construe
The substratum is very slowly permeable. R
penetrate to and tend to mat on the surface
consolidated substratum. Some roots enter
substratum through cracks. Water moves on
~he substratum i~ winter. Available water
15 low. Runoff IS slow, and the erosion ha
Slight.
This soil is used for urban development.
pability unit IVe-2; woodland group 3d2.
Arents, Alderwood material, 6 to IS perc
slopes (AmC).--This soil has convex slopes.
are rectangUlar in shape and range from 10
about 450 acres in size.
October 27, 2005
City of Renton
PlanninglBuilding/Public Works
1055 S Grady Way
Renton, W A 98055
Attention: Arneta Henninger
Re: Kennydale CaJtf
1322 Lake Washington Blvd
Dear Arneta:
LPD Engineering, PLLC
This letter is to follow-up our conversation yesterday regarding the stonn water quality treatment for the proposed
commercial development at 1322 Lake Washington Blvd in Renton. Attached is a preliminary site layout sketch.
Existing site
The existing site slopes up from a low point along Lake Washington Blvd westerly towards the 1405 right of way. The
slopes vary from 15% up to 40% and greater (Please note that a protected slope exemption has been granted for this
project). The eastern portion of the site has an average slope of 17%. The site is in an Aquifer Protection Zone 2.
Proposed development
The proposed development will be a 3 story mixed use building with associated parking. Given the topography of the
existing site, a number of structural retaining walls will be included in the proposed design. To minimize the impact to
the steeper portion of the site to the west, proposed improvements are located to the east as much as possible. The
building has been sited fronting the street as encouraged by land use to facilitate pedestrian access and enhance the
aesthetic of the street.
Storm drainage
Per on our conversation, I understand that the proposed stonn drainage design shall be required to meet requirements
ofthe 1990 King County Surface Water Design Manual (KCSWDM). Based on these requirements it appears that the
project will be required to provide basic water quality treatment for the runoff from impervious areas subject to
vehicular use (over 5,000 sf proposed). Per KCSWDM and City of Renton Code it appears that the only approved
method of basic water quality treatment is a biofiltration swale.
We request an adjustment of the drainage be granted to allow use ofthe Stonnwater Management, Inc.'s Stonnfilter
treatment system in lieu of a biofiltration swale on this site. Although a biofiltration swale could be sited in the
landscaped area between the proposed building and the right of way, on the downstream portion of the site, we believe
the use of a Stonnfilter would result in a superior design due to the following:
I. The only practical spot for a biofiltration swale given the site topography is on the eastern end of the site adjacent
to the Lake Washington Blvd. right of way. A proposed swale would have to be located parallel to the sidewalk
along the property frontage. The slope along the sidewalk here is approximately 5% which is typically too steep
for a biofiltration swale. The swale will require grading some steep slopes, possibly retaining walls or rockeries
LPD Engineering 7936 Seward Park Avenue South, Seattle, Washington 98118 Phone/Fax: (206) 725-1211
which could create restrictions or safety issues for pedestrians in the area that we are trying to encourage
pedestrian activity.
2. The use of an underground stormwater quality treatment facility will allow the full width of the buffer between the
right of way and the building to be landscaped, which could provide an enhancement to the community and the
aesthetic of the building.
3. Water quality treatment -Washington State Department of Ecology has approved use of the proposed Stormfilter
Treatment System as a basic stormwater treatment practice for total suspended solids (TSS) removal (please see
the attached Ecology memorandum, or refer to the following link:
http://www . ecy. wa. gov/programs/wq/ stormwa lcr/newtechluse designations/stormfilter guld.pdf
Our proposed design would be in accordance with Ecologies requirements.
Attached is a sketch of the preliminary site layout. Please consider the information outlined above and let us know if
the City of Renton will consider the use of a Stormwater Management Inc.' s Stormfilter Treatement System in lieu of a
biofiltration swale for basic water quality treatment. Please let me know if you need further information or if you have
any questions. Thank you for your consideration of our request
n
, ~tne ng, PLLC
Jeff Lamoureux PE
LPD Engineering 7936 Seward Park Avenue South, Seattle, Washington 98118 Phone/Fax: (206) 725-1211
Geotechnical Engineering
Water Resources
Environmental Assessments and
Remediation
Sustainable Development Services
Geologic Assessments
Associated Earth Sciences, Inc.
CtJ~'f'trt7'!f:if ~t'll'f q/JeIWC6'
Subsurface Exploration, Geologic Hazard, and
Preliminary Geotechnical Engineering Report
KENNYDALE CAFE
Renton, Washington
Prepared for
Pool Brothers Construction, LLC/
HearthStone Homes, LLC
Project No. KE04520A
February 27,2006
Associated Earth Sciences, Inc.
February 27, 2006
Project No. KE04520A
iliw~~~
eetehrafil1J 251jears o(.S'ervice
Pool Brothers Construction, LLC/HearthStone Homes, LLC
P.O. Box 3023
Renton, Washington 98056
Attention: Mr. Matt Pool
Subject: Subsurface Exploration, Geologic Hazard, and
Preliminary Geotechnical Engineering Report
Kennydale Cafe
1322 Lake Washington Boulevard North
Renton, Washington
Dear Mr. Pool:
We are pleased to present the enclosed copies of the above-referenced report. This report
summarizes the results of our subsurface exploration, geologic hazard, and preliminary
geotechnical engineering studies and offers recommendations for the preliminary design and
development of the proposed project. Our recommendations are preliminary in that building
plans/construction details have not yet been finalized.
We have enjoyed working with you on this study and are confident that the recommendations
presented in this report will aid in the successful completion of your project. If you should
have any questions or if we can be of additional help to you, please do not hesitate to call.
Sincerely,
ASSOCIATED EARTH SCIENCES, INC.
Kirkland, Washington
~!HA"
Kurt D. Merriman, P.E.
Principal Engineer
KDMIJi./
KE04520A2
Projecls\20040520\KE\WP
Kirldand Office· 911 FdihAvenue, Suite 100· Kirkland, WA 98033· P 1(425) 827-7701. F I (425) 827-5424
Everen Office· 2911 1/2 HewinAvenue, Suite 2· Lvemt, WA 98201 • P 1(425) 259-0522· F 1(425) 252-3408
\v\v\,\;ac.sgeo,cofll
SUBSURFACE EXPLORATION, GEOLOGIC HAZARD, AND
PRELIMINARY GEOTECHNICAL ENGINEERING REPORT
KENNYDALE CAFE
Renton, Washington
Prepared for:
Pool Brothers Construction, LLCI
HearthStone Homes, LLC
P.O. Box 3023
Renton, Washington 98056
Prepared by:
Associated Earth Sciences, Inc.
911 5th Avenue, Suite 100
Kirkland, Washington 98033
425-827-7701
Fax: 425-827-5424
February 27, 2006
Project No. KE04520A
Kennydale Cafe
Renton, Washington
1.0 INTRODUCTION
Subsuiface Exploration. Geologic Hazard, and
Preliminary Geotechnical Engineering Repon
Project and Site Conditions
I. PROJECT AND SITE CONDITIONS
This report presents the results of our subsurface exploration, geologic hazard, and preliminary
geotechnical engineering study for the proposed Kennydale Cafe to be located at 1322 Lake
Washington Boulevard North in Renton, Washington. Our recommendations are preliminary
in that building plans/construction details have not yet been finalized. The approximate
location of the subject site is shown on the Vicinity Map, Figure 1. The property boundaries
and the locations of the explorations conducted at the site, as well as other pertinent site
features, are shown on the Site and Exploration Plan, Figure 2. In the event that any changes
in the nature, design, or locations of the structures are planned, the conclusions and
recommendations contained in this report should be reviewed and modified, or verified, as
necessary.
