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HEPWORTH - PAWLAI< GEOTECHNICAL
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SUBSOIL STUDY
FOR FOUNDATION DESIGN
PROPOSED RESIDENCE
PARCEL 1, WINDANCE RANCH
COUNTY ROAD 151
GARFIELD COUNTY, COLORADO
JOB NO. 112 026A
MAY 30, 2012
PREPARED FOR:
SHANNON BURKE
347 GLENCOE STREET
DENVER, COLORADO 80222
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TABLE OF CONTENTS
PURPOSE AND SCOPE OF STUDY 1
PROPOSED CONSTRUCTION 1
SITE CONDITIONS - 2 -
FIELD EXPLORATION 2 -
SUBSURFACE CONDITIONS - 3 -
FOUNDATION BEARING CONDITIONS - 3 -
DESIGN RECOMMENDATIONS - 4 -
FOUNDATIONS - 4 -
FOUNDATION AND RETAINING WALLS ... - 5 -
FLOOR SLABS - 7 -
UNDERDRAIN SYSTEM - 7 -
SURFACE DRAINAGE - 8 -
PERCOLATION TESTING - 9 -
LIMITATIONS 9 -
FIGURE 1 - LOCATIONS OF EXPLORATORY BORINGS AND PERCOLATION
TEST HOLES
FIGURE 2 - LOGS OF EXPLORATORY BORINGS
FIGURE 3 - LEGEND AND NOTES
FIGURES 4 and 5 - SWELL -CONSOLIDATION TEST RESULTS
FIGURE 6 - GRADATION TEST RESULTS
TABLE 1 - SUMMARY OF LABORATORY TEST RESULTS
TABLE 2 - PERCOLATION TEST RESULTS
PURPOSE AND SCOPE OF STUDY
This report presents the results of a subsoil study for a proposed residence to be located
on Parcel 1, Windance Ranch, County Road 151, south of Sweetwater in Garfield
County, Colorado. The project site is shown on Figure 1. The purpose of the study was
to develop recommendations for the foundation design. The study was conducted in
accordance with our agreement for geotechnical engineering services to Shannon Burke
dated April 20, 2012.
A field exploration program consisting of exploratory borings was conducted to obtain
information on the subsurface conditions. Samples of the subsoils obtained during the
field exploration were tested in the laboratory to determine their classification,
compressibility or swell and other engineering characteristics. The results ofthe field
exploration and laboratory testing were analyzed to develop recommendations for
foundation types, depths and allowable pressures for the proposed building foundation.
This report summarizes the data obtained during this study and presents our conclusions,
design recommendations and other geotechnical engineering considerations based on the
proposed construction and the subsurface conditions encountered.
PROPOSED CONSTRUCTION
The residence will be a two story wood frame structure over crawlspace located on the
site as shown on Figure 1. The attached garage will have a slab -on -grade floor. Grading
for the structure is assumed to be relatively minor with cut depths from about 3 to 5 feet.
We assume relatively light foundation loadings, typical ofthe proposed construction. The
on-site septic disposal location is planned to the northeast ofthe residence as shown on
Figure 1.
If building loadings, location or grading plans change significantly from those described
above, we should be notified to re-evaluate the recommendations contained in this report.
Job No. 112 026A
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SITE CONDITIONS
The site is vacant and the ground surface appears mostly natural. The terrain is strongly
sloping down to the northeast. Elevation difference across the building site is estimated
at about 4 to 5 feet. The site is at the edge of a moderately thick aspen stand with open
meadow/pasture to the east in the building area. There is a small irrigation ditch to the
west of the building site along the edge ofthe aspen grove that was flowing water at the
time of our field exploration, Vegetation consists of grass and weeds. There were
scattered partly buried cobbles on the ground surface. Elevation of the site is estimated at
about 8,500 feet,
FIELD EXPLORATION
The field exploration for the project was conducted on May 2, 2012. Two exploratory
borings (Borings 1 and 2) were drilled in the general proposed building area at the
locations shown on Figure 1 to evaluate the subsurface conditions. Profile Boring 1 and
Profile Boring 2 were drilled at the two alternate septic disposal sites. The boring
locations were coordinated with Scott Green in the field. The borings were advanced
with 4 inch diameter continuous flight augers powered by a truck -mounted CME -45B
drill rig. The borings were logged by a representative of 1-lepworth-Pawlak Geotechnical,
Inc.
