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ARCHIVED REPORTS_1999
Environmental Health - Public
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4400 - Solid Waste Program
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ARCHIVED REPORTS_1999
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Last modified
7/17/2020 3:53:09 PM
Creation date
7/3/2020 10:40:34 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1999
RECORD_ID
PR0440001
PE
4433
FACILITY_ID
FA0004514
FACILITY_NAME
AUSTIN ROAD/ FORWARD LANDFILL
STREET_NUMBER
9069
Direction
S
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
STOCKTON
Zip
95215
CURRENT_STATUS
02
SITE_LOCATION
9069 S AUSTIN RD
P_LOCATION
01
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4433_PR0440001_9069 S AUSTIN_1999.tif
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EHD - Public
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Austin Road Landfill Appendix D <br /> Contaminant Plume Characterization Report Aquifer Test Methods <br /> Background Monitoring <br /> The initialP hase of the aquifer testing consisted of a pretest monitoring of water levels in each <br /> observation well. One of the wells,MW-12(Figure 1-2),was also used throughout the five aquifer <br /> test phases to identify local trends in the water table surface. As shown on Table D-1,well MW-12 <br /> is located the greatest distance from either extraction well yet it is close enough to the test site that <br /> fluctuations in its water levels should be representative of larger-scale influences affecting the entire <br /> study area. <br /> Identifying ambient(background)water level trends,as represented by the water level data in MW- <br /> 12, is important because the aquifer test analysis methods assume there are no fluctuations in the <br /> water table surface other than those produced by pumping from the test wells EW-1 and EW-2. To <br /> meet this assumption,the regional background fluctuations must be removed from the data sets of <br /> the aquifer test observation wells as a pre-evaluation data correction. Regional/background <br /> fluctuations in the water table in the vicinity of the ARL are likely caused by changes in barometric <br /> pressure,infiltration of rainfall into the aquifer,and from pumping of nearby wells. <br /> Pretest water level measurements from the observation wells showed similar trends to each other, <br /> verifying that regional factors affected the aquifer in the vicinity of the ARL site in a consistent <br /> manner. The pretest water level data also indicated that well MW-12 generally was representative <br /> of the background fluctuations,and could be used for this purpose throughout the remaining test <br /> phases. <br /> Recovery n inPhases <br /> As mentioned in Section 2.3,the ARL aquifer test was designed to cause minimal disturbance to the <br /> operation of the site's groundwater remediation system. This was accomplished by turning off each <br /> extraction well,in sequence,and then turning them back on in sequence. In terms of the aquifer <br /> test,this meant that the recovery phase of each well occurred first then was followed by the <br /> pumping phase. The following summarizes the different test phases,their starting time and <br /> duration: <br /> Test Phase Event . tar Date.Time <br /> Recovery-1 EW-1 off December 4,11:10 am 5650 min <br /> Recovery-2 EW-2 off December 8,9:20 am 5680 min <br /> Pumping-1 EW-1 on December 12,8:00 am 4380 min <br /> Pumping-2 EW-2 on December 15,9:00 am 4430-5840 min <br /> The test phases continued until a sufficient change in water levels were recorded in a majority of the <br /> observation wells,as determined through repeated review of water level data while the tests were <br /> being conducted. Extraction well operations were controlled by the onsite remediation system <br /> operator,Dennis Young. <br /> Water level measurements were collected from the Trolls during each test phase on a logarithmic <br /> scale starting at a 0.005 minute measurement interval and gradually increasing until reaching a <br /> CDM Camp Dresser&McKeeD-3 <br /> W:\REPORTS\STOCKTO~LPLUME.OMPPO.WPD CS OZO <br /> City of Stockton 199 SO <br /> 0855-0006 <br />
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