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3500 - Local Oversight Program
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PR0544468
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Last modified
5/16/2019 4:30:55 PM
Creation date
5/16/2019 4:23:57 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
WORK PLANS
RECORD_ID
PR0544468
PE
3528
FACILITY_ID
FA0025278
FACILITY_NAME
RENTAL MACHINERY COMPANY
STREET_NUMBER
1821
Direction
E
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95205
CURRENT_STATUS
02
SITE_LOCATION
1821 E CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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24 July 1997 <br /> AGE-NC Project No. 97-0349 <br /> Page 2of5 <br /> 2.3. REGIONAL GEOLOGIC SETTING <br /> The site is located in the eastern portion of the Great Valley geomorphic province of California. The <br /> valley is a nearly flat,elongate trough trending northwest and southeast for approximately 450 miles. <br /> The valley is enclosed by the granitic Sierra Nevada on the east and the sedimentary and <br /> metamorphic Coast Ranges on the west. The surficial and upper several hundred feet of subsurface <br /> layers consist primarily of unconsolidated alluvial and floodplain deposits(predominantly sand, silt, <br /> and clay)of Quaternary age, which were derived from the mountains of the Sierra Nevada. Beneath <br /> the upper sedimentary deposits lie a thick sequence of marine deposits of Mesozoic age, which in <br /> turn are underlain by a pre-Jurassic complex of igneous and metamorphic basement rock. <br /> 2.4. GROUND WATER DEPTH AND FLOW DIRECTION <br /> The estimated depth to ground water at the site is 50 feet below surface grade (bsg) based on <br /> information from Lines of Equal Depth of Water Wells Fall 1993, published by the San Joaquin <br /> County Flood Control District and Water Conservation ,District and ground water depth <br /> measurements in monitoring wells located approximately 400 feet north and 200 feet south of the <br /> site (Re-Manufacturing). <br /> Ground water flow direction, as determined from the Re-Manufacturing site, is south-southeast. <br /> However,due to seasonal variations in ground water depth, flow direction may vary. The uppermost <br /> ground water flows in an unconfined aquifer. With increasing depth, the aquifer becomes semi- <br /> confined, due to the presence of mixed heterogeneous layers of sediments. <br /> 3.0. SCOPE OF WORK <br /> The scope of work includes the collection and analysis of subsurface soil samples from the former <br /> UST area. AGE proposes to collect soil samples using direct push technology (DPT). Initially, one <br /> soil probe boring will be advanced within the former UST excavation; the probe boring will be <br /> advanced to a depth of approximately 50 feet or until groundwater is encountered. If necessary, <br /> additional soil probe borings will be advanced to adequately characterize the lateral and vertical <br /> extent of hydrocarbon-impacted soil. <br /> 3.1. PROBING AND SAMPLING <br /> Soil probe borings will be advanced using a Geoprobe 5400 soil probing unit equipped with 1.125- <br /> inch diameter probe rods and an attached 2.15-inch diameter soil sampler. The initial probe boring <br /> Advanced GeoEnvironmental,Inc. <br />
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