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GEOTECHNICAL ENGINEERING STUDY
9.4 ACRE SITE
WASHINGTON TECHNICAL CENTER
RENTON, WASHINGTON
E-884-11
FOR
HOLVICK deREGT ROERING
hL
r IJ
Geotechnical Engineering and Geology
August 21 , 1985 E-884-11
i
Holvick deRegt Koering
1000 SW 7th
Renton, Washington 98055
Attention: Mr. Loren Davis
References : Earth Consultants, Inc.
Report E-884 dated April 22 , 1981
I
Earth Consultants, Inc .
Report E-884-1 dated December 22, 1981 j
Gentlemen:
We are pleased to submit herewith our report entitled "Geotech-
• nical Engineering Study, 9.4 Acre Site, Washington Technical
Center, Renton, Washington. " This report presents the results of
our field exploration, laboratory tests, and engineering analysis .
The purpose and scope of our study was outlined in our proposal
dated June 25, 1985 . Previous Studies were conducted on and near
the subject site by Earth Consultants, Inc. Results of these
studies were reported in the referenced reports.
Our study indicates that in the proposed building area there
exists soft, compressible soils near the ground surface. To re-
duce potential foundation settlement, it is recommended th4t the i
conventional spread or continuous footings be founded on two feet I
of structural fill. The structural fill distributes the loads to
the underlying soil, thus reducing the effective bearing pres-
sures . Buildings constructed after primary settlements induced by
the structural fill have been realized may experience post-
construction settlements on the order of one to two inches .
Differential settlements between lightly loaded and heavily loaded
columns may be approximately one-half of these values . If these
settlements cannot be tolerated, we recommend that the building
area be surcharged. If these settlements can be tolerated, the
fills needed to prepare the site for construction should be
allowed to remain in-place until the settlements have stabilized.
This should take about three to five weeks. The following
• sections of this report describe our study and contain recommenda-
tions regarding foundation design criteria, earthwork
considerations, and site drainage .
1805 - 136th Place N.E.. Suite 101, Bellevue. Washington 98005
Phone: r2061 643-3780/Seattle (206) 464-1584
Holvick deRegt Koering E-884-11
August 21 , 1985 Page 2
This report has been prepared for specific application to this
project in accordance with generally accepted geotechnical
engineering practices for the exclusive use of Holvick deRegt
Koering and their representatives. No other warranty, expressed
or implied, is made. We recommend that this report, in its
entirety, be included in the project contract documents for the
information of the contractor.
PROJECT DESCRIPTION
At the time our study was performed, the site and proposed
building locations were as shown schematically on the Boring and
Probe Location Plan, Plate 2.
Based on our discussions with your architect, we understand
that it is planned to construct four, single-story, concrete
tilt-up office buildings with design floor loads of one hundred
fifty ( 150 ) pounds per square foot (psf) . Building No. 4 is
proposed on Lot No. 3 and Buildinq Numbers 5, 6 and 7 are proposed
on Lot No. 4 . We understand that maximum column loads are
approximately 40 kips . It is anticipated that approximately three
feet of structural fill will be required to achieve final proposed
grades .
If any of the above design criteria change, we should be
consulted to review the recommendations contained in this report.
In any case, it is recommended that Earth Consultants, Inc.
provide a general review of the final design.
SITE CONDITIONS
Surface
The proposed 9. 4 acre building site is located on Powell
Avenue SW and just north of SW 7th Street in Renton, Washington.
The property is adjacent to an existing structure and railroad
tracks on the south, to Powell Avenue SW on the west, and to
vacant property on the north and the east. The site is relatively
flat except for an existing fill approximately five feet high on
the western portion of Lot No. 3 . At the time of our exploration,
the site was covered with tall grass and brush with trees on the
northern portion of the property. Surficial soils were generally
dry and stable.
Subsurface
The site was explored by drilling two test borings and
advancing three Dutch Cone probes. Other locations were explored
during our referenced studies on or near the subject site.
Exploration locations are shown on Plate 2 . Please refer to the
Earth Consultants, Inc.
Holvick deRegt Koering E-884-11
August 21 , 1985 Page 3
boring logs, Plates 4 and 5, and the Dutch Cone logs, Plates 7
through 9, for a detailed description of the conditions
encountered at each location explored. A description of the field
exploration methods and laboratory testing program is included in
this report following the Discussion and Recommendations section.
The following is a generalized description of the subsurface
conditions encountered.
Our borings and probes generally encountered soft, moderately
compressible clayey silts underlain by medium dense to dense
gravels . Boring B-101 and Probe P-103 encountered approximately
twenty (20) feet of soft, compressible soils beneath the existing
ground surf ace. Approximately thirteen (13 ) feet of soft soils
were encountered in Boring B-102. Probes P-101 and P-102
encountered approximately ten feet ( 10 ) of soft, compressible
soils. Clayey silts encountered generally exhibit low plasticity
with Liquid Limits ranging from 35 to 40 and Plastic Indexes
ranging from 7 to 9 . A moderately plastic clayey silt was
encountered in Boring B-101 . This silt has a Liquid Limit of 50
and a Plastic Index of 17 .
