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ARCHIVED REPORTS_XR0011735
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ARCHIVED REPORTS_XR0011735
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Last modified
10/10/2020 11:30:50 PM
Creation date
6/23/2020 3:55:02 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011735
RECORD_ID
PR0515450
PE
2960
FACILITY_ID
FA0012153
FACILITY_NAME
SOUTH SHORE PARCEL
STREET_NUMBER
0
STREET_NAME
WEBER
STREET_TYPE
AVE
City
STOCKTON
Zip
95202
CURRENT_STATUS
01
SITE_LOCATION
WEBER AVE
QC Status
Approved
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Appendix B Cone Penetration Test Boring Investigation <br /> Phase lI ESA Multi-Modal Station"Six-Block Project" <br /> January 6,2003 <br /> Page 3 of 3 <br /> t. 3.0 DISCUSSION OF RESULTS <br /> The geologic logs from borings CPT I through CPT5 were compared in order to evaluate the lateral <br /> continuity of the subsurface lithology beneath the site Representative geologic cross-sections depicting <br /> the subsurface lithology of the site were prepared by integrating the Information contained In each of the <br /> CPT logs and selected Geoprobe and detection boring logs Geologic cross-section locations are shown in <br /> Figure 5, Appendix A Geologic cross-section A-A' (Figure 12, Appendix A) was constructed along an <br /> east/west orientation, looking to the north, and geologic cross-section B-B' (Figure 13, Appendix A) was <br /> constructed along a northwest/southeast orientation, looking to the northeast The CPT bonngs indicate <br /> the subsurface geology beneath the site is generally homogeneous below the six-block area Eolian sands, <br /> represented in the area on published geologic maps, were not noted in any of the borings completed <br /> during this investigation <br /> Soils encountered in the CPT borings were predominantly interbedded clays and silts with sporadically <br /> occurring thin beds of stiff fine-grained material and sand From the surface to a depth of approximately <br /> 27 5 feet bgs (CPT1) to 36 5 feet bgs (CPT4), the subsurface lithology is generally composed of <br /> interbedded layers of clay and silt with transitional layers of clayey silt and silty clay With the exception <br /> of the soils encountered in CPTI, the silt and clayey silt soils are more prevalent in this zone than the <br /> clay-rich soils In CPTI, primarily silty soils and clayey soils were encountered in roughly equivalent <br /> abundance Sand and silty sand layers that may correspond to water-bearing zones were generally <br /> encountered at or near the basal portions of this uppermost subsurface zone <br /> Sand and silty sand layers encountered between approximately 27 5 feet and 39 feet bgs in the CPT <br /> borings appear to represent a continuous sand and silty sand unit and likely correspond to the first <br /> groundwater at depth across the site Sand and silty sand layers were encountered at approximate depths <br /> . of 28 to 32 feet bgs and 108 to 115 feet bgs in CPT1, 30 to 31 feet bgs and 43 feet bgs In CPT2, 28 to 33 <br /> feet bgs in CPT3, 36 to 39 feet bgs and 115 to 120 feet bgs in CPT4, and 34 to 36 feet bgs, 95 to 97 feet <br /> bgs, 109 to 115 feet bgs, 119 to 121 feet bgs, 134 to 137 feet bgs, and 170 to 174 feet bgs in CPT5 The <br /> detection and hydropunch borings were advanced to approximate depths of 45 feet bgs to collect <br /> groundwater samples from this shallow zone <br /> Interbedded silts, clayey silts, silty clays, and clays comprise the majority of the subsurface between <br /> approximately 39 feet and 110 feet bgs With the exception of CPT2, the primarily silty soils and clayey <br /> soils were encountered in roughly equivalent abundance to a depth of approximately 110 feet bgs The <br /> soils encountered in CPT2 were predominantly silts and clayey silts with sparsely interbedded clay-rich <br /> soil layers <br /> A semi-continuous sand layer was encountered at an approximate depth of 117 to 119 feet bgs in borings <br /> CPT4 and CPT5 In CPT5, this sand layer was separated from another sand layer between approximate <br /> depths of 109 feet and 115 feet bgs by a predominantly silty layer This upper member of the lower sand <br /> unit was also encountered in CPTI at an approximate depth of 108 to 115 feet bgs Boring PAI and <br /> hydropunch boring HBK4-730-1 were advanced to approximate depths of 114 feet bgs and 110 feet bgs, <br /> respectively, to collect groundwater samples from the deeper zone The logs for borings CPT2 and CPT3 <br /> do not indicate the presence of a potentially water-bearing semi-contmuous sand unit at these depths <br /> Other discontinuous sand and/or silty sand layers were encountered at approximate depths of 43 feet bgs <br /> in CPT2 and 95 to 97 feet bgs in CPT5 <br /> I <br /> Based on the soils encountered in CPT5 at depths greater than 120 feet bgs, the site subsurface is <br /> comprised primarily of interbedded silts, clays, and transitional soils between these types to an <br /> approximate depth of 170 feet bgs Additional deep sand and silty sand layers were encountered in CPT5 <br /> • at approximate depths of 134 to 137 feet bgs and 170 to 173 feet bgs <br />
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