HomeMy WebLinkAboutSoils Report for Foundation Design 11.07.2007GeoteCh
HEPWORTH - PAWLAK GEOTECHNICAL
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SUBSOIL
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SUBSOIL STUDY
FOR FOUNDATION DESIGN
PROPOSED SCHNEIDER RESIDENCE
LOT E-52, ASPEN GLEN SUBDIVISION
KINGFISHER LANE
GARFIELD COUNTY, COLORADO
JOB NO. 107 0760
NOVEMBER 7, 2007
PREPARED FOR:
JORDAN ARCHITECTURE
ATTN: BRAD JORDAN
P.O. BOX 1031
GLENWOOD SPRINGS, COLORADO 81602
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TABLE OF CONTENTS
PURPOSE AND SCOPE OF STUDY - I -
PROPOSED CONSTRUCTION - 1 -
SITE CONDITIONS _ _
SUBSIDENCE POTENTIAL
FIELD EXPLORATION -3 -
SUBSURFACE CONDITIONS -3 -
DESIGN RECOMMENDATIONS - 4 -
FOUNDATIONS - 4 -
FLOOR SLABS - 5 -
SURFACE DRAINAGE - 5 -
LIMITATIONS - 6 -
REFERENCES - 7 -
FIGURE 1 - LOCATION OF EXPLORATORY BORINGS
FIGURE 2- LOGS OF EXPLORATORY BORINGS
FIGURE 3- LEGEND AND NOTES
FIGURE 4- GRADATION TEST RESULTS
PURPOSE AND SCOPE OF STUDY
This report presents the results of a subsoil study for the proposed Schneider residence to
be located on Lot E-52, Aspen Glen Subdivision, Kingfisher Lane, 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 Jordan
Architecture dated October 3, 2007. Chen-Northem, Inc. (1991 and 1993) previously
conducted preliminary geotechnical engineering studies for the development and
preliminary plat design.
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 and other
engineering characteristics. The results of the 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 proposed residence will be a two story wood frame structure with an attached garage.
Ground floor will be structural over a crawlspace for the living areas and slab -on -grade in
the garage. There will be a second story of living space above the garage. Grading for
the structure is assumed to be relatively minor with cut depths between about 3 to 4 feet.
We assume relatively light foundation loadings, typical of the proposed type of
construction.
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If building loadings, Iocation or grading plans change significantly from those described
above, we should be notified to re-evaluate the recommendations contained in this report.
SITE CONDITIONS
The site was vacant at the time of our field exploration. There is an existing pond to the
east of the lot. The ground surface is relatively flat with a gentle slope down to the
northwest at grades up to about 6% and about 2 feet of elevation difference. Vegetation
consists of grass and weeds. Scattered cobbles were exposed on the ground surface.
SUBSIDENCE POTENTIAL
Bedrock of the Pennsylvanian age Eagle Valley Evaporite underlies the Aspen Glen
development. These rocks are a sequence of gypsiferous shale, fine-grained
sandstone:isiltstone and limestone with some massive beds of gypsum. There is a
possibility that massive gypsum deposits associated with the Eagle Valley Evaporite
underlie portions of the lot. Dissolution of the gypsum under certain conditions can cause
sinkholes to develop and can produce areas of localized subsidence. During previous
studies in the area, several broad subsidence areas and smaller size sinkhole areas were
observed scattered throughout the Aspen Glen development, predominantly on the east
side of the Roaring Fork River (Chen -Northern, Inc., 1993). The nearest sinkhole was
mapped about 450 feet to the southwest of Lot E-52 and a broad subsidence area was
mapped just to the north of the lot. These sinkholes appear similar to others associated
with the Eagle Valley Evaporite in areas of the Roaring Fork River valley.