Sandy gravels were generally encountered beneath the
compressible clayey silt stratum. Gravels are medium dense and
grade to dense with depth. Gravels were encountered to the
maximum depth explored at each location.
Groundwater
The groundwater levels observed while drilling are shown on
the boring logs. Since the groundwater levels did not have time
to stabilize, slotted pipe standpipes were installed in Borings
B-101 and B-102. Readings taken eleven ( 11 ) days after the
completion of the borings are also shown on the boring logs.
Groundwater was encountered at eight to ten feet beneath the
existing grade. The groundwater seepage level is not static, thus
one may expect fluctuations in the level depending on the amount
of rainfall, surface water runoff, and other factors. Generally
the water level is higher in the wetter winter months.
DISCUSSION AND RECOMMENDATIONS
General
As previously described, the ground surface is underlain by
soft, compressible clayey silts above gravels. The thickness of
the compressible soil stratum encountered varies from
approximately ten feet at the locations of Probes P-101 and P-102
(Buildings 5 and 6) to approximately twenty ( 20 ) feet at the
locations of Boring B-101 and Probe P-103 (Building 4 ) . To
Earth Consultants, Inc.
Holvick deRegt Koering E-994-11
August 21 , 1985 Page 4
provide adequate support , buildings may be supported on
conventional individual and continuous spread footings bearing on
at least two feet of structural fill . Building slabs and pavement
sections may be supported on at least one foot of structural.
We understand that approximately three feet of structural fill
will be required to achieve proposed finished grades . We
anticipate that this fill will induce settlements on the order of
three to five inches, the higher values achieved at the greater
depths of soft soils. Buildings constructed after primary
settlements induced by the structural fill have been realized may
experience post-construction settlements on the order of one to
two inches. Based on the soil profile encountered in Probes P-101
and P-102 (Buildings 5 and 6) , approximately one inch of total
post-construction settlement would be anticipated. Buildings
constructed in areas where the soft , compressible stratum is'
thicker, such as that encountered in Boring B-101 , B-102 and P-103
(Buildings 4 and 7 ) , may experience post-construction settlements,
on the order of two inches. Differential settlements between
lightly loaded and heavily loaded columns may be approximately
one-half of these values. If these settlements cannot be
tolerated, we recommend that the building area be surcharged. If
a surcharge fill is not used, we recommend that the structural
fill be placed as early in the construction schedule as possible,
to induce anticipated settlements prior to building construction.
We recommend that settlement markers be placed during the
placement of structural and surcharge fills and during the pre-
loading period. Building construction may proceed when
anticipated settlements have stabilized.
Foundations
The proposed structure may be supported on conventional conti-
nuous and spread footings bearing on at least two feet of
structural fill. Overexcavation of soil below the footing may be
required depending on final site grades. Fill placed under
footings should extend outwards from the edge of the footings at
least a distance equal to the depth of the structural fill.
Exterior footings should be bottomed at a minimum depth of twelve
( 12 ) inches below the lowest adjacent outside finish grade.
Interior footings may be at a depth of twelve (12) inches below
the top of the slab. Footings bearing on at least two feet of
structural fill may be designed for a bearing pressure of two
thousand (2000) psf. Continuous and individual spread footings
should have minimum widths of twelve (12 ) and eighteen (18 )
inches, respectively. A one-third increase in the above bearing
pressures may he used when considering short term wind or seismic
loads.
Earth Consultants. Inc.
Holvick deRegt Koering E-884-11
August 21 , 1985 Page 5
Lateral loads due to wind or seismic forces may be resisted by
friction between the foundations and the supporting compacted fill
subgrade or by passive earth pressure on the foundations . For the
latter, the foundations must be backfilled with a compacted fill
meeting the requirements of structural fill . A coefficient of
friction of 0 .35 may be used between the structural foundation
concrete and the supporting subgrade . The passive resistance of
well compacted fill may be taken as equal to the pressure of a
fluid having a density of three hundred (300 ) pounds per cubic
foot (pcf ) .
We recommend that drains be placed around all perimeter foot-
ings. The drains should be constructed with a four inch diameter
perforated pipe bedded and covered with free draining gravel. The
drains should have a positive gradient towards suitable discharge
facilities . The footing drainage system should not be tied into
the roof drainage system until the drains are tightlined well away
from the building. The footing excavation should be backfilled
with granular soil except for the top foot which should be
backfilled with a relatively impermeable soil such as silt, clay
or topsoil. Alternatively, the surface can be sealed with asphalt
or concrete pavements .
