HomeMy WebLinkAboutSubsoil Study for Foundation Design 02.12.2024l{3n Kuma & A*soclabs, lnc.@
Geotechnical and Materials Engineers
and Environmental Scientists
An Employsc OrvnGd Compony
5020 County Road 154
Glenwood Springs, CO 81601
phone: (970) 945-7988
fax: (970) 945-8454
email: kaglenwood@kumarusa.com
www.kumarusa.com
Oflfice Locations: Denver (HQ), Parker, Colorado Springs, Fort Collins, Glenwood Springs, and Summit County, Colorado
SUBSOIL STUDY
FOR FOUNDATION DESIGN
PROPOSED RESIDENCE
5970 COUNTY ROAD 109
GARFIELD COUNTY, COLORADO
PROJECT NO.23-7-705
FEBRUARY 12,2024
PREPARED FOR:
TODD CHRISTMAN
5970 COUNTY ROAD 109
CARBONDALE, COLORADO 81623
todd@ unionpropertvcapital.com
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TABLE OF CONTENTS
PURPOSE AND SCOPE OF STUDY
PROPOSED CONSTRUCTION
SITE CONDITIONS
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a-J-
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SUBSIDENCE POTENTIAL.
FOI.INDATIONS ....
FLOOR SLABS......:
FIELD EXPLORATION
SUBSURFACE CONDITIONS ......
DESIGN RECOMMENDATIONS ...... - 5 -
6-
UNDERDRAIN SYSTEM.............. ..., 6 .
SURFACE DRAINAGE ,,..7 .
LIMITATIONS 7-
FIGURE 1 - LOCATION OF EXPLORATORY BORINGS
FIGURE 2 - LOGS OF EXPLORATORY BORINGS
FIGURE 3 - GRADATION TEST RESULTS
TABLE 1 _ SUMMARY OF LABORATORY TEST RESULTS
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PURPOSE AND SCOPE OF STUDY
This report presents the results ofa subsoil study for a proposed residence to be located at
5970 County Road 109, Garfield County, Colorado. The project site is shown on Figure l.
The purpose of the study was to develop recommendations for the foundation design. The
study was conducted in accordance with our proposal for geotechnical engineering services
to Todd Christman dated December 15, 2023.
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 reporl 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 one- and two-story structure with an attached
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a below grade mechanical room. Ground floors will either be slab-on -grade or over
craw the residence and slab in the garage and ADU. Gradi ng for the structure
is assumed to be relatively minor with cut depths between about Z'to 10 feet. We assume
relatively light foundation loadings, typical of the proposed type of construction.
If building loadings, location or grading plans change significantly from those desuibed above,
we should be notified to re-evaluate the recommendations contained in this report.
SITE CONDITIONS
The lot was occupied with an existing residence which will be razed and the new residence
constructed in its place. Vegetation consists of grass with trees and landscaping. The ground
surface through most of the proposed building footprint has a gentle to moderate slope down
toward the Crystal River which borders the lot on the northeast side. The ground surface wis
covered in2to 3 inches of patchy snow.
SUBSIDENCE POTENTIAL
Bedrock of the Pennsylvanian Age Eagle Valley Evaporite underlies most of the lower Roaring
Fork valley, including the subject site. These rocks are a sequence of gypsiferious shale, fine-
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grained sandstone/siltstone, 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 property. Dissolution of the gypsum under certain conditions can cause sinkholes
to develop and can produce areas of localized subsidence. During previous work in the arca,
several broad subsidence areas and sinkholes have been observed. These sinkholes appear
similar to others associated with the Eagle Valley Evaporite in areas of the lower Roaring Fork
River valley.
No evidence of subsidence or sinkholes was observed on the property or 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 at the
site throughout the service life of the structure, in our opinion is low, however the owner should
be aware 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 January 23,2024. Three 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-458 drill rig. The borings were logged by a representative of Kumar and
Associates.
Samples of the subsoils were taken with a l3A rnch 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. In
Boring l, below about 6 inches of topsoil, the subsoils consist of dense sandy gravel and cobbles
with probable boulders (river alluvium) down to the explored depth of 3% feet. In Boring 2,
below about 6 inches of topsoil, and in Boring 3, below about 6 inches of road base gravel and
6 inches of topsoil. The subsoils consist of about lYzto 2 feet of medium dense sandy gravel and
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clay underlain by dense silty sandy gravel and cobbles with probable boulders (river alluvium)
down to the maximum explored depths of 3 and 4 feet, respectively. Drilling in the dense
granular soils with auger equipment was difficult due to the cobbles and boulders and drilling
refusal was encountered in all three borings in the deposit.
