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SU0004149
Environmental Health - Public
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SU0004149
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Last modified
10/27/2020 1:00:10 PM
Creation date
9/6/2019 10:44:51 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004149
FACILITY_NAME
QX-96-0001
STREET_NUMBER
36869
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
36869 S KOSTER RD
RECEIVED_DATE
9/22/1996 12:00:00 AM
QC Status
Approved
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\MIGRATIONS\K\KOSTER\36869\QX-96-01_EIR 96-3\SU0004149\PUB REC REL APPL.PDF
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kTJ KLE1NFELDEP <br /> monitoring wells will be to monitor for a potential perched groundwater zone between the <br /> settling pond and the Delta Mendota Canal and in the vicinity of the California Aqueduct. <br /> The well borings will be advanced usinga truck-mounted drill rig g equipped with 8-inch hallow <br /> stem augers. During the advancement of the well borings, soil samples will be collected at 10- <br /> foot intervals and at each significant lithologic unit for lithologic classification only. Discrete <br /> E samples will not be collected in coarse gravel and cobble zones. Lithologic classification will be <br /> based on the Unified Soil Classification System. Currently, based on our experience, we do not <br /> anticipate encountering groundwater during advancement/installation of these three monitoring <br /> wells. <br /> Three 2-inch PVC monitoring wells will be installed in each of the three borings located near the <br /> Delta Mendota Canal and California Aqueduct. DSS has reported that the depth of the Delta <br /> Mendota Canal invert is approximately 20 feet below ground surface. Kleinfelder assumes the <br /> California invert depth is approximately the same. Therefore the three shallow monitoring wells <br /> will be screened from approximately 15 to 35 feet below ground surface (bgs). The proposed <br /> screened interval is estimated to span a depth of approximately 5 feet above and 15 feet below <br /> the Delta Mendota Canal and California Aqueduct invert depth. The monitoring wells will be <br /> generally constructed as described for monitoring wells in Attachment B. The monitoring well <br /> locations and elevations will be surveyed by DSS, so that subsequent water level sounding data can <br /> be utilized in determining groundwater flow directions and gradient as described in Attachment B. <br /> { <br /> Task E03—Monitoring Well Development and Well Survey O tional Task <br /> A minimum of forty-eight hours after installation, the three new monitoring wells may be <br /> developed to remove sediment from the bottom of each monitoring well, remove sediment laden <br /> water, and to increase the hydraulic radius of the monitoring wells. Kleinfelder anticipates the three <br /> shallow wells will be dry and therefore will not need to be developed. However, if water is present, <br /> the wells will be developed based upon approval of Task E03. Development will be performed <br /> using a pump and/or bailer as generally described in Attachment B. <br /> Kleinfelder understands the top of casing of each of the three proposed well and three existing <br /> production/irrigation wells will be surveyed by DSS personnel for location and elevations. <br /> Elevations will be surveyed to the nearest 1/100'h of a foot. <br /> Task E04—Well Samplin2 and Monitoringf <br /> DEEP IRRIGATION/PRODUCTION WELLS <br /> Water level measurements will be made in three existin irri anon/ roduction wells (Plate 1 at the � <br /> beginnin of the sam ling round rior to ur in ands lin he wells. The;depth to <br /> groundwater will be measured in each well according to the protocol described in Attachment B. <br /> The depth to water measurements will be converted to relative groundwater elevations with respect <br /> to mean sea level or a local benchmark by subtracting them from the surveyed casing elevations. <br /> 20-YPO-212R/2000P29112000W027 Page 3 of 7 <br /> 2000 Kleinfelder,Inc. August 16,2000 <br />
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