• Slab-on-Grade Floors
Slab-on-grade floors may be supported on at least one foot of
structural fill . At the time of our exploration, surficial soils
were generally dry and stable. If construction is conducted
during wet weather, a greater thickness of fill and/or a
stabilization fabric may be necessary. The slab should be
provided with a minimum of four inches of free draining sand or
-gravel. We also recommend that a vapor barrier such as a 6 mil
plastic membrane be placed beneath the slab to reduce water vapor
transmission through the slab and the resultant moisture
accumulation. Two inches , of sand may be placed over the membrane
for protection during construction and to aid in curing of the
concrete.
Surcharge Program
As indicated earlier in this report, if the anticipated
settlements cannot be tolerated, we recommend that the building
area be surcharged with a minimum of three feet of fill . This
surcharge is in addition to any structural fill materials required
to achieve design finish grades . The top of the surcharge fill
should extend at least five feet beyond the edges of the proposed
building. We estimate that the surcharge fill will need to remain
in place approximately three to five weeks to permit primary
settlements to be completed, after which, building construction
may be started.
Earth Consultants. Inc.
Holvick deRegt Koering E-884-11
August 21, 1985 Page 6
Before placing the surcharge fill, structural fill should be
placed, if necessary, to the design finish grade. Depending on
site grades , it may be necessary to excavate soil to provide the
required thickness of structural fill below footings and slabs.
Alternately the footing excavation can be done after removal of
the surcharge fill.
The surcharge fill does not have to meet any specific require-
ments except that it should have a minimum in-place total density
of one hundred twenty ( 120 ) pcf . However, if the surcharge fill
is to be later used as fill on another part of the site, we
recommend it meet the requirements for structural fill, i.e. ,
contain no organics and be compactible. Structural fill to be
placed in wet weather should contain no more than 5 percent fines
passing the No. 200 sieve. The side slopes of the surcharge fill
should be inclined no steeper than 1 : 1 (Horizontal:Vertical ) . No
fill for landscaping purposes should be placed near the building
since any additional fill could induce further settlement .
Prior to placement of the surcharge fill, we recommend
installation of at least three settlement markers per building
• within the pre-load area. These markers should be protected from
disturbance by construction equipment . The markers should be
surveyed by Earth Consultants, Inc. personnel or a licensed
surveyor during fill and surcharge placement and at intervals of
2, 4 , 8, 16 (and so forth) days after completion of the surcharge
fill placement . The initial reading should show the natural
ground elevation, and readings taken during surcharge placement
should show the surcharge fill thickness .
We will evaluate the settlement readings. Once the required
settlement has been reached, the surcharge may be removed. The
exposed subgrade should be proofrolled, and any loose pockets
exposed should be overexcavated and replaced by structural fill .
Site Drainage
Groundwater was encountered in our borings at depths ranging
from eight to ten feet. It is not anticipated that groundwater
will be encountered during construction. However, it has been our
experience that groundwater levels change significantly due to
changes . in rainfall amounts , surface drainage or other factors .
If seepage is encountered in the excavation, the water should be
drained away from the site by use of drainage ditches, perforated
pipe or French drains, or by pumping from sumps interconnected by
shallow connector trenches at the bottom of the excavation.
The site should be graded so that surface water is directed
off the site and away from the tops of slopes . water should not
be allowed to stand in any area where buildings, slabs, or
Earth Consultants, Inc.
Holvick deRegt Koering E-884-11
August 21 , 1985 Page 7
pavements are to be constructed. During construction, loose
surfaces should be sealed at night by compacting the surface soils
to reduce the infiltration of rain into the soils . Final site
grades should allow for drainage away from the building founda-
tions . We suggest that the ground be sloped 3 percent for a
distance of at least ten feet away from the buildings except in
areas that are to be paved.
Pavement Areas
All parking and roadway areas may be supported on a minimum of
twelve (12) inches of structural fill placed in accordance with
the Site Preparation section of this report . At the time of our
exploration, surficial soils were generally dry and stable. If
construction is conducted during wet weather, a greater thickness
of structural fill or a stabilization fabric may be needed to
stabilize soft, wet or unstable areas . The upper twelve (12)
inches of pavement subgrade should be compacted to at least 95
percent of the maximum density . Below this level a compactive
effort of 90 percent would be adequate. The pavement section for
lightly loaded traffic and parking areas should consist of two
' inches of asphalt concrete (AC) over four inches of crushed rock
base (CRB ) or three inches of asphalt treated base (ATtB ) . Heavier
loaded areas would require thicker sections. We will be pleased
to assist you in developing appropriate pavement sections or
specifications for heavy traffic zones, if needed.
Site Preparation and General Earthwork
To maintain the integrity of the surface soils, stripping of
the • sod should be avoided where possible. Buildings and pavement
areas should be cleared of any surface debris and any other
deleterious matter, such as trees , brush, fences, etc. The grass
cover should be mowed •and hauled off the site. Fills may be
placed directly on the sod cover in areas where fills are at least
two feet deep.
Structural fill under floor slabs and footings should be
placed in horizontal lifts and compacted to a minimum 95 percent
of the maximum dry density in accordance with ASTM Test Designa-
tion D-1557-70 (Modified Proctor) . The fill materials should be
placed at or near the optimum moisture content. Fill under
pavements and walks should also be placed in horizontal lifts and
compacted to 90 percent of maximum density except for the top
twelve (12) inches which should be compacted to 95 percent of
. maximum density .
