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Geotechnical Report
10814 SE 173rd St. Renton
Report Date: 12/9/2015
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Dear Client,
As requested, we have conducted a geotechnical soil investigation for 10814 SE 173rd St.
Renton concerning soil permeability and classification. Our findings and design criteria are
enclosed.
We trust the information provided is sufficient for your current needs. If you have any
questions please contact us.
Regards,
Cash M. Carr PE.
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Subsurface Exploration and Geotechnical Engineering Study
Regarding: Soil Permeability
Introduction
This report presents the results of our subsurface investigation and geotechnical report for
the residence located at 10814 SE 173rd St. Renton in regards to soil permeability.
Purpose and Scope
This subsurface investigation and geotechnical report is intended to determine and
present our finding for soil permeability and recommend procedures for infiltration.
Limitations
The scope of this report is limited to drainage. Structural and bearing considerations have
not been included in the scope of this report.
Field Explorations
A geotechnical borehole was constructed to a depth of 4’, a depth which is sufficient for
determining the capacity for storm water infiltration from the surface. Test was performed by
professional engineer Cash M. Carr and geologist Jackie Perkins. Disturbed samples were taken
at the lowest point on the property, as in our judgment, this point will be the worst case for
runoff saturation. Sampling was performed by professional engineer Cash M. Carr and geologist
Jackie Perkins. Our sample log is presented below.
Laboratory Testing
This grain size analysis sampled four feet of soil from the site at 10814 SE 173 St, Renton.
Samples were obtained on site, where initial observations were recorded. The samples were dried for five
days before being processed through 10, 20, 40, 60, 80, and 100 sieves.
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RESULTS:
Foot 1
Initial observations: extremely organically rich, very dark brown, moderate moisture content, grains are
rounded and range 0.2 -3.0mm with occasional fine gravel.
Starting weight: 5.4 oz*
Sieve Weight (oz) Percent wt % Passing
10 1.9 36.5 63.5
20 1.1 21.2 42.3
40 1.8 34.6 7.7
60 0.3 5.77 1.92
80 0.05 0.96 0.96
100 0.05 0.96 0.00
Total: 5.2
D10= 0.35
D30= 0.65
D60= 1.7
Cu= 4.86
Cc= 0.710
* Ounces were used in this procedure as the available scale did not produce decimals for grams.
Particle size distribution curve for foot 1:
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Foot 2
Initial observations: some organic material, moderately moist, dark brown, fine sand with silt and some
gravel, small grains are clumping together.
Starting weight: 6.1oz
Sieve Weight (oz) Percent wt % Passing
10 2.4 40.0 60.0
20 1 16.7 43.3
40 2.3 38.3 5.0
60 0.2 3.33 1.67
80 0.05 0.83 0.83
100 0.05 0.83 0.00
Total: 6.0
D10= 0.47
D30= 0.55
D60= 2
Cu= 4.255
Cc= 0.322
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Particle size distribution curve for foot 2:
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Foot 3
Initial observations: moderately moist, dark/medium orange brown, coarse sand and fine gravel with
some fine sand, a few very coarse gravel clasts (bordering on small cobbles) approximately 4cm diameter,
smaller grains clumping together from moisture.
Starting weight: 5.9
Sieve Weight (oz) Percent wt % Passing
10 2.3 39.7 60.3
20 1.2 20.7 39.7
40 1.9 32.8 6.9
60 0.3 5.2 1.7
80 0.05 0.9 0.9
100 0.05 0.9 0.0
Total: 5.8
D10= 0.46
D30= 0.59
D60= 2
Cu= 4.35
Cc= 0.378
Particle size distribution curve for foot 3:
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Foot 4
Initial observations: Organically rich, dark orange brown, fine gravels with sand and silt, some medium
gravel clasts, finer grains clump together due to moisture.
Starting weight: 7.9
Sieve Weight (oz) Percent wt % Passing
10 3.4 43.6 56.4
20 1.1 14.1 42.3
40 2.5 32.1 10.3
60 0.7 9.0 1.3
80 0.05 0.6 0.6
100 0.05 0.6 0.0
Total: 7.8
D10= 0.425
D30= 0.63
D60= 2
Cu= 4.71
Cc= 0.467
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Particle size distribution curve for foot 4:
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DATA ANALYSIS
Each of the samples yielded uniformity coefficients <6 and coefficients of gradation <1,
categorizing the soil as poorly graded gravelly sand (SP) under the grading criteria of the Unified Soil
Classification System. The top foot of soil may also be considered peat (PT) due to high organic content,
dark brown to black color, and fibrous texture. The soil is overall texturally classified as loamy sand with
gravel.
SOURCES OF ERROR
Several sources of error arose from the available equipment. The sieve with the largest diameter
mesh (no. 10) would only allow particles smaller than 2mm to pass through, which fails to allow for
distinction between coarse sand grains and gravels. This may cause the soil to be classified as more
poorly graded than it truly is. The presence of gravels and small cobbles in the soil should be taken into
account for the purpose of geoengineering, however the majority of the soil is comprised of sand.
For each sample the weight of the soil retained by the 80 and 100 sieves were between 0 and 0.1
ounces. For each of these measurements 0.05oz was recorded in order to maintain that this particle size
was present in the sample, however never greater than 1% by weight.
Soil samples were tested for permeability by spreading a ½” layer of soil from each sample across
a #80 mesh sieve. Soils were weted to saturation prior to saturation as permeability was significantly
higher in dry soil. The fully saturated condition tested represents worst case permeability.
PERMABILITY TESTING
Sample 1 Sample 2 Sample 3 Average
Soil Sample Thickness (in) 0.5 0.5 0.5
Time (s) 31 29 31
h1 (water column height start) 1 1 1
h2 (water column height end) 0.5 0.5 0.5
K (in/s) 0.012138306 0.012975 0.012138
K (in/hr) 44 47 44 45
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VICINITY MAP
TEST SITE ON
SOUTH SIDE OF
RESIDENCE
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Summary of Test Results
BOREHOLE 1
LOCATION: 44’ NORTH OF C.L. OF SE 173st, 22’ EAST OF WEST PROPERTY LINE.
0
2’
Extremely organic, rich, very dark brown, moderate moisture
content, grains are rounded and range 0.2 -3.0mm with
occasional fine gravel
TERMINATION OF TEST
SAMPLE 4
SAMPLE 2
SAMPLE 1 1’
3’
4’
SAMPLE 3
Some organic material, moderately moist, dark brown, fine
sand with silt and some gravel, small grains are clumping
together.
Moderately moist, dark/medium orange brown, coarse sand
and fine gravel with some fine sand, a few very coarse gravel
clasts (bordering on small cobbles) approximately 4cm
diameter, smaller grains clumping together from moisture.
Organic, rich, dark orange brown, fine gravels with sand and
silt, some medium gravel clasts, finer grains clump together
due to moisture.
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Conclusions
We have determined that the site is constructed upon a silt. We have furthermore
calculated that your soil has a permeability of 45 inches/hour. Hardpan was not detected to the
limits of the test dept. Soils can generally and conservatory be classified as sandy loam due to the
large amounts of organics present and generally coarse grained nature of the soil. A limited
infiltration system is recommended for this site. A trench length of 125’ is recommend for this
site.