1.1 Purpose and Scope
The purpose of this study was to provide subsurface data to be used in the preliminary design
and development of the above-mentioned project. Initial site exploration was conducted during
the month of September 2004 and consisted of excavation of five exploration pits within the
central portion of the site. Our current study, as outlined in our February 6, 2006 proposal,
included a review of available geologic literature, drilling of two exploration borings, and
performing geologic studies to assess the type, thickness, distribution, and physical properties
of the subsurface sediments and shallow ground water conditions. Data obtained during our
September 2004 exploration is used as a part of this report. Geotechnical engineering studies
were also conducted to assess the types of suitable foundations, allowable foundation soil
bearing pressures, anticipated settlements, basement/retaining wall lateral pressures, floor
support recommendations, and drainage considerations. This report summarizes our previous
and current fieldwork and offers preliminary development recommendations based on our
present understanding of the project.
I. 2 Authorization
Verbal authorization to proceed with this study was granted by Mr. Matt Pool of Pool Brothers
Construction, LLC/HearthStone Homes, LLC. Our recent study was accomplished in general
accordance with our scope of work dated February 6, 2006. This report has been prepared for
the exclusive use of Pool Brothers Construction, LLC/HearthStone Homes, LLC and their
agents for specific application to this project. Within the limitations of scope, schedule, and
budget, our services have been performed in accordance with generally accepted geotechnical
engineering and engineering geology practices in effect in this area at the time our report was
prepared. No other warranty, express or implied, is made.
February 27, 2006 ASSOCIATED EARTH SCIENCES, INC.
MTIld, KE04520A2 -Projecrsl20040520lKEIWP Page 1
Kermydale Cafe
Renton, Washington
2,0 SITE AND PROJECT DESCRIPTION
2.1 Site Description
Subsurface Exploration, Geologic Hazard, and
Preliminary Geotechnical Engineering Report
Project and Site Conditions
The subject site is located at 1322 Lake Washington Boulevard North in Renton, Washington.
The site is currently vacant; however, based on the existence of concrete basement walls and
charred remains of wood flooring and walls within the western portion of the site, it appears
that the site has previously been occupied.
The site is bounded on the north by vacant land, on the south by a vehicle storage yard, on the
east by Interstate 405 (1-405), and on the west by Lake Washington Boulevard North. The site
ascends toward the east from the western property line. Slope gradients range from
approximately 15 percent within the western portion of the site to in excess of 40 percent
within the eastern portion of the site. Overall topographic relief across the site is on the order
of 100 feet.
Midway up the slope within the central portion of the site, what appears to be an unimproved
path or roadway extending in a northeasterly direction across the slope face was observed. No
information regarding construction of this feature was available to us, but it appears as if it
may have been created by north-south excavation across the slope face. The area is now
partially overgrown with blackberry vines and deciduous trees.
Vegetation within the western portion of the site in the vicinity of the previously existing
structure consists of blackberry vines. A single pine tree exists adjacent to the southwest
corner of the remaining foundation. Vegetation across the central and eastern portions of the
site consists of a moderate coverage of deciduous trees with brush and blackberry vines
comprising much of the understory.
2.2 Proposed Construction
It is our understanding that project plans include construction of a four-unit townhouse above a
3,200 square foot restaurant. The lower-level, daylight restaurant will be excavated into the
existing hillside above Lake Washington Boulevard North. Based on Sheet A8 "Elevations"
and on Sheet A9 "Details" dated January 6, 2006 by Rick Anderson, Architect, a split-level
parking lot is to be created upslope from the proposed structure. Access to the parking area
will be via a paved driveway extending upslope from Lake Washington Boulevard North along
the south side of the proposed structure. The western (lower) portion of the parking lot is at
an elevation approximately 10 feet above Lake Washington Boulevard North. The eastern
(upper) portion of the parking lot is at an elevation approximately 30 feet above adjacent Lake
Washington Boulevard North. A four-car garage is to be built within the northeast portion of
the upper parking lot. Retaining walls to a height of 15 feet are anticipated.
February 27, 2006 ASSOCIATED EARTH SCIENCES, INC.
MTIJd -KE04520A2 -ProjectsI20040520IKEIWP Page 2
Kennydale Caje
Renton, Washington
3.0 SUBSURFACE EXPLORATION
Subsurface Exploration, Geologic Hazard, and
Preliminary Geotechnical Engineering Report
ProjeCi and Site Conditions
Previous site exploration consisted of excavation of five exploration pits during the month of
September 2004 to evaluate near-surface conditions within the "roadway" feature within the
central portion of the site. The exploration pit logs are resubmitted as a part of this report.
Current exploration consisted of advancement of two exploration borings; one within the lower
portion of the site and one midway upslope in the vicinity of the proposed cut for the eastern
parking lot wall. The various types of sediments, as well as the depths where the
characteristics of the sediments changed, are indicated on the exploration logs presented in the
Appendix. It should be noted that the depths indicated on the attached logs where conditions
changed may represent gradational variations between sediment types in the field. Our
explorations were located in the field relative to topographic information provided to us. The
approximate locations of the explorations are shown on the Site and Exploration Plan,
Figure 2.
The conclusions and recommendations presented in this report are based, in part, on the
exploration pits excavated during our earlier (September 2004) exploration and on our current
borings. Because of the nature of exploratory work below ground, extrapolation of subsurface
conditions between field explorations is necessary. It should be noted that differing subsurface
conditions may sometimes be present due to the random nature of deposition and the alteration
of topography by past grading and/or filling. The nature and extent of any variations between
the field explorations may not become fully evident until construction. If variations are
observed at that time, it may be necessary to re-evaluate specific recommendations in this
report and make appropriate changes.
3.1 Exploration Pits
The exploration pits completed during September 2004 were excavated with a track-mounted
excavator provided for our use. The exploration pits permitted direct, visual observation of
subsurface conditions. Materials encountered in the exploration pits were studied and
classified in the field by a geotechnical engineer from our firm. All exploration pits were
backfilled immediately after examination and logging. Selected samples were then transported
to our laboratory for further visual classification and testing, as necessary. The exploracion
logs presented in the Appendix are based on [he field logs and inspection of the samples
secured.
3.2 Exploration Borings
The exploration borings were completed by advancing a hollow-stem auger with a portable
drill rig subcontracted to us. During the drilling process, samples were obtained at 2.5-to 5-
foot-depth intervals. The borings were continuously observed and logged by a geotechnical
engineer from our firm. The exploration logs presented in the Appendix are based on the field
logs, drilling action, and inspection of the samples secured.
February 27, 2006 ASSOCIATED EARTH SCIENCES, INC.
MTlld -KE04520A2 -Projects12004()5201KE1WP Page 3
Kennydale Caje
Renton, Washington
Subsuiface Exploration, Geologic Hazard, and
Preliminary Geotechnical Engineering Report
Project and Site Conditions
Disturbed, but representative samples were obtained by using the Standard Penetration Test
(SPT) procedure in accordance with American Society for Testing and Materials (ASTM):D
1586. This test and sampling method consists of driving a standard 2-inch, outside-diameter,
split-barrel sampler a distance of 18 inches into the soil with a 140-pound hammer free-falling
a distance of 30 inches. The number of blows for each 6-inch interval is recorded, and the
number of blows required to drive the sampler the final 12 inches is known as the Standard
Penetration Resistance ("N") or blow count. If a total of 50 blows are recorded within one 6-
inch interval, the blow count is recorded as the number of blows for the corresponding number
of inches of penetration. The resistance, or N -value, provides a measure of the relative density
of granular soils or the relative consistency of cohesive soils; these values are plotted on the
attached boring logs.