Sainples of the subsoils were taken with 1% inch and 2 inch I.A. spoon samplers. The
samplers were driven into the subsoils at various depths with blows from a 140 pound
hammer falling 30 inches. This test is similar to the standard penetration test described
by ASTM Method D-1586. The penetration resistance values are an indication of the
relative density or consistency ofthe subsoils. Depths at which the samples were taken
and the penetration resistance values are shown on the Logs of Exploratory Borings,
Figure 2. The samples were returned to our laboratory for review by the project engineer
and testing.
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SUBSURFACE CONDITIONS
Graphic logs ofthe subsurface conditions encountered at the site are shown on Figure 2.
The subsoils encountered in Borings 1 and 2, below about 2 to 2'/z feet of organic topsoil,
consisted of sandy to very sandy clay with scattered gravel and cobbles. The clay was
stiff to very stiff with depth and extended down to the drilled depths of 31 and 21 feet.
The subsoils encountered in Profile Boring 1, below about 11/2 feet of topsoil, consisted of
medium dense, clayey to very clayey sandy gravel with cobbles and sandy clay zones that
extended down to the drilled depth of 9 feet. The subsoils encountered in Profile Boring
2, below about 2 feet of topsoil, consisted of stiff, sandy clay with scattered gravel and
cobbles that extended down to the drilled depth of 9 feet.
Laboratory testing performed on samples obtained from the borings included natural
moisture content and density, gradation analyses, and Atterberg limits. Results of swell -
consolidation testing performed on relatively undisturbed drive samples of the clay soils,
presented on Figures 4 and 5, indicate generally moderate compressibility under
conditions of light loading and wetting. Two ofthe samples showed a low swell potential
when wetted under a constant light surcharge. Results of gradation analyses performed
on a small diameter drive sample (minus 11/2 inch fraction) ofthe gravel soils from Profile
Boring 1 are shown on Figure 6. The laboratory testing is summarized in Table 1.
Free water was encountered in Boring 1 at the time of drilling and when checked 12 days
later at depth of about 17 feet. No free water was encountered in Boring 2 or in Profile
Borings 1 and 2. The subsoils were moist to very moist becoming wet with depth in
Boring 1.
FOUNDATION BEARING CONDITIONS
Based on the proposed cut depths and the residence location, the sandy clay soils will
probably be encountered at subgrade level. Theses soils possess low bearing capacity and
low to moderate settlement potential. Spread footings bearing on these soils appear
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feasible for foundation support of the building with some risk of movement. Based on
our experience with this type of soil condition, in the area, the low expansion potential
encountered in the samples can be neglected in the foundation design, but the exposed
bearing soils should be further evaluated at the time of construction.
A lower risk foundation with respect to settlement would be to place several feet of
structural fill below the spread footings or a relatively deep foundation system such as
helical piers or screw piles bearing in suitable soils. Provided below are
recommendations for spread footings bearing on the natural soils. If recommendations
for spread footings bearing on structural fill or a helical pier or screw pile foundation
system are desired, we should be contacted.
DESIGN RECOMMENDATIONS
FOUNDATIONS
Considering the subsurface conditions encountered in the exploratory borings and the
nature of the proposed construction, we recommend the building be founded with spread
footings bearing on the natural soils with some risk of movement.
The design and construction criteria presented below should be observed for a spread
footing foundation system.
1) Footings placed on the undisturbed natural soils should be designed for an
allowable bearing pressure of 1,500 psf. Based on experience, we expect
movement of footings designed and constructed as discussed in this
section will be about 1 to 11/2 inches and probably occur over time.
