HomeMy WebLinkAboutSubsoil StudyICrtiiffi fi*är:Ë:if '!nÊ;;'*^
An Employcc Owncd Compony
5020 County Road 154
Glenwood Springs, CO 8 160 I
phone: (970)945-7988
fax: (970) 945-8454
email : kaglenwood@kumarusa.com
www.kumarusa.com
Office Locations: Denver (HQ), Parker, Colorado Springs, Fort Collins, Glenwood Springs, and Summit County, Colorado
RECEIVED
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SUBSOIL STUDY
FOR FOUNDATION DESIGN
PROPOSED RESIDENCE
LOT 390 PHASE 3, TRONBRTDGE
BLUE HERON DRIVE
GARFIELD COUNTY, COLORADO
PROJECT NO. 21-7-435
JULY 8,2021
PREPARED FOR:
SCIBO LLC
ATTN: LUKE GOSDA
0115 BOOMERANG ROAD, SUrTE 52018
ASPEN, COLORADO 81601
lu ke.gosda@sunriseco.com
TABLE OF CONTENTS
PIJRPOSE AND SCOPE OF STI"IDY......
PROPOSED CONSTRUCTION
SITE CONDITIONS.....
GEOLOGY
FIELD EXPLORATION
SUBSURFACE CONDITIONS
FOUNDATION BEARING CONDITIONS ..
DESIGN RECOMMENDATIONS ........
FOUNDATIONS
FLOOR SLABS
UNDERDRAIN SYSTEM...
SURFACE DRAINAGD...............
LIMITATIONS.
FIGURE 1 - LOCATION OF EXPLORATORY BORINGS
FIGURE 2 - LOGS OF EXPLORATORY BORINGS
FIGURE 3 - LEGEND AND NOTES
FIGURE 4 - SWELL-CONSOLIDATION TEST RESULTS
FIGURE 5 - GRADATION TEST RESULTS
TABLE 1- SUMMARY OF LABORATORY TEST RESULTS
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Kumar & Associates, lnc. @ Project No. 2l-7-435
PURPOSE AND SCOPE OF STUDY
This report presents the results of a subsoil study for a proposed residence to be located on
Lot39, Phase 3, Ironbridge, Blue Heron Drive, 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 SCIB, LLC dated May 10, 2021.
A field exploration program consisting of exploratory borings was conducted to obtain
information on the subsurface conditions. Samples of the subsoils obtained during the f,teld
exploration were tested in the laboratory to determine their classification, compressibility or
swell and other engineering characteristics. The results of the field exploration and laboratory
testing were analyzedto 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
At the time of our study, design plans for the residence had not been developed. The building is
proposed within the upper part of the building envelope shown on Figure 1. For the purposes of
our analysis, we assume the proposed residence will be a wood frame structure over a crawlspace
with an afÍached slab-on-grade garage. Grading for the structure is assumed to be relatively
minor with cut depths between about 2 to 3 feet. V/e assume relatively light foundation loadings,
typical of the proposed type of construction.
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.
SITE CONDITIONS
The subject site was vacant at the time of our field exploration. The ground surface is gently
sloping down to the north in the proposed building area with a steep slope down to the rear
(north side) of the lot at a grade of approximately 30 percent. Vegetation consists of sparse grass
and weeds. The downhill side of Blue Heron Drive appears to be a fill bench for residence
Kumar & Associates, lnc. o Project No.2l-7-435
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construction placed during the subdivision dcvclopmcnt. Thc Roaring Fork Rivcr is locatcd
downhill about Vomile to the north.
GEOLOGY
The geologic conditions were described in a previous report conducted for planning and
preliminary design of the overall subdivision development by Hepworth-Pawlak Geotechnical
(now Kumar & Associates) dated October 29,1997, Job No. I91 327. The natural soils on the
lot mainly consist of sandy silt and clay alluvial fan deposits overlying gravel terrace alluvium of
the Roaring Fork River. The river alluvium is mainly a clast-supported deposit of rounded
gravel, cobbles, and boulders typically up to about 2 to 3 feet in size in a silty sand matrix and
overlies siltstone/claystone bedrock.
Bedrock of the Pennsylvanian age Eagle Valley Evaporite underlies the Ironbridge subdivision.
