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HomeMy WebLinkAboutSubsoil Study for Foundation Design 09.29.2021l(ln Kumar&Assoc¡ates, lnc. 5020 County Road 154 Geotechnical and Materials Engineers Glenwood Springs, CO g1601 and Environmentalsc¡ent¡sts phonà: (g7O) g45_7ggS fax: (970) 945-8454 email: kaglenwood@kumarusa.com An Employcc Owncd Compony www'kumarusa'com Office Locations: Denver (HQ), Parker, Colorado Springs, Fort Collins, Glenwood Springs, and Summit County, Colorado SUBSOIL STUDY FOR FOUNDATION DESIGN PROPOSED RESIDENCE LOT ?0,IRONBRIDGE, PHASE 3 1820 RIVER BEND WAY GARFIELD COUNTY, COLORADO PROJECT NO. 21-7-684 SEPTEMBER29,202l PREPARED FOR: SCIB, LLC ATTN: LUKE GOSDA 0115 BOOMERANG ROAD, SUITE 52018 ASPEN, COLORADO 81611 lu ke.gosda@sunriseco.com TABLE OF CONTENTS PURPUSH AND STJUPE U¡'S'I'UDY PROPOSED CONSTRUCTION SITE CONDITIONS.. SUBSIDENCE POTENTIAL.... FIELD EXPLORATION SUBSURFACE CONDITIONS FOUNDATION BEARING CONDITIONS ... DESIGN RECOMMENDATIONS . FOUNDATIONS FLOOR SLABS UNDERDRAIN SYSTEM. SURFACE DRAINAGE............... LIMITATIONS. FIGURE 1 . LOCATION OF EXPLORATORY BORINGS FIGTIRE 2 - LOGS OF EXPLORATORY BORINGS FIGURE 3 - LEGEND AND NOTES FIGURE 4 - SWELL-CONSOLIDATION TEST RESULTS FIGURE 5 - GRADATION TEST RESULTS TABLE I - SUMMARY OF LABORATORY TEST RESULTS I 1 1 ......- 3 - 1 a .-J 4 4 5 5 6 ..-6- Kumar & Associates, lnc.Project No. 21-7-684 PURPOSE AND SCOPE OF STUDY This report presents the results ofa subsoil study for a proposed residence to be located on Lot21,Ironbridge, Phase 3,1820 River Bend V/ay in 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 August 2,2021' A fîeld exploration program consisting of two 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, compressibility or swell potential, 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 At the time of our study, design plans for the residence had not been developed. The building is proposed within the building envelope shown on Figure 1. For the purposes of our analysis, we assume the proposed residence will be a one- or two- story wood-frame structure over a crawlspace with an attached slab-on-grade garage. Grading for the structure is assumed to be relatively minor with cut depths between about 2 to 5 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 described above, we should be notified to re-evaluate the recommendations contained in this report. SITE CONDITIONS The lot was vacant and appeared to have had minor cut and fill grading, likely during the subdivision development. According to historical Google Eartho aerial images dating back to lgg3,minimal site disturbance occurred on Lot20 between successive photos dated from 2007 and20l1. The surface of the lot slopes gently down to the northeast with about 3 feet of elevation difference across the assumed building area. A moderately steep slope then descends Kumar & Associates, lnc.Project No, 21-7-684 I in the middlo part and becomes gentle in the north part indicated by the contour lines on Figurc 1. Elevation diffr:r'ence aùl'oss the lot is about 20 feet. Vegetation consists of sparse grasses and weeds on the upper lot portion, oak brush on the steeper transition slope, and grasses, weeds atld scattered brush on the lower level. The Roaring Fork River is located immediately to the northeast. SUBSIDENCE POTENTIAI, 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, TggT,Job No. Ig7 32j. The natural soils on the lot mainly consist of sandy silty 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 about2 fo 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 locahzed,subsidence. A sinkhole occurred in the parking lot acljoining the golf cart storage tent in January 2005 was backf,rllcd 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 20 tlrmughout the service life of the proposed building, in our opinion, is low; however, the owner should be made 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 f'or the project was conducted on August 25, 2021. Two explo ratory borings were drilled at the approximate locations showr on Figure 1 tg evaluate the