HomeMy WebLinkAboutSoils Report 01.24.2018H.PVKUMAR 5020 County Road 154
Glenwood Springs, CO 81ô01
Phone: (970) 945-7988
Fax (970) 945-8454
Email : hpkglenwood@kumarusa.com
Geotechnical Engineering I Engineering Geology
Materials Testing I Environmental
Office Locations: Denver (HQ), Parker, Colorado Springs, Fort Collins, Glenwood Springs, Summit County, Colorado
January 24,2018
Steven I(oski
306 Rabbit Road
Carbonclale, Colorado 81 623
steven @ tomroachfl oors.com
Project No.17-7-842
Subject:Subsoil Study for Foundation Design, Proposed Residence, Lol7, Stirling Ranch,
405 Skipper Drive, Missouri Heights, Garfield County, Colorado
Dear Steven:
As requested, H-P/Kumar performed a subsoil study for design of foundations at the subject site.
The stucly was conducted in accordance with our agreement for geotechnical engineering
services to you dated November 29,2011. The data obtained and our recommendations based on
the proposed constrnction and subsulface conditions encountered are presented in this report.
Proposed Construction: Design plans were pleliminary at the time of our stuciy. The proposecl
4,000 sqllare foot residence will be 1 and 2 story wood frame construction over a crawlspace or
basement located on the site as shown on Figure 1. Cut depths are expected to range between
about 2 to 8 feet. Founclation loadings for this type of construction are assulned to be relatively
light and typical of the proposed type of construction.
If building conditions or foundation loadings are significantly differeut from those described
above, we should be notifiecl to re-evahrate the recornmenclations presented in this report.
Site Conditions: The lot was vacant with a gravel driveway and water line into the site. The lot
slopes gently to moderately down to the east with grades of 2 to 10 percent. South of the
building area, the lot slopes steeply down to the south. Vegetation at the site consists of pinon
and juniper trees with sparse grass and weeds. Scattered basalt cobbles and boulders wers
observed on the ground surface.
Subsurface Conditions: The subsurface conditions at the site were evaluated by excavating two
exploratory pits at the approximate locations shown on Figure 1. The logs of the pits are
presented on Figure 2. The subsoils encountered, below about l to lVz feet of topsoil, consist of
basalt gravel, cobbles and boulders in a calcareous sandy silt matrix down to the maximum depth
a-L-
explored, \Vz feet. Results of swell-consolidation tcsting pcrfonned on a relatively undisturbed
sample of the sandy silt matrix soils, presented on Figure 3, indicate low comptessibility under
existing low moisture conditions and light loading and a moderate collapse potential (settlement
under constant load) when wetted. Results of graclation analyses performed on samples of the
basalt rock soils (minus lVz and 5 inch fraction) obtained from the site are presented on Figure 4.
The laboratory testing is summarized on Table 1. No free water was observed in the pits at the
time of excavation and the soils were slightly moist to moist.
Foundation Recommendations: Considering the subsoil conditions encountered in the
exploratory pits and the nature of the proposed construction, we recomlnend spread footings
placed on the undisturbed natural basalt rock soil designed for an allowable soil bearing pressure
of 2,000 psf for support of the ploposed residence. The matrix soils tend to compress after
wetting and there could be some post-construction foundation settlement. Footings shoulcl be a
minimum width of 16 inches for continuous walls and2 feet for columns. The topsoil and loose
disturbed soils encountered at the foundation bearing level within the excavation should be
removed and the footing bearing level extended down to the untlistulbed nal"ural soils. Ht-rles
below footing grade caused by basalt boulder removal should be backfilled with concrete or
imported 3/c-inchroad base compacted to at least 987o of the maximum standard Proctor density.
Exterior footings should be provided with adequate cover above their bearing elevations fol frost
protection. Placement of footings at least 36 inches below the exterior grade is typically used in
this area. Continuous foundation walls should be reinforced top and bottom to span local
anomalies such as by assuming an Llnsupported length of at least 14 feet. Foundation walls
acting as retaining strltctures should be designed to resist a lateral earth pressure based on an
equivalent fluid unit weight of at least 50 pcf for the on-site soil as backfill, excluding rock larger
than about 6 inches.
Floor Slabs: The natural on-site soils, exclnsive 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 free-draining gravel should be placed beneath basement level slabs to facilitate drainage.