These rocks are a sequence of gypsiferous shale, fine-grained sandstone and siltstone with some
massive beds of gypsum and limestone. Dissolution of the gypsum under certain conditions can
cause sinkholes to develop and can produce areas of loçalized subsidence. A sinkhole occurred
in the parking lot adjoining the golf cart storage tent in January, 2005 located about %nlle to the
south of Lot 39 which was backfilled and compaction grouted. To our knowledge, that sinkhole
has not shown signs of reactivation such as ground subsidence since the remediation. Sinkholes
possibly related to the Evaporite were not observed in the immediate area of the subject lot.
Based on our present knowledge of the subsurface conditions at the site, it cannot be said for
certain that sinkholes related to the underlying Evaporite will not develop. The risk of future
ground subsidence on Lot 39 throughout the service life of the proposed building, in our opinion,
is low; however, the owner should be made aware ,¡f the potential f,¡r sinkh,¡le devel,rpment. If
further investigation of possible cavities in the bedrock below the site is desired, we should be
contacted.
FIELD EXPLORATION
Tlre field exploration for the pro.iect was conducted on June 14, 2021. Two exploratory borings
were drillecl at the locations shown on Figure 1 to evaluate the snbsurface conclitions. The
borings were advanced with 4-inch diameter continuous flight augers powered by a truck-
mounted CME-458 drill rig. The horings were logged hy a representative of Kumar &
Associates, Inc.
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Samples of the subsoils were taken with 1%-inch and 2-inch I.D. 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 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 l,Yzto 8 feet of relatively dense, mixed clay, silt, sand and gravel fill
overlying nllto3vz feet of stiff, sandy silt and clay soils. Dense, slightly silty sandy gravel with
cobbles was encountered below the silt and clay soils at depths of 5 to 8 feet down to the
maximum explored depth of I5Yz feet. Drilling in the dense granular soils with auger equipment
was difficult due to the cobbles and boulders and drilling refusal was encountered in Boring 2.
Laboratory testing performed on samples obtained from the borings included natural moisture
content and density and gradation analyses. Results of swell-consolidation testing performed on
relatively undisturbed drive samples, presented on Figure 4, indicate low to moderate
compressibility under conditions of loading and wetting. Results of gradation analyses
performed on small diameter drive samples (minus llz-inch fraction) of the coarse granular
subsoils are shown on Figure 5. The laboratory testing is summarized in Table 1.
No free water was encountered in the borings at the time of drilling and the subsoils were
slightly moist.
FOUNDATION BEARING CONDITIONS
Spread footing foundations placed on the relatively dense fill soil above the natural silty clay
soils or on the natural silty clay soils should be adequate for support of the proposed residence
with relatively low settlement potential. Footings bearing entirely on the dense gravel soils
should have a low settlement risk. The bearing condition of the soils exposed in the excavation
should be fuither evaluated at the time of construction.
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DßSIGN RE COMMDNDATIONS
FOUNDATIONS
Considering the subsurface conditions encountered in the exploratory borings and the nature of
the proposed construction, we recommend the building be fbunded with spread footings bearing
on the relatively dense fill soils or the natural silty clay soils if encountered.
The clesign ancl constntction criteria presented below should be observed for a spread footing
foundation system.
1) Footings placed on the relatively dense fill soils or the underlying stiff silty clay
soils should be designed for an allowable bearing pressure of 1,500 psf. Based on
experience, we expect initial settlement of footings designed and constructed as
discussed in this section will be about 1 inch or less. Post-construction settlement
could be around 1 inch mainly if the bearing soils are wetted.
2) The footings should have a minimum width of 18 inches for continuous walls and
2 feet for isolated pads.
3) Exterior footings and footings beneath unhcatcd arcas should bc 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 12 feet.
Foundation walls acting as retaining structures should also be designed to resist a
lateral carth prcssurc corrcsponding to an cquivalcnt fluid unit weight of at least
55 pcf.
5) Any topsoil and loose disturbed soils should be removed and the footing bearing
level extended down to the relatively dense fill soils or to the stiff silty clay soil
beneath the fill. The exposed soils in footing area should then be moistened and
compactecl. Additional stnrctural fill can consist of the onsite soils compacted to
at least 98% of standard Proctor density at near optimum moisture content. New
structural fill should extend laterally beyond the footing edges a distance equal to
at least one-half the fill depth below the footing.
6) A representative of the geotechnical engineer should observe all footing
excavations prior to concrete placement to evaluate bearing conditions.