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 I%-inch fraction) of the coarse granular subsoils are shown on Figure 3. 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.
DESIGN RECOMMENDATIONS
FOLINDATIONS
Considering the subsurface conditions encountered in the exploratory borings and the nature of
the proposed construction, we recommend the buildings be founded with spread footings bearing
on the natural granular soils.
The design and construction criteria presented below should be observed for a spread footing
foundation system.
1) Footings placed on the undisturbed natural granular soils should be designed for
an allowable bearing pressure of 3,000 psf. Based on experience, we expect
settlement of footings designed;d'ffited as discussed in this section will
be about I inch or less.
2) The footings should have a minimum width of_Ejnches for continuous walls and
2.feet-fot 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 3_6 inches below exterior grade is typically used in this
atea.
4) Continuous foundation walls should be reinforced top and bottom to span local
anomalies such as by assuming an unsupported length of at least l0 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
45 pcf for the onsite sand and gravel soil as backfill.
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All topsoil, clay soil, existing fill and any loose or disturbed soils should be
removed and the footing bearing level extended down to the relatively dense
natural granular soils. The exposed soils in footing area should then be moistened
and compacted.
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 granular 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 well graded
sand and gravel (such as road base) should be placed beneath interion slabs-on-grade for
subgrade support. This material should consist of minus 2-inch aggregate with at least 50%
retained on the No. 4 sieve and less than l2%o passing the No. 200 sieve. A minimum 4-inch
layer of free draining gravel should be placed beneath the below grade mechanical room floor
slab to facilitate drainage. This material should consist of minus 2-inch aggregate with at least
50Yo rctained on the No. 4 sieve and less than 2%o passing the No. 200 sieve.
All fill materials for supporl of floor slabs should be compacted to at least 95o/o of maximum
standard Proctor density at a moisture content near optimum. Required fill can consist of the
on-site granular soils or suitable imported granular fil1 devoid of vegetation, topsoil and
oversized rock.
L]NDERDRAIN SYSTEM
It has been our experience in the area that local perched groundwater can develop during times of
heavy precipitation or seasonal runoff. Frozen ground during spring runoffcan create a perched
condition. We recommend below-grade construction, such as retaining walls, crawlspace and
basement areas, be protected from wetting and hydrostatic pressure buildup by an underdrain and
wall drain system.
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 I foot below lowest adjacent finish grade and sloped at a minimum l%o to
a suitable gravity outlet or drywell. Free-draining granular material used in the underdrain
s)
6)
Kumar & Associates, lnc, @ Project No. 23-7-705
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system should contain less than 2o/o 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 l% feet
deep.
SURFACE DRAINAGE
The following drainage precautions should be observed during construction and maintained at all
times after the residence has been completed:
l) 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 95o/o 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 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. Free-draining wall backfill should be
covered with filter fabric and capped with about 2 feet of the on-site finer graded
soils to reduce surface water infiltration.
4) Roof downspouts and drains should discharge well beyond the limits of all
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 i, 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
Kumar & Associates, lnc. o Project No. 23.7.705
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should provide continued consultation and field services during construction to review and
monitor the implonentation of our recommendations, and to veriry 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 bearing strata and testing of structural fill by a representative of
the geotechnical engineer.
Respectfully Submitted,
Kumsr & Asss!€iates, In*"
David A. Noteboom, StaffEngineer
Reviewed by:
Steven L. Pawlak,
SLP/kac
Cc: Hinge Architects &es{@Jsp&ardqEts,q{s " e**il
Kssst*& Acseeffi& Fne" a Fro,ssi Sls. t97-ffi
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15 0
APPROXIMATE SCALE_FEET
109 *TO COUNTY ROAD
12.20'
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x-7 -7A5 Kumar & Associates LOCATION OF TXPLORATORY BORINGS Fig. 1
F
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s
F
F
I
BORING 1
EL. 6,1 02'
BORING 2
EL. 6,1 04'
BORINO 3
EL. 6,1 00'
0
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0
F
LrJtdt!
IrFo-
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F
Lrl
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tdo
33/12
WC=5.6
*4=31
-2OO=23
26/6,1s/o
21/12
WC=11.1
*4=17
-2OO=34
25/2, 1o/o
LEGEND
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GRAVEL DRIVEWAY FILL; DENSE, MOIST/FROZEN, MIXED GRAY AND BROWN
TOPSOTL; ORGANTC SANDY S|LT, SLIGHTLY CLAYEY WrrH SCATTERED GRAVEL, F|RM/FROZEN,
MOIST, DARK BROWN.
