HomeMy WebLinkAboutRS_Geotechnical _Report_210529_V1
NELSON GEOTECHNICAL ASSOCIATES, INC.
February 26, 2021
Mr. Long Nguyen
11904 SE 228th Place
Kent, Washington 98051
VIA Email: longdnguyen@gmail.com
Geotechnical Engineering Evaluation
Nguyen Aberdeen Avenue NE Short Plat Residential Development
2309 Aberdeen Avenue NE
Renton, Washington
NGA File No. 1227220
Dear Mr. Nguyen:
We are pleased to submit the attached report titled “Geotechnical Engineering Evaluation – Nguyen
Aberdeen Avenue NE Short Plat Residential Development – 2309 Aberdeen Avenue NE – Renton,
Washington.” This report summarizes our observations of the existing surface and subsurface
conditions within the site and provides general recommendations for the proposed site development.
Our services were completed in general accordance with the proposal issued to you on January21, 2021.
The property is currently vacant but was previously occupied with an existing single-family residence
within the western portion of the property. The ground surface within the property is relatively level to
gently sloping down from the west to the east. We understand that the proposed development will
include construction of three new single-family residences and associated roadways and underground
utilities.
We explored the subsurface conditions within the site with eleven trackhoe excavated test pits
explorations. The explorations extended to depths in the range of 5.5 to 11.5 feet below the existing
ground surface. Our explorations indicated that the site was underlain by surficial undocumented fill
soils with competent native glacial outwash soils at depth.
It is our opinion that the proposed site development is feasible from a geotechnical engineering
standpoint, provided that our recommendations for site development are incorporated into project
plans. In general, the native glacial bearing soils underlying the site should adequately support the
planned structures. Foundations should be advanced through any loose and/or undocumented fill soils
down to the competent glacial bearing material interpreted to underlie the site, for bearing capacity and
settlement considerations. These soils should generally be encountered between approximately 2.0 to
6.0 feet below the existing ground surface, based on our explorations. The deepest areas of
undocumented fill were generally encountered within the lower very eastern portion of the property. If
deeper areas of loose soils or undocumented fill are encountered in unexplored areas of the site, they
should be removed and replaced with structural fill for foundation and pavement support.
Geotechnical Engineering Evaluation NGA File No. 1227220
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NELSON GEOTECHNICAL ASSOCIATES, INC.
Specific grading and stormwater plans have not been finalized at the time this report was prepared.
However, we understand that stormwater from the proposed development may be directed into on-site
infiltration systems, if feasible. The City of Renton uses the 2016 King County Surface Water Design
Manual, as amended by the City of Renton Storm Water Manual to determine the design of infiltration
facilities. According to this manual and the City of Renton requirements, on-site infiltration testing
consisting of the small Pilot Infiltration Test (PIT) is used to determine the long-term design infiltration
rates. Based on the results of our on-site infiltration testing and granular nature of the native glacial
outwash soils encountered within the western and central portion of the site, it is our opinion that the
onsite native outwash soils within the western and central portion of the property are conducive for
traditional stormwater infiltration methods. However, it is our opinion that stormwater infiltration is
not feasible within the very eastern portion of the property due to the overall depth of the
undocumented fill and presence of perched groundwater encountered at depth within our eastern
explorations. This is discussed in more detail in the attached report.
In the attached report, we have also provided general recommendations for site grading, slabs-on-
grade, structural fill placement, retaining walls, erosion control, and drainage. We should be retained to
review and comment on final development plans and observe the earthwork phase of construction. We
also recommend that NGA be retained to provide monitoring and consultation services during
construction to confirm that the conditions encountered are consistent with those indicated by the
explorations, to provide recommendations for design changes should the conditions revealed during
construction differ from those anticipated, and to evaluate whether or not earthwork and foundation
installation activities comply with contract plans and specifications.
It has been a pleasure to provide service to you on this project. Please contact us if you have any
questions regarding this report or require further information.
Sincerely,
NELSON GEOTECHNICAL ASSOCIATES, INC.
Khaled M. Shawish, PE
Principal Engineer
TABLE OF CONTENTS
INTRODUCTION .......................................................................................................... 1
SCOPE......................................................................................................................... 1
SITE CONDITIONS ........................................................................................................ 2
Surface Conditions ........................................................................................................ 2
Subsurface Conditions .................................................................................................. 2
Hydrogeologic Conditions............................................................................................. 3
SENSITIVE AREA EVALUATION ..................................................................................... 4
Seismic Hazard .............................................................................................................. 4
Erosion Hazard .............................................................................................................. 4
CONCLUSIONS AND RECOMMENDATIONS .................................................................. 5
General ......................................................................................................................... 5
Erosion Control ............................................................................................................. 6
Site Preparation and Grading ....................................................................................... 6
Temporary and Permanent Slopes ............................................................................... 7
Foundations .................................................................................................................. 8
Retaining Walls ............................................................................................................. 9
Structural Fill ............................................................................................................... 10
Slab-on-Grade ............................................................................................................. 11
Pavements .................................................................................................................. 11
Utilities ........................................................................................................................ 11
Site Drainage ............................................................................................................... 12
CONSTRUCTION MONITORING .................................................................................. 14
USE OF THIS REPORT ................................................................................................. 14
LIST OF FIGURES
Figure 1 – Vicinity Map
Figure 2 – Site Plan
Figure 3 – Soil Classification Chart
Figures 4 through 6 – Exploration Logs
Geotechnical Engineering Evaluation
Nguyen Aberdeen Avenue NE Short Plat Residential Development
2309 Aberdeen Avenue NE
Renton, Washington
INTRODUCTION
This report presents the results of our geotechnical engineering investigation and evaluation of the planned
residential development project in Renton, Washington. The project site is located at 2309 Aberdeen
Avenue NE, as shown on the Vicinity Map in Figure 1. The purpose of this study is to explore and
characterize the site’s surface and subsurface conditions and to provide geotechnical recommendations for
the planned site development.