2) The footings should have a minimum width of 16 inches for continuous
walls and 2 feet for isolated pads.
3) Exterior footings and footings beneath unheated areas should be provided
with adequate soil cover above their bearing elevation for frost protection.
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Placement of foundations at least 48 inches below exterior grade is
recommended for this area of Garfield County.
4) Continuous foundation walls should be heavily reinforced top and bottom
to span local anomalies and better withstand the effects of some
differential settlement such as by assuming an unsupported length of at
least 14 feet. Foundation walls acting as retaining structures should also
be designed to resist lateral earth pressures as discussed in the "Foundation
and Retaining Walls" section of this report.
5) The topsoil and any loose disturbed soils should be rernoved and the
footing bearing level extended down to the firm natural soils. Track -
mounted equipment should be used where needed to avoid disturbance of
the bearing soils. If water seepage is encountered, the footing areas should
be dewatered before concrete placement. Soft subgrade areas should be
stabilized prior to the footing construction. The stabilization can probably
be done by subexcavating 11/2 to 2 feet of the subgrade soils and replacing
thele with imported coarse granular soils such as crushed rock.
6) A representative of the geotechnical engineer should observe all footing
excavations prior to concrete placement to evaluate bearing conditions.
FOUNDATION AND RETAINING WALLS
Foundation walls and retaining structures which are laterally supported and can be
expected to undergo only a slight amount of deflection should be designed for a lateral
earth pressure computed on the basis of an equivalent fluid unit weight of at least 55 pcf
for backfill consisting of the on-site soils. Cantilevered retaining structures which are
separate from the building and can be expected to deflect sufficiently to mobilize the full
active earth pressure condition should be designed for a lateral earth pressure computed
on the basis of an equivalent fluid unit weight of at least 50 pcf for backfill consisting of
the on-site soils. The wall backfill should not contain topsoil or oversized rocks.
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All foundation and retaining structures should be designed for appropriate hydrostatic and
surcharge pressures such as adjacent footings, traffic, construction materials and
equipment. The pressures recommended above assume drained conditions behind the
walls and a horizontal backfill surface. The buildup of water behind a wall or an upward
sloping backfill surface will increase the lateral pressure imposed on a foundation wall or
retaining structure. An underdrain should be provided to prevent hydrostatic pressure
buildup behind walls.
Backfill should be placed in uniform lifts and compacted to at least 90% of the maximum
standard Proctor density at a moisture content near optimum. Backfill in pavement and
walkway areas should be compacted to at least 95% of the maximum standard Proctor
density. Care should be taken not to overcompact the backfill or use large equipment
near the wall, since this could cause excessive lateral pressure on the wall, Some
settlement of deep foundation wall backfill should be expected, even if the material is
placed correctly, and could result in distress to facilities constructed on the backfill.
We suggest imported granular soils for backfilling foundation walls and retaining
structures because their use results in lower lateral earth pressures and the backfill will
help to improve the subsurface drainage. Subsurface drainage recommendations are
discussed in more detail in the "Underdrain System" section of this report. Imported
granular wall backfill should contain less than 15% passing the No. 200 sieve and have a
maximum size of 6 inches.
The lateral resistance of foundation or retaining wall footings will be a combination of the
sliding resistance of the footing on the foundation materials and passive earth pressure
against the side of the footing. Resistance to sliding at the bottoms of the footings can be
calculated based on a coefficient of friction of 0.35. Passive pressure of compacted
backfill against the sides of the footings can be calculated using an equivalent fluid unit
weight of 325 pcf for moist condition. The coefficient of friction and passive pressure
values recommended above assume ultimate soil strength. Suitable factors of safety
should be included in the design to limit the strain which will occur at the ultimate
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strength, particularly in the case of passive resistance. Fill placed against the sides of the
footings to resist lateral loads should be compacted to at least 95% of the maximum
standard Proctor density at a moisture content near optimum.