Sinkholes were not observed in the immediate area of the subject lot. No evidence of
cavities was encountered in the subsurface materials; however, the exploratory borings
were relatively shallow, for foundation design only. Based on our present knowledge of
the subsurface conditions at the site, it cannot be said for certain that sinkholes will not
develop. The risk of future ground subsidence on Lot E-52 throughout the service life of
the proposed residence, in our opinion, is low; however, the owner should be made aware
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of the potential for sinkhole development. If further investigation of possible cavities in
the bedrock below the site is desired, we should be contacted.
FIELD EXPLORATION
The field exploration for the project was conducted on October 30, 2007. Two
exploratory borings were drilled at the locations shown on Figure 1 to evaluate the
subsurface conditions. 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 Hepworth-Pawlak Geotechnical, Inc.
Samples of the subsoils were taken with a I% inch I.D. spoon sampler. The sampler was
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 of the 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.
SUBSURFACE CONDITIONS
Graphic logs of the subsurface conditions encountered at the site are shown on Figure 2.
The subsoils consist of about 1 foot of topsoil overlying relatively dense, slightly silty
sandy gravel with cobbles and boulders to the drilled depths of 11 and 141/.. feet.
Laboratory testing performed on samples obtained from the borings included natural
moisture content and gradation analyses. Results of gradation analyses performed on
small diameter drive samples (minus 11:2 inch fraction) of the coarse granular subsoils are
shown on Figure 4.
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No free water was encountered in the borings at the time of drilling and the subsoils were
slightly moist.
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 granular subsoils.
The design and construction criteria presented below should be observed for a spread
footing foundation system.
I) Footings placed on the undisturbed natural granular subsoils should be
designed for an allowable bearing pressure of 3,000 psf. Based on
experience, we expect settlement of footings designed and constructed as
discussed in this section will be about 1 inch or less.
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.
Placement of foundations at least 36 inches below exterior grade is
typically used in this area.
4) Continuous foundation walls should be reinforced top and bottom to span
local anomalies such as by assuming an unsupported length of at least 10
feet. Foundation walls acting as retaining structures should also be
designed to resist a lateral earth pressure corresponding to an equivalent
fluid unit weight of at least 50 pcf.
5) The topsoil and any loose or disturbed soils should be removed and the
footing bearing level extended down to the natural granular soils. The
exposed soils in footing area should then be moistened and compacted.
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6) A representative of the geotechnical engineer should observe all footing
excavations prior to concrete placement to evaluate bearing conditions.
FLOOR SLABS
The natural on-site soils, exclusive of topsoil, are suitable to support lightly loaded slab -
on -grade construction. To reduce the effects of some differential movement,
nonstructural 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 interior slabs -on -grade 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 fill can
consist of the on-site soils devoid of vegetation, topsoil and oversized rock.
SURFACE DRAINAGE
The following drainage precautions should be observed during construction and
maintained at all times after the residence has been completed:
I) Inundation of the 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° o of the maximum standard Proctor density in
pavement and slab areas and to at Ieast 90% of the maximum standard
Proctor density in landscape areas.
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3) The ground surface surrounding the exterior of the building should be
sloped to dram away from the foundation in all directions. We
recommend a minimum slope of 6 inches in the first 10 feet in unpaved
areas and a minimum slope of 3 inches in the first 10 feet in paved areas.
4) Roofdownspouts and drains should discharge well beyond the limits of al
backfill.
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
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
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bearing strata and testing of structural fill by a representative of the geotechnical
engineer.
Respectfully Submitted,
HEPWORTH - PAWLAK GEOTECHNICAL, INC.
Jordy Z. Adamson, Jr., P.E.
Reviewed by:
Steven L. Pawlak, P.E.
JZAJvad
REFERENCES
Chen -Northern, Inc., 1991, Preliminary Geotechnical Engineering Study, Proposed
Aspen Glen Development, Garfield County, Colorado, prepared for Aspen Glen
Company, dated December 20, 1991, Job No. 4 112 92.
Chen -Northern, Inc., 1993, Geotechnical Engineering Study for Preliminary Plat Design,
Aspen Glen Development, Garfield County, Colorado, prepared for Aspen Glen
Company, dated May 28, 1993, Job No. 4 112 92.