The property is currently vacant but was previously occupied with an existing single-family residence within
the western portion of the property. The ground surface within the property is relatively level to gently
sloping down from the west to the east. We understand that the proposed development will include
construction of three new single-family residences and associated roadways and underground utilities.
Final development and grading plans have not been prepared at the time this report was issued. Final
stormwater plans have also not been developed, however, we understand that stormwater may be
directed to on-site infiltration systems, if feasible. The existing site layout is shown on the Site Plan in
Figure 2.
SCOPE
The purpose of this study is to explore and characterize the site surface and subsurface conditions and
provide general recommendations for site development.
Specifically, our scope of services included the following:
1. Review available soil and geologic maps of the area.
2. Explore the subsurface soil and groundwater conditions within the site with trackhoe
excavated test pits. Trackhoe was subcontracted by NGA.
3. Perform grain-size sieve analysis on soil samples, as necessary.
4. Provide recommendations for structure foundations.
5. Provide recommendations for earthwork.
6. Provide recommendations for temporary and permanent slopes.
7. Provide recommendations for retaining walls.
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8. Provide recommendations for slab and pavement subgrade preparation.
9. Provide recommendations for utility installation.
10. Provide long-term design infiltration rates based on on-site Pilot Infiltration Testing (PIT)
per the 2016 King County Surface Water Design Manual. Location and depth of tests were
determined by the civil engineer. Water for the tests was secured by client.
11. Provide recommendations for infiltration system installation.
12. Provide recommendations for site drainage and erosion control.
13. Document the results of our findings, conclusions, and recommendations in a written
geotechnical report.
SITE CONDITIONS
Surface Condition
The site consists of a roughly square-shaped parcel covering approximately 0.84 acres. The site is currently
vacant but was previously occupied by a single-family residence within the western portion of the site.
Topography within the western and central portion of the slopes gently down from the western property
line to the eastern portion of the property. The eastern portion of the property is generally level. The site
is generally vegetated by grass-covered yard areas, young to mature trees, and landscaping. A horseshoe-
shaped gravel driveway is located within the eastern portion of the property. The property is bound to the
north, south, and west by single-family residences, and to the east by Aberdeen Avenue NE. We did not
observe surface water within the site during our site visit on February 5, 2021.
Subsurface Conditions
Geology: The geologic units for this site are shown on Preliminary Geologic Map of Seattle and Vicinity,
Washington, by Waldron, H.H., Leisch, B.A., Mullineaux, D.R., and Crandell, D.R., (USGS, 1961). The site is mapped as
younger gravel (Qyg) with younger sand (Qys) and alluvium (Qa) mapped nearby. The younger gravel and
sand deposits are described as fine to coarse sand that contains varying amounts of gravel. The alluvium is
described as silt with varying amounts of sand and organic material. Our explorations generally
encountered fine to coarse sand with varying amounts of gravel and silt within the western and central
portion of the property that we interpreted as younger gravel outwash soils. Our explorations within the
very eastern portion of the property generally encountered silt with sand and silty fine to medium sand
that we interpreted as native alluvium and younger sand deposits at depth.
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Explorations: The subsurface conditions within the site were explored on February 5, 2021 by excavating
eleven test pits with a mini-trackhoe extending to depths in the range of 5.5 to 11.5 feet below the existing
ground surface. The approximate locations of our explorations are shown on the Site Plan in Figure 2. A
geologist from NGA was present during the explorations, examined the soils and geologic conditions
encountered, obtained samples of the different soil types, and maintained logs of the test pits.
The soils were visually classified in general accordance with the Unified Soil Classification System, presented
in Figure 3. The logs of our explorations are attached to this report and are presented as Figures 4 through
6. We present a brief summary of the subsurface conditions in the following paragraph. For a detailed
description of the subsurface conditions, the logs of the explorations should be reviewed.
At the surface of all of our explorations, we encountered approximately 0.5 to 6.0 feet of surficial grass and
loose to medium dense dark brown silty fine to medium sand with varying amounts of gravel, organics and
debris that we interpreted as surficial topsoil and/or undocumented fill soils. Underlying the surficial
topsoil/undocumented fill soils within Test Pit 1, 2, 8, and 9 within the eastern portion of the site, we
encountered medium dense/stiff orange-brown to gray-brown silty fine to medium sand and silt with fine
sand with varying amounts of gravel and organics that we interpreted as younger sand and alluvium
deposits, respectively. Below the surficial topsoil and/or the undocumented fill in Test Pits 3 through 7, 10,
and Infiltration Pit 1, we encountered medium dense to dense fine to coarse sand with varying amounts of
silt and gravel that we interpreted as native younger gravel soils. All of our test pits were terminated within
the native younger gravel and sand soils at depths in the range of 5.5 to 11.5 feet below the existing ground
surface.
Hydrogeologic Conditions
We encountered minor to moderate groundwater seepage within Test Pits 1 and 8 at a depth of 8.0 feet
below the existing ground surface. We interpreted this groundwater seepage to be perched groundwater.
Perched water occurs when surface water infiltrates through less dense, more permeable soils and
accumulates on top of a relatively low permeability material. Perched water does not represent a regional
groundwater "table" within the upper soil horizons. Perched water tends to vary spatially and is dependent
upon the amount of rainfall. We would expect the amount of perched groundwater to decrease during
drier times of the year and increase during wetter periods.
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SENSITIVE AREA EVALUATION
Seismic Hazard
We reviewed the 2018 International Building Code (IBC) for seismic site classification for this project.
Since competent glacial soils are inferred to underlie the site at depth, the site conditions best fit the IBC
description for Site Class D.
Table 1 below provides seismic design parameters for the site that are in conformance with the 2018
IBC, which specifies a design earthquake having a two percent probability of occurrence in 50 years
(return interval of 2,475 years), and the 2008 USGS seismic hazard maps.
Table 1 – 2018 IBC Seismic Design Parameters
Site Class Spectral Acceleration
at 0.2 sec. (g)
Ss
Spectral Acceleration
at 1.0 sec. (g)
S1
Site Coefficients Design Spectral
Response
Parameters
Fa Fv SDS SD1
D 1.473 0.542 1.000 1.500 0.958 0.542
The spectral response accelerations were obtained from the USGS Earthquake Hazards Program
Interpolated Probabilistic Ground Motion website (2008 data) for the project latitude and longitude.