FLOOR SLABS
The natural on-site soils, exclusive of topsoil, are suitable to support lightly loaded slab -
on -grade construction. There maybe some risk of slab heave if potentially expansive
clay soils underlie the slab and become wetted. We should further evaluate the expansive
potential of the slab subgrade at the time of construction to determine if mitigation is
needed.
To reduce the effects of some differential movement, floor slabs should be separated from
all bearing walls and columns with expansion joints which allow unrestrained vertical
movement. Floor slab control joints should be used to reduce damage due to shrinkage
cracking. The requirements for joint spacing and slab reinforcement should be
established by the designer based on experience and the intended slab use. A minimum 4
inch layer of free -draining gravel should be placed beneath slabs for support and to
facilitate drainage. This material should consist of minus 2 inch aggregate with at least
50% retained on the No. 4 sieve and less than 2% passing the No. 200 sieve.
All fill materials for support of floor slabs should be compacted to at least 95% of
maximum standard Proctor density at a moisture content near optimum. Required frill can
consist of the on-site soils devoid of topsoil and oversized rocks, or a suitable granular
material can be imported.
LINDERDRAIN SYSTEM
Free water was encountered during our exploration below proposed excavation depths but
it has been our experience in mountainous areas and where clay soils are present that
groundwater level can rise and/or perched groundwater can develop during times of
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heavy precipitation or seasonal runoff. Frozen ground during spring runoff can also
create a perched condition, We recommend below -grade construction, such as retaining
walls, crawlspace and basement areas, be protected from wetting and hydrostatic pressure
buildup by an underdrain system.
The drain should consist of drainpipe placed in the bottom of the wall backfill and
surrounded above the invert Ievel with free -draining granular material. The drain should
be placed at each level of excavation and at least 11/2 feet below lowest adjacent finish
grade and sloped at a minimum 1% to a suitable gravity outlet, Free -draining granular
material used in the underdrain system should contain less than 2% passing the No. 200
sieve, less than 50% passing the No. 4 sieve and have a maximum size of 2 inches. The
drain gravel should be separated from the wall backfill with filter fabric such as Mirafz
140N.
SURFACE DRAINAGE
The following drainage precautions should be observed during construction and
maintained at all times after the building has been completed:
1) Inundation ofthe foundation excavations and underslab areas should be
avoided during construction.
2) Exterior backfill should be adjusted to near optimum moisture and
compacted to at least 95% ofthe maximum standard Proctor density in
pavement and slab areas and to at Ieast 90% of the maximum standard
Proctor density in landscape areas.
3) The ground surface surrounding the exterior of the building should be
sloped to drain away from the foundation in all directions. We
recommend a minimum slope of 12 inches in the first 10 feet in unpaved
areas and a minimum slope of 3 inches in the first 10 feet in paved areas.
Free -draining wall backfill should be capped with about 2 feet of the on-
site soils to reduce surface water infiltration.
Job No. 112 026A
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4) Roof downspouts and drains should discharge well beyond the limits of all
backfill.
PERCOLATION TESTING
Percolation tests were conducted on May 5, 2012 to evaluate the feasibility of an
infiltration septic disposal system at the site. One profile boring (Profile Boring 1) was
drilled and four percolation holes (P-1, P-2, P-3 and P-4) were excavated at the locations
shown on Figure 1. The test holes were hand dug in the bottom of shallow backhoe
trenches and soaked with water one day prior to testing. The soils encountered in the
percolation holes were more clayey than those encountered in Profile Boring 1 and
consisted of sandy clay with scattered gravel and cobbles. The test P-3 location was
gravelly and the P-4 location contained minor gravel. No free water was encountered in
the profile borings at the time of drilling. The sandy clay soils probably classify as Sandy
Clay Loam with variable gravel content as per USDA system. Percolation tests were not
requested at the Profile Boring 2 location due to the clay soils with minor gravel content.
