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ARCHIVED REPORTS XR0009473
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3500 - Local Oversight Program
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PR0544711
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ARCHIVED REPORTS XR0009473
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Last modified
7/30/2019 3:10:39 PM
Creation date
7/30/2019 2:20:06 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009473
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 Monitoring Report, July-September 1994 2 <br /> Manna Pro, 4004 South EI Dorado, Stockton, CA October 14, 1994 <br /> Groundwater Monitoring Data <br /> On July 14, 1994, 10 existing groundwater monitoring wells were monitored for depth to water (DTW) <br /> DTW measurements were also taken from the groundwater extraction well (EW-1) and the three <br /> observation wells (OB-1, OB-2, and OB-3) The DTW measurements were taken from surveyed points at <br /> the top of each well casing, which are referenced to an arbitrary datum (designated as 15 feet) The <br /> groundwater elevations this quarter decreased an average of 1 73 feet since the April 1994 elevations <br /> were measured A potentiometnc surface map, based on groundwater monitoring data collected on <br /> July 14, 1994, is presented in attachment 1, figure 1 The results of groundwater monitoring are included <br /> in attachment 2, table 1 The groundwater elevation data collected from MWA was not used in the <br /> construction of the potentiometric surface map since it is believed not representative of the water level <br /> elevation conditions in the area As shown in figure 1, the average groundwater gradient in the site <br /> vicinity is approximately 0 0018 foot per foot radiating from the area of monitoring well MW-6 The site's <br /> groundwater flow direction has changed from radiating in a north-northwest direction the previous <br /> quarter to a south-southeast direction during this reporting period However, because of relatively <br /> shallow groundwater gradient this is not considered significant <br /> Groundwater Quality Data <br /> The 10 monitoring wells were sampled on July 14, 1994 Before sampling, the static water in the wells <br /> 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 each <br /> sample was collected, using an Alconox and water solution and rinsed with deionized water Three <br /> well-casing volumes of groundwater were purged from the wells or purged until the well became dry <br /> The wells were allowed to recharge to approximately 80 percent of static water level before samples <br /> were collected <br /> Samples were collected using well 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 and <br /> accompanied the samples for quality assurance and control <br /> 0096RO24 202 <br /> GROUNDWATER <br /> TECHNOLOGY, INC <br />
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