Hazards associated with seismic activity include liquefaction potential and amplification of ground motion.
Liquefaction is caused by a rise in pore pressures in a loose, fine sand deposit beneath the groundwater
table. It is our opinion that the medium dense or better glacial outwash deposits interpreted to underlie
the site and nearby vicinity have a low potential for liquefaction or amplification of ground motion.
Erosion Hazard
The criteria used for determination of the erosion hazard for affected areas include soil type, slope
gradient, vegetation cover, and groundwater conditions. The erosion sensitivity is related to vegetative
cover and the specific surface soil types, which are related to the underlying geologic soil units. The Soil
Survey of King County Area, Washington, by the Natural Resources Conservation Service (NRCS), was
reviewed to determine the erosion hazard of the on-site soils. The surface soils for this site were mapped
as Indianola loamy sand, 5 to 15 percent slopes. The erosion hazard for this material is listed as slight. This
site is relatively level to gently sloping and there are no steep slopes on the property. It is our opinion that
the erosion hazard for site soils should be low in areas where the site is not disturbed.
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CONCLUSIONS AND RECOMMENDATIONS
General
It is our opinion that the planned development within the site is generally feasible from a geotechnical
standpoint. Our explorations indicated that the site is generally underlain by competent native glacial till
soils at depth throughout the site. The native glacial bearing soils encountered at depth should provide
adequate support for foundation, slab, and pavement loads. We recommend that the planned structure be
designed utilizing conventional shallow foundations. Footings should extend through any loose soil or
undocumented fill soils and be founded on the underlying medium dense or better native glacial till soils, or
structural fill extending to these soils.
The medium dense or better native glacial bearing soils should typically be encountered approximately 2.0
to 6.0 feet below the existing surface, based on our explorations. In general, the competent native glacial
soils were shallower within the western portion of the site and were deepest within the very eastern
portion of the site. We should note that localized areas of deeper unsuitable soils and/or undocumented
fill could be encountered at this site. This condition would require additional excavations in foundation,
slab, and pavement areas to remove the unsuitable soils.
Based on the results of our on-site infiltration testing and soil explorations throughout the site, it is our
opinion that the onsite native granular outwash soils encountered within the western and central portion
of the site are conducive for full stormwater infiltration methods. However, due to the deeper
undocumented fill soils and presence of perched groundwater within our very eastern explorations, it is our
opinion that stormwater infiltration is not feasible within the very eastern portion of the property. This is
further discussed in the Site Drainage section of this report.
The surficial soils encountered on this site are considered moisture-sensitive and will disturb easily when
wet. We recommend that construction take place during the drier summer months, if possible. If
construction is to take place during wet weather, the soils may disturb, and additional expenses and delays
may be expected due to the wet conditions. Additional expenses could include the need for placing a
blanket of rock spalls to protect exposed subgrades and construction traffic areas. Some of the native on-
site soils may be suitable for use as structural fill depending on the moisture content of the soil during
construction. NGA should be retained to determine if the on-site soils can be used as structural fill material
during construction.
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Erosion Control
The erosion hazard for the on-site soils is interpreted to be slight to moderate for exposed soils, but actual
erosion potential will be dependent on how the site is graded and how water is allowed to concentrate.
Best Management Practices (BMPs) should be used to control erosion. Areas disturbed during construction
should be protected from erosion. Erosion control measures may include diverting surface water away
from the stripped or disturbed areas. Silt fences and/or straw bales should be erected to prevent muddy
water from leaving the site. Disturbed areas should be planted as soon as practical and the vegetation
should be maintained until it is established. The erosion potential of areas not stripped of vegetation
should be low.
Site Preparation and Grading
After erosion control measures are implemented, site preparation should consist of stripping the topsoil,
undocumented fill and loose soils from foundation, slab, pavement areas, and other structural areas, to
expose medium dense or better native bearing glacial soils. The stripped soil should be removed from the
site or stockpiled for later use as a landscaping fill. Based on our observations, we anticipate stripping
depths of 2.0 to 6.0 feet, depending on the specific locations. In general, the competent native glacial soils
were shallower within the western portion of the property and deeper within the eastern portion of the
property. However, additional stripping may be required if areas of deeper undocumented fill and/or loose
soil are encountered in unexplored areas of the site.
After site stripping, if the exposed subgrade is deemed loose, it should be compacted to a non-yielding
condition and then proof-rolled with a heavy rubber-tired piece of equipment. Areas observed to pump or
weave during the proof-roll test should be reworked to structural fill specifications or over-excavated and
replaced with properly compacted structural fill or rock spalls. If loose soils are encountered in the
pavement areas, the loose soils should be removed and replaced with rock spalls or granular structural fill.
If significant surface water flow is encountered during construction, this flow should be diverted around
areas to be developed, and the exposed subgrades should be maintained in a semi-dry condition.
If wet conditions are encountered, alternative site stripping and grading techniques might be necessary.
These could include using large excavators equipped with wide tracks and a smooth bucket to complete site
grading and covering exposed subgrade with a layer of crushed rock for protection. If wet conditions are
encountered or construction is attempted in wet weather, the subgrade should not be compacted as this
could cause further subgrade disturbance. In wet conditions, it may be necessary to cover the exposed
subgrade with a layer of crushed rock as soon as it is exposed to protect the moisture sensitive soils from
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disturbance by machine or foot traffic during construction. The prepared subgrade should be protected
from construction traffic and surface water should be diverted around areas of prepared subgrade.
The site soils are considered to be moisture-sensitive and will disturb easily when wet. We recommend that
construction take place during the drier summer months if possible. However, if construction takes place
during the wet season, additional expenses and delays should be expected due to the wet conditions.
Additional expenses could include the need for placing a blanket of rock spalls on exposed subgrades,
construction traffic areas, and paved areas prior to placing structural fill.