We understand that imported structural fill will be required
for site preparation. Ideally, structural fill to be placed in
wet weather should consist of a granular material with a maximum
Earth Consultants, Inc.
Holvick deRegt Koering E-884-11
August 21 , 1985 Page 8
size of three inches and no more than 5 percent fines passing the
No. 200 sieve. During dry weather, any compactible non-organic
soil can be used as structural fill.
FIELD EXPLORATION AND LABORATORY TESTING
Our field exploration was performed on July 11, 1985 .
Subsurface conditions at the site were explored by drilling two
borings and advancing three Dutch Cone probes to a maximum depth
of twenty nine (29) feet below the existing grade . The borings
were drilled by Drilling Unlimited using a truck-mounted drill
rig. Continuous flight, hollow stem augers were used to advance
and support the boreholes during sampling. The Dutch Cone is
equipped with a friction sleeve which allows the shaft resistance
to be measured in addition to the point resistance at the top of
the probe . Approximate soil classifications can be inferred : by
comparing the point resistance to the friction on the sleeve. A
direct correlation is obtained between the point resistance and
the bearing capacity of the soil. Soil samples are not obtained
from the Dutch Cone probes . The locations of the borings and
probes were approximately determined by tape measurements from
approximate property corners . Elevations of borings and probes
were approximately determined by a hand level from an arbitrary
elevation datum. The locations and elevations of the borings and
probes should be considered accurate only to the degree implied by
the method used. These locations are shown on the Boring and
Probe Location Plan, Plate 2.
The field exploration was continuously monitored by a
= geotechnical engineer from our firm who classified the soils
encountered and maintained a log of each boring, obtained
representative samples, measured groundwater levels, recorded
probe readings and observed pertinent site features . Slotted
standpipes were installed in Borings B-101 and B-102 to monitor
groundwater levels. All samples were visually classified in
accordance with the Unified Soil Classification System which is
presented on Plate 3 , Legend. Logs of the borings are presented
on Plates 4 and 5. The final logs represent our interpretations
of the field logs and the results of the laboratory examination
and tests of field samples. The stratification lines on the logs
represent the approximate boundary between soil types . In
actuality, the transition may be gradual. Logs of the Dutch Cone
probes are presented on Plates 7 through 9 . The "friction ratio"
shown on the plates is the unit resistance of the friction sleeve
expressed as a percentage of the unit point resistance . The soil
stratigraphy interpreted from the probes indicates fine scale
stratification not always obtained from borings .
Earth Consultants, Inc.
Holvick deRegt Koering E-884-11
August 21 , 1985 Page 9
In each boring, Standard Penetration Tests (SPT) were per-
formed at selected intervals in accordance with ASTM Test Designa-
tion D-1586. A Shelby tube sampler was used to obtain less
disturbed soil samples at selected depths. In addition, the split
spoon samples were driven with a one hundred forty ( 140 ) pound
hammer falling thirty (30) inches.
Shear strengths of undisturbed soils were measured where prac-
tical in the field with a torvane. These results are recorded on
the boring logs at the appropriate sample depth.
Representative soil samples were placed in closed containers
and returned to our laboratory for further examination and test-
ing. Visual classifications were supplemented by index tests such
as Atterberg Limits on representative samples . Moisture determina-
tions were performed on all samples. Results of moisture
determinations , together with classifications , are shown on the
boring logs included in this report.
A consolidation test was conducted on a relatively undisturbed
representative sample taken with a Shelby tube sampler to evaluate
the consolidation characteristics of the site soils. In addition,
the time readings were taken at several points of loading to
evaluate the time rate of settlement . The results of this test
are shown on Plate 6, Consolidation Test Data.
LIMITATIONS
Our recommendations and conclusions are based on the site
materials observed, selective laboratory testing and engineering
analyses. The conclusions and recommendations are professional
opinions derived in accordance with current standards of practice .
No warranty is expressed or implied.
The recommendations submitted in this report are based upon
the data obtained from the borings and probes. Soil and ground-
water conditions between exploration locations may vary from those
encountered by the borings and probes. The nature and extent of
variations between exploration locations may not become evident
until construction. If variations then appear, Earth Consultants,
Inc. should be allowed to reevaluate the recommendations of this
report prior to proceeding with the construction.
Additional Services
It is recommended that Earth Consultants, Inc . provide a
general review of the final design and specifications to verify
that the earthwork and foundation recommendations have been
properly interpreted and implemented in the design and in the con-
struction specifications .
Earth Consultants. Inc.
Holvick deRegt Koering E-884-11
August 21, 1985 Page 10
It is also recommended that Earth Consultants , Inc. be
retained to provide geotechnical services during construction.
This is to observe compliance with the design concepts, specifica-
tions or recommendations and to allow design changes in the event
ssubsurface conditions differ from those anticipated prior to the
start of construction.
