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ARCHIVED REPORTS_XR0012598
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3500 - Local Oversight Program
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PR0545566
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ARCHIVED REPORTS_XR0012598
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Entry Properties
Last modified
10/10/2020 11:48:13 PM
Creation date
3/17/2020 4:52:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012598
RECORD_ID
PR0545566
PE
3528
FACILITY_ID
FA0005479
FACILITY_NAME
MANTECA BEAN CO
STREET_NUMBER
229
STREET_NAME
MOFFAT
STREET_TYPE
BLVD
City
MANTECA
Zip
95336
CURRENT_STATUS
02
SITE_LOCATION
229 MOFFAT BLVD
P_LOCATION
04
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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.,� `��*� y_.`z-; y :. �y � -,• �;� 'ter '�r �:�' �=: 1 a�' �.,(��a3�+`� �� ,�•� ,�.s �. aa =u =tai <br /> P� f ii MA i4' - <br /> .`+ :._ <br /> ssr k• , <br /> v s <br /> . r <br /> a. 4- <br /> 1,.l <br /> 20 <br /> 3.4.2 Cone of Depression And Capture Zona <br /> After well development, an aquifer test will be conoucted on the pumping well. Water table <br /> onitorod using <br /> ill be M <br /> elevation changes In the recovery well and three adjacent monitoring whlndevics. Upon completion <br /> pressure transducers attached to a microprocessor-controlled data colla hydraulic <br /> of the aquifer test the data will be downloaded to a personal computer ll al o used ed calculate on a number <br /> conductivity and storativity of the water-bearing zone• fiend gauging l$ ent the data. In addition, all the <br /> of additional monitoring wails during the aquifer test to supe <br /> --• uged before the start of the pump test(static gradient),and before <br /> monitoring wefts at the site will 4e ga <br /> its completion(24-hour cone of depression induced by pumping the recovery ) <br /> tt is considered representative of this <br /> As stated in the Section 2.2, a transn:lssivity of 500 gpd! <br /> pture zone of the <br /> water-bearing <br /> zone. Because the groundwater gradient is slight,the downgradient ca <br /> well pumping at 10 gpm will be approximately that of the cone of depression. Based on a logarithmic <br /> the cone of depression is expected to <br /> approximation to the Theis equation (f=reeze and Cherry, 1979)�determinedill be ng tura zone of the <br /> ba approximately 13t1 feet in radius. Figaro 10illustrates the expected extentthfet�tpfe liable results of <br /> pumping well. The true extent of the capture zone wthe system' <br /> the aquifer test under the sustained pump rate proposed for <br /> 3.4.3 pump Size <br /> aquifer to=t,groundwater extraction will probably be accomplished <br /> Contingent on the results of the At i O gpm,this <br /> using a 1I2 horsepower QRS Environmental Equipment Water Table Depression Pump. <br /> ainst a calculated total dynamic head of 92 feet(Appendix ill)- The <br /> pump supplies 990 feet of head ag <br /> hich <br /> pump system includes an intrinsically safe water sensor ox that houses fusessstarti g capacitor andta <br /> of water in the recovery well, The system utilizes a start b when the water level drops <br /> surge protector, and a control panel that automatically shuts on the pump <br /> be level, The pump and panel are explosion proof for installation in a Class fthis <br /> I, Duipment <br /> - <br /> below the probe 1]rawings of this eq 'p <br /> environment.as defined by the tae�alve,nal `re flowrmeter�ands sample ports will be installed in the water line <br /> are included in Appendix Il. A gat <br /> in the treatment compound area. <br /> 3.5 Groundwater Treatment <br /> 3.5.1 Air Stripping <br /> A schematic drawing of the groundwater treatment system is cted groundwater. T e towern air will <br /> stripping <br /> tower will be utilized to remove volatile hydrocarbons from the extracted g <br /> TvCHNOLOG1•,INC. <br />
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