Wet weather grading will also require additional erosion control and site drainage measures. Some of the
native on-site soils may be suitable for use as structural fill, depending on the moisture content of the soil
at the time of construction. NGA should be retained to evaluate the suitability of all on-site and imported
structural fill material during construction.
Temporary and Permanent Slopes
Temporary cut slope stability is a function of many factors, including the type and consistency of soils,
depth of the cut, surcharge loads adjacent to the excavation, length of time a cut remains open, and the
presence of surface or groundwater. It is exceedingly difficult under these variable conditions to estimate a
stable, temporary, cut slope angle. Therefore, it should be the responsibility of the contractor to maintain
safe slope configurations at all times as indicated in OSHA guidelines for cut slopes.
The following information is provided solely for the benefit of the owner and other design consultants and
should not be construed to imply that Nelson Geotechnical Associates, Inc. assumes responsibility for job
site safety. Job site safety is the sole responsibility of the project contractor.
For planning purposes, we recommend that temporary cuts in the upper undocumented fill/surficial soils
be no steeper than 2 Horizontal to 1 Vertical (2H:1V). Temporary cuts in the competent native glacial
outwash soils at depth should be no steeper than 1.5H:1V. If significant groundwater seepage or surface
water flow were encountered, we would expect that flatter inclinations would be necessary.
We recommend that cut slopes be protected from erosion. The slope protection measures may include
covering cut slopes with plastic sheeting and diverting surface runoff away from the top of cut slopes. We
do not recommend vertical slopes for cuts deeper than four feet, if worker access is necessary. We
recommend that cut slope heights and inclinations conform to appropriate OSHA/WISHA regulations.
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Permanent cut and fill slopes should be no steeper than 2H:1V. However, flatter inclinations may be
required in areas where loose soils are encountered. Permanent slopes should be vegetated, and the
vegetative cover maintained until established.
Foundations
Conventional shallow spread foundations should be placed on medium dense or better native glacial
outwash soils or be supported on structural fill or rock spalls extending to those soils. Native medium
dense or better glacial bearing soils should be encountered approximately 2.0 to 6.0 feet below the existing
ground surface based on our explorations. We typically encountered deeper areas of surficial
undocumented fill soils within our explorations within the eastern portion of the site, and shallower
undocumented fill soils within the western portion of the site.
Where undocumented fill or less dense soils are encountered at footing bearing elevation, the subgrade
should be over-excavated to expose native bearing soil. The over-excavation may be filled with structural
fill, or the footings may be extended down to the competent native soils. If footings are supported on
structural fill, the fill zone should extend outside the edges of the footing a distance equal to half of the
depth of the over-excavation below the bottom of the footing. In case of excessive undocumented fill
thickness, deep foundation options may be required. NGA is available to work with the structural engineer
to explore those options.
Footings should extend at least 18 inches below the lowest adjacent finished ground surface for frost
protection and bearing capacity considerations. Foundations should be designed in accordance with the
2018 IBC. Footing widths should be based on the anticipated loads and allowable soil bearing pressure.
Water should not be allowed to accumulate in footing trenches. All loose or disturbed soil should be
removed from the foundation excavation prior to placing concrete.
For foundations constructed as outlined above, we recommend an allowable bearing pressure of not more
than 2,000 pounds per square foot (psf) be used for the design of footings founded on the medium dense
or better native soils or structural fill extending to the competent native bearing material. The foundation
bearing soil should be evaluated by a representative of NGA. We should be consulted if higher bearing
pressures are needed. Current IBC guidelines should be used when considering increased allowable bearing
pressure for short-term transitory wind or seismic loads. Potential foundation settlement using the
recommended allowable bearing pressure is estimated to be less than 1-inch total and ½-inch differential
between adjacent footings or across a distance of about 20 feet, based on our experience with similar
projects.
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Lateral loads may be resisted by friction on the base of the footing and passive resistance against the
subsurface portions of the foundation. A coefficient of friction of 0.35 may be used to calculate the base
friction and should be applied to the vertical dead load only. Passive resistance may be calculated as a
triangular equivalent fluid pressure distribution. An equivalent fluid density of 200 pounds per cubic foot
(pcf) should be used for passive resistance design for a level ground surface adjacent to the footing. This
level surface should extend a distance equal to at least three times the footing depth.
These recommended values incorporate safety factors of 1.5 and 2.0 applied to the estimated ultimate
values for frictional and passive resistance, respectively. To achieve this value of passive resistance, the
foundations should be poured “neat” against the native medium dense soils or compacted fill should be
used as backfill against the front of the footing. We recommend that the upper one foot of soil be
neglected when calculating the passive resistance.
Retaining Walls
Specific grading plans for this project were not available at the time this report was prepared but retaining
walls may be incorporated into project plans. In general, the lateral pressure acting on retaining walls is
dependent on the nature and density of the soil behind the wall, the amount of lateral wall movement
which can occur as backfill is placed, wall drainage conditions, and the inclination of the backfill. For walls
that are free to yield at the top at least one thousandth of the height of the wall (active condition), soil
pressures will be less than if movement is limited by such factors as wall stiffness or bracing (at-rest
condition). We recommend that walls supporting horizontal backfill and not subjected to hydrostatic
forces, be designed using a triangular earth pressure distribution equivalent to that exerted by a fluid with a
density of 35 pcf for yielding (active condition) walls, and 55 pcf for non-yielding (at-rest condition) walls.
A seismic design loading of 8H should also be included in the wall design, where “H” represents the total
height of the wall.
These recommended lateral earth pressures are for a drained granular backfill and are based on the
assumption of a horizontal ground surface behind the wall for a distance of at least the height of the wall,
and do not account for surcharge loads. Additional lateral earth pressures should be considered for
surcharge loads acting adjacent to walls and within a distance equal to the height of the wall. This would
include the effects of surcharges such as traffic loads, floor slab loads, slopes, or other surface loads. We
could consult with the structural engineer regarding additional loads on retaining walls during final design,
if needed.
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The lateral pressures on walls may be resisted by friction between the foundation and subgrade soil, and by
passive resistance acting on the below-grade portion of the foundation. Recommendations for frictional
and passive resistance to lateral loads are presented in the Foundations subsection of this report.