The samples obtained from the split-barrel sampler were classified in the field and
representative portions placed in watertight containers. The samples were then transported to
our laboratory for further visual classification and laboratory testing, as necessary.
4.0 SUBSURFACE CONDITIONS
Review of the regional geologic map entitled Draft Geologic Map of King County, Washington
by Derek Booth, Ralph Haugerud, and Jill Sacket (December 27, 2002) indicates that the area
of the subject site is underlain by pre-Fraser deposit soil. Our interpretation of the sediments
encountered in our exploration pits and borings is in general agreement with the regional
geologic map.
Subsurface conditions at the project site were inferred from the field explorations accomplished
for this study. Additional regional geologic information was provided through review of
applicable geologic literature. As shown on the attached exploration logs, sediments
encountered in our exploration pits and borings generally consisted of pre-Fraser deposits
overlain by topsoil/disturbed soil. The following section presents more detailed subsurface
information organized from the youngest to the oldest sediment types.
4.1 Stratigraphy
Topsoil/Disturbed Soil
A surficial layer of topsoil/disturbed soil was encountered in the explorations at the site. This
surficial soil consisted generally of a brown to dark brown mixture of silt and sand in a loose
condition. The topsoil/disturbed soil layer ranged in thickness from approximately 1 to 5 feet.
Due to the low density observed, the existing topsoil/disturbed soil layer is not considered
suitable in its existing condition for foundation or pavement support. Based on site grades
shown on the project plans provided to us, these materials will be removed from within the
building areas as part of site grading and excavation activity.
February 27, 2006 ASSOCIATED EARTH SCIENCES, INC.
MTlld -KE04520A2 -Projeclsl20040520lKEI WP Page 4
Kennydale Cafe
Remon, Washington
Pre-Fraser Deposits
Subsurface Exploration, Geologic Hazard, and
Preliminary Geotechnical Engineering Report
Project and Site Conditions
Beneath the surficial soil, sediments consisting of weakly to moderately oxidized silts and fine
to coarse sand with faint to prominent laminations were encountered. These sediments are
interpreted to be pre-Fraser deposits. Based on the relatively fine-grained nature of the soils
encountered, these soils were likely deposited in a low-energy environment, such as a lake,
and are therefore referred to as lacustrine deposits. The upper, approximately 2 to 3 feet of
these deposits were observed to be in a weathered, relatively loose condition, not considered to
be suitable for foundation or pavement support without recommended remedial densification,
as described herein.
Below the weathered zone, the lacustrine deposits were observed to be in a dense to very dense
condition and are considered suitable for support of foundation loads and pavement support
with proper preparation. Lacustrine deposits are composed primarily of silt and fine sand,
considered highly moisture-sensitive, and are highly prone to disturbance when wet site or
weather conditions exist. Vigilance will be required when foundation bearing soils composed
of lacustrine deposits are exposed to prevent disturbance and resulting increased costs for
removing the disturbed soils and restoring suitable support conditions.
4.2 Hydrology
No ground water seepage was encountered during our September 2004 exploration. Lenses of
very moist to wet soil were encountered below a depth of approximately 5 feet in both
exploration borings advanced during our February 2006 exploration. This is consistent with a
type of ground water seepage known as interflow. Interflow consists of surface water that
infiltrates through relatively permeable soils and becomes trapped or perched atop underlying,
low-permeability surfaces or layers. Perched zones of ground water may also occur within
pre-Fraser deposit soil in areas where these sediments exhibit increases in permeability due to
localized grain size variations. Ground water measured within exploration borings EB-I and
EB-2 after completion of drilling was encountered at a depth of 18 feet below lowest adjacent
ground surface. No monitoring wells were installed during our current exploration program.
It should be noted that the occurrence and level of ground water seepage at the site may vary in
response to changes in season, precipitation, irrigation, and other factors. Perched and
interflow seepage should be expected during the wetter winter and spring months and
following periods of heavy or sustained precipitation.
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II. GEOLOGIC HAZARDS AND MITIGATIONS
Based on information obtained from the City of Renton's web site
http://rentonnet.org/MapGuide/maps/ParceLmwf , the project is in an area of mapped erosion
hazards, moderate landslide hazards, and regulated slopes ranging from 15 to < 90 percent.
The hazards and regulated slopes are discussed in the following sections and recommended
mitigation measures presented in conformance with the Renton Critical Areas Ordinance
No. 5137. The following discussion of potential geologic hazards is based on the geologic,
slope, and shallow ground water conditions as observed and discussed herein.
5.0 LANDSLIDE HAZARDS AND RECOMMENDED MITIGATION
Observation of site slopes revealed no evidence of instability or past landslide activity.
Unweathered, dense to very dense soil underlying the surficial stratum at the site is not
considered likely to be mobilized due to relatively high strength related to density.
Based on site observation, it is our opinion that the soils (to a depth of approximately 2 to 8
feet) across the surface of the site slopes possess a moderate potential for shallow slumps. The
risk of shallow soil movement within the surficial soil increases substantially following
extended periods of wet weather or during moderate to large seismic events. The potential for
shallow surficial slope instability will be reduced by proper site drainage, retaining wall
construction, impact wall construction, and placement of a debris fence along the top of the
impact wall, as discussed later in this report.
In our opinion, the proposed development will not adversely affect existing site hazards. The
proposed improvements may eliminate or stabilize some of the landslide hazard and steep slope
areas. As designed, the parking area provides a "buffer" of approximately 100 feet between
steep slope areas and the proposed habitable structure. In our opinion, no additional buffers
from the existing steep slopes or landslide hazard areas are necessary or recommended
provided recommendations contained in this report are followed during construction and
maintenance of the planned improvements.
The uppermost wall of the upper parking area should be designed with an additional 4 feet of
height (freeboard) above the retained slope. This freeboard will act as an impact wall to
impede soil slumps reducing the potential for damage to the proposed structures. Some soil
may slough over the freeboard and debris fence along the upslope side of the upper park ing lot
if accumulated debris is not periodically removed from the behind the wall. It is possible that
the wall could be overtopped during a worst case slide or seismic event. Debris fencing should
be installed along the top of the impact wall. The debris fence should consist of a 4-foot-high
cyclone fence above the 4-foot structural impact wall mentioned above. Access for small
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equipment should be provided to maintain the area behind the catchment wall free from debris
and maintain intended function.
As with all slopes, surface drainage should be properly controlled and directed away from
sloping areas. Downspouts from roofs should be tightlined into suitable storm water drainage
systems. At no time should fill be pushed over the top of banle Uncontrolled fill over tops of
slopes may promote landslides or debris flow activity.
6.0 SEISMIC HAZARDS AND RECOMMENDED MITIGATION
Earthquakes occur in the Puget Lowland with great regularity. The vast majority of these
events are small and are usually not felt by people. However, large earthquakes do occur as
evidenced by the 1949, 7.2-magnitude event; the 1965, 6.5-magnitude event; and the 2001,
6.8-magnitude event. The 1949 earthquake appears to have been the largest in this region
during recorded history and was centered in the Olympia area. Evaluation of earthquake
return rates indicates that an earthquake of the magnitude between 5.5 and 6.0 is likely within
a given 20-year period.
Generally, there are four types of potential geologic hazards associated with large seismic
events: 1) surficial ground rupture, 2) seismically induced landslides, 3) liquefaction, and
4) ground motion. The potential for each of these hazards to adversely impact the proposed
project is discussed below.