This material shoulcl consist of minus ?. inch aggregate with less fhan 507o passing the No. 4
sieve and less than 2o/o passing the No. 200 sieve.
H-P!KUMAR
Project No.17-7-842
-3 -
All fill materials for support of floor slabs should be compacted to at least 95Vo of maximum
standard Proctor density at a moisture content near optimum. Required fill can consist of the on-
site soils or a suitable imported granular material such as 3/q-inch road base devoid of vegetation,
topsoil and oversized rock.
Underdrain System: Although free water was not encountered during our exploration, it has
been our experience that local perched groundwater can develop during times of heavy
precipitation or seasonal runoff. Frozen ground during spling runoffcan also create a perched
condition. We recommend below-grade construction, such as retaining walls, deep crawlspace
(greater than 4 feet) and basement areas, be protected from wetting and hydrostatic pressure
buildup by an underdrain system.
The drains should consist of drainpipe placed in the bottom of the wall backfill surrounded above
the invert level with free-draining granular matelial. The drain should be placed at each level of
excavation and at least I foot below lowest adjacent finish grade and sloped at a minimum IVo to
a suitable gravity outlet. Free-draining granular material used in the underdrain system should
contain less than 27o passing the No. 200 sieve, less than 507o passing the No. 4 sieve and have a
maximum size of 2 inches. The drain gravel backfill should be at least lVzfeet deep.
Surface Drainage: The following clrainage precautions should be observed during construction
and maintained at all times after the residence has been completed:
1) Inundation ofthe foundation excavations and underslab areas should be avoided
during construction.
2) Exterior backfill should be adjusted to near optimum moisture and compacted to
at least 957o of the maximum standard Proctor density in pavement and slab areas
and to at least 90% of the maximum standard Proctor density in lanciscape areas.
Free-clraining wall backfill shoulcl be cappecl with about 2 feet of the on-site, finer
graded soils to reduce surface water infiltration.
3) The gror.rnd surface surrounding the exterior of the building should be sloped to
drain away from the foundation in all directions. W'e recommend a minimum
slope of 12 inches in the first 10 feet in unpaved areas and a minimum slope of 3
inches in the first 10 feet in pavement and walkway areas.
4) Roof downspouts ancl drains should discharge well beyond the limits of all
backfill. Graded swales should have a minimum slope of 37o.
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 waranty either
H-PÈKUIVIAR
Project No.17-7-842
-4-
express or implied. The conclusions ancl recommendations submitted in this report are basecl
upon the data obtained from the exploratory pits excavated at the locations indicated on Figure 1
and to the depths shown on Figure 2, 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
abont 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 pits 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 at once so re-evaluation of the
recommendations may be made.
This report has been prepared for the exclusive use by our client for design pulposes. 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 ancl
monitclr the irnplerrentation of our recommettdations, aud to verify that the recolunenclations
have been appropriately interpreted. Significant design changes may require additional analysis
or modifications to the recommendations presented herein. We recommend on-site observation
of excavations and foundation bearing strata ancl testing of structural fill by a representative of
the geotechnical engineer.
If you have any questions or if we may be of further assistance, please let us know
Respectfully Submitted,
H.P+ KUMAR
Daniel E. Hardin, P
Reviewed by: SLP
DEFVkac
attachments Figure I - Location of Exploratory Pits
Figure 2 - Logs of Exploratory Pits
Figure 3 - Swell-Consolidation Test Results
Figure 4 - Gradation Test Results
1'able 1 - Summary of Laboratory Test Results
cc JessPeclersen@
H-PèKUMAR
Project No.17-7-842
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17 -7 -842 H-PryKUMAR LOCATION OF EXPLORATORY PITS Fig. 1
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LEGEND
TOPSOIL; ORGANIC SILT AND CLAY, SANDY, FIRM, MOIST, DARK BROWN
BASALT GRAVEL COBBLES AND BOULDERS (GM) IN SANDY SILT MATRIX, DENSE, SLIGHTLY
MOIST, BROWNISH WHITE, CALCAREOUS.
F HAND DRIVEN 2_INCH DIAMETER LINER SAMPLE.
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DISÏURBED BULK SAMPLE.
NOTES
1. THE EXPLORATORY PITS WERE EXCAVATED WITH A JOHN DEERE sOG BACKHOE ON DECEMBER
8, 2017.