All wall backfill should be well compacted as outlined in the Structural Fill subsection of this report. Care
should be taken to prevent the buildup of excess lateral soil pressures due to over-compaction of the wall
backfill. This can be accomplished by placing wall backfill in 8-inch loose lifts and compacting the backfill
with small, hand-operated compactors within a distance behind the wall equal to at least one-half the
height of the wall. The thickness of the loose lifts should be reduced to accommodate the lower
compactive energy of the hand-operated equipment. The recommended level of compaction should still be
maintained.
Permanent drainage systems should be installed for retaining walls. Recommendations for these systems
are found in the Subsurface Drainage subsection of this report. We recommend that we be retained to
evaluate the proposed wall drain backfill material and observe installation of the drainage systems.
Structural Fill
General: Fill placed beneath foundations, pavement, or other settlement-sensitive structures should be
placed as structural fill. Structural fill, by definition, is placed in accordance with prescribed methods and
standards, and is monitored by an experienced geotechnical professional or soils technician. Field
monitoring procedures would include the performance of a representative number of in-place density tests
to document the attainment of the desired degree of relative compaction. The area to receive the fill
should be suitably prepared as described in the Site Preparation and Grading subsection prior to beginning
fill placement.
Materials: Structural fill should consist of a good quality, granular soil, free of organics and other
deleterious material, and be well graded to a maximum size of about three inches. All-weather fill should
contain no more than five-percent fines (soil finer than U.S. No. 200 sieve, based on that fraction passing
the U.S. 3/4-inch sieve). Some of the more granular native on-site soils may be suitable for use as structural
fill, but this will be highly dependent on the moisture content of these soils at the time of construction. We
should be retained to evaluate all proposed structural fill material prior to placement.
Fill Placement: Following subgrade preparation, placement of structural fill may proceed. All filling should
be accomplished in uniform lifts up to eight inches thick. Each lift should be spread evenly and be
thoroughly compacted prior to placement of subsequent lifts. All structural fill underlying building areas
and pavement subgrade should be compacted to a minimum of 95 percent of its maximum dry density.
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Maximum dry density, in this report, refers to that density as determined by the ASTM D-1557 Compaction
Test procedure. The moisture content of the soils to be compacted should be within about two percent of
optimum so that a readily compactable condition exists. It may be necessary to over-excavate and remove
wet soils in cases where drying to a compactable condition is not feasible. All compaction should be
accomplished by equipment of a type and size sufficient to attain the desired degree of compaction and
should be tested.
Slab-on-Grade
Slabs-on-grade should be supported on subgrade soils prepared as described in the Site Preparation and
Grading subsection of this report. We recommend that all floor slabs be underlain by at least six inches of
free-draining gravel with less than three percent by weight of the material passing Sieve #200 for use as a
capillary break. A suitable vapor barrier, such as heavy plastic sheeting (6-mil, minimum), should be placed
over the capillary break material. An additional 2-inch-thick moist sand layer may be used to cover the
vapor barrier. This sand layer may be used to protect the vapor barrier membrane and to aid in curing the
concrete.
Pavements
Pavement subgrade preparation and structural filling where required, should be completed as
recommended in the Site Preparation and Grading and Structural Fill subsections of this report. The
pavement subgrade should be proof-rolled with a heavy, rubber-tired piece of equipment, to identify soft
or yielding areas that require repair. The pavement section should be underlain by a stable subgrade. We
should be retained to observe the proof-rolling and recommend repairs prior to placement of the asphalt or
hard surfaces.
Utilities
We recommend that underground utilities be bedded with a minimum six inches of pea gravel prior to
backfilling the trench with on-site or imported material. Trenches within settlement sensitive areas should
be compacted to 95 percent of the modified proctor as described in the Structural Fill subsection of this
report. Trench backfill should be compacted to a minimum of 95 percent of the modified proctor maximum
dry density. Trenches located in non-structural areas and five feet below roadway subgrade should be
compacted to a minimum 90 percent of the maximum dry density. The trench backfill compaction should
be tested.
Geotechnical Engineering Evaluation NGA File No. 1227220
Nguyen Aberdeen Avenue NE Short Plat Residential Development February 26, 2021
Renton, Washington Page 12
NELSON GEOTECHNICAL ASSOCIATES, INC.
Site Drainage
Infiltration: The subsurface soils within our explorations at depth generally consisted of granular glacial
outwash soils to the depths explored within the western and central portion of the site and native alluvial
soils within the very eastern portion of the property. In accordance with the 2016 King County Surface
Water Design Manual (KCSWDM), we conducted one Small PIT within Infiltration Pit 1 within the central
portion of the property as shown on the attached Site Plan in Figure 2. Infiltration Pit 1 measured 4.0-feet
long by 3.0-feet wide by 8.0-feet deep. Due to the granular nature of the site soils and the maximum
capacity of the on-site water source, we were only able to maintain approximately 2.0-inches of standing
water within Infiltration Pit 1 instead of the recommended 12-inches. This level was maintained for
approximately 6 hours for the pre soak period of the test.
After the 6-hour soaking period was completed, the water level was maintained at approximately 2-inches
for one hour for the steady-state period with the maximum flow rate of the on-site water source. At this
time, the water flow rate into the hole was monitored with a Great Plains Industries (GPI) TM 050 water
flow meter. The maximum flow rate of the on-site water source for Infiltration Pit 1 stabilized at 6.67
gallons per minute (400.2 gallons per hour), which equates to an approximate infiltration rate of 53.50
inches per hour. The water was shut off after the steady-state period of the test and was monitored for the
falling head portion of the test. After 2 minutes, the water level within the pit had fully infiltrated resulting
in an infiltration rate of 60.0 inches per hour.
It is our opinion that the native granular outwash soils encountered at depth within the western and central
portion of the property are suitable for traditional stormwater infiltration. The subsurface soils within the
western and central portion of the property generally consisted of granular outwash sand soils at depth.