subsurface conditions. The borings were advanced with 4-inch diameter continuous flight augers powered by a truck-mountcd CME-458 drill rig. The borirrgs were logged by a representative of Kumar & Associates, Inc. Kumar & Associates, lnc,Project No.21.7.684 -J- Samples of the subsoils were taken with l%-inch and 2-inch LD. California or split-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. Below a thin topsoil or f,rll layer about T to l% feet thick and 4% feet of stiff to very stiff, slightly sandy to sandy silty clay in Boring 2,very dense, silty sandy gravel and cobbles with probable boulders was encountered down to the maximum explored depth of 11 feet. This fill was probably placed as part of initial subdivision development. Drilling in the coarse granular materials with auger equipment was diffîcult due to the cobbles and probable boulders and practical drilling refusal was encountered in the deposit. Laboratory testing performed on samples obtained from the borings included natural moisture content and density, swell-consolidation and gradation analyses. Results of swell-consolidation testing performed on a relatively undisturbed drive sample of clay soils, presented on Figure 4, indicate low compressibility under existing low moisture conditions and light loading and a moderate expansion potential when wetted under a constant light surcharge. Results of gradation analyses performed on small diameter drive samples (minus l%-inch fraction) of the 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 The upper clay soils encountered in the borings possess low bearing capacity and typically have a low to moderate settlement potential if wetted. Testing indicates the clay soil has a moderate expansion potential when wetted. Our experience in the area indicates the swell potential is minor (if any) and can be discounted in foundation design. Shallow spread footings placed on the upper natural soils can be used for support of the proposed residence with a risk of foundation movement mainly if the clay bearing soils become wetted. Alternatively, potential Kumar & Associates, lnc.Project No.21-7-684 -4- movcment can be reduced hy removing ancl replacing the clay soils below foundatiolts with compacted structural fill. Proper surface drainage as described in this report will bc critical to the long-term performance of the structure. DESIGN RECOMMENDATIONS FOUNDATIONS Considering the subsurface conditions encouutered in the exploratory borings antl the nature of the proposed construction, the building can be founded with 1) spread footings bearing on the upper natural soils, or 2) spread footings bearing on compacted structural fill or densc granular subsoils. The design and construction criteria presented below should be observed for a spread footing foundation system. 1) F'ootings placed on the upper natural soils can be designed for an allowable bearing pressure of 1,500 psf. Footings placed on undisturbed natural granular soils or structural fill can be designed for an allowable bearing pressure of 3000 psf. Based on experience, we expect initial settlement of footings aesrgi;trand constructed as discussed in this section will be about I inch or less. Additional differential movement up to about 1 inch could occur mainly if the clay bearing soils are wetted. 2) The footings should have a minimum width of 18 inches for continuous walls and 2 feet for isqlated 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 I area. below exterior grade is typically used in this 4)Continuous foundation walls should be heavily reinforced top and bottom to span local anomalies such as by assuming an unsupported length of at least 12 feet. Founclation walls acting as retaining structures should also be designed to resist a lateral earth pressure of 55 pcf for the on-site fine-grained materials or 45 pcf for the on-site granular materials. Topsoil, fill and any loose disturbed soils should be removed and the footing bearing level extended down to the firm natural soils or compacted structural fiIl. The exposed soils in footing area should then be moistened and compacted. 