Kumar & Associates, lnc. @ Project No. 21.7.435
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FLOOR SLABS
The on-site soils, exclusive of topsoil, are suitable to support lightly loaded slab-on-grade
construction. 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 relatively
well graded sand and gravel, such as road base, should be placed beneath garage level slabs for
support. This material should consist of minus 2-inch aggregate with at least 50% retained on
the No. 4 sieve and less than I2o/o passing the No. 200 sieve.
All fill materials for support of floor slabs should be compacted to at least 95Yo 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.
UNDERDRAIN SYSTEM
The proposed shallow (less than 4 feet) crawlspace and slab-on-grade garage should not require a
perimeter underdrain system provided that the site grading recommendations contained in this
report are followed. We recommend that below-grade construction, such as retaining walls, deep
crawlspace and basement areas, be protected from wetting and hydrostatic pressure buildup by
an underdrain system.
If installed, the drains should consist of drainpipe placed in the bottom of the wall backfill
surrounded above the invert level with free-draining granular material. The drain should be
placed at each level of excavation and at least 1 foot below lowest adjacent f,rnish grade and
sloped at a minimum IYo to a suitable gravity outlet or drywell based in the gravel soils. Free-
draining granular material used in the underdrain system should contain less than 2Yo passingthe
No. 200 sieve, less than 50% passing the No. 4 sieve and have a maximum size of 2 inches. The
drain gravel backfill should be at least I% feet deep. An impervious membrane such as 30 mil
PVC should be placed beneath the drain gravel in a trough shape and attached to the foundation
wall with mastic to prevent wetting of the bearing soils.
Kumar & Associates, lnc. o Project No. 21-7-435
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SURFACE DRAINAGE
Proper surface grading and drainage will be critical to prevent wetting of the bearing soils and
satisfactory perfonnance of the foundation. The following drainage precautions should be
observed during construction and maintained at all times after the residence has been completed:
1) 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 95Yo of the maximum standard Proctor density in pavement and slab areas
and to at least 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 inchcs in the first 10 feet in paved areas. Free-draining wall backfill (if any)
should be capped with about 2 feet of the on-site soils to reduce surface water
infiltration.
4) Roof downspouts and drains should discharge well beyond the limits of all
backfill.
5) Landscaping which requires regular heavy inigation should be located at least
10 feet from foundation walls. Consideration should be given to use of xeriscape
to reduce the potential for wetting of soils below the building caused by irrigation.
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 concernecl 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 pertbrmed. lf 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.
Kumar & Associates, lnc. @ Project No.21-7-435
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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 recofitmendations, and to veriff that the recommendations
have been appropriately interpreted. Significant design changes may require additional analysis
or modifications to the recoûìmendations 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,.
Kumar & Associateso
James H. Parsons, P
Reviewed by:ffi*/.
Steven L. Pawlak, P.E.
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Kumar & Associates, lnc.(i Project No. 21-7-435
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LOT 40
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LOT
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APPROXIMATE SCALE-FEET
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LOT 39
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PROPERTY
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BORING 1
12,6.e1a
21 -7 -435 Kumar & Associates LOCATION OF TXPLORATORY BORINGS 1Fig
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BORING
EL. 1 03
1 BORING 2
EL. 101.5'
0 0
23/ 12
WC=5.5
DD= 1 00
-200=69
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WC=6.3
DD= 1 08
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20 20
WC= 1 .0
+4=65
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21 -7 -435 Kumar & Associates LOGS OF EXPLORATORY BORINGS Fig. 2
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LEGEND
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FILL: SLIGHTLY GRAVELLY SANDY SILTY CLAY, VERY STIFF, SLIGHTLY MOIST, TAN TO LIGHT
BROWN.
CLAY AND SILT (CL-ML): SANDY, VERY STIFF, SLIGHTLY MOIST, LIGHT BROWN TO TAN
GRAVEL (CU): SINOY, SLtcHTLy StLTy W|TH COBBLES, PROBABLE BOULDERS, DENSE,
SLIGHTLY MOIST, LIGHT BROWN, ROUNDED ROCK.