We have selected the most conservative measured field rate of 53.5 in/hr obtained from the falling head
portions of the test in our infiltration pit to be utilized in determining the long-term design infiltration rate
for the infiltration systems within the western and central portions of the property. We referenced
Equation 5-11 within Chapter 5.2.1 of the (KCSWDM) that applies correction factors to the field measured
infiltration rate to generate a long-term design infiltration rate. Correction factors of 0.50, 0.90, and 0.80
were utilized in this equation for Ftesting, Fgeometry, Fplugging respectively, resulting in an infiltration rate of 19.25
inches per hour, to be utilized to design any on-site infiltration systems founded within the native granular
outwash soils within the western and central portions of the property. We recommend that the base of the
infiltration systems within the western and central portions of the property be terminated within the native
granular outwash soils encountered at approximately 0.5 to 6.0 feet below the existing ground surface
within the western and central portions of the property. We recommend that stormwater infiltration
systems not be located within the eastern portion of the property due to the presence of surficial
Geotechnical Engineering Evaluation NGA File No. 1227220
Nguyen Aberdeen Avenue NE Short Plat Residential Development February 26, 2021
Renton, Washington Page 13
NELSON GEOTECHNICAL ASSOCIATES, INC.
undocumented fill and perched groundwater encountered at depth within our explorations within the very
eastern portion of the property. NGA should be retained to observe infiltration trench excavations.
The stormwater manual recommends a three-foot separation between the base of an infiltration system
and any underlying bedrock, impermeable horizon, or groundwater. We did not encounter groundwater
seepage within our test pit explorations within the western and central portion of the site to a depth of
approximately 11.5 feet below the existing ground surface. We recommend that the base of any proposed
infiltration systems be located to maintain minimum separation from any groundwater and impermeable
horizons in accordance with the stormwater manual and the City of Renton requirements. We also
recommend that any proposed infiltration systems be placed as to not negatively impact any proposed or
existing nearby structures and also meet all required setbacks from existing property lines, structures, and
sensitive areas as discussed in the drainage manual. Infiltration systems should not be located within
proposed fill areas within the site associated with site grading or retaining wall backfill as such condition
could lead to failures of the placed fills and/or retaining structures. We recommend that the base of the
on-site infiltration systems be extended through the upper undocumented fill and surficial soils and
terminated within the native glacial outwash soils encountered at depth throughout the site. We should be
retained during construction to evaluate the soils exposed in the infiltration systems to verify that the soils
are appropriate for infiltration.
Surface Drainage: The finished ground surface should be graded such that stormwater is directed to an
approved stormwater collection system. Water should not be allowed to stand in any areas where footings,
slabs, or pavements are to be constructed. Final site grades should allow for drainage away from the
residences. We suggest that the finished ground be sloped downward at a minimum gradient of three
percent, for a distance of at least 10 feet away from the residences. Surface water should be collected by
permanent catch basins and drain lines and be discharged into an approved discharge system.
Subsurface Drainage: If groundwater is encountered during construction, we recommend that the
contractor slope the bottom of the excavation and collect the water into ditches and small sump pits where
the water can be pumped out and routed into a permanent storm drain.
We recommend the use of footing drains around the structures. Footing drains should be installed at least
one foot below planned finished floor elevation. The drains should consist of a minimum 4-inch-diameter,
rigid, slotted or perforated, PVC pipe surrounded by free-draining material wrapped in a filter fabric. We
recommend that the free-draining material consist of an 18-inch-wide zone of clean (less than three-
percent fines), granular material placed along the back of walls. Pea gravel is an acceptable drain material.
Geotechnical Engineering Evaluation NGA File No. 1227220
Nguyen Aberdeen Avenue NE Short Plat Residential Development February 26, 2021
Renton, Washington Page 14
NELSON GEOTECHNICAL ASSOCIATES, INC.
The free-draining material should extend up the wall to one foot below the finished surface. The top foot
of backfill should consist of impermeable soil placed over plastic sheeting or building paper to minimize
surface water or fines migration into the footing drain. Footing drains should discharge into tightlines
leading to an approved collection and discharge point with convenient cleanouts to prolong the useful life
of the drains. Roof drains should not be connected to wall or footing drains.
CONSTRUCTION MONITORING
We should be retained to provide construction monitoring services during the earthwork phase of the
project to evaluate subgrade conditions, temporary cut conditions, fill compaction, and drainage system
installation.
USE OF THIS REPORT
NGA has prepared this report for Mr. Long Nguyen and his agents, for use in the planning and design of the
development on this site only. The scope of our work does not include services related to construction
safety precautions and our recommendations are not intended to direct the contractors’ methods,
techniques, sequences, or procedures, except as specifically described in our report for consideration in
design. There are possible variations in subsurface conditions between the explorations and also with time.
Our report, conclusions, and interpretations should not be construed as a warranty of subsurface
conditions. A contingency for unanticipated conditions should be included in the budget and schedule.
We recommend that NGA be retained to provide monitoring and consultation services during construction
to confirm that the conditions encountered are consistent with those indicated by the explorations, to
provide recommendations for design changes should the conditions revealed differ from those anticipated,
and to evaluate whether or not earthwork and foundation installation activities comply with contract plans
and specifications. We should be contacted a minimum of one week prior to construction activities and
could attend pre-construction meetings if requested.
Within the limitations of scope, schedule, and budget, our services have been performed in accordance
with generally accepted geotechnical engineering practices in effect in this area at the time this report was
prepared. No other warranty, expressed or implied, is made. Our observations, findings, and opinions are
a means to identify and reduce the inherent risks to the owner.
o-o-o
Geotechnical Engineering Evaluation NGA File No. 1227220
Nguyen Aberdeen Avenue NE Short Plat Residential Development February 26, 2021
Renton, Washington Page 15
NELSON GEOTECHNICAL ASSOCIATES, INC.
It has been a pleasure to provide service to you on this project. If you have any questions or require further
information, please call.
Sincerely,
NELSON GEOTECHNICAL ASSOCIATES, INC.