The following plates are attached and complete this report :
Plate 1 Vicinity Map
Plate 2 Boring and Probe Location Plan
Plate 3 Legend
Plates 4 and 5 Boring Logs
Plate 6 Consolidation Test Data
Plates 7 through 9 Dutch Cone Probe Logs
Plates 10 through 15 Exploration Logs from
Referenced Report
Respectfully submitted,
'•. ��s EARTH CONSULTANTS , INC.
le' r • '1'
• . . ; y f J IC
James R. Finley, Jr. , P. E.
G Chief Engineer
JWJ/JRF/tm f .�
Earth Consultants. Inc.
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Reference
Pierce County / Map 34
By Thomas Brothers Maps
Date 1983
Vicinity Map
! Washington Technical Center
Earth Renton, Washington
Consultants Inc. _
GEOTECHNICAL ENGINEERING & GEOLOGY Proj. No. 884-I I Date July 187 Plate I
I
1
7 e B-9
P-1O2 t P'101 tiparonmote scar
0 50 ID-) 20-M.
l Lot 4 B-1O2 LFGCnD
eB-e t - - - - ^ !r B-101 Approximate Boring
N , Local ion
t �
Lot 3 I --� L P IOi Probe
L o+2 Dutch Cone
HT ',P 4 Probe Location
P-3 tom----
W 4 P•1O3 Pro erty Previous Bering frtrr, EC.I.
I Report Doted 12/22/61
B 101 t , Previous Boring from E.C.I.
Repo-1 Doted 4/9/79
......._ ............................................ Previ;,Jc Dutch Cone Probe
• , , from E C.1 Repot Dated
Fuhre ROW 12/22/81
I l ; ✓ ®8-102 Proposed Building
i...........—_:- , ,
8-1O1 ' ;
,...............
,
1 Existin Building
I 1 g 9
Refert�ce:
S.W. 7th STREET sire Pion
By The Moehlurn Group Architects
Doted 5/27/e5
Earth :'� I !.
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Consultants Inc.- � 1
G,OU CHNICAL [N..Nrf oiN6 [ G[OlOor
Boring and Probe Location Plan
Washington Technical Center
Renton, Woshington
P.oj Nu 88411 Dols Judy -BS Ptak 2
MAJOR DIVISIONS GRAPH LETTER TYPICAL DESCRIPTION
SYMBOL SYMBOL
°'77 GW weii-Graaea Gravels.Gravel-Sand
Gravel ; " ° •.° g`N
Mixtures. Little Or Na fines
And Clean Gravels
Gravelly (little or no fires) • •. GP Poorly-Graded Gravels.Gravel-
Coarse Sails ♦ gP Sand Mixtures, Little Or No Fines
Grained
Solis More Than GM Silty Gravels.Gravel-Sand-
50% Coarse Gravels With gm Silt Mixtures
Fraction Fines(appreciable
Retained On amount of fines! GC Clayey Graveis.Gravel-Sand-
No- 4 Sieve gC Clay Mixtures
SW Well-Graded Sands. Gravelly
Sand °°°°° o,1 Sw Sands. Little Or No Fines
And Clean Sand
Sandy (little or no fines) SP Poorly
More Than Graded Sands. Gravelly
50`° Material SoiiS S� Sands. Little Or No Fines
Larger Than More Than SM
No. 200 Sieve Silty Sands. Sand- Silt Mixtures
50% Coarse
Size Sands With ST
Fraction Fines iappreciaole
Passing No 4 amount of fines: SC
Sieve Sc Clayey Sands. Sand•Clay Mixtures
ML Inorganic Silts d Very Fine Sands.Rocx Flour.Sdty-
- I ( nil Clayey Fine Sands.Clayey Silts w/ Slight Plasticity
Fine Slits Liquid Limit CL Inorganic Clays Of Low To Medium Plasticity.
Grained And Less Than 50 CI Gravelly Clays, Sandy Clays, Silty Clays. Lean
Sods Clays
Organic Silts And Organic
III i t7p
L O) Silty Clays Of Low Plasticity
HInorganic Slits. Micaceous Or Diatomaceous Fine
More Than mh Sand Or Silty Sods
50a Material Silts Liquid LimitSmaller Than H norganc Clays Of High
No. 200 Sieve Ana Greater Than 50 ChPlasticity. Fat Clays
ClaysSize
H Organic Clays Of Medium To High
Oh Plasticity. Organic Silts
_ , T Peat. Humus, Swamp Sods
Hignly Organic Sods pt With High Organic Contents
Topsoil -. Humus And Duff Layer
(A� k Fill Hignly Variable Constituents
r`
Y
The Discussion In The Text 01 --is deport Is Necessary For A Proper Understanding
Of Tne Nature Of 7.,e Material Presented In The Attached Logs
Notes:
Dual symbols are used to indicate borderline soil classification.Upper
case letter symbols designate sample classifications based upon lab-
oratory testing; lower case letter symbols designate classifications not
verified by laboratory testing.
