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ARCHIVED REPORTS_XR0012037
Environmental Health - Public
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2900 - Site Mitigation Program
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PR0541653
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ARCHIVED REPORTS_XR0012037
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Last modified
10/10/2020 10:55:16 PM
Creation date
7/9/2020 8:32:54 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012037
RECORD_ID
PR0541653
PE
2965
FACILITY_ID
FA0023871
FACILITY_NAME
TOP FILLING STATION
STREET_NUMBER
101
Direction
S
STREET_NAME
WILSON
STREET_TYPE
WAY
City
STOCKTON
Zip
95205
APN
15125307
CURRENT_STATUS
01
SITE_LOCATION
101 S WILSON WAY
P_LOCATION
01
QC Status
Approved
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EHD - Public
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11 March 2002 <br /> AGE-NC Project No 95-0130 <br /> IPage 5 of 13 <br /> Jackson-Hallenbeck-Stockton (JHS) association The JHS soils are located within basins, and <br /> generally consist of moderate to poorly drained fine textured soils The soils are generally derived <br /> from both marine and non-manne sediment, and are generally formed in alluvium derived from <br /> mixed rock sources <br /> The Modesto,Riverbank, Turlock Lake Formations and overlying recent alluvium are the principal <br />' source of domestic ground water in the 13,500 square-mile San Joaquin Valley Ground Water Basin <br /> (Basin 5-22) This basin is drained primarily by the San Joaquin River The nearest surface water <br /> feature in the vicinity of the property is the Stockton Deep Water Channel, located approximately <br />' 3,000 feet west of the property <br />' 2 5 GROUND WATER DEPTH AND FLOW DIRECTION <br /> The estimated depth to ground water at the site is approximately 40 feet below surface grade (bsg) <br />' based on information from Lanes of Equal Depth of Water Wells Spring 1999, published by the San <br /> Joaquin County Flood Control District and Water Conservation District(SJCFCD) Based on review <br /> • of a regional ground water elevation map published by the SJCFCD, the prevailing ground water <br /> flow direction in central Stockton is generally toward the northeast, although flow directions may <br /> be both locally and seasonably variable <br /> Based on data collected during the December 2001 ground water monitoring event, first observed <br /> ground water was approximately 42 feet bsg, the ground water flow direction was inferred to be <br /> towards the northeast at a calculated gradient of 0 002 Ground water flow direction at the site was <br /> inferred towards the northeast from sixteen consecutive quarterly ground water monitoring events <br /> between September 1997 and December 2001 <br /> 3.0. SCOPE OF WORK <br />' AGE proposes to drill and install nine wells screened through Vadose Zone (located between <br /> surface grade and 40 feet bsg)and Hydrologic Unit 1 (located between 40 and 57 feet bsg) one <br /> 6-inch diameter ground water extraction well(EW-1)will be screened between 35 feet and 55 <br /> feet bsg, one 4-inch diameter SVE well(VW-4)will be screened between 10 and 40 feet bsg, <br /> one 2-inch diameter IAS well(AW-1)will be screened between 50 and 55 feet bsg,two 2-inch <br />' diameter ground water monitoring wells(MW-8 and MW-9)will be screened between 35 and <br /> 55 feet bsg (Figure 2) AGE proposes to advance four additional multi-level ground water <br /> monitoring wells to depths of 145 feet bsg to characterize and delineate the off-site vertical extent <br /> of petroleum hydrocarbon-impacted ground water MW IO- 1 tw 13 " <br /> • Following installation of the above referenced wells, a series of pilot tests will be performed <br /> Advanced GeoEnviron mental,Inc <br />
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