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ARCHIVED REPORTS_XR0009337
Environmental Health - Public
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EHD Program Facility Records by Street Name
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3500 - Local Oversight Program
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PR0545660
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ARCHIVED REPORTS_XR0009337
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Last modified
5/12/2020 2:45:44 PM
Creation date
5/12/2020 2:12:22 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009337
RECORD_ID
PR0545660
PE
3528
FACILITY_ID
FA0003909
FACILITY_NAME
PORT OF STOCKTON
STREET_NUMBER
2201
Direction
W
STREET_NAME
WASHINGTON
STREET_TYPE
ST
City
STOCKTON
Zip
95203
APN
14503001
CURRENT_STATUS
02
SITE_LOCATION
2201 W WASHINGTON ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Lithologic data at Site 3 indicate that, in general, the interval from roughly 13 to 23 feet bgs beneath <br /> the former tanks comprises mostly silt, clayey silt, and clay Silty sand occurs below this interval, ' <br /> which grades downward into loose, dark gray to greenish-gray, poorly-graded sand This dark gray <br /> sand was observed in all three bonngs from approximately 30 to 41 feet bgs, the total depth ' <br /> explored during this investigation <br /> Data from nearby studies indicate that the current depth to groundwater in the vicinity ranges from ' <br /> about 5 to 10 feet bgs(SPDC, 1998, and EMCON, 1998) Seasonal fluctuations in the water table <br /> appear to range from about 3 to 5 feet,with some as much as 6 to 9 feet Tank removal inspection <br /> records for Port sites (dating back to 1987) indicate that no groundwater was encountered during ' <br /> excavation or soil resampling to a depth of as much as 16 feet bgs Water levels in this area have <br /> risen as much as 8 feet since 1994, 2 to 3 feet of which appear to be attributable to the heavy and ' <br /> prolonged El Nino rainfalls of last winter Water levels measured in the three borings at Site 3 on <br /> August 7 ranged from about 9 5 to 12 feet bgs Based on nearby studies (SPGC, 1998 & EMCON, <br /> 1998) groundwater flow directions in the vicinity appear to be variable, ranging from west , <br /> northwest to east southeast Flow direction changes may be due to tidal influences produced by the <br /> deep water channel to the north and the San Joaquin River to the west and southwest of the Port ' <br /> complex <br /> 3.0 PROPOSED P <br /> SCOPE OF WORK <br /> The proposed scope of work includes advancing three borings, one in the vicinity of the USTs, one ' <br /> in the vicinity of the dispenser, and one in the northwest corner of the site, using the hollow-stem <br /> auger method Each of these bonngs will be completed as a monrtonng well and developed , <br /> Subsequently, each well will be sampled on a quarterly basis for analysis of PHCs and determination <br /> of groundwater gradient In addition, a supply well survey will be conducted in the vicinity of the <br /> site to evaluate the effects of potential migration of PHCs from the site A Technical Report will , <br /> be prepared including documentation of field work, results of the initial groundwater sampling, and <br /> a summary of findings from the supply well survey <br /> 1 <br /> This work plan will be carried out under the supervision of a California registered geologist The <br /> procedures for completing the scope of work are summarized in the following subsections ' <br /> 3.1 INSTALLATION OF MONTTORING WELLS ' <br /> Prior to initiating any field work, an application for"Permit to Construct Monitoring Wells and/or ' <br /> Soil Borings for the Purpose of Subsurface Investigation," will be submitted to and approval <br /> &3„dcl„„%-M 4 PHILIP P. Ross, R.G. ' <br />
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