I 2-O.D. SPLIT SPOON SAMPLER C TORVANE READING. tsf
2.4-I.D. RING SAMPLER OR qu PENETROMETER READING,tsf
SHELBY TUBE SAMPLER
P SAMPLER PUSHED W MOISTURE. percent of dry weight
SAMPLE NOT RECOVERED pcf DRY DENSITY.pounds per cubic ft.
Q WATER LEVEL (DATE) LL LIQUID LIMIT,percent
WATER OBSERVATION WELL PI PLASTIC INDEX
LEGEND
Earth i
,. II
r
cons ltanu Inc.
GEOTECHNICAL ENGINEERING 9c GEOLOGY Proj. No.334-ll Date July`85 Plate 3
BORING NO. 101
Logged By JWJ
Date 7-11-85 ELEV.
us (N)
Graph CS Soil Description D filth Sample Blows M
Ft.
silty GRAVEL mixed with toposoil, dry,
VT
MH brown rusty clayey SILT, moist to wet, 7 41 LL = 50
soft — PI = 17
5 24"push 40
LL = 40
I ML brown clayey SILT, wet, very soft PI 9
fI Q 1/18" 40 C 1
� tsf
�!i grades to
7-22-
;ICI! gray, with thin sand lenses 10
i 2 48 c .1tsf
with thin sand layer at 13'
3 41
i
15
becoming soft with thin organic silt 3 59 c .15
lenses tsf
with thin sand layer at 19' 20
sp gray gravelly SAND, coarse grained, 26 24
meidum dense
25
with sandy GRAVEL layers, dense
34 20
Boring terminated at 29' beneath existing grade. Groundwater observation
well installed to bottom of boring. Bottom 10' slotted. Boring backfilled
with drill cuttings.
* DATUM: Slab grade - existng building to south
BORING LOG
WASHINGTON TECHNICAL CENTER
Earth
RENTON, WASHINGTON
�
Consultants Inc.
GEOTECHNICAL ENGINEERING & GEOLOGY Proj. No. 884-11 Date July '85 Plate 4
BORING NO. 102
Logged By JWJ L
Date 7-11-85us ELEV.
(N)
Graph CS Soil Description Depth Sample Blows M
Ft.
I I ml brown sandy SILT, dry,loose
;! ICI grayish rusty clayey SILT, moist, very _
l l ML soft 3 35 c
LL �1 3t�f
i I
becoming wet and brown mottled PI = 7
5 2 37
color to gray and becoming medium stiff c '3tsi
II 4" push 39 c =•25tsf
ji19
LL = 38
j DI
10 2 40 = 8
-22-8 5
l;l�ll
.�. •�. . 12 48
:• :• gp gray sandy GRAVEL with silt lenses, 15
�4�' ' medium dense to dense
4 . :� . .�
28 20
♦ , 20
�� layered with sand, medium dense
19 14
• dense
.25
33 20
Boring terminated at 29' below existing grade. Groundwater observation
well installed to bottom of boring. Bottom 10' slotted. Boring backfilled
with drill cuttings.
BORING LOG
WASHINGTON TECHNICAL CENTER
Earth RENTON, WASHINGTON
Consultants Inc.
GEOTECHNICAL ENGINEERING & GEOLOGY rProj. No. 884-11 Date July '85 ?late 5
0
(
5
U
CL
Z 10
0
a.
� I
O `
U I
15
I
20
.062 .125 .25 .5 1.0 2.0 4.0 8.0
2.6
cTa 2..4
v� 2.3 ( �
2.2
2.1
2.0
PRESSURE , tsf
Liquid Plastic PlasticityMoisture Dry
Key Boring Depth USCS Soil Description Limit Limit Index Content, W a Density
y No. (ft.) (pc'.)
io % % Before After
O B-101 6.0 ML SILT 40 31 9 40.1 33.2 80.6
. CONSOLIDATION TEST DATA
�� WASHINGTON TECHNICAL CENTER
Earth I 1 I i !�II RENTON, WASHINGTON
I
Consultants Inc.
GEOTECHNICAL ENGINEERING & GEOLOGY Proj. No-884-11 Date July '85 Plate 6
Dutch Cone Log P-1 Q 1
Cone Penetration Reswance Friction Death
-Ton/Sq. Ft.- Ratio Meters ELEV. _ 0±
1 t s to 20 so !CC zoo 30C 400 4 e Iz I Soil Interpretation
! clayey SILT, soft to medium
1 stiff
In;i 16
Z
I I I� IIIII I I
I I I I
3 to
IIII l
IiILI
l
gP sandy GRAVEL with silt lenses,
4 meidum dense to dense
I ! Ilil I I I S
I I Ill I I I I I I
I I I i t
e
! 1 ill l �illlll I ZO
I I III' I I ii �
I 1 1 IIII I 11 I l i
I l i l i l I I I lii,. I I I
IIII 't 7
• i i Probe terminated at 23' beneath
I
existing grade. Total system
s refusal.
