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3500 - Local Oversight Program
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PR0544230
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Entry Properties
Last modified
3/5/2019 8:30:09 PM
Creation date
3/5/2019 3:51:09 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
WORK PLANS
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 5 of 6 <br /> Hydrogeoiogic Unit 7 (HU7)- Extending from 82 feet to total depth of the boring(100 feet bsg), <br /> HU7 is composed primarily of stiff,fine-grained clayey 'Its,silty clays,and clay.A thin,cemented <br /> sand is encountered at approximately 94 feet to 95 feet bs .Hydraulic conductivity generally ranges <br /> between 1 x 10-5 and 1 x 10-15 cm/s for clays, silts, and sti , fine-grained soils. HU7 is characterized <br /> by varying pore pressures ranging between moderate and very high and is identified as a confining <br /> layer. <br /> i <br /> SITE CONCEPTUAL MODEL <br /> Based on the data collected to date from soil boring ins t llation and sampling,AGE has developed <br /> a site conceptual model for the release, migration, and distribution of the contaminants in the <br /> subsurface as described below: <br /> The site surface is essentially flat land that is developed as a truck and auto plaza. The majority of <br /> the ground surface is covered by an asphalt or concrete c ap.In general,a clayey silt layer extending <br /> from surface grade to approximately 30 feet bsg unde lies the assessed portion of the property <br /> (vadose zone & HUI). Beneath the clayey silt layer is a fine-grained layer consisting of silty sand <br /> to fine sand(HU2),which is encountered from approxi ately 30 feet to 38 feet bsg. HU2 has the <br /> characteristics of an aquifer, or the water table. <br /> Beneath the silty sand to sand layer are alternating layers of stiff,fine-grained soils and sandy soils. <br /> The stifffine-grained layers act as confining layers,retarc ing the vertical migration of contaminants. <br /> The sandy layers act as migratory flow units, allowin contaminants to migrate vertically and <br /> laterally away from the source. <br /> During site assessment activities in July andAugust 004 and July 2005, saturated soil, or the <br /> capillary fringe,was first encountered at approximately 5 feet to 30 feet bsg.Based on information <br /> from quarterly monitoring events performed by AGE, ground water flow is generally toward the <br /> northeast. However,this may be greatly modified by local recharge and discharge patterns. <br /> Site assessment activities to date defined two areas where soil is impacted by concentrations of <br /> petroleum hydrocarbons. The maximum petroleum by rocarbon concentrations were detected in <br /> pilot soil borings MW-4 and MW-6 at depths of 15 feet and 35 feet bsg, respectively (TPH-d: <br /> 2,600 mg/kg and 2,500 mg/kg). Until the monitoring well installation conducted in July 2005,the <br /> maximum petroleum hydrocarbon concentration(110 g/kg TPH-d)was detected adjacent to the <br /> former piping sample Iocation P 13,at 15 feet bsg in soil probe boring B3.Petroleum hydrocarbons <br /> were also detected at a concentration of 12 mg/kg in the soil sample collected from boring B7 at <br /> 30 feet bsg, adjacent to piping sample P7. Soil samples collected at 60 feet and 90 feet bsg from <br /> boring CPT-1 were impacted by petroleum hydrocarbons:TPH-g was detected at concentrations of <br /> 2.1 mg/kg (CPT 1-60) and 6.3 mg/kg (CPT 1-90); TPH d was detected at a concentration of 110 <br /> Advanced GeoEnvironmental,Inc. <br />
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