5) Kumar & Associates, lnc,Project No.21-7-684 -5- Structural fill should be compacted to at least 98% of standard Proctor density at near optimum moisture content and extent beyond the footing edges a distance at least one-half the depth of fill below the footing. 6) A representative ofthe geotechnical all excavations prior to concrete placement to evaluate bearing conditions. FLOOR SLABS The natural clay soils possess an expansion potential and slab heave could occur if the subgrade soils were to become wet. Vy'e should observe the soil conditions exposed at the time of excavation and evaluate them for swell-compression potential and possible mitigation such as sub-excavation and replacement with structural fill. Slab-on-grade construction can be used provided precautions are taken to limit potential movement and the risk of distress to the building is accepted by the owner. A positive way to reduce the risk of slab movement, which is commonly used in the area, is to construct structurally supported floors over crawlspace. 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. Slab reinforcement and control joints should be established by the designer based on experience and the intended slab use. A minimum 4-inch layer of sand and gravel should be placed immediately beneath garage level slabs-on-grade for support. This material should consist of minus 2-inch aggregate with less fhan 50Yo passing the No. 4 sieve and less than I2o/o passing the No. 200 sieve. Required fill beneath slabs should consist of suitable onsite sandy gravel or imported granular material, excluding topsoil and oversized rocks. The fill should be spread in thin horizontal lifts, adjusted to near optimum moisture content, and compacted to at least 95o/o of the maximum standard Proctor density. All vegetation, topsoil and loose or disturbed soil should be removed prior to fill placement. UNDERDRAIN SYSTEM It is our understanding the ground level, finished floor elevation of the residence is at or above the surrounding grade. Therefore, a foundation drain system is not recommended. It has been our experience in the area and where clay soils are present that local perched groundwater can Kumar & Associates, lnc.Project No, 21-7-684 -6- develop during times of heavy precipitation or seasonal runoff. Frozen ground during spring runoff can create a perched condition. 'We recommend below-grade construction, such as retaining walls and basement areas, if provided, be protected from wetting and hydrostatic pressure buildup by an underdrain and wall drain system. An underdrain is not recommended around the slab-at-grade garage and crawlspase area to help limit the potential lor wetting below the shallow fbotings. If the finished floor elevation of the proposed structure has a floor level below the surrounding grade or a taller crawlspace is constructed, we should be contacted to provide recommendations for an underdrain system. All earth retaining structures should be properly drained. SURFACE DRAINAGE It willbe critical to the building performance to keep the bearing soils dry. The following drainage 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 95o/o of the maximum standard Proctor density in pavement and slab areas and to at least 90Yo of the maximum standard Proctor tlensity 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 inches in the first 10 feet in paved areas. Graded swales should have a minimum slope of 3%. 4) Roof downspouts and drains should discharge well beyond the limits of all backfill. 5) Landscaping which requires regular heavy irrigation should be located at least l0 feet from foundation walls. Consideration shoulcl 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 conductcd in accorclance with generally accepted geotechnical engineering principles and practices in this area atthis time. We make no warranty either express or implied. Kumar & Associates, lnc.Project No.21-7-684 -7 - 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 theìecommendations 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 and monitor the implementation of our recommendations, and to veriff 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, Kurnar & Associateso Inc. -1\r^nV-- Mark Gayeski, E.I.T. Reviewed by: Steven L. SLPlkac f.t(- P u,15222 ó t, Kumar & Associates, lnc Project No, 21-7-684 I E e c':)MMot\l i\Hh.A PARCEL NO. 239501 424007 e+-ú- BLUE HERC,N DE"VE.LOPMENT COMPANY PARcEL No. 239501230103 ¡+ \\ ,3ð% BORING 1 w4 -..3uux"ti,. *,.J4ï \\ .Ys >Qjg."