6.1 Surficial Ground Rupture
The nearest known fault trace to the project site is the Seattle Fault located approximately
7 miles to the north. Recent studies by the U.S. Geological Survey (e.g., Johnson et aI., 1994,
Origin and Evolution of the Seattle Fault and Seattle Basin, Washington, Geology, v. 22,
pp. 71-74; and Johnson et aI., 1999, Active Tectonics of the Seattle Fault and Central Puget
Sound Washington -Implications for Earthquake Hazards, Geological Society of America
Bulletin, July 1999, v. 111, n. 7, pp. 1042-1053) have provided evidence of surficial ground
rupture along a northern splay of the Seattle Fault. The recognition of this fault splay is
relatively new, and data pertaining to it are limited with the studies still ongoing. According to
the U. S. Geological Survey studies, the latest movement of this fault was about 1,100 years
ago when about 20 feet of surficial displacement took place. This displacement can presently
be seen in the form of raised, wave-cut beach terraces along Alki Point in West Seattle and
Restoration Point at the south end of Bainbridge Island. The recurrence interval of movement
along this fault system is still unknown. although it is hypothesized to be in excess of several
thousand years. Due to the suspected long recurrence interval, the potential for surficial
ground rupture is considered to be low during the expected life of the proposed structures.
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6.2 Seismically Induced Landslides
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The potential risk of damage to the proposed development by seismically induced landsliding is
discussed in Section 5.0. In general, ground motion associated with strong seismic shaking
significantly increases the risk of shallow landsliding within the surficial site soil.
6.3 Liquefaction
Liquefaction is a temporary loss in soil shear strength that can occur when loose granular soils
below the ground water table are exposed to cyclic accelerations, such as those that occur
during earthquakes. The observed site soils were generally dense and are not expected to be
prone to liquefaction. A detailed liquefaction analysis was not completed as a part of this
study, and none is warranted, in our opinion.
6.4 Ground Motion
Based on the encountered stratigraphy, it is our opinion that any earthquake damage to the
proposed structures, when founded on suitable foundation bearing strata in accordance with the
recommendations provided in this report, would be caused by the intensity and acceleration
associated with the event and not any of the above-discussed impacts. Design of the project
should be consistent with 2003 International Building Code (lBC) guidelines. In accordance
with the 2003 IBC, the following values should be used:
Site Class C (Table 1615.1.1)
Ss = 138% (Figure 1615[1])
SI = 48 % (Figure 1615[2])
7.0 EROSION HAZARDS AND MITIGATION
The sediments underlying the site generJlly contain silt and sand and will be sensitive to
erosion, especially in the sloping portions of the site. In order to reduce the amount of
sediment transport off the site during construction, the following recommendations should be
followed.
I) Silt fencing should be placed around the lower perimeter of all cleared area(s). The
fencing should be periodically inspected and maintained, as necessary, to ensure proper
function.
2) To the extent possible, earthwork-related construction should proceed during the drier
periods of the year, and disturbed areas should be revegetated as soon as possible.
Temporary erosion control measures should be maintained until permanent erosion
control measures are established.
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3) Areas stripped of vegetation during construction should be mulched and hydroseeded,
replanted as soon as possible, or otherwise protected. During winter construction,
hydroseeded areas should be covered with clear plastic to facilitate grass growth.
4) If excavated soils are to be stockpiled on the site for reuse, measures should be taken to
reduce the potential for erosion from the stockpile. These could include, but are not
limited to, covering the pile with plastic sheeting, the use of low stockpiles in flat areas,
and the use of straw bales/silt fences around pile perimeters.
5) Interceptor swales with rock check dams should be constructed to divert storm water
from construction areas and to route collected storm water to an appropriate discharge
location.
6) A rock construction entrance should be provided to reduce the amount of sediment
transported off-site on truck tires.
7) All storm water from impermeable surfaces, including driveways and roofs, should be
tightlined into approved facilities and not be directed onto or above steeply sloping
areas.
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Preliminary Design Recommendations
III. PRELIMINARY DESIGN RECOMMENDATIONS
8.0 INTRODUCTION
Our exploration indicates that, from a geotechnical engineering standpoint, the proposed
project is feasible provided the recommendations contained herein are properly followed. The
bearing stratum ranges in depth beneath existing ground surface from approximately 2 to 8
feet. Conventional shallow foundations and standard pavement sections should perform well
with proper subgrade preparation in most areas.
8.1 Site Preparation
Site preparation of building and pavement areas should include removal of existing
foundations, trees, brush, debris, and any other deleterious materials. All existing fill around
the pre-existing structure should be removed from within building/pavement areas. Existing
septic systems should be decommissioned in accordance with Renton Health Department
requirements and removed from beneath any areas where structures or paving are planned. If
any water wells exist on-site, they should be decommissioned by a licensed well driller in
accordance with Washington Administrative Code (WAC) Section 173-160. If any heating oil
storage tanks or other similar structures are present on-site, they should be decommissioned
and removed in accordance with applicable Washington State Department of Ecology
(Ecology) regulations. Any depressions below planned final grades caused by demolition
activities should be backfilled with structural fill, as discussed under the Structural Fill section.
Organic topsoil should be removed from areas where new buildings, paving, or other
structures are planned. After stripping, remaining roots and stumps should be removed from
structural areas. All soils disturbed by stripping and grubbing operations should be
recompacted as described below for structural fill.
Once excavation to sub grade elevation is complete, the resulting surface should be proof-rolled
with a loaded dump truck or other suitable equipment. Any soft, loose, or yielding areas
should be excavated to expose suitable bearing soils. The subgrade should then be compacted
to at least 95 percent of the modified Proctor maximum dry density as determined by the
ASTM:D 1557 test procedure. Structural fill can then be placed to achieve desired grades, if
needed.
8.2 Site Disturbance
Some of the on-site soils contain substantial fine-grained material that makes them moisture-
sensitive and subject to disturbance when wet. The contractor must use care during site
preparation and excavation operations so that the underlying soils are not softened. If
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disturbance occurs, the softened soils should be removed and the area brought to grade with
structural fill.
8.3 Winter Construction
Based on the high in-situ moisture content of site soils observed during our February 2006
exploration, it may be necessary to dry a significant portion of site soils during favorable dry
weather conditions to allow them to be reused in structural fill applications. If construction
takes place in winter, drying is not expected to be feasible, and we anticipate that most or all of
the site soils will be unsuitable for structural fill applications. Even during dry weather, site
soils excavated for installation of buried utilities might not be suitable for utility backfill under
paving or other structures. We recommend budgeting for backfill of buried utility trenches in
structural areas with select, imported structural fill. If earthwork will be completed during
winter months, we recommend budgeting to construct all structural fills with select, imported
fill materials. For summer construction, significant, but unavoidable effort will be needed to
scarify, aerate, and dry site soils to reduce moisture content prior to compaction in structural
fill applications. Care should be taken to seal all earthwork areas during mass grading at the
end of each workday by grading all surfaces to drain and sealing them with a smooth-drum
roller. Stockpiled soils that will be reused in structural fill applications should be covered
whenever rain is possible.
If winter construction is expected, crushed rock fill could be used to provide construction
staging areas. The stripped sub grade should be observed by the geotechnical engineer, and
should then be covered with a geotextile fabric, such as Mirafi 500X or equivalent. Once the
fabric is placed, we recommend using a crushed rock fill layer at least 10 inches thick in areas
where construction equipment will be used. If desired, planned roadways can be paved with
asphalt treated base (ATB) for construction staging, as described in the Pavement
Recommendations section of this report.