The percolation test results are presented in Table 2. No test was performed in test hole
P-4 due to water still remaining in hole when we returned the next day for the percolation
testing. The percolation test results indicate rates of 240, 80 and 60 minutes per inch in
tests P-1, P-2 and P-3, respectively. Based on the subsurface conditions encountered and
the percolation test results, the tested area is not suitable for a'conventional infiltration
septic disposal system. A civil engineer should design the infiltration septic disposal
system. Additional percolation testing could be done to locate a more suitable site for
subsurface infiltration.
LIMITATIONS
This study has been conducted in accordance with generally accepted geotechnical
engineering principles and practices in this area at this time. We make no warranty either
express or implied. The conclusions and recommendations submitted in this report are
based upon the data obtained from the exploratory borings drilled at the locations
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indicated on Figure 1, the proposed type of construction and our experience in the area.
Our services do not include determining the presence, prevention or possibility of mold or
other biological contaminants (MOBC) developing in the future. If the client is
concerned about MOBC, then a professional in this special field of practice should be
consulted. Our findings include interpolation and extrapolation of the subsurface
conditions identified at the exploratory borings and variations in the subsurface
conditions may not become evident until excavation is performed. If conditions
encountered during construction appear different from those described in this report, we
should be notified so that re-evaluation of the recommendations may be made.
This report has been prepared for the exclusive use by our client for design purposes. We
are not responsible for technical interpretations by others of our information. As the
project evolves, we should provide continued consultation and field services during
construction to review and monitor the implementation of our recommendations, and to
verify that the recommendations have been appropriately interpreted. Significant design
changes may require additional analysis or modifications to the recommendations
presented herein. We recommend on-site observation of excavations and foundation
bearing strata and testing of structural fill by a representative of the geotechnical
engineer.
Respectfully Submitted,
HEPWORTH - PAWLAK GEfi�ICAL, INC.
David A. Young, P. E.
Reviewed by:
2-216° Z
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�9 d ICNA LSA y ��
Steven L. Pawlak, P. E.
DAY/ljg
cc: Scott Green Excavating — Scott Green (sgegypsum cr gmail.com)
Job No. 112 026A
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ENS
P
ASPEN rl�,
GROVE-{'
Yhmi
EXISTING ACCESS ROAD
IRRIGATION
DITCH
P-1
P 2 P-3
PROFILE BORING 1
•
PROPP-4LD
LEA
FIELD
•BORING 2
PROPOSED
55' X32'
HOUSE
TO COUNTY ROAD 151
PROFILE BORING 2
•
PROPOSED
WELL
PROPOSED
ACCESS ROAD
Jaw -
APPROXIMATE SCALE:
1"=60'
112 026A
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HEPWOFTIH-PAWL KGEOTECHNICAL.
LOCATIONS OF EXPLORATORY BORINGS
AND PERCOLATION TEST HOLES
FIGURE 1
DEPTH - FEET
0
5
10
15
20
25
30
35
112 026A
BORING 1
12
0
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
12/12
17/12
1 WC=22.3
DD= 100
14/12
WC=31.7
DD=89
12/12
WC=20.4
DD=103
22/12
20/12
BORING 2
8/12
WC=30.3
DD=91
-200=81
10/6, 30/6
18/12
WC=16.6
DD=111
• •
•^ 15/12
/ WC=15.4
DD=116
' r -200=51
•
i/I 18/12
PROFILE PROFILE
BORING 1 BORING 2
7: o
6/6,20/6
WC=6.7
+4=53
-200=21
12/6,26/6
NOTE: Explanation of symbols is shown on Figure 3.
Gtech
I IEPWORTH-PAWLAK GEOTECHN1CAI
r
r
•
•
r
r
•
•
•
11
25/12
25/12
LOGS OF EXPLORATORY BORINGS
5
10
15
20
25
30
35
DEPTH - FEET
FIGURE 2
LEGEND:
•
•
TOPSOIL; organic silty sandy clay, roots, moist to very moist, dark brown.
