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ARCHIVED REPORTS XR0009487
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0544711
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ARCHIVED REPORTS XR0009487
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Last modified
7/30/2019 3:07:00 PM
Creation date
7/30/2019 2:28:16 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009487
RECORD_ID
PR0544711
PE
3528
FACILITY_ID
FA0005478
FACILITY_NAME
CUTTER LUMBER
STREET_NUMBER
4004
Direction
S
STREET_NAME
EL DORADO
STREET_TYPE
ST
City
STOCKTON
Zip
95206
APN
17525005
CURRENT_STATUS
02
SITE_LOCATION
4004 S EL DORADO ST
P_LOCATION
99
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Quarterly Groundwater Monitonng Report, October-December 1994 2 <br /> Manna Pro,4004 South EI Dorado, Stockton, CA January 19, 1995 <br /> Groundwater Monitoring Data <br /> On October 12, 1994, 10 existing groundwater monitoring wells were monitored for depth to water <br /> (OTW) DTW measurements were also taken from the groundwater extraction well (EW-1) and the <br /> three observation wells (OB-1, OB-2, and 0131-3) The DTW measurements were taken from surveyed <br /> points at the top of each well casing, which are referenced to an arbitrary datum (designated as <br /> 15 feet) The groundwater elevations this quarter decreased an average of 1 36 feet since the April <br /> 1994 elevations were measured The results of groundwater monitoring are Included in <br /> attachment 2, table 1 A potentiometric surface map, as interpreted from the data In table 1, is <br /> presented In attachment 1, figure 1 The groundwater elevation data collected from MW-1 was not <br /> used in the construction of the potentiometric surface map since it is believed not representative of <br /> the water level elevation conditions in the area As shown in figure 1, the average groundwater <br /> gradient in the site vicinity is approximately 0 002 foot per foot radiating from the area of former <br /> excavation The groundwater flow direction radiates from the former excavation area in a north- <br /> northwesterly direction The current groundwater flow has returned to the historic direction <br /> following the previous quarter's flow which was to the south-southeast <br /> Groundwater Quality Data <br /> The 10 monitoring wells were sampled on October 12, 1994 Before sampling, the static water in the <br /> well was purged to collect samples representative of aquifer conditions The pH, temperature, and <br /> conductivity were measured with a YSI 3650 meter during purging Equipment was cleaned after <br /> each sample was collected, using an Alconox and water solution, and rinsed with de-ionized water <br /> Three well-casing volumes of groundwater were purged from the wells or the wells were purged until <br /> dry The wells were allowed to recharge to approximately 80 percent of the static water level before <br /> samples were collected <br /> Samples were collected using dedicated, polyurethane, disposable bailers and placed Into sample <br /> containers supplied by the laboratory performing the analyses Samples were labeled, placed in an <br /> Ice-chilled Insulated chest and transported to GTEL Environmental Laboratories, Inc in Concord, <br /> California, accompanied at all times by a chain-of-custody record A trip blank was also collected <br /> and accompanied the samples for quality assurance and control <br /> Samples from October 12, 1994, sampling event were analyzed by the laboratory for <br /> • aromatic volatile organics and total petroleum hydrocarbons-as-gasoline (TPH-g) using <br /> Environmental Protection Agency (EPA) Method 8020 and gas chromatography/flame- <br /> ionization detector (GC/FID), respectively <br /> • total dissolved lead using EPA Method 7421 <br /> 00968015 202 <br /> EE9GROUNDWATER <br /> TEaiNoLocy, INC <br />
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