Lee S. Bellah, LG
Project Geologist
Khaled M. Shawish, PE
Principal
LSB:KMS:dy
Six Figures Attached
LOG OF EXPLORATION
DEPTH (FEET) USC SOIL DESCRIPTION
DJO:DPN NELSON GEOTECHNICAL ASSOCIATES, INC.
FILE NO 1227220
FIGURE 4
INFILTRATION PIT ONE
0.0 – 3.5 GRASS UNDERLAIN BY LIGHT BROWN TO DARK BROWN, SILTY FINE TO MEDIUM SAND WITH
GRAVEL, COBBLES, IRON OXIDE WEATHERING, ORGANICS, AND ROOTS
(LOOSE TO MEDIUM DENSE, MOIST) (FILL)
3.5 – 5.5 ORANGE-BROWN TO BROWN, SILTY FINE TO MEDIUM SAND WITH ROOTS, IRON OXIDE
WEATHERING, GRAVEL, COBBLES, AND TRACE ORGANICS (MEDIUM DENSE, MOIST) (FILL)
5.5 – 10.0 SP-SM GRAY-BROWN TO GRAY, FINE TO COARSE SAND WITH GRAVEL, COBBLES, SILT, ROOTS,
AND IRON OXIDE WEATHERING (MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE NOT COLLECTED
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
TEST PIT CAVING WAS NOT ENCOUNTERED
TEST PIT WAS COMPLETED AT 10.0 FEET ON 2/5/21
TEST PIT ONE
0.0 – 3.0 GRASS UNDERLAIN BY BROWN TO LIGHT BROWN, SILTY FINE TO MEDIUM SAND WITH
GRAVEL, ROOTS, AND ORGANICS (LOOSE TO MEDIUM DENSE, MOIST) (FILL)
3.0 – 5.0 DARK BROWN TO BLACK, SILTY FINE TO MEDIUM SAND WITH GRAVEL, TRACE ROOTS, AND
ORGANICS (LOOSE TO MEDIUM DENSE, MOIST) (FILL)
5.0 – 8.0 ML GRAY TO GRAY-BROWN, SILT WITH FINE SAND, ORGANIC PARTICULATE, IRON OXIDE
STAINING (STIFF TO VERY STIFF, MOIST)
8.0 – 10.0 SP-SM GRAY TO GRAY-BROWN, FINE TO MEDIUM SAND WITH SILT
(MEDIUM DENSE TO DENSE, MOIST TO WET)
SAMPLES WERE COLLECTED AT 5.5 AND 8.5 FEET
GROUNDWATER SEEPAGE WAS ENCOUNTERED AT 8.0
TEST PIT CAVING WAS NOT ENCOUNTERED
TEST PIT WAS COMPLETED AT 10.0 FEET ON 2/5/21
TEST PIT TWO
0.0 – 3.0 GRASS UNDERLAIN BY BROWN, SILTY FINE TO MEDIUM SAND WITH ROOTS, ORGANICS,
AND GRAVEL (LOOSE TO MEDIUM DENSE, MOIST) (FILL)
3.0 – 5.0 DARK BROWN TO BLACK, SILTY FINE TO MEDIUM SAND WITH GRAVEL, ROOTS, ORGANICS,
ASPHALT CHUNKS AND TRACE COBBLES (LOOSE TO MEDIUM DENSE, MOIST) (FILL)
5.0 – 10.0 SM ORANGE-BROWN TO BROWN, SILTY FINE TO MEDIUM SAND WITH GRAVEL
(MEDIUM DENSE, MOIST)
SAMPLES WERE NOT COLLECTED
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
TEST PIT CAVING WAS NOT ENCOUNTERED
TEST PIT WAS COMPLETED AT 10.0 FEET ON 2/5/21
LOG OF EXPLORATION
DEPTH (FEET) USC SOIL DESCRIPTION
DJO:DPN NELSON GEOTECHNICAL ASSOCIATES, INC.
FILE NO 1227220
FIGURE 5
TEST PIT THREE
0.0 – 0.5 GRASS UNDERLAIN BY SILTY, FINE TO MEDIUM SAND WITH ROOTS, ORGANICS, AND
GRAVEL (LOOST TO MEDIUM DENSE, MOIST) (FILL)
0.5 – 1.5 SM GRAY-BROWN, SILTY FINE TO MEDIUM SAND WITH GRAVEL AND IRON OXIDE STAINING
(MEDIUM DENSE, MOIST)
1.5 – 10.5 SP BROWN-GRAY FINE TO COARSE SAND WITH GRAVEL AND TRACE SILT
(MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE COLLECTED AT 3.0, 6.0, AND 9.0 FEET
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
SLIGHT TEST PIT CAVING WAS ENCOUNTERED BETWEEN 4.0 AND 10.0 FEET
TEST PIT WAS COMPLETED AT 10.5 FEET ON 2/5/21
TEST PIT FOUR
0.0 – 0.5 GRASS UNDERLAIN BY DARK BROWN SILTY FINE TO MEDIUM SAND WITH GRAVEL, ROOTS,
AND ORGANICS (LOOST TO MEDIUM DENSE, MOIST) (FILL)
0.5 – 3.0 SM BROWN-GRAY, SILTY FINE TO MEDIUM SAND WITH GRAVEL (MEDIUM DENSE, MOIST)
3.0 – 10.0 SP BROWN-GRAY, FINE TO COARSE SAND WITH GRAVEL AND TRACE SILT
(MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE COLLECTED AT 5.0 AND 9.0 FEET
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
TEST PIT CAVING WAS ENCOUNTERED BETWEEN 5.0 AND 10.0 FEET
TEST PIT WAS COMPLETED AT 10.0 FEET ON 2/5/21
TEST PIT FIVE
0.0 – 1.5 GRASS UNDERLAIN BY DARK BROWN TO ORANGE BROWN, SILTY FINE TO COARSE SAND
WITH GRAVEL, TRACE COBBLES, AND IRON OXIDE WEATHERING
(LOOSE TO MEDIUM DENSE, MOIST) (FILL)
1.5 – 11.0 SP GRAY TO ORANGE-GRAY, FINE TO COARSE SAND WITH GRAVEL, ROOTS, IRON-OXIDE