2. THI LOCATIONS OF THE EXPLORATORY PITS WERE MEASURED APPROXIMATELY BY PACING FROM
FEATURES SHOWN ON THE SITE PLAN PROVIDED,
3. THE ELEVATIONS OF THE EXPLORATORY PITS WERE OBTAINED BY INTERPOLATION BETWEEN
CONTOURS ON THE SITE PLAN PROVIDED.
4. THE EXPLORATORY PIT LOCATIONS AND ELEVATIONS SHOULD BE CONSIDERED ACCURATE ONLY
TO THE DEGREE IMPLIED BY THE METHOD USED.
5, IHE LINES BETWEEN MATERIALS SHOWN ON THE EXPLORATORY PIT LOGS REPRESÊ,N]'IHË
APPROXIMATE BOUNDARIES BEÏWEEN MATERIAL TYPES AND THE TRANSITIONS MAY BE GRADUAL.
6. GROUNDWATER WAS NOT ENCOUNTERED IN THE PITS AT THE TIME OF DIGGING. PITS WERE
BACKFILLED SUBSEQUENT TO SAMPLING.
7. LABORATORY TEST RESULTS:
WC = WATER CONTENT (%) (ASTM D 2216);
DD = DRY DENSTTY (pct) (aSrU D 2216);
+4 = PERCENTAGE RETAINED ON NO. 4 SIEVE (ISTU O AZZ);
-2oo = PERCENTAGE PASSING NO. 200 SIEVE (ASTM D 1 1 40)
17 -7 -842 H-PVKUMAR LOGS OF EXPLORATORY PITS Fig, 2
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t.0 APPLIED PRESSURE - KSF IO
SAMPLE OFI Calcoreous Sondy Silf Molrix
FROM:Pit2@5.5'
WC = 8.0 %, Dù = 79 pcl
ADDITIONAL COMPRESSION
UNDER CONSTANT PRESSURE
DUE TO WETTING
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17 -7 -842 H-PryKUMAR SWELL-CONSOLIDATION TEST RESULTS Fig. 3
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DIAMETER OF PARTICLES IN MILLIMETERS
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CLÁY TO SILT COBBLES
GRAVEL 23 % SAND 6T %
LIOUID LIMIÏ PLASTICIÍY INDEX
SAMPLE OF: Colcoreous Silþ Sond wllh Grovel
SILT AND CLAY 16 %
FROM:Pit1O3'-4'
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IN MILLIMETERS
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CLAY TO SILT COBBLES
GRAVEL 43
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SAND 41 7T SILT ANO CLAY
LIOUID LIMIT PLASÎICIIY INDEX
SAMPLE 0F: Colcoreous S¡lly Sond ond Groval FROM: Pil 2 O 6'-6,5'
16 I
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opprovol of l(umor t AE¡oc¡oh¡, lnc.Sl.v. onoly¡¡¡ l.sflng ¡. Þ.rfom.d ln
occordoncr wlth ASTM 0,t22, ASTI¡ Cf36ond/or ASIM Dll¡10.
HYDROMETER ANALYSIS SIEVÉ ANALYSIS
T¡UE RADITGS
24 HnS 7 HRS
U,S, STANOARO SÊRIES CLUR SOUARE OPENINCS
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FINE MEDIUM ICOARSE FINE COARSE
HYDRÓMEfER ANÂLYSIS SIEVE ANALYSIS
ilYE RADINGS
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17 -7 -842 H-PryKUMAR GRADATION TEST RESULTS Fig. 4
H,P*KUMARTABLE 1SUMMARY OF LABORATORY TEST RESULTSProject No.17-7-842SOILTYPET6Calcareous Silty Sand withGravelCalcareous Sandy SiltMatrixCalcareous Silty Sand andGravelUNCONFINEDCOMPRESSIVESTRENGTH(PSF)ATTERBERG LIMITSPLASTICINDEX(%\LIQUIDLIMIT(%lPERCENTPASSINGNO.200SIEVE16GRADATIONSAND%l6t4TGRAVEL(%)2343NATURALDRYDENSITYlocfl79NATURALMOISTURECONTENT(%l8.0SAMPLE LOCATIONDEPTHlfil3-43V26-6VzPIT12