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ARCHIVED REPORTS_XR0012666
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0545907
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ARCHIVED REPORTS_XR0012666
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Last modified
7/23/2020 3:10:10 PM
Creation date
7/23/2020 2:54:55 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012666
RECORD_ID
PR0545907
PE
3528
FACILITY_ID
FA0005259
FACILITY_NAME
GUILD WINERY
STREET_NUMBER
1
STREET_NAME
WINEMASTERS
STREET_TYPE
WAY
City
LODI
Zip
95240
APN
04908033
CURRENT_STATUS
02
SITE_LOCATION
1 WINEMASTERS WAY
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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r .' . <br /> J. H. KLEINFELDER &ASSOCIATES <br /> File: W-2006-1 <br /> December 16, 1965 <br /> Page 13 <br /> the west of the excavated area and MW-4 to the southeast <br /> of the excavated area had lower concentrations of <br /> gasoline related constituents. The concentrations of <br /> constituents are oeiow detectable limits in the \rater <br /> - sample collected on August 13, 1985 from MW-2. <br /> A limited pump test (6 hours) , utilizing the production <br /> well was conducted on October 1 , 1985 by a Kleinfelder <br /> hydrogeoingist and a 24 hour pump test was conducted <br /> between October 15 and 16. The pump test was conducted <br /> to assess what effect the production well may have.haa <br /> during it's previous use on the local shallow ground <br /> _. water gradient. During both Dump tests, the production <br /> well was run continuously at a flow rate of 4.25 gni <br /> Water levels in the four monitoring wells were recorded <br /> during the entire test. At no time was there any <br /> drawdown observed in any of the monitoring wells. The <br /> continuous pumping of the production well did not affect <br /> the local shallow ground water gradient beneath the tank <br /> excavation. J. H. Kleinfelder and Associates was not <br /> able to obtain any information on the history or the <br /> construction of the production well. The depth of the <br /> well and the depths of the perforations and pump are <br /> unknown at this time but is likely draining from a deeper <br /> zone. J. H. Kleinfelder could not measure the water <br />
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