8.4 Temporary Cut Slopes
In our opinion, stable construction slopes should be the responsibility of the contractor and
should be determined during construction. For estimating purposes, however, we anticipate
that temporary, unsupported cut slopes in the topsoil or disturbed/weathered pre-Fraser deposit
soil can be planned at 1.5H:IV (Horizontal:Vertical) or flatter; temporary, unsupported cut
slopes in the dense, unweathered, pre-Fraser deposit soil can be planned at IH:IV or flatter.
These slope angles are for areas where ground water seepage is not encountered and assume
that surface water is not allowed to flow across the temporary slope faces. If ground or
surface water is present when the temporary excavation slopes are exposed, flatter slope angles
will be required. As is typical with earthwork operations, some sloughing and raveling may
occur, and cut slopes may have to be adjusted in the field. In addition, WISHAfOSHA
regulations should be followed at all times.
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9.0 PERMANENT SLOPES
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Permanent slopes proposed for the site should be planned at a gradient no steeper than
2.6H:IV. As with all slopes, surface drainage should be properly controlled and directed
away from sloping areas. Downspouts from roofs should be tightlined into suitable storm
water drainage systems. At no time should fill be pushed over the top of bank. Uncontrolled
fill over tops of slopes may promote landslides or debris flow activity.
10.0 STRUCTURAL FILL
Structural fill may be necessary to establish desired grades. All references to structural fill in
this report refer to subgrade preparation, fill type, placement, and compaction of materials, as
discussed in this section. If a percentage of compaction is specified under another section of
this report, the value given in that section should be used.
After stripping, planned excavation, and any required overexcavation have been performed to
the satisfaction of the geotechnical engineer/engineering geologist, the exposed ground surface
should be recompacted to 90 percent of ASTM:D 1557.
In lieu of recompaction in areas where the subgrade contains too much moisture, we
recommend that the stripped subgrade be overlain by an engineering stabilization fabric, such
as AMOCO 2002 (or equivalent), with the edges of the fabric overlapped in accordance with
the manufacturer's recommendations. A minimum of 12 inches of clean, free-draining
structural fill compacted to a minimum of 95 percent of ASTM:D 1557 should be placed over
the fabric. The structural fill should then be proof-rolled with a loaded dump truck to
pretension the fabric and identify any soft spots in the fill. Upon completion of proof-rolling,
additional structural fill should be placed, if necessary, to obtain desired grades.
After recompaction of the exposed ground is tested and approved, or a free-draining rock
course is laid, structural fill may be placed to attain desired grades. Structural fill is defined as
non-organic soil, acceptable to the geotechnical engineer, placed in maximum 8-inch loose lifts
with each lift being compacted to 95 percent of ASTM:D 1557. In the case of roadway and
utility trench filling, the backfill should be placed and compacted in accordance with codes and
standards acceptable to the governing agency. The top of the compacted fill should extend
horizontally outward a minimum distance of 3 feet beyond the locations of the perimeter
footings or roadway edges before sloping down at a maximum angle of 2H: IV.
Fill placed on slopes steeper than 5H: 1 V should be benched into dense till or suitable bedrock
during grading to establish a good contact and minimize the potential for development of a slip
plane. Benches should expose at least 4 feet (vertical) of strata acceptable to the geotechnical
engineer or geologist. All fills proposed over a slope should be reviewed by our office prior to
construction.
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The contractor should note that any proposed import fill soils must be evaluated by Associated
Earth Sciences, Inc. (AESI) prior to their use in fills. This would require that we have a
sample of the material at least 72 hours in advance to perform a Proctor test and determine its
field compaction standard. Soils in which the amount of fine-grained material (smaller than the
No. 200 sieve) is greater than approximately 5 percent (measured on the minus No.4 sieve
size) should be considered moisture-sensitive. Use of moisture-sensitive soil in structural fills
should be limited to favorable dry weather and dry subgrade conditions. The on-site soils
contained substantial amounts of silt and are considered highly moisture-sensitive when
excavated and used as fill materials. We anticipate that due to mixing of soils as they are
excavated, most excavated site soils will require aeration and drying prior to compaction in
structural fill applications. Construction equipment traversing the site when the soils are wet
can cause considerable disturbance.
If fill is placed during wet weather or if proper compaction cannot be obtained, a select, import
material consisting of a clean, free-draining gravel and/or sand should be used. Free-draining
fill consists of non-organic soil with the amount of fine-grained material limited to 5 percent by
weight when measured on the minus NO.4 sieve fraction and at least 25 percent retained on
the No.4 sieve.
1l.0 FOUNDATIONS
Spread footings may be used for building support when they are founded on approved
structural fill placed as described above, or on suitable native stratum prepared as
recommended in this report. Where existing fill is present below final grades, it should be
removed and replaced with structural fill, which is also suitable for foundation support.
Footings may be designed for an allowable foundation soil bearing pressure of 3,000 pounds
per square foot (psI), including both dead and live loads. Footings supported entirely on
unweathered, pre-Fraser deposit soil may be designed for an allowable foundation soil bearing
pressure of 5,000 psf, including both dead and live loads. An increase of one-third may be
used for short -term wind or seismic loading. Perimeter footings should be buried at least
18 inches into the surrounding soil for frost protection. However, all foundations must
penetrate to the prescribed bearing stratum, and no foundations should be constructed in or
above loose, organic, or existing fill soils. In addition, all footings must have a minimum
width of 18 inches.
Anticipated settlement of footings founded as recommended should be on the order of ')4 inch
or less with differential settlement of 12 inch or less. However, disturbed material not
removed from footing trenches prior to footing placement could result in increased settlements.
All footing areas should be inspected by AESI prior to placing forms and steel to verify that
the foundation subgrades are undisturbed and construction conforms to the recommendations
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contained in this report. Such inspections may be required by the City of Renton. Perimeter
footing drains should be provided, as discussed under the section on Drainage Considerations.
It should be noted that the area bounded by lines extending downward at IH: 1 V from any
footing must not intersect another footing or intersect a filled area that has not been compacted
to at least 95 percent of ASTM:D 1557. In addition, a 1.5H: 1 V line extending down and away
from any footing must not daylight because sloughing or raveling may eventually undermine
the footing. Thus, footings should not be placed near the edge of steps or cuts in the bearing
soils.
12.0 FLOOR SUPPORT
If crawl space floors are used, an impervious moisture barrier should be provided above the
soil surface within the crawl space. Slab-on-grade floors may be used over medium dense to
very dense native soils, or over structural fill placed as recommended in the Site Preparation
and Structural Fill sections of this report. Slab-on-grade floors should be cast atop a minimum
of 4 inches of pea gravel or "clean" crushed rock to act as a capillary break. The floors
should also be protected from dampness by covering the capillary break layer with an
impervious moisture barrier at least 10 mils in thickness.
13.0 DRAINAGE CONSIDERATIONS
We observed ground water at a depth of 18 feet below ground surface in exploration borings
EB-I and EB-2. Lenses of wet soils were observed in exploration borings EB-l and EB-2
suggesting the possibility of interflow within relatively permeable soil above less permeable
soil. Therefore, prior to site work and construction, the contractor should be prepared to
provide temporary drainage and subgrade protection, as necessary.