I I I I I I I I IIII I i ! III I
i I I l u I� gill
9-
1 1
11 1 30
IJJM
II I I III
I I I I Ili I 1 1
10
! 'I I II I uil I
I 35
11101 II
I I I lily I I I I I
I 1 I I I I I
12
40
I I I I I I •n I I
I I I IIII Ii I I
I I II III,, I I
IIII II i I I I
Ii I
u I I
1 1 1 1 Uhl 14
I I III I I ' I
I II I
I
I
IS
I I I I ( IIII IIII t l 1 1 1
DUTCH CONE LOG
! WASHINGTON TECHNICAL CENTER
Earth RENTON, WASHINGTON
Consultants Inc. p
GEOTECHNICAL ENGINEERING & GEOLOGY Proj. No. 884-11 Date July :8:511ate 7
Dutch Cone Log P-102
Cone Penetration Resistance Fr ction Death
-Ton/Sq. Ft.- Ratio Meters Feet ELEV. _ -1±
I 2 s 10 20 50 10o 200 xo-CC • e 12 Soil Interprelotion
I II ! I II 11'Ili
I III i !ii�l,: I
T:II' 1 ml clayey SILT, soft, low plasticit
f with clayey or organic layer at
I I ;III I !I 1
3 6'
:u
2
II'll sand layer, very loose, from 7
to 9'
�
9
I iII 11 ni � I
1 IIII t I• l l 4
gp sandy GRAVELS, medium dense to
dense
iII It
ML
II
I I1.., e 20 Probe terminated at 18` beneath
IIlil Ili ' existing grade. Total system
i I I II1 I I l i
refusal.
8
I I I I ijlli - 1
I I I '.III I•I I l l
! ! I I 1 I I
9 30
I i u I I I I I
I 1 Ili I I I I I
I I I I I I I I illll I ! f
10
I I t l ;II I I I
I I 11 i n: I I I
35
I I IIIT-
MH 12
III l i 40
I I I I I I l i l l l l
I I Wit
t !
. I I
I I hilllilt
II 1 ! ! !
! II 45
14
{ I 1 I I
15
I I I
I I 11 I
1 ! I
I II I I IIII I I I I SO
. DUTCH CONE LOG
WASHINGTON TECHNICAL CENTER
Earth RENTON, WASHINGTON
Consultants Inc.
r/V
GEOTECHNICAL ENGINEERING 11 GEOLOGY Prof. No.884-11 Date July 185 1 Plate 8
Dutch Cane Log P-1 03
Cone Penetration Resistonce Frirlan ELEV. -1±
De th
-Ton/Sq. Ft.- Ratio Meters Feet
1 z s w 20 50 Ioc 210 roc•oo . a a Soil Interpretation
I l i I
1 sm clayey SILT, soft, layered with
s ml sandy silt and silty sand, very
41' 1 1 "' loose
III
2
I I I ! 1 1 1 .,I
possible organic layer at 6'
I I I Ilu I
3
to
I i ,
I ! I I
4
1 1 ili I I I
I IIII ! r
�ji, I gp sandy GRAVEL, medium dense to
I I IIII I ,
dense
I I 7
„' ; Probe terminated at 22' beneath
• II
existing grade. Total system
refusal.
e
•i I I 11 ��1'� l i I
I I I I Will I I I
I I ! I III! I I I ; 1 9
I III III I 30
I I I I
I 1 1 i!I I I I
10 Wll
i I III I I I I I
I I Mill
I I nl I ! I
- I I ill Ilni I i l l
I Ir, I I
I I I I�I Iltii I I I � I
I I III III!II ! I I IZ
I I III IIi11 I I I I
I I I I I1"I I 1
I I II I I Will iI I 1
1 I'II I I I I
I I Ills l 45
I uii I 14
I I I ( I (IIII I I
I III I, I I
I III I I I I
! !I I 15
46 DUTCH CONE LOG
! WASHINGTON TECHNICAL CENTER
Earth RENTON, WASHINGTON
Consultants Inc.
GEOTECHNICAL ENGINEERING & GEOLOGY Proj. No.884-11 Date July:8:5
Plate 9
BORING NO. 9
ELEVATION
Graph US Soil Description Depth Sample Blows/ Wn Dennsity
ry
CS (ft. ) Ft. gyp) �pcf)
IIII 6 40
2 41
I ML Brown, clayey SILT to silty CLAY
with some organics, wet, very soft 5
li CL to medium stiff. 1 43
�I
7 36
83
'Ili i qu = 1 tsr"
l� 10
itLL = 42
3 39 PI = 16
! 82
15
4 97
organic SILT layer at 18 feet
/ "20
29/7
35 16
GP Blue, sandy GRAVEL to gravelly SAND
SP with 2 inch layers of -silty SAND, wet, 25
dense to very dense.
60 9
�. . . 50/0"
Boring terminated at 32 feet on 3/15/79.
Water observation well installed.