^$ 9r*""S I ¡Yb-ru\ -,9 C, ,P o BORING 2 -\:: g RIVER BEND WAY ------>'*,--1---- @-\ M 50 APPROXIMATE SCALE_FEET 11 2 tt -.3i'.1,i?åu. * 21 -7 -684 Kumar & Associates LOCATION OF TXPLORATORY BORINGS Fig. WC= 1 .0 +4=54 -2QO=12 BORING 1 EL. 5936' BORING 2 EL. 5959.5' 0 0 66/ 12 11 /12 WC=9.5 DD=99 -200=86 5 37 /6, 51 /6 27/6, sO/4 t-t¡l l¡J L! I-t-o- L¡Jô l-.-t!l¡ltL IIt-fLt¡lo 10 10 50/2.5 33/6, 50/3 15 15 Fig. 2LOGS OF EXPLORATORY BORINGSKumar & Associates21 -7 -684 I I Ê I I LEGEND N roesorr-; SANDy ro vERy sANDy srLT wrïH GRAVEL AND oRGANrcs, 'LTGHTL' Morsr, TANNro BRowN.r-¡I FILL: SILTY CLAY AND SAND WITH GRAVEL AND SCATTERED CoBBLES, FIRM oR MEDIUMDENSE, SLIGHTLY MOIST, TAN. 71gyy..lçL); ^sltGHrly sANDy ro sANDy, srlry, TRA.E cALcAREous, srFF To vERy stFF, t,/isLrcHTLv Morsr, TAN, Low puslCrry. F:Vt |.."f.J9.RåY+ ¡fD- g9BP.lql_(9!)¡._s_l-LTY, SANDY wtrH PRoBABLE SMALL B0ULDERS, vERy DENSE, [é.lsucHrly Morsr, LTGHT TO'MED|UM TAN AND ORAV. ROUñOEO ROCX. DRIVE SAMPLE, 2-INCH I.D. CALIFORNIA LINER SAMPLE I I DRIVE SAMPLE, 1 J/B-tNcH r.D. spLrr spooN sTANDARD pENETRATToN TEST. 66/12 PilT'^.'Tl'-.i',1*uu','#-Iid[?JEå'i: 'JHJ.'f,F'31u,',3å ii iR;fiP8ND HAMMER f enncrrcAL AUGER REFUSAL. NOTES THE EXPLORATORY BORINGS WERE DRILLED ON AUGUST 25, 2021 WITH A 4-INCH DIAMETERCONTINUOUS-FLIGHT POWER AUGER. THE LOCATIONS OF THE EXPLORATORY BORINGS WERE MEASURED APPROXIMATELY BY PACINGFROM FEATURES SHOWN ON THE SITE PLAN PROVIDED. THE ELEVATIONS OF THE EXPLORATORY BORINGS WERE OBTAINED BY INTERPOLATION BETWEENCONTOURS ON THE SITE PLAN PROVIDED. THE EXPLORATORY BORING LOCATIONS AND ELEVATIONS SHOULD BE CONSIDERED ACCURATEONLY TO THE DEGREE IMPLIED BY THE METHOD USED. THE LINES BETWEEN MATERIALS SHOWN ON THE EXPLORATORY BORING LOGS REPRESENT THEAPPROXIMATE BOUNDARIES BETWEEN MATERTAL TypES AND lu¡ rRnrsnoNs MAy BE cRADUAL. GROUNDWATER WAS NOT ENCOUNTERED IN THE BORINGS AT THE TIME OF DRILLING. 2. 3. 4. 5. 6 7 LABORATORY TEST RESULTS:wc = wATER CONTENT (%) (ASTM D2216);DD = DRY DENSTTY (pct) (lsrv D2216);+4 = pERCENTAGE RETATNED ON NO. 4 STEVE (ASTM D69r5);-200= PERCENTAGE PASS|NG NO. 2OO SteVe ladrv D114O).' 21 -7 -684 Kumar & Associates LEGEND AND NOTES Fig. 3 I I I ¡ E ? I SAMPLE OF: Silty Cloy FROM:Boring2@2.5' WC = 9.5 %, DD = 99 pcf -ZQQ = 86 % D-4546. tn lnc. S{€ll EXPANSION UNDER CONSTANT PRESSURE UPON WETTING 3 ñ JJ LJ =t/', I zotr o Jo U''z.o() 2 1 0 -1 2 -3 -4 1.0 APPLIED PRESSURE - KSF 10 r00 21 -7 -684 Kumar & Associates SWELL-CONSOLIDATION TEST RTSULTS Fig. 4 100 90 80 70 60 50 10 30 20 to o 10 za 50 ,+0 50 60 70 ao 90 = U . ei .oo5 .009 too.500 t9 DIAMETER OF 132 MILLIMETERS CLAY TO SILT COBBLES GRAVEL 54 % SAND LIQUID LIMIT SÁMPLE OF: Silly Sondy Grovet 31 % PLASTICITY INDEX SILT AND CLAY 12 % FROM: Boring 1 O 2.5' & 5' (Comblned) Thsso l€sl raeulls opply only lo lhc sompl€s whlch wôrå loslêd. Thslosllng roport shqll nol bo rcÞroducsd, exc€pl lñ full, wllhout lhe wrillen opprovql of Kumor & AsloclqlÇs, lno. Slovo qnolyll! lcsllng l! pcrformcd ln occordonco wlth ASIM D6915, ASTM D7928, ASTM C156 qndlor ASTM Dll¡lo. I.{YDROMSTER AIIALY6IE SIEVE AI.IALTSIS CLEAR SQUARE OPENINGS t/A' a/^ô I t/r' READINCS HRS MIN 7 HRSI5 MIN U.S. SÎANÞARD SERIES t+o I l I I I I I I j SAND GRAVEL FINE MEDTUM lCOanSE FINE COARSE 21 -7 -684 Kumar & Associates GRADATION TEST RESULTS Fig. 5 I (+rt *r#*['fflî:Ë:inlrÍå *' "TABLE 1SUMMARY OF LABORATORY TEST RESULTSSilty Sandy GravelSilty ClaySOIL TYPEUNCONFINEDCOMPRESSIVESTRENGTHPLASTICINDEXLIMITSLIQUID LIMIT86PERCENTPASSING NO.200 stEvE2134SAND(%)54GRADATION(%)GRAVEL99NATURALDRYDENSITY019.5NATURALMOISTURECONTENT2/22Y2 &.5combinedDEPTH2BORING1SAMPLENo.2l-7-684