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CORRESPONDENCE_2011
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PR0440003
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CORRESPONDENCE_2011
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Last modified
4/27/2021 2:41:31 PM
Creation date
7/3/2020 11:04:47 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
CORRESPONDENCE
FileName_PostFix
2011
RECORD_ID
PR0440003
PE
4434
FACILITY_ID
FA0003698
FACILITY_NAME
CORRAL HOLLOW LANDFILL
STREET_NUMBER
31130
STREET_NAME
CORRAL HOLLOW
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
25303010
CURRENT_STATUS
01
SITE_LOCATION
31130 CORRAL HOLLOW RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\cfield
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4434_PR0440003_31130 CORRAL HOLLOW_2011.tif
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EHD - Public
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Currently, groundwater at the site is monitored by network of six monitoring wells: <br />Wells MW -4, MW -5, MW -8, and SB -1 monitor a shallow aquifer. Wells MW -6 and MW <br />® 7 monitor a deeper aquifer. <br />In August 2011, the County submitted an EMP Workplan to further characterize the <br />nature and extent of VOCs migrating from the CHSL in accordance with the Order. The <br />workplan outlined a program for temporary and permanent well construction, sampling, <br />analysis, and data evaluation. This Workplan was approved by RWQCB staff in late <br />August 2011. A revision to this EMP workplan allowing the use of Hydropunch'"° <br />sampling methods for temporary well construction was submitted and approved by <br />RWQCB staff in September 2011. <br />3.1 Well Construction Methods <br />In accordance with the workplan, the County's drilling contractor, Gregg Drilling, Inc., <br />drilled three temporary boreholes - MW -9, MW -10, and MW -11— at the locations <br />shown on Figure 1. Boreholes were drilled using eight -inch diameter hollow stem <br />auger techniques under the direct field supervision of a State of California Certified <br />Engineering Geologist and Certified Hydrogeologist. Lithologic samples were collected at <br />five-foot intervals and logged by the field geologist to ensure proper stratigraphic <br />correlation with existing site monitoring wells. Boreholes were advanced through the <br />Holocene alluvium and into the Pleistocene Corcoran Clay member of the Tulare <br />Formation. Logs of boreholes are presented in Attachment 1. <br />Once the Corcoran Clay was reached, drilling stopped to prepare the Hydropunch'"^ <br />sampler. Attempts to drive the Hydropunch'" into the Corcoran Clay were unsuccessful <br />as a result of the density and stiffness of the formation. Under the advisement of the <br />field geologist and in accordance with the first version of our approved workplan, the <br />driller was directed to advance the borehole into the Corcoran Clay until water was <br />encountered. A one -inch diameter Schedule 40 PVC casing with 0.010 -inch slots was <br />installed at this depth, and the borehole was backfilled with No. 2/12 sand until the <br />perforated section of the casing was surrounded by the sand pack. The temporary wells <br />were secured at the ground surface using plywood weighted down with sand bags. <br />Temporary well construction information is summarized on the following table: <br />Well Completion ReportIC Page ■ 2 <br />Corral Hollow Sanitary Landfill A S S O 6 1 A T H 3 <br />December 15, 2011 <br />
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