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ARCHIVED REPORTS_XR0003562
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0545335
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ARCHIVED REPORTS_XR0003562
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Last modified
2/11/2020 6:47:26 PM
Creation date
2/11/2020 11:18:53 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0003562
RECORD_ID
PR0545335
PE
3528
FACILITY_ID
FA0003603
FACILITY_NAME
TESORO (SPEEDWAY XP) 68152
STREET_NUMBER
401
Direction
W
STREET_NAME
KETTLEMAN
STREET_TYPE
LN
City
LODI
Zip
95240
APN
04513019
CURRENT_STATUS
02
SITE_LOCATION
401 W KETTLEMAN LN
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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�i <br /> Ji <br /> El Dorado Environmental, Inc. <br /> 2221 Goldorado Trail, EI Dorado, California 95623 (916)626-3898 <br /> Fax(916)626-3899 <br /> August 30, 1995 <br /> Mr. Kenneth Earnest <br /> Environmental Specialist <br /> Ultramar Inc. <br /> 525 West Third Street <br /> Hanford, California 93232-0466 <br /> Subject: Third Quarter 1995 Ground Water Monitoring Report <br /> Beacon Station 0513 <br /> 401 West Kettleman Lane, Lodi, California <br /> Dear Mr. Earnest: <br /> El Dorado Environmental, Inc. (EDE)has prepared this report to document the results of quarterly <br /> ground water monitoring conducted on July 21, 1995 at the subject site (Figure 1). The monitoring, <br /> conducted by Doulos Environmental(Doulos), included measurements of depth to ground water, <br /> subjective analysis for the presence or absence of free product, ground water purging and collection <br /> of ground water samples. Doulos reports that all field activities pertaining to events in this report <br /> were conducted according to the Ultramar Field Procedures described in Attachment A. <br /> GROUND WATER ELEVATIONS <br /> Prior to purging,Doulos collected depth to ground water measurements. Doulos field data sheets are <br /> contained in Attachment B. Ground water level data collected since September 1993 are summarized <br /> in Table 1. On the basis of the current measurements, ground water flows toward the southeast <br /> (Figure 2) at a gradient of less than 0.01 foot per foot. Ground water elevation has decreased an <br /> average of 1.94 feet compared to the last monitoring event. <br />
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