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ARCHIVED REPORTS_1988_1
Environmental Health - Public
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ARCHIVED REPORTS_1988_1
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Last modified
7/17/2020 3:52:44 PM
Creation date
7/3/2020 11:04:04 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1988_1
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\rtan
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FilePath
\MIGRATIONS\SW\SW_4434_PR0440003_31130 CORRAL HOLLOW_1988_1.tif
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EHD - Public
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u <br />1 <br />n <br />C <br />1 <br />The following monitoring system is proposed to bring the facility into <br />compliance with Title 23, Subchapter 15, Article 5 of the CAC. The <br />proposed system is based on the current understanding of hydrogeologic <br />conditions at the site. Following installation of the proposed <br />system, new information on the hydrogeologic conditions will be <br />evaluated and the need for additional wells or characterization will <br />be assessed. <br />The proposed ground -water monitoring system is intended to fulfill <br />SWAT detection monitoring requirements, as well as to provide back- <br />ground and compliance points for ongoing monitoring according to <br />Subchapter 15 requirements. The proposed ground -water monitoring <br />network includes three deep wells and two shallow wells. Proposed <br />surface -water sampling is discussed in Section III.B. No unsaturated <br />(vadose) zone monitoring is proposed for this site, as discussed in <br />Section III.E. Chemical characterization of the unsaturated zone will <br />be performed as detailed in Section III.F. <br />The results of a recent investigation into subsurface conditions at <br />the site indicate that the Corcoran Clay Member of the Tulare Forma- <br />tion lies in the shallow subsurface of the northern half of the <br />landfill (EMCON Associates, 1988). A perched zone of ground water may <br />occur locally on or within the Corcoran Clay at an approximate depth <br />of 20 feet. A deep regional aquifer occurs at an approximate depth of <br />250 feet. Therefore, to comply with Section 2553(a) of Subchapter 15, <br />which requires detection of fluids at the earliest possible opportuni- <br />ty, the proposed monitoring network is designed to sample ground water <br />in the shallow perched zone (if confirmed by further drilling), as <br />well as the deep regional aquifer. <br />Initially, five monitoring wells are proposed: three monitoring wells <br />to monitor the deep regional aquifer and two shallow wells to monitor <br />any perched ground water. Well MW -1 (see Figure 2) is intended to <br />D <br />cmrnn <br />
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