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ARCHIVED REPORTS XR0004103
Environmental Health - Public
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ARCHIVED REPORTS XR0004103
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Last modified
4/2/2019 4:00:23 PM
Creation date
4/2/2019 3:46:59 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004103
RECORD_ID
PR0544300
PE
3528
FACILITY_ID
FA0003855
FACILITY_NAME
TESORO (SHELL) 68153
STREET_NUMBER
2448
Direction
W
STREET_NAME
KETTLEMAN
STREET_TYPE
LN
City
LODI
Zip
95240
APN
05814001
CURRENT_STATUS
02
SITE_LOCATION
2448 W KETTLEMAN LN
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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EI Dorado Environmental, Inc. <br /> .' 2221 Goldorado Trail, El Dorado, California 95623 (916)626-3898 <br /> Fax(916)626-3899 <br /> i <br /> January 4, 1996 <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 #696 <br /> 2448 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 September 27, 1995 at the subject site (Figure 1). The <br /> monitoring, conducted by Doulos Environmental (Doulos), included measurements of depth to <br /> ground water, subjective analysis for the presence or absence of free product, ground water purging <br /> and collection of ground water samples. Doulos reports that all field activities were conducted in <br /> accordance with the Ultramar Field Procedures described in Attachment A. <br /> GROUND WATER ELEVATIONS <br /> Prior to purging, Doulos collected depth to ground water measurements. Copies of Doulos' field <br /> data sheets are contained in Attachment B. Ground water elevation data collected since March 1992 <br /> are summarized in Table 1. Historical ground water elevation data are contained in Attachment C. <br /> On the basis of the current measurements, there are components of ground water flow toward the <br /> south, southwest, and east (Figure 2). The ground water gradient is approximately 0.05 foot per <br /> foot. Ground water levels have decreased an average of 1.57 feet compared to the last monitoring <br /> event. <br />
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