GRAVEL AND COBBLE (GM) SANDY, S|LTY, PROBABLE BOULDERS, DENSE, SLtcHTLy MO|ST,
MIXED GRAY AND BROWN WITH RED.
GRAVEL AND CLAY (Gc-cL); SANDY, SILTY, MEDIUM DENSE, MOIST, DARK BROWN MlX.
DR|VE SAMP:E, 1 S/9-|NCH r.D. SPL|T SPOON STANDARD PENETRATTON TEST.
33/ 12 DRIVE SAMPLE BLOW COUNT. INDICATES THAT 33 BLOWS OF A 1 4O-POUND HAMMER
FALTING 30 INCHES WERE REQUIRED TO DRIVE THE SAMPLER 12 INCHES.
PRACTICAL AUGER REFUSAL.
NOTES
1. THE EXPLORATORY BORINGS WERE DRILLED ON JANUARY 23, 2024 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.
3. THE ELEVATIONS OF THE EXPLORATORY BORINGS WERE OBTAINED BY INTERPOLATION BETWEEN
CONTOURS ON THE SITE PLAN PROVIDED.
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 RESULTSI
WC = WATER CONTENT (%) (ASTM D2216);
+4 = PERCENTAGE RETAINED ON NO. 4 SIEVE (ASTM D6913);
-200= PERCENTAGE PASSING No.200 SIEVE (ASIM 01140).
i
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23-7 -7 05 Kumar & Associates LOGS OF EXPLORATORY BORINGS Fig. 2
6
I
t00
90
EO
70
ao
50
40
30
20
10
o
HYDROMETER ANALYSIS
IIME REAOINGS
HRS 7 HRS
SIEVE ANALYSIS
.1.
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-.-"j* -i i,,,i,:,,i,,,,:.':: ,:j:r.,::i:.;j-;:,f;l,t;,1--t,i,L.';',.t'itt.-;,i;,,,tt,t,i '-,j,'.,i'j,..,t,i
o
to
20
30
40
50
60
70
ao
so
100
=b
.300 r .500
.125
PARTICLES
1.18
2.O
ILLIMETERS
152
DIAMETER OF INM
CLAY TO SILT COBBLES
GRAVEL 31 % SAND 16 %
LIQUID LIMIT - PLASTICITY INDEX
SAMPLE OF: Sllly Grovelly Sond
SILT AND CLAY 23%
FROM:Boringl@2'
2
&
too
90
80
70
50
40
30
ao
t0
0
to
20
30
40
50
60
70
80
90
?b
&
.123
ARTICLES IN
2,O
D OF
CLAY TO SILT COBBLES
GRAVEL 17 % SAND
LIQUID LIMIT
SAMPLE OF: GroYelly Cloy€y Sond
49%
PLASTICITY INDEX
SILT AND CLAY 34 %
only lo lh6
FROM:BoringS@2'sompl6s which Iho
losllng roport shqll nol bo r€producod,
oxcopt ln full, wlthoul the wrlll€n
opprovol of Kumor & Assoclol€s, lnc,
Sleve onolysls t.sllng ls p.rformsd ln
qccordonc€ wlth ASTM 06313, ASTM 07928,
ASTM Cl36 ond,/or ASTM Dl140.
SAND GRAVEL
FINE MEDTUM lcornse FIN E COARSE
HYDROMETER ANALYSIS
HRS 7 HRS
SIEVE ANALYSIS
OPENINCS
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--t, ti,r,,tt ,i.t. ,t;,.j ,',,-i it,r tt-'i,,,--..,,1.,',t .,,,J ,,
'''''\
SAND GRAVEL
FI NE MEDTUM lcoansE FINE COARSE
23*7 -705 Kumar & Associates GRADATION TEST RISULTS Fig.3
ICA*iffift*trfffi$f i*"'
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TABLE 1
SUMMARY OF LABORATORY TEST RESULTS
No.23-7-705
SAMPT LOCATION noN AT LIMITS
BORING
tffl
OEPTH
r0l.1
NATURAL
MOISTURE
CONTENT
NATURAL
DRY
DENSITY
16cll
GRAVEL
(:/"1
SAND
Pl
PERCENT
PASSING NO,
200 stEVE
to/"\
LIQUID LIMIT
tr/^\
PLASTIC
INDEX
(osf)
UNCONFINED
COMPRESSIVE
STRENGTH SOIL TYPE
I 2 5.6 3l 46 Silty Gravelly Sand
3 2 1l.t 17 49 34 Gravelly Clayey Sand