CLAY (CL); silty, sandy to occasionally very sandy, gravelly with cobble zones, stiff to very stiff with depth, moist
to very moist becoming wet with depth in Boring 1, mixed brown, calcareous zones, medium to high plasticity.
GRAVEL (GC); with cobbles, clayey to very clayey with sandy, clay zones, medium dense, moist, brown, medium
plastic fines.
Relatively undisturbed drive sample; 2 -inch I.D. California liner sample.
Drive sample; standard penetration test (SPT), 1 3/8 inch I.D. split spoon sample, ASTM D-1586.
Drive sample blow count; indicates that 17 blows of 140 pound hammer falling 30 inches were required to drive
1712
the California or SPT sampler 12 inches.
0,12
Free water depth measured in boring and number of days following drilling measurement was taken.
Depth at which Boring 1 caved when checked on May 14, 2012. Boring 2 was dry to the drilled depths of 21 feet.
NOTES:
1. Exploratory borings were drilled on May 2, 2012 with 4 -inch diameter continuous flight power auger.
2. Locations of exploratory borings were measured approximately by pacing from approximate field staked building
corners.
3.. Elevations of exploratory borings were not measured and the logs of exploratory borings are drawn to depth.
4. The exploratory boring locations should be considered accurate only to the degree implied by the method used.
5. The lines between materials shown on the exploratory boring logs represent the approximate boundaries between
material types and transitions may be gradual.
6. Water level readings shown on the logs were made at the time and under the conditions indicated. Fluctuations in
water level may occur with time. No free water was encountered in Boring 2.
7. Laboratory Testing Results:
WC = Water Content (% )
DD = Dry Density ( pct )
+4 — Percent retained on the No. 4 sieve
-200 = Percent passing No. 200 sieve
112 026A
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HEPWORTH•PAWLAK GEOTECHNICAL
LEGEND AND NOTES
FIGURE 3
COMPRESSION - EXPANSION (% )
COMPRESSION - EXPANSION (% )
1
0
1
2
3
4
1
0
1
2
3
4
01
0
10 10
APPLIED PRESSURE (ksf )
100
Moisture Content = 22.3 percent
Dry Density = 100 pcf
Sample of: Sandy Clay
From: Boring 1 at 5 Feet
Moisture Content = 31.7 percent
Dry Density = 89 pcf
Sample of: Sandy Clay
From: Boring 1 at 10 Feet
°N\N.\\\,0
Expansion
upon
wetting
,
01
0
10 10
APPLIED PRESSURE (ksf )
100
APPLIED PRESSURE (ksf )
0
112 026A
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SWELL -CONSOLIDATION TEST RESULTS
FIGURE 4
Moisture Content = 31.7 percent
Dry Density = 89 pcf
Sample of: Sandy Clay
From: Boring 1 at 10 Feet
Expansion
upon
wetting
1
1
0
10 10
APPLIED PRESSURE (ksf )
0
112 026A
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tii:r.1m,,IP;IfFAWlr.r:;nu atrj,c.AL
SWELL -CONSOLIDATION TEST RESULTS
FIGURE 4
COMPRESSION - EXPANSION (% )
COMPRESSION (% )
1
0
1
2
3
4
0
1
2
3
4
5
0.1
0
10 10
APPLIED PRESSURE ( ksf )
100
Moisture Content = 30.3 percent
Dry Density = 91 pcf
Sample of: Sandy Clay
From: Baring 2 at 2 Feet
Moisture Content = 16.6
Dry Density = 111
Sample of: Sandy Clay
From: Boring 2 at 10 Feet
percent
pcf
•
•
I
•
C\
Expansion •
upon
wetting
Compression
upon
wetting
0.1
0
10 10
APPLIED PRESSURE ( ksf )
100
112 026A
APPLIED PRESSURE ( ksf )
GeStech
HEPWORTH-PAWLAK GEOTECHNIGA9.