Job No. 107 0760
APPROXIMATE SCALE
1"=30'
LOT E-51
107 0760
1000
\
\
1001
LOT E-52
• BORING 2
r
PROPOSED
RESIDENCE
BORING 1
•
HEPWORTH.PAWLAK GEOTECHNICAL.
1000
KINGFISHER DRIVE
1001
1002 1
1
- 1
--�
1
\
1002
LOCATION OF EXPLORATORY BORINGS
LOT E-53
Figure 1
1005
1000
995
990
985
BORING 1
ELEV.= 1002'
20/6,18/3
4' 45/12
WC=1.7
s a +4=48
-200=9
BORING 2
ELEV.= 1000'
Q
.e.
So'
• �S
sa
47/12
28/6,23/3
WC- 1 7
+4=61
-200=8
60/12
31/6,19/3
d1
Note: Explanation of symbols is shown on Figure 3.
1005
1000
995
990
985
Elevation - Feet
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Hepworth—Pawlak Geotechnical
LOGS OF EXPLORATORY BORINGS
Figure 2
LEGEND_
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TOPSOIL; sandy silt and clay, organics, roots, firm, slightly moist, brown
GRAVEL (GP -GM); sandy, slightly silty, with cobbles and boulders, dense, slightly moist, brown.
Drive sample; standard penetration test (SPT), 1 3/8 inch LD. split spoon sample, ASTM D-1586.
45/12 Drive sample blow count: indicates that 45 blows of a 140 pound hammer falling 30 inches were
required to drive the SPT sampler 12 inches.
NOTES:
1. Exploratory borings were drilled on October 30, 2007 with 4 -inch diameter continuous flight power auger.
2. Locations of exploratory borings were measured approximately by pacing from features shown on the site plan
provided.
3. Elevations of exploratory borings were obtained by interpolation between contours shown on the site plan provided
and checked by instrument level.
4. The exploratory boring locations and elevations 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. No free water was encountered in the borings at the time of drilling. Fluctuation in water level may occur with time.
7. Laboratory Testing Results
WC a Water Content (%)
+4 = Percent retained on the No. 4 sieve
-200 Percent passing No 200 sieve
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LEGEND AND NOTES
Figure 3
'CENT RETAIN BA
ENT RETAIN It
HYDROMETER ANALYSIS I SIEVE ANALYSIS I
TIME READINGS f U.S. STANDARD SERIES 1 CLEAR SQUARE OPENINGS
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COBBLES
GRAVEL 48 %
LIQUID LIMIT %
SAMPLE OF: Slightly Silty Sand and Gravel
SAND 43 %
SILT AND CLAY 9 %
PLASTICITY INDEX %
FROM: Boring 1 at 5 Feet
HYDROMETER ANALYSIS U.S.SIEVE ANALYSIS 1
TIME READINGS STANDARD SERIES 1 CLEAR SQUARE OPENINGS I
45
IN. 15 MIN 60MIN19MIN 4 MIN. 1 MIN. #200 #100 #50 #30 #16 #8 #4 318' 3/4' 1 112' 3' 5'6' 8'
—�, 100
10
20
30
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50
60
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100
001 002 005 009 019 037 074 150 300 .600 1 18 2.36
DIAMETER OF PARTICLES IN MILLIMETERS
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GRAVEL 61 %
LIQUID LIMIT %
SAMPLE OF: Slightly Silty Sandy Gravel
107 0760
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Hepworth—Pawlak Geatechnieol
MEDIUM 1 COARSE
s -ems
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90
80
70
so
50
40
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4 75 9.512 519 0 37 5 76.2 12152 203
FOIE I comsE
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SAND 31 % SILT AND CLAY 8 %
PLASTICITY INDEX %
FROM: Boring 2 at 5 and 10 Feet, Combined
GRADATION TEST RESULTS
`CENT PA kC
Figure 4