All footing walls, basement walls, and retaining walls should be provided with a drain at the
footing elevation. Drains should consist of rigid, perforated, polyvinyl chloride (PVC) pipe
surrounded by washed pea gravel. The level of the perforations in the pipe should be set at the
bottom of the footing at all locations, and the drain collectors should be constructed with
sufficient gradient to allow gravity discharge away from the buildings. In addition, all
foundation walls taller than 3 feet should be lined with a minimum, 12-inch-thick, washed
gravel blanket that ties into the footing drain. The gravel blanket should extend up the back of
the wall to within 1 foot of finished grade where less permeable soil can be used as a cap over
the drain rock to reduce infiltration of surface water. Roof and surface runoff should not
discharge into the footing drain system, but should be handled by a separate, rigid, tightline
drain. In planning, exterior grades adjacent to foundations should be sloped downward away
from the structures to achieve surface drainage.
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14.0 CAST-IN-PLACE RETAINING WALLS AND BASEMENT WALLS
Walls that are free to yield laterally at least 0 1 percent of their height should be designed
using "active" equivalent fluid pressures. Fully restrained, rigid walls that cannot yield should
be designed using "at-rest" equivalent fluid pressures. The following table provides
appropriate active, at-rest, and passive equivalent fluid pressures (and associated friction
coefficients) for the anticipated project wall design conditions. For walls located adjacent to
areas that are subject to vehicle traffic, a surcharge equivalent to 2 feet of retained soil should
be added to the wall height in determining lateral design forces.
Active At-Rest Passive
Backslope Equivalent Equivalent Equivalent
Conditions Fluid Pressure Fluid Pressure Fluid Pressure Friction
Rock/Soil Type (Horizontal: Vertical) (pcf)' (pel) (pel) Coefficient
Topsoil! Horizontal 50 70 200 0.20
disturbed soil
Topsoill 2H: 1 V maximum 80 95 200 0.20
disturbed soil
Structural fill Horizontal 35 55 300 0.35
Structural fill 2H: 1 V maximum 65 80 300 0.35
Unweathered Horizontal 30 50 350 0.40
pre-Fraser deposit soil
Unweathered 2H: 1 V maximum 60 75 350 0.40
pre-Fraser deposit soil
* pef -pounds per CUblC foot
Lateral loads for footings may be designed using a combination of lateral sliding resistance
along the bottom of footings and passive earth pressure against the sides of footings. Lateral
sliding resistance may be determined by mUltiplying the dead load by the coefficient of friction
listed for the appropriate stratum in the table presented above. Passive earth pressure (passive
equivalent fluid pressure) should be assumed to be zero at the surface of the bearing stratum
and may be assumed to increase with depth in bearing stratum at the rate indicated in the table.
Lateral bearing and lateral sliding resistance may be combined.
A II backfill behind walls or around foundation units should be placed as per our
recommendations for structural fill and as described in this section of the report. Where east-
in-place retaining walls face structural fill, the backfill should consist of on-site or imported
granular fill compacted to 90 percent of ASTM:D 1557 using light compaction equipment
only. A higher degree of compaction is not recommended, as this will increase the pressure
acting on the wall. A lower compaction may result in settlement of slab-on-grades or other
improvements placed above the walls. Thus, the compaction level is critical and must be
tested by our firm during placement. Surcharges from adjacent footings, heavy construction
equipment, or sloping ground (where not indicated) must be added to the above values.
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Perimeter footing drains and wall backdrains
discussed under Drainage Considerations.
14.1 Impact Walls
Subsurface Exploration, Geologic Hazard, and
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Preliminary Design Recommendations
should be provided for all retaining walls, as
In order to mitigate the potential risk of damage to the proposed structures by shallow-seated
landsliding, we recommend that the retaining walls proposed for the upslope side of the upper
parking lot be extended a minimum of 4 feet above the adjacent ground surface to act as a
catchment for landslide debris that may come off of the upper slope. For design purposes, we
estimated that a small debris flow could impact the proposed wall with a dynamic force of
500 pounds per horizontal foot of wall. This value assumes a debris flow with a mass of
125 pounds per cubic foot (pcf) traveling at a velocity of 6 feet per second. It must be
understood that estimating the depth and speed of a debris flow is not an exact science. The
structural engineer should note that no factors of safety were applied to our calculations;
rather, we expect that the designer will apply an appropriate factor of safety to such a scenario.
Our assumptions were based on the thickness of the weathered soil unit encountered on the
slope above the proposed parking lot. However, future debris flows may vary from those
estimated. As such, the owner must understand and accept the risk of building at the base of a
slope and that future slope failures may damage the parking lot/garage and/or parked vehicles.
Debris fencing should be installed along the top of the impact wall. The debris fence should
consist of a 4-foot-high cyclone fence above the 4-foot structural impact wall mentioned above.
Access for small equipment should be provided to maintain the area behind the impact wall
free from debris and maintain intended function.
The temporary cut to be made in surface soil exposed on the existing easterly ascending slope
east of the proposed upper parking lot should be restored as soon as possible following wall
construction to minimize the risk of surficial soil movement. Restoration may be accomplished
by placement of structural fill in conformance with the recommendations presented in this
report.
15.0 PAVEMENT RECOMMENDATIONS
The proposed parking lot and access drive will either be constructed on undisturbed, dense
native soils, or on structural fill placed am] compacted on top of these suitable native soils.
Preparation of pavement sub grade areas ;hould follow the recommendations of the Site
Preparation and Structural Fill sections of this report. The proposed subgrade, whether it is
dense native soils or compacted structural fill, should have a minimum density of 95 percent
based on the ASTM:D 1557 test procedure within the upper foot below the pavement section.
Because much of the on-site soil encountered during exploration appeared to be above optimum
moisture content at the time of our exploration program, remedial sub grade preparation might
be required below the paving. Remedial preparation measures could include removal of some
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of the existing site soils below the planned pavement section and restoring the planned
subgrade elevation with select, imported structural fill, treating the native soil sub grade with
Portland cement to stabilize the wet soils, or aeration and drying of existing soils prior to
compaction of the road subgrades. We recommend that the final determination of how to
prepare the road subgrades be made at the time of construction when weather and field
conditions are known.
Where roadways are built near the crest of a slope, such as the western edge of the upper
parking lot, all fill beneath the roadway and within the roadway embankment should be
properly keyed into the suitable native soils and compacted to 95 percent of ASTM:D 1557, as
discussed in the previous section. Subsequent to compaction or recompaction, the subgrade
should be proof-rolled with a loaded dump truck. Any deflecting areas or soft spots detected
during proof-rolling should be excavated and replaced with properly compacted structural fill.
Upon completion of any recompaction and proof-rolling, a pavement section consisting of 2V2
inches of asphalt concrete pavement (ACP) underlain by 4 inches of 1 \4-inch crushed surfacing
base course is recommended for car parking areas. In driveway areas, a heavier section,
consisting of a minimum of 3 inches of ACP underlain by 6 inches of 1 \4-inch crushed rock
base course is recommended. The upper 1 inch of 1 \4-inch crushed rock can be replaced with
1 V2 inches of 5 Is-inch crushed rock as a leveling course, if desired. The crushed rock course
must be compacted to at least 95 percent of the maximum density.
All depths given are compacted depths, All paving materials, base course materials, and
placement procedures should comply with suitable standard specifications, such as the
Washington State Department of Transportation (WSDOT) Standard Specifications for Road,
Bridge, and Municipal Construction, or other suitable specifications.