DRIVE SAMPLE, 2_INCH I.D. CALIFORNIA LINER SAMPLE
i DRIVE SAMPLE, 1 3/8-|NCH t.D. SpLrT SPOON STANDARD pENETRATTON TEST.
cz/tc DRIVE SAMPLE BLOW COUNT. INDICATES THAT 23 BLOWS OF A 14O-POUND HAMMER2¿t tz FALLTNG J0 TNcHES wERE REQUIRED To DRtvE THE sAMpLER t2 tNcHES.
I enacrrcAL AUGER REFUSAL.
NOTES
1 , THE EXPLORATORY BORINGS WERE DRILLED ON JUNE 1 4, 2021 WITH A 4-INCH DIAMETER
CONTINUOUS-FLIGHT POWER AUGER.
2. THE LOCATIONS OF THE EXPLORATORY BORINGS WERE MEASURED APPROXIMATELY BY PACING
FROM FEATURES SHOWN ON THE SITE PLAN PROVIDED.
5. THE ELEVATIONS OF THE EXPLORATORY BORINGS WERE OBTAINED BY INTERPOLATION BETWEEN
CONTOURS ON THE SITE PLAN PROVIDED AND THE ASSUMED CONTOUR ELEVATION.
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 THE TRANSITIONS MAY BE GRADUAL.
6. GROUNDWATER WAS NOT ENCOUNTERED IN THE BORINGS AT THE TIME OF DRILLING
7. LABORATORY TEST RESULTS:
WC = WATER CONTENT (%) (ASTM D2216);
DD = DRY DENSITY (PCt) (ISTM D2216);+4 = PERCENTAGE RETAINED ON NO. 4 SIEVE (ASTM D6913);
-2oo= PERCENTAGE PASSING N0. 200 SIEVE (ASTM D1140).
21 -7 -435 Kumar & Associates LEGEND AND NOTES Fig. 5
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SAMPLE 0F: Slightly Grovelly Sondy Silty Cloy (Fill)
FROM:Boringl@5'
WC = 6.7 %, DD = 106 pcf
ADDITIONAL COMPRESSION
UNDER CONSTANT PRESSURE
DUE TO WETTING
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APPLIED PRESSURE - KSF
SAMPLE OF: Sondy Cloy ond Silt
FROM:Boring2@2.5'
WC = 6.5 %, DD = 108 pcf
ADDITIONAL COMPRESSION
UNDER CONSTANT PRESSURE
DUE TO WETTING
21 -7 -435 Kumar & Associates SWELL_CONSOLIDATION TEST RESULTS Fig. 4
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ÐIAMETER OF IN MI RS
CLAY TO SILT COBBLES
GRAVEL 65 % SAND 25
LIQUID LIMIT
SAMPLE OF: Slighlty Silty Scndy Grovel
%
PLASTICITY INDEX
SILT AND CLAY 10 %
FROM: Boring 2 gt 7.5' & 10' COMBINED
Th6s6 t€sl rosulls opply only lo lhe
somples whlch woro loslod. fhellsllng reporl shqll nol bs reproducod,
€xcapl ln full, wllhoul lh€ wrlll€n
opprovol of Kumor & AssocÌol€s, lnc.
Slovo onolysls l€sllng ls p€rformod ln
occordonca wlth ASTM D69,l5, ASTM D7928,
ASÍM Cl36 ond/or ASIM 011,10.
HYDROMETER ANALYSIS SIEVE ANALYSIS
TIME REÂDINCS
24 HRS 7 HRS
CLEAR SQUARE OPENINGS
t/an I tltr
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U.S. STANDARD SERIES
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SAND GRAVEL
FINE MEDTUM ICOARSE FINE COARSE
21 -7 -435 Kumar & Associates GRADATION TEST RTSULTS Fis. 5
I (+rt iiË*å'ffifffifn'iiÍ å' *"TABLE 1SUMMARY OF LABORATORY TEST RESULTSNo.21-7-435Sandy Clay and SiltSlightly Silty Sandy GravelSlightly Gravelly SandySiltv Clav Gill)0125651061086.3016.7Slightly Gravelly SandySOIL TYPE1005.52t/,691ATÏERBERG LIMITSGRADATIONSAMPLE LOCATIONDEPTHBORINGLIQUID LIMlTUNCONFINEDCOMPRESSIVESÏRENGTHPERCENTPASSING NO.200 sIEVENATURALDRYDENSITYNATURALMOISTURECONTENTSANDt:/,)GRAVEL(%)PLASTICINDEX52%1% &, r0combined2