WEATHERING, COBBLES, AND TRACE SILT (MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE COLLECTED AT 5.0 AND 9.0 FEET
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
SLIGHT TEST PIT CAVING WAS ENCOUNTERED AT 1.5 FEET
TEST PIT WAS COMPLETED AT 11.0 FEET ON 2/5/21
TEST PIT SIX
0.0 – 1.0 GRASS UNDERLAIN BY DARK BROWN TO ORANGE-BROWN, SILTY FINE TO COARSE SAND
WITH GRAVEL, TRACE COBBLES, AND IRON OXIDE WEATHERING
(LOOSE TO MEDIUM DENSE, MOIST) (FILL)
1.0 – 3.0 GRAY TO GRAY-BROWN, SILTY FINE SAND WITH ROOTS, ORGANICS, AND GRAVEL (LOOSE
TO MEDIUM DENSE, MOIST) (FILL)
3.0 – 5.5 DARK BROWN TO BROWN, SILTY FINE TO MEDIUM SAND WITH GRAVEL, TRACE ROOTS,
ORGANICS, IRON OXIDE WEATHERING, AND TRACE COBBLES
(LOOSE TO MEDIUM DENSE, MOIST) (FILL)
5.5 – 11.5 SP GRAY TO ORANGE-GRAY, FINE TO COARSE SAND WITH GRAVEL, ROOTS, IRON OXIDE
WEATHERING, COBBLES, AND TRACE SILT (MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE COLLECTED 2.0, 5.0, AND 10 FEET
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
TEST PIT CAVING WAS NOT ENCOUNTERED
TEST PIT WAS COMPLETED AT 11.5 FEET ON 2/5/21
LOG OF EXPLORATION
DEPTH (FEET) USC SOIL DESCRIPTION
DJO:DPN NELSON GEOTECHNICAL ASSOCIATES, INC.
FILE NO 1227220
FIGURE 6
TEST PIT SEVEN
0.0 – 3.0 GRASS UNDERLAIN BY LIGHT BROWN TO BROWN, SILTY FINE TO MEDIUM SAND WITH
ROOTS, ORGANICS, AND GRAVEL (LOOSE TO MEDIUM DENSE, MOIST) (FILL)
3.0 – 6.0 ORANGE-BROWN TO BROWN, SILTY FINE TO MEDIUM SAND WITH GRAVEL, TRACE
COBBLES, IRON OXIDE WEATHERING, AND ROOTS
(LOOSE TO MEDIUM DENSE, MOIST) (FILL)
5.5 – 11.5 SP GRAY TO ORANGE-GRAY, FINE TO COARSE SAND WITH GRAVEL, ROOTS, IRON OXIDE
WEATHERING, COBBLES, AND TRACE SILT (MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE COLLECTED 2.0, 5.0, AND 10 FEET
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
TEST PIT CAVING WAS NOT ENCOUNTERED
TEST PIT WAS COMPLETED AT 11.5 FEET ON 2/5/21
TEST PIT EIGHT
0.0 – 4.5 GRASS UNDERLAIN BY DARK BROWN TO GRAY-BROWN, SILTY FINE TO MEDIUM SAND WITH
ROOTS, GRAVEL, ORGANICS, AND IRON OXIDE STAINING
(LOOSE TO MEDIUM DENSE, MOIST) (FILL)
4.5 – 7.0 SM BROWN TO GRAY-BROWN, SILTY FINE TO MEDIUM SAND WITH TRACE GRAVEL, IRON OXIDE
WEATHERING AND TRACE ROOTS (MEDIUM DENSE TO DENSE, MOIST TO WET)
7.0 – 10.5 SM GRAY TO GRAY-BROWN, SILTY FINE TO MEDIUM SAND WITH TRACE IRON OXIDE STAINING
(MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE COLLECTED 6.0 AND 10.0 FEET
GROUNDWATER SEEPAGE WAS ENCOUNTERED AT 8.0 FEET
TEST PIT CAVING WAS NOT ENCOUNTERED
TEST PIT WAS COMPLETED AT 10.5 FEET ON 2/5/21
TEST PIT NINE
0.0 – 4.5 GRASS UNDERLAIN BY DARK BROWN TO GRAY-BROWN, SILTY FINE TO MEDIUM SAND WITH
ROOTS, GRAVEL, ORGANICS, AND IRON OXIDE STAINING
(LOOSE TO MEDIUM DENSE, MOIST) (FILL)
4.5 – 8.0 SM ORANGE-BROWN TO BROWN, SILTY FINE TO MEDIUM SAND WITH TRACE GRAVEL, IRON
OXIDE WEATHERING AND TRACE ROOTS (MEDIUM DENSE TO DENSE, MOIST TO WET)
8.0 – 10.5 SM GRAY TO GRAY-BROWN, SILTY FINE TO MEDIUM SAND WITH TRACE IRON OXIDE STAINING
(MEDIUM DENSE TO DENSE, MOIST)
SAMPLE WAS COLLECTED 10.0 FEET
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
SLIGHT TEST PIT CAVING WAS ENCOUNTERED AT 8.0 FEET
TEST PIT WAS COMPLETED AT 10.5 FEET ON 2/5/21
TEST PIT TEN
0.0 – 3.0 GRASS UNDERLAIN BY ORANGE BROWN, SILTY FINE TO MEDIUM SAND WITH GRAVEL,
TRACE COBBLES, AND IRON OXIDE WEATHERING (LOOSE TO MEDIUM DENSE, MOIST) (FILL)
3.0 – 5.5 SP GRAY TO ORANGE-GRAY, FINE TO COARSE SAND WITH GRAVEL, ROOTS, IRON OXIDE
WEATHERING, COBBLES, AND TRACE SILT (MEDIUM DENSE TO DENSE, MOIST)
SAMPLES WERE NOT COLLECTED
GROUNDWATER SEEPAGE WAS NOT ENCOUNTERED
TEST PIT CAVING WAS NOT ENCOUNTERED
TEST PIT WAS COMPLETED AT 5.5 FEET ON 2/5/21