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ARCHIVED REPORTS_XR0004954
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0545585
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ARCHIVED REPORTS_XR0004954
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Entry Properties
Last modified
9/15/2020 11:57:30 PM
Creation date
3/19/2020 3:23:30 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004954
RECORD_ID
PR0545585
PE
3528
FACILITY_ID
FA0000212
FACILITY_NAME
Mossdale Chevron
STREET_NUMBER
444
Direction
W
STREET_NAME
MOSSDALE
STREET_TYPE
RD
City
LATHROP
Zip
95330
CURRENT_STATUS
02
SITE_LOCATION
444 W MOSSDALE RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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' 04 June 2001 <br /> • AGE-NC Project 99-0570 ' <br /> Page 2 of 3 <br />' custody form, stored In a chilled container and transported under chain-of-custody to McCampbell <br /> Analytical, Inc (MAI), a California Department of Health(DHS)-certified laboratory, for analysis <br /> 22 GROUND WATER ANALYSIS <br />' Ground water samples were analyzed for the following analytes <br />' Total petroleum hydrocarbons quantified as gasoline (TPH-g) and diesel (TPH-d) in <br /> accordance with EPA Method 8015 Modified, <br /> Volatile aromatic hydrocarbons-benzene,toluene, ethylbenzene and total xylenes (BTE&X� <br />' in accordance with EPA Method 8020, and <br /> Oxygenated compounds - dr-Isopropyl ether (DIPE), ethyl tertiary-butyl ether (ETBE), <br />' methyl tertiary-butyl ether (MTBE), tertiary-amyl methyl ether (TAME), tertiary butanol <br /> (TBA), ethyldrbrormde (EDB) and 1,2-dichloroethane (1,2-DCA) In accordance with EPA <br /> Method 8260-Modified, respectively <br /> 1• <br /> 1 3.0. FINDINGS <br /> Ground water elevation, flow direction and gradient were determined from field data collected on <br /> 1 08 January 2001, the contaminant impact to ground water was assessed from the laboratory data <br /> 1 3 1 GROUND WATER ELEVATION AND GRADIENT <br /> The average relative ground water elevation on 08 January 2001 was approximately -10 feet with <br /> I an average depth to water of 15 3 feet below well casing grade The top of the ground water table <br /> occurred within the screened intervals of the wells Ground water was inferred to be flowing to the <br /> north and northeast (Figure 3) with a significant hydraulic gradient of 0 029 feet/feet <br /> 3 2 ANALYTICAL RESULTS OF GROUND WATER SAMPLES <br /> I TPH- and TPH-d were detected in two of the ground water samples TPH- was detected in well <br /> g �' P g <br /> samples MW-1 and MW-2 at concentrations of 95 micrograms per liter (gg/1) and 2,700 �rg/l, <br /> respectively TPH-d was detected In the same samples at 84 µg/l and 1,600 µg/l, respectively <br /> Advanced GeoEtivirournental,Inc <br />
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