•
Driving Energy: 140 lb. Weight Droppina 30 inches PLATE 11
W. 0. No. E-884 Earth Consultants
BORING NO. 8
ELEVATION
N Dry
Graph US Soil Description Depth Sample Blows/ Wn Density
CS (ft. ) Ft. (Pcf)
it ... 6 40
Mottled gray to brown and blue, inter-
IL bedded clayey SILT, SILT and silt 5
SM Y Y Y 11 27
SAND, wet, medium stiff to loose.
<f � l LL = 36
5 40 PI = 9
80
?aa�Iil 0 7 45
,I I
III
:ail l 10 41)
SM Blue-green becoming blue, slightly
Sp silty SAND grading to sandy GRAVEL,
.:4: GP dense becoming very dense. 47 8
20
.. .. .f . 50/611 7
.. . ..
Boring terminated at 23.5 feet on 3/14/79.
No distinct groundwa-ter elevation noted.
•
Driving Energy: 140 lb. Weight Droppina 30 inches PLATE to
W. 0. No. E-884 Earth Contnitants
BORING NO. 101
Logged By CRL 16±
Data 11/17/81 ELEV.
(N)
Graph CS Soil Description Delp Sample Slow$ t%)
Ft
SM Brown silty fine SAND, wet, loose
I
2 43 qu<0.5 ter
5 LL=45,PI=6
j) 2 59 qu=0.5 is
!f� s
13/1 8 --
1
Brown-gray mottled clayey SILT, wet,
1� qu=0.5 is ,
j ML soft to medium stiff 7 49 72 pcf,
(grades gray below 15' ) tv=0.27ts
ii (with silty sand layer at 11') I 3 42 qu=0.5 tsf
I' 15 5 44 75 pcf'
,III,
i q� 0:5 is
I tv=0.12ts
5 46 LL=38,P1=8
(grades with thin beds of organic silt 20 qu=O.S is
below 20' )
IIIII,I I 5 48 qu=0.75ts
1.0 is
25
a*�
Get `Gray sandy GRAVEL with silt, wet, dense I 41 7
GP 30
47 9
Boring terminated at 3 below existing gra e. Groundwater
observation well installed to bottom of boring.
BORING LOG
SPRINGBROOK TECHNICAL CENTER
Earth RENTON, WASHINGTON
C NU-U1tanU Inc.
GEOTECHNICAL ENGINEERING Q GEOLOGY Prof. No.884-1 Date Dec. '81 Plie 12
BORING NO.
Logged By CRL 19+
Date 11/20/81 ELEV.
(N)
Graph CS Soil Description Depth Sample Blows M
Ft.
ML Brown sandy SILT with clay, wet, loose
2 45
qu=0.5 tsf
5
5 65 q =0.5 is
tv=0.1 ts "
MH Brown gray mottled clayey SILT, wet, 1 6 50 72 pc',
ML soft to medium stiff, with loose silty q =0.5 is
'ii( : , sand layers at 3, 6, 13, and 18' 10 tk.224:51
f i i I I 8 44 75 pcf
(grades gray below 12' ) q =0.5 to
I
u0.75 tsi
� 8 35
jl �� i tv=0.15ts
�II� 15 qu=0.75ts
i, ;i
q =0.75tsf
OH Brown organic SILT, wet, medium stiff I 5 64 u c
20 L =55 ,PI=
=:` . Sill
SP Gray SAND with gravel and silt, wet, 38 20
dense 25
■:;N'; grades below 25' to
; GM
! Sandy GRAVEL with silt, wet, very dense
,�
� . V : GP
' T.. .. 52 --
Boring terminate at below existing grade.
Groundwater observation well installed at 24' below existing grade.
• BORING LOG
SPRINGBROOK TECHNICAL CENTER
Ea2'th RENTON, WASHINGTON
Consultants Luc.
GEOTECHNICAL ENGINEERING R GEOLOGY Prof. No.884-1 Dete Dec. '81 Platte 13
�B■■/W��d■■ ■0■�■ Rom■
SILTS and SANDS, loose
it®mp ■1■
�m■■mu�m■®11■■■m■ ® CLAYS and -
��■■■//11 ��■ ■■■I■
Ing soft
um■m■ �—
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MOMME
■ m■ 4■ml■�■ .� dense s ra■■s■o
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ERMA
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MMMM
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DUTCH CONE LOG
�m�//In�m�mumlmnlm■ mm�
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jSPRINGBROOK TECHNICAL CENTER
ENGINEERINGEarth
Consultants Inc.
GEOTECHNICAL D.
■■mt■a■mn�■t■ta®ntA■mi . -
■>•■p■t■aW ■■1■ SANDS and SILTS, loose
CLAYS and SILTS, very soft to
ENEEMN
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�■■■■■M MEMMEM It
w �_�
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awl NEEMEW
■■t■■>•■ ■■■MINEW
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Consultants Inc.
GEOTECHNICAL
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•
ENGINEERINGDate Dec.