All structural fill and all native subgrades less than 4 feet below fmished grade for a planned
roadway should be compacted to 95 percent of the modified Proctor maximum dry density, as
determined by ASTM:D 1557. Prior to structural fill placement or to placement of base
course materials over native subgrades, the area should be proof-rolled under the observation
of AESI with a loaded dump truck or other suitable equipment to identify any soft or yielding
areas. Any soft or yielding areas should be repaired prior to continuing work,
Depending on construction staging and desired performance, the crushed base course material
may be substituted with ATB beneath the final asphalt surfacing. The substitution of ATB
should be as follows: 4 inches of crushed rock can be substituted with 3 inches of A TB, and 6
inches of crushed rock may be substituted with 4 inches of ATB. ATB should be placed over a
suitable native or structural fill sub grade compacted to minimum 95 percent minimum density,
and a 1112-to 2-inch thickness of crushed rock to act as a working surface. If ATB is used for
construction access and staging areas, some rutting and disturbance of the A TB surface should
be expected, The general contractor should remove affected areas and replace them with
properly compacted ATB prior to final surfacing,
February 27, 2006 ASSOCIATED EARTH SCIENCES, INC.
MTlld -KE04520A2 -Projeclsl20040520lKEIWP Page 17
Kennydale cafe
Renton, Washington
Subsurface Exploration, Geologic Hazard, and
Preliminary Geotechnical Engineering Report
Preliminary Design Recommendations
16.0 PROJECT DESIGN AND CONSTRUCTION MONITORING
At the time of this report, site development plans, site grading plans, structural plans, and
construction methods have not been finalized and the recommendations presented herein are
preliminary. We are available to provide additional geotechnical consultation as the project
design develops and possibly changes from that upon which this report is based. We
recommend that AESI perform a geotechnical review of the plans prior to final design
completion. In this way, our earthwork and foundation recommendations may be properly
interpreted and implemented in the design.
We are also available to provide geotechnical engineering and monitoring services during
construction. The integrity of the foundations for buildings and of new pavement depends on
proper site preparation and construction procedures. In addition, engineering decisions may
have to be made in the field in the event that variations in subsurface conditions become
apparent. Construction monitoring services are not part of the current scope of work. If these
services are desired, please let us know and we will prepare a cost proposal.
We have enjoyed working with you on this study and are confident that these recommendations
will aid in the successful completion of your project. If you should have any questions or
require further assistance, please do not hesitate to call.
Sincerely,
ASSOCIATED EARTH SCIENCES, INC.
Kirkland, Washington
Maire Thornton, P.E.
Senior Project Engineer
Attachments: Figure 1:
Figure 2:
Appendix:
February 27, 2006
Vicinity Map
Site and Exploration Plan
Exploration Logs
MTlld -KE04520A2 -ProjectsI20040520IKEIWP
r
!
I EXPIRES 11/20/ or Q
Kurt D. Merriman, P.E.
Principal Engineer
ASSOCIATED EARTH SCIENCES, INC.
Page 18
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Sciences, Inc.
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VICINITY MAP
KENNYDALE CAFE
RENTON, WASHINGTON
, '" :'~~ ,
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FIGURE 1
DATE 2106
PROJ. NO, KE04520A
;:. ,/
,00 30'
-/
~" ~ ::
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Iros,,:., .
//1/7910/7
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~ SCALE: " = 30'
~ ~ Reference: Rick Anderson Architect, Floor Plan A1 #0205
-Dated 7-22-05
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10
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~ APPROXIMATE LOCATION
OF EXPLORATION PIT
TYP (09104)
"'-.
---
APPROXIMATE LOCATION
OF EXPLORATION BORING
TYP (02106)
~=================================================== t ASloclated Earth Sclencel, Inc.
~~ i ~ ~ [Ji ~
SITE AND EXPLORATION PLAN
KENNYDALE CAFE
RENTON, WASHINGTON
FIGURE 2
DATE 2106
PROJ. NO. KE04520A
APPENDIX
LOG OF EXPLORATION PIT NO. EP-1
This log is part of the report prepared by Associated Earth Sciences, Inc. (AESI) for the named project and should be
read tqgether with that report for complete interpretation. This summary applies only to the location of this trench at the
time of excavation. Subsurface conditions may change at this location with the passage of time. The data presented are
a simptfication of actual conditions encountered.
DESCRIPTION
Topsoil
Loose, dry 10 damp, dark brown, silty fine SAND, root hairs. 1 -
2 -
- - - - - - - - - - - - - - - - - - - --Pre FraserDeposlt - ---- - ---- - - - - - - - - - ---
Medium dense to dense, damp, light brown, SILT, consolidated, horizontal stratification.
3 -,-Dense-;-darrip,-gray,line-to coarse SAND wlth-gravefand-cobbies. horfzo-ntalstratificatlon.-- - - ---
4 -1
5 -
6
Bottom of exploration pit at depth 6 feet
No ground water/seepage. Slightly caving within sand. 7 -
8 -
9 -
10 -
11 -
12 -
13 -
14 -
15 -
16 -
17 -
18 -
19 -
~ 20
~--------------------------------------------------------------------------------------------,c
I
~
~
~
~
~
~
~
M
~ r
Logged by: MT
Approved by:
Pool Brothers-Lake Washington Boulevard-Renton
Renton, WA
Associated Earth Sciences, Inc.
~~~[J4~
Project No. KE04520A
September 2004
~---------------------------------------------------------------------------------------------
1 -
LOG OF EXPLORATION PIT NO. EP-2
This log is part of the report prepared by Associated Earth Sciences, Inc. (AESI) for the named project and should be
read together with that report for complete interpretation. This summary applies only to the location of this trench at the
time of excavation. Subsurface conditions may change at this location with the passage oftime. The data presented are
a simplfication of actual conditions encountered.
DESCRIPTION
Topsoil
Loose, dry to damp, dark brown, silty fine to medium SAND, root hairs.
2 -L ____________________________________________________ _
I Pre Fraser Deposit 3 --l
i
4 -Medium dense to dense, damp, light brown, SILTSTONE, horizontal stratification.
5 -
6 -
7 -
8
9 -
10 -
11 -
12
13
14
15 -
16 -
17
18 -
19 i
Bottom of exploration pit at depth 8 feet
No ground water/seepage. No caving.
8--~2~O-------------------N ____________________________________________________________ __
'"'
~
'" ~
~
M t;
Logged by: MT
Approved by:
Pool Brothers-Lake Washington Boulevard-Renton
Renton, WA
Associated Earth Sciences, Inc.
~~~~~
Project No. KE04520A
September 2004
~---------------------------------------------------------------------------------------
g
R
'" o
LOG OF EXPLORATION PIT NO. EP-3
This log is part of the report prepared by Associated Earth Sciences, Inc. (AESI) for the named project and should be
read togetner with that report for complete interpretation. This summary applies only to the location of this trench at the
time of excavation. Subsurface conditions may change at this location with the passage of time. The data presented are
a simplfication of actual conditions encountered,
DESCRIPTION
Topsoil
1 -Loose, dry to damp, dark brown, silty fine to medium SAND.
2 -
3 -------------------------------------------------------Pre Fraser Deposits" Weathered
4 -Medium dense, damp, light brown, fine sandy SILT, silty fine SAND, few root hairs.
5 -I--- - - - - - - - - - - - - - - --Pre-Fraser-Deposits --:: Unweathered-- - - - - - - - - - - - - - ---
6 -Dense, damp, light brown to light gray, SILTSTONE.
7 -
8 ~----------------------
9 -
10 -
11 -
12 -
13 -
14
15 --
16
17 -
18 -
19 -
Bottom of exploration pit at depth 8 feet
No ground water/seepage. No caving.
§ 20
~---------------------------------------------------------------------------------------
~ Pool Brothers-Lake Washington Boulevard-Renton
~ Renton, WA
~
~
Logged by: MT
Approved by:
Associated Earth Sciences, Inc.
