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ARCHIVED REPORTS XR0001088
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3500 - Local Oversight Program
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PR0544230
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ARCHIVED REPORTS XR0001088
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Entry Properties
Last modified
3/5/2019 8:34:50 PM
Creation date
3/5/2019 3:58:54 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001088
RECORD_ID
PR0544230
PE
3528
FACILITY_ID
FA0003829
FACILITY_NAME
VANCO TRUCK-AUTO PLAZA
STREET_NUMBER
1033
Direction
W
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16323041
CURRENT_STATUS
02
SITE_LOCATION
1033 W CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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. Site Background Information Vanco Truck & Auto Plaza <br />' Page 3 of 5 <br /> analyzed <br />' STRATIGRAPHY <br /> In general, light brown to orange brown, fine-grained soil consisting of clayey silt to silty clay was <br /> encountered from surface grade to 25 feet bsg,characteristically,the material had low plasticity and <br />' toughness with a dry to slightly moist moisture content Brownish-gray or brown,moist to saturated, <br /> poorly graded sandy silt to fine sand was encountered between 25 feet and 35 feet bsg A sandy silt <br /> to silt was encountered at approximately 35 feet to 40 feet bsg From.40 feet bsg to total depth,the <br />' stratigraphy is dominated by alternating layers of silty sand or silt and clayey silts to clay layers The <br /> layers vary in thickness from approximately 5 feet to 15 feet <br /> 1 <br /> HYDROGEOLOGIC MODEL <br />' Based on the 05 August 2004 CPT results, AGE developed a preliminary subsurface model of the <br /> site sediment stratigraphy comprised of eight Informal zones a vadose(unsaturated)zone and seven <br /> lie hydrogeologlc units Hydro geologic,or hydrostratigraphic,units(HUs)are defined as a body of rock <br /> or sediment that has hydrogeologlc characteristics (i e hydraulic conductivity, pore pressure, etc ) <br /> that make it distinct from surrounding bodies of rock or sediment(S anders, 19 9 8),or a part of a body <br /> of rock that forms a distinct hydrologic unit with respect to the flow of ground water(Maxey, 1964) <br /> A`flow unit' may be defined as a hydrogeologlc unit characterized by significantly greater hydraulic <br /> conductivity values than overlying and underlying units, a flow unit is capable of serving as a <br />' preferred migration route, and could potentially allow migration of large contaminant masses over <br /> great distances <br />' The model_presented Is Interpretational and will be modified as more data is collected The eight <br /> vertical zones are Identified as follows (depths are approximate aiid can vary by several-feet across <br /> the site) <br /> Vadose/First Water Zone-This zone extends from surface grade to approximately 20 feet bsg Static <br /> water is at 20 feet bsg in the monitoring wells, however, the first saturated soil samples were <br /> collected at 30 feet bsg This indicates that the water table is confined by the overlying fine-grained <br /> materials This zone is characterized by moderate pore pressures <br /> Hydrogeologic Unit 1 (HU 1) - Extending from 20 feet to approximately 30 feet bsg, HU 1 is <br /> comprised predominantly of sandy silt,clayey silt,and silt Dominant hydraulic conductivities,based <br />' on CPT soil behavior types(SBTs),range between 1 x 10`and 1 X 10"8 centimeters per second(cm/s) <br /> for silty to clayey type soils This interval is characterized by generally moderate pore pressures <br /> Advanced GeoEnvironmental,Inc <br />
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