SWELL -CONSOLIDATION TEST RESULTS
0
FIGURE 5
Moisture Content = 16.6
Dry Density = 111
Sample of: Sandy Clay
From: Boring 2 at 10 Feet
percent
pcf
•
•
Compression
upon
wetting
1
1
0 10
1C
112 026A
APPLIED PRESSURE ( ksf )
GeStech
HEPWORTH-PAWLAK GEOTECHNIGA9.
SWELL -CONSOLIDATION TEST RESULTS
0
FIGURE 5
PERCENT RETAINED
HYDROMETER ANALYSIS
SIEVE ANALYSIS
TIME READINGS
24NR. 7NR
45 MIN. 15 MIN, 60MIN, 1911119. 4 MIN. 1 M114. #
0
10
20
30
40
50
60
70
60
90
100
.001 .002 .005 .009 .019 .037 .074 .150 .300 .600 1 10 2.30 4.75 0 5 125 19.0
#100
U.S. STANDARD SERIES
#50
#30 0 1
#4
310'
CLEAR SOUARE OPENINGS
3!4' 1 112'
3' 5 6 B'
DIAMETER OF PARTICLES IN MILLIMETERS
100
90
60
70
60
50
40
30
20
10
0
37.5 762 l27152 203
CLAY TO SILT
5A1413
GRAVEL
FINE
MEDIUM
COARSE
FINE
COARSE
C060LES
Gravel 53 %
Sample of: Clayey Sandy Gravel
Sand 26 %
Silt and Clay 21 %
From: Profile Boring 1 at 2 1/2 Feet
PERCENT PASSING
112 026A
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HEPWORTH•PAWLAK GEOTECHNICAL
GRADATION TEST RESULTS
FIGURE 6
HEPWORTH-PAWLAK GEOTECHNICAL, INC.
TABLE 1
SUMMARY OF LABORATORY TEST RESULTS
Job No. 112 026A
SAMPLE LOCATION
NATURAL
MOISTURE
CONTENT
(%)
NATURAL
DRY
DENSITY(ado)
(pcf)
GRADATION
PERCENT
PASSING
N0.200
SIEVE
ATTERBERG LIMITS
AASHTO
CLASSIFICATION
SOIL OR
BEDROCK TYPE
BORING
DEPTH
(ft)
GRAVEL
SAND
(,f0}
LIQUID
LIMIT
PLASTIC
INDEX
1
5
22.3
100
Sandy Clay
10
31.7
89
Sandy Clay
15
20.4
103
Sandy Clay with Gravel
2
2
30.3
91
Sandy Clay
10
16.6
111
Sandy Clay
15
15.4
116
51
Very Sandy Clay
Profile
Boring
1
21/2
6.7
Clayey Sandy Gravel
HEPWORTH-PAWLAK GEOTECHNICAL, INC.
TABLE 2
PERCOLATION TEST RESULTS
JOB NO. 112 026A
HOLE NO.
HOLE
DEPTH
(INCHES)
LENGTH OF
INTERVAL
(MIN)
WATER
DEPTH AT
START OF
INTERVAL
(INCHES)
WATER
DEPTH AT
END OF
INTERVAL
(INCHES)
DROP IN
WATER
LEVEL
(INCHES)
AVERAGE
PERCOLATION
RATE
(MIN./INCH)
P-1
24
10
71/4
71/4
0�
240
71/4
71
118
71/
71
0
71/
7%
0
71
71/
0
7%
7%
0
7
7
%
7
7
0
P-2
30
10
61/4
6'
0
80
61/
611
%
6%
53/
%
5
555/
'/
g1/4
5%
5%
%
53/
5'
%
51/
5!
%
51
5
1/
P-3
20
10
4%
41/4
a
60
41/
41/
0
41/
4'
'
41%
3%
1/
3'
35
1/4
35/
31/
%
31
3%
%
3%/
314
1/4
Note: Percolation test holes were hand dug in the bottom of backhoe trenches and
soaked on May 4, 2012. Percolation tests were conducted on May 5, 2012. The
average percolation rates were based on the last three readings of each test.
615-1
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t It
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g tg
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