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ARCHIVED REPORTS XR0001861
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3500 - Local Oversight Program
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PR0544482
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ARCHIVED REPORTS XR0001861
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Last modified
5/21/2019 4:50:15 PM
Creation date
5/21/2019 4:34:52 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001861
RECORD_ID
PR0544482
PE
3528
FACILITY_ID
FA0000556
FACILITY_NAME
CHEROKEE LANE SERVICE STATION*
STREET_NUMBER
900
Direction
S
STREET_NAME
CHEROKEE
STREET_TYPE
LN
City
LODI
Zip
95240
APN
04742007
CURRENT_STATUS
02
SITE_LOCATION
900 S CHEROKEE LN
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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f <br /> B ®®rad® Envir®nmenta0, Mc. <br /> .* 2221 Goldorado Trail, El Dorado, California 95623 (916)626-3898 <br /> Fax(916)626-3899 <br /> August 23, 1996 <br /> I <br /> Mr Kenneth Earnest <br /> Environmental Specialist <br /> Ultramar Inc <br /> 525 West Third Street <br /> Hanford, California 93232-0466 <br /> Subject Second Quarter 1996 Ground Water Monitoring Report <br /> Former Beacon Station 4695 <br /> 900 South Cherokee 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 June 24, 1996 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 were conducted in accordance with <br /> 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 February <br /> 1992 are summarized in Table 1 Historical ground water elevation data are included in Attachment <br /> C On the basis of the current measurements, ground water flows toward the south-southeast (Figure <br /> 2) at a gradient of less than 0 01 foot per foot Ground water levels decreased an average of 1 67 <br /> feet compared to the last monitoring event <br />
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