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ARCHIVED REPORTS XR0009431
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0544711
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ARCHIVED REPORTS XR0009431
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Last modified
7/30/2019 3:17:50 PM
Creation date
7/30/2019 2:06:12 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009431
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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a <br /> • Quarterly Groundwater Monitoring Report, December, 1992--February, 1993 April 15, 1993 <br /> Manna Pro, 4004 South EI Dorado, Stockton, CA 2 <br /> Groundwater Morntorina Data <br /> On February 3, 1993, 10 existing groundwater monitoring wells were monitored for depth to water <br /> (DTW) The DTW measurements were taken from surveyed points at the top of each well casing, <br /> which are referenced to a common datum (designated as 100 feet) The February 1993 <br /> groundwater elevations increased an average of 4 30 feet compared with October 1992 elevations <br /> The results of groundwater monitoring are included in Attachment 3, Table 1 A potentiometric <br /> surface map, as interpreted from the data in Table 1, is presented in Attachment 2, Figure 1 As <br /> shown in Figure 1, the average groundwater gradient in the site vicinity is approximately 0 006 ft/ft <br /> toward the north Previous potentiometric surface maps, constructed using data from wells MW-1 <br /> through MW-6, showed the gradient to the west-southwest The San Joaquin County Flood Control <br /> and Water Conservation District potentiometric surface maps (1985 and 1991) show the groundwater <br /> gradient generally toward the north, suggesting that the previous water levels measured in wells <br /> MW-1 through MW-6 were hydraulically influenced by the excavation With the additional data from <br /> wells MW-7 through MW-10, the potentiometric surface map shows an overall gradient consistent <br /> with the regional flow and also shows the hydraulic effect (mounding) near the tank excavation <br /> Groundwater Duality Data <br />.� The 10 monitoring wells were sampled on February 3, 1993, after groundwater-level monitoring The <br /> wells were purged to collect samples representative of aquifer conditions The pH, temperature, and <br /> conductivity were measured with a YSI 3650 meter during purging Wells MW-1 and MW-6 bailed <br /> dry after purging less than 4 well volumes of groundwater Four well volumes of groundwater were <br /> removed from wells MW-2, MW-3, MW-4, MW-5, MW-7, MW-8, MW-9, and MW-10 The wells were <br /> allowed to recharge to approximately 80 percent of static water level before samples were collected <br /> Samples were collected using a Teflon® bailer and placed into sample containers supplied by the <br /> laboratory performing the analyses Equipment was cleaned after each sample was collected, using <br /> an Alconoxe' and water solution and rinsed with de-ionized water A field blank and ansate sample <br /> were collected in the field for Quality Assurance/Quality Control (QA/QC) measures Samples were <br /> labeled and placed in an ice-chilled cooler for transport to GTEL Environmental Laboratories, Inc in <br /> Concord, California, and were accompanied at all times by a chain-of-custody record <br /> Samples from the February 3, 1993, sampling event were analyzed by the laboratory for <br /> ■ Aromatic volatile organics and total petroleum hydrocarbons-as-gasoline (TPH-G) <br /> using Environmental Protection Agency (EPA) Methods 5030 and 8020 and modified <br /> EPA Method 8015, <br /> ■ Total dissolved lead using EPA Method 7421 <br /> R2819A3 DH <br /> EM GROUNDWATER <br /> TECHNOLOGY, INC <br />
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