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ARCHIVED REPORTS_XR0005376
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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3500 - Local Oversight Program
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PR0545520
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ARCHIVED REPORTS_XR0005376
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Last modified
3/13/2020 2:50:17 AM
Creation date
3/12/2020 11:15:40 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0005376
RECORD_ID
PR0545520
PE
3528
FACILITY_ID
FA0006186
FACILITY_NAME
U S RENTALS
STREET_NUMBER
1444
Direction
E
STREET_NAME
MARIPOSA
STREET_TYPE
RD
City
STOCKTON
Zip
95205
CURRENT_STATUS
02
SITE_LOCATION
1444 E MARIPOSA RD
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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1 <br /> ' 1444 MARIPOSA ROAD <br /> . WKA No 2307 02 <br /> December 4, 1992 <br /> ' Page 2 <br /> ' building An empty shed is located approximately 40 feet south of the vacant building and an Enactive <br /> well is located immediately south of the shed. Maintenance records for the well indicate that the total <br /> depth of the well is 191 feet, the last water level measurement was taken in 1990 when the depth to <br /> ' water was approximately 73 feet below site grade The remainder of the site is an asphalt-paved parking <br /> lot formerly used for customer parking and equipment storage <br /> ' The subject site and surrounding areas are relatively flat, surface elevation on site is approximately 26 <br /> feet above sea level Charter Way bounds the site to the north, beyond which is commercial <br /> ' development, and a vacant lot bounds the property to the east Learned Avenue bounds the property <br /> to the south, beyond which is residential development, and Mariposa Road bounds the property to the <br /> west, beyond which is commercial development <br /> PHYSIOGRAPHIC AND HYDROGEOLOGIC SETTING <br /> The site is located in the central portion of the Great Valley geomorphic province of California The <br /> I ' Great Valley is bounded by the mountains and foothills of the Sierra Nevada Range to the east and the <br /> California Coast Ranges to the west The geologic formations of the Great Valley are typified by thick <br /> sequences of alluvial sediments deposited during the filling of a large ancient basin Alternating layers <br /> ' of silty clay and clayey silt ranging from one to five feet in thickness were observed in the tank <br /> excavation during overexcavation operations <br /> ' The site lies within the San Joaquin River Ground Water Basin (California Department of Water <br /> Resources, 1986) Ground water was encountered at a depth of approximately 73 feet below grade <br /> during the last pump maintenance event in 1990 <br /> ' PREVIOUS WORK BY WKA <br /> On October 29 and September 2 and 9, 1992, our firm observed the excavation of a total of <br /> ' approximately 1500 cubic yards of soil from the vicinity of the former underground storage tanks <br /> Eleven sort samples were obtained from the sidewalls and bottom of the excavation, sample locations <br /> ' and depths are shown on Plate 2 Laboratory test results for the sidewall samples, EX4-22' through <br /> EX10-22', revealed non-detectable concentrations of Total Petroleum Hydrocarbons (TPH)`as gasoline, <br /> diesel, and motor oil and non-detectable concentrations of Benzene, Toluene, Ethylbenzene, and Total <br /> Xylenes (BTEX). Results for the bottom samples, EX1-30', EX2-30', and EX3-27', revealed TPH as <br /> • gasoline concentrations ranging from non-detectable concentrations to 25,000 mg/kg (diesel and motor <br /> oil range hydrocarbons were not detected in the samples), benzene concentrations ranging from 0 046 <br /> o <br /> `�W <br /> Recycled paper Er ASSOCIATES INC <br />
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