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ARCHIVED REPORTS_XR0003771
EnvironmentalHealth
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2900 - Site Mitigation Program
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PR0540905
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ARCHIVED REPORTS_XR0003771
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Last modified
2/3/2020 10:06:44 AM
Creation date
2/3/2020 9:11:13 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0003771
RECORD_ID
PR0540905
PE
2960
FACILITY_ID
FA0023406
FACILITY_NAME
SIERRA LUMBER MANUFACTURERS
STREET_NUMBER
375
Direction
W
STREET_NAME
HAZELTON
STREET_TYPE
AVE
City
STOCKTON
Zip
95205
APN
147120808
CURRENT_STATUS
01
SITE_LOCATION
375 W HAZELTON AVE
P_LOCATION
01
QC Status
Approved
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SJGOV\sballwahn
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EHD - Public
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15 February 2000 <br /> AGE-NC Project No 98-0448 <br /> Page 12 of 33 <br />' 51 PROCEDURES <br /> The pump test consisted of extracting ground water from well EW-1 utilizing a 4-inch diameter <br /> Grundfos Redl-flo pump into a 6,500-gallon aboveground Baker storage tank The pump test utilized <br />' pressure transducers that were deployed in wells MW-1, MW-2, MW-4A and EW-1 to measure <br /> difference In ground water levels during ground water pumping, ground water level measurements <br />' were continuously recorded utilizing an Aqulstar data logger(Appendix A) <br /> The pumping rate was determined by measuring the time required to fill a 5-gallon bucket from the <br /> Ipumping discharge hose Initially, ground water was pumped from EW-1 at a rate of 13 gallons per <br /> minute (gpm) but was decreased to 8 GPM afer 8 minutes of pumping operation and was then <br /> increased to 10 GPM after 40 minutes Approximately 4,500 gallons of purged ground water were <br />' removed from EW- 1 during operation of the pump test <br /> Draw-down versus time for wells MWA, MW-2, MW-4A and EW-1 was graphed on semi- <br /> lognthmnc paper (Appendix J) Utilizing the Jacob straight-line method, the transmnssivity and <br /> storativnty for each well were determined(Appendix K) The radius of influence was then determined <br /> by graphing the draw-down in each well at a specific time versus distance (Appendix J) <br /> Following the ground water pump test, a ground water sample was collected from the 6,500-gallon <br /> aboveground storage Baker Tank utilizing a new, disposable polyethylene bailer and four 40-m1 <br /> EPA-approved VOA vials containing 0 5 ml 18% hydrochloric acid as a preservative Care was <br /> taken to ensure that visible air bubbles were not present in the vials after filling and capping Ground <br /> water sample containers were labeled with the sample location, date, time, and sampler's Initials <br /> Each ground water sample was logged on a chain-of-custody form,placed in a chilled container and <br /> transported to a California Department of Health Services (DHS)-certified laboratory for analysis <br /> I, for TPH-g by EPA Method 8015 Modified and BTEX/MTBE by EPA Method 8020 <br /> 52 GROUND WATER PUMP TEST RESULTS <br /> Pumping rates fluctuated between 8 and 13 GPM during the pump test The greatest draw-down from <br /> Iextraction well EW-1 was observed at 22 5 feet after 160-minutes of pumping operation, however, <br /> at this time draw-down from MW-4A(located 4 feet to the south) was observed to be approximately <br /> 1 22 feet, draw-down from MW-2 (located 10 feet to the northwest) was observed to be <br /> approximately 1 15 feet, and draw-down from MW-1 (located 15 feet to the west-southwest) was <br /> observed to be 0 74 feet <br /> The transmissnvlty value for well EW-1 was calculated at 347 5 gai/day-ft , transmnsslvlty values <br /> from MW-1,MW-2 and MW-4A ranged between 4,185 gal/day-ft and 9,533'gal/day-ft Calculations <br /> Advanced GeoEnviron mental,Inc <br /> I . <br />
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