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ARCHIVED REPORTS XR0001684
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ARCHIVED REPORTS XR0001684
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Last modified
5/17/2019 3:14:19 PM
Creation date
5/17/2019 2:25:51 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001684
RECORD_ID
PR0522479
PE
2957
FACILITY_ID
FA0015299
FACILITY_NAME
GEWEKE LAND DEVELOPMENT & MARKETING
STREET_NUMBER
16
Direction
S
STREET_NAME
CHEROKEE
STREET_TYPE
LN
City
LODI
Zip
95240
APN
04323013
CURRENT_STATUS
01
SITE_LOCATION
16 S CHEROKEE LN
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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19 February 2002 <br /> AGE-NC Project No 95-0109 <br /> Page 3 of 6 <br /> f <br /> r31 STRATIGRAPHY <br /> Based on the findings from the CPT soil borings, cross section A-A' was constructed to depict <br /> r ' _general llthology beneath the site (Figure 3) Generally, silty sand, sand to gravelly sand were -' <br /> encountered at depths between 5 and 20 feet bsg, 30 and 40 feet bsg, 45 and 55 feet bsg, 65 and <br /> 100 feet bsg, 120 and 125 feet bsg and 135 and 142 feet bsg Fine grained, sandy silt, clayey silt and <br />' silt were observed at all other depths CPT computer-generated boring logs are included In <br /> Appendix A <br />' 3 2 HYDROGEOLOGICAL MODEL <br />' Based on the CPT results and comparison with soil descriptions from borings previously advanced <br /> on the site, AGE has developed a preliminary subsurface model of the site soil stratigraphy <br />' compnsed of four informal zones, a vadose (unsaturated) zone and three hydrologic units <br /> Hydrologic units may be defined as significant vertical intervals of soil having significant lateral <br /> extent and having similar hydrologic characteristics(i e hydraulic conductivity,transmissivity,etc ) <br />' • over its vertical and horizontal extent A `flow unit' may be defined as a hydrologic unit and is r <br /> characterized by significantly greater hydraulic conductivity values than overlying and underlying <br /> units A flow unit is capable of serving as a preferred migration route, and could potentially allow <br />' migration of large contaminant masses over great distances <br /> The model presented is interpretational and will be modified as more data is collected The four <br />' vertical zones identified are as follows (depths are approximate and can vary by several feet across <br /> the site) <br />' The vadose zone from surface grade to approximately 27 feet bsg consists primarily of sand(surface <br /> to 15 feet bsg at CPT-3) Fine grained,high pore pressure soil predominates from 27 to 45 feet bsg <br /> on-site(15 to 32 feet bsg at CPT-3), and low pore pressure sand, locally cemented sand, increasing <br />' fine grained material with thin high pore pressure intervals increase toward the south (CPT-3) <br /> Q <br /> r Hydrologic Unit 1 (HU 1),at the top of the current saturated zone,extends from 55 feet to 64 feet bsg <br />' on-site and vanes to 69 feet bsg toward CPT-3 The soil consists of moderate to high pore pressure <br /> cemented sand, silt, silty sand, and undefined stiff fine grained material, thin low pore pressure <br /> r <br /> intervals occur south of the site <br /> Hydrologic Unit 2 (HU2) extends from 64 to 99 feet bsg on-site and vanes from 69 to 96 feet bsg <br /> at CPT-3 The soil consists of gravelly sand and sand on-site(CPT-1 and CPT-2)with increasing silt <br /> south of the site (CPT-3), the unit has very low pore pressure on-site with development of <br /> intercalated high and low pore pressure intervals at CPT-3 <br /> Advanced GeoEnvironmental,Inc <br /> r <br /> I <br />
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