~~~~~
Project No. KE04520A
September 2004
~ --------------------------------------------------------------
LOG OF EXPLORATION PIT NO. EP-4
--------------------------------------,--
This log is part of the report prepared by Associated Earth Sciences, Inc. (AESI) for the named project and should be
read together with that report for complete interpretation. This summary applies only to the location of this trench at the
time of excavation. Subsurface conditions may change at this location with the passage of time. The data presented are
a simplfication of actual conditions encountered.
DESCRIPTION
Topsoil
1 ,=-oS'~Ld...rYJQ. ,!a..r:np,_d~r!5 QrQ""n-,-~I!y .!i,,-eJ~fl2~!Y'!l§~f'!.~ !.oQ~h~i~,--______________ ...J
Pre Fraser Deposits
2 -
Medium dense to dense, damp, light brown to gray, SANDY GRAVEL with cobble, stratified. 3 -
4
5 -
6 -Sandier at 6'.
7 -
8
9 -
10 -
11 -
12 -
13 -
14 -
15 -
16 -
17 -
18 -
19 -
Dense, moist, light gray, fine sandy SILT.
Bottom of exploration pit at depth 8 feet
No ground water/seepage. No caving.
~~~o---------------------------a :---------------------------------------------------------------------------------------
"" ~
~
~
~
~
" ~
<l
M :=
Logged by: MT
Approved by:
Pool Brothers-Lake Washington Boulevard-Renton
Renton, WA
Project No. KE04520A
September 2004
Associated Earth Sciences, Inc.
~~~~~
~---------------------------------------------------------------------------------------
LOG OF EXPLORATION PIT NO. EP-5
r----,------------~ -------------------------,----0
This log is part of the report prepared by Associated Earth Sciences, Inc. (AESI) for the named project and should be
read together with that report for complete interpretation. This summary applies only to the location of this trench at the
time of excavation. Subsurface conditions may change at this location with the passage of time. The data presented are
a simplficatlon of actual conditions encountered.
DESCRIPTION
Topsoil
1 -Loose, dry to damp, dark brown, silty fine to medium SAND, roots.
2 -
r-----------------------------------------------------Pre Fraser Deposits· Weathered
3 -
Medium dense, damp, light gray, fine sandy SILT, few roots. 4 -
6 -~Dense, damp, light gray, SILTSTONE.
7 -
8 -
9 -
10 -
11 -
12 -
13 -
14 -
15 -
16 -
17 -
18 -
19 -
Bottom of exploration pit at depth 6 feet
No ground water/seepage. No caving.
r
§-~20r------------------------------------:---------------------------------------------------------------------------------------
M
~
Logged by: MT
Approved by:
Pool Brothers-Lake Washington Boulevard-Renton
Renton, WA
Associated Earth Sciences, Inc.
~~~[!j~
Project No. KE04520A
September 2004
~---------------------------------------------------------------------------------------
Associated Earth Sciences, Inc. Exploration Log
~ ~ n [!i 0 Project Number
I
Exploration Number
I
Sheet
KE04520A EB-1 1 of 1
Project Name Kennj'dale Cafe Ground Surface Elevation (ft)
Location Renton WA Datum i'JIA
Driller/Equipment CN Drillin~ Date StarUFinish 219106,219106
Hammer Weight/Drop 14Q# /30' Hole Diameler (in)
-
g ~ ~ = * w u-0 .-0 ",Ie .!1 '<=.0 Iii 1 Blows/Foot '" .<= 0. o.E --'w f-a s E i"» 5:E" ~ '" :;; .!!.Q '" T ro ClU) ~Ill .<= 0 U) 0 i5 DESCRIPTION t)
10 20 30 40
S-1 Topsoil/Disturbed Soil 3 ""~ Moist, dark brown to orange·brown, silty fine SAND, organic roots. 4
4
S-2 Moist to very moist, light orange-brown, fine to coarse SAND. 2 "". 3
3
l-S r-0La.!l9~ @i!1a1LofL $taiDing-.at~Q[It9._cL few_rOi)~. ______________
S-3 4 "" Pre-Fraser Deposit 4
Very moist to wet, olive-brown, fine to very fine SAND, trace silt 3
I S-4 Very moist to wet, olive-brown, very fine SAND with silt, horizontal 3
"'" stratification. 7
B
1-10 I S-5
Wet with depth, stratified horizontal lenses of orange oxidation. 4
"'" B
7
S-6
Wet, olive-brown to gray, fine to medium SAND to fine sandy SILT, 7
horizontal stratification. 13 29 ,.
15 Wet, olive, fine SAND with silt, horizontal light orange oxidation zones. S-7 23
33 66
33
S-8 Wet, olive-brown, SILT/fine SAND to wet, gray, medium to coarse SAND, :!. 23
slight orange oxidation. 32 7.
44
20 Wet, gray, medium to coarse SAND. 33 S-9 0/ 501 "
S-10 Wet. ara.v. fine to coarse SAND to wet olive-brown, SILT. 0/
501 "
Bottom of exploration boring at 23 feet
I-25
30
I
35
I
~ I • I
2
I • I
Sampler Type (ST);
rn 2" 00 Split Spoon Sampler (SPT) 0 No Recovery M -Moisture Logged by: MT
rn 3" 00 Split Spoon Sampler (D & M) Il Ring Sample '¥-Water Level () Approved by:
~ Grab Sample 0 Shelby Tube Sample.t: Water Level at time of drilling (ATD)
Associated Earth Sciences, Inc. Exploration Log
~ ~ ~ ~ ~ ----
Project Number
I
Exploration Number
I
Sheet
KE04520A EB-2 1 of 1
Project Name K!lnn~dale Cafe Ground Surface Elevation 1ft)
Location Renton WA ----Datum tIIllI
Driller/Equipment CN Drillin~ Date Start/Finish 219106,219106
Hammer WeighUDrop 140# 13Q' Hole Diameter (in)
----
c ~ = ~ g '" <>-0 ;; ., .-0 =~ .,!!1 Blows/Foot ~
~ 0. ~"" --'~ I-o.E ~-~ ~ 15. S E I!!,., 5:~ .!.Q ~ ~ T '" CJUl 0 gal 5 0 Ul DESCRIPTION u 10 20 30 40 0
~ Disturbed Soil 1 S-l Wet, olive-brown, silty fine SAND. 1 ""2
1
[ S-2
Wet. olive-brown, silty fine SAND. 2
""6 2
4
5 [ ---------------------------------
S-3
Pre-Fraser Deposit 6 1"11 Wet, olive-brown, silty fine SAND to fine SAND, faint horizontal 6
stratification. s
[ S-4
Wet, olive-brown, fine SAND, trace silt, faint horizontal stratification. 7
""34 I Very moist. gray, medium to coarse SAND. 13
21
10 [ Wet, olive-brown, fine SAND, trace silt, faint horizontal stratification.
5-5 •
"" 7 20
27 ,
15 [ Very moist, olive and gray, fine SAND/SIL T and coarse SAND, faint
5-6 16
"" 7 horizontal stratification, interbedded. 23
24
Gravelly at 17'.
'"
20
Bottom at exploration boring at 20.5 feet
25
30
35 I ,
,
,
,
,
~ I • 2 .
-Sampler Type (ST):
rn 2" 00 Split Spoon Sampler ISPT) 0 No Recovery M -Moisture logged by: MT
rn 3" 00 Split Spoon Sampler 10 & M) IJ Ring Sample '¥ Water Level 0 Approved by:
'~ Grab Sample [] Shelby Tube Sample.!. Water Level at time of drilling (A TO)