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ARCHIVED REPORTS XR0009475
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0544711
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ARCHIVED REPORTS XR0009475
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Last modified
7/30/2019 3:10:02 PM
Creation date
7/30/2019 2:20:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009475
RECORD_ID
PR0544711
PE
3528
FACILITY_ID
FA0005478
FACILITY_NAME
CUTTER LUMBER
STREET_NUMBER
4004
Direction
S
STREET_NAME
EL DORADO
STREET_TYPE
ST
City
STOCKTON
Zip
95206
APN
17525005
CURRENT_STATUS
02
SITE_LOCATION
4004 S EL DORADO ST
P_LOCATION
99
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Pilot Testing Report and Conceptual Corrective Action Plan .July 15, 1994 <br /> Manna Pro, 4004 South EI Dorado, Stockton, CA 30 <br />' The migration of dissolved-phase BTEX and TPH follows the general direction of the <br /> groundwater gradient <br /> t - 335 pounds of TPH are estimated to be dissolved in the groundwater at the site <br /> 31,134 pounds of TPH are estimated to be adsorbed to the soil on site <br /> - A groundwater pumping test was conducted from October 19 through 22, 1993 <br /> The pumping test continued for 3 days and provided essential details for estimating <br /> groundwater flow and design criteria for hydrocarbon recovery systems <br /> - The pumping test was conducted at a 5-inch-diameter extraction well (EW-1) at a <br /> flow rate of 1 3 gpm The drawdown monitored at this recovery well was 5 3 feet <br />' after 4,500 minutes of continuous pumping A distance-drawdown graph and <br /> computer model was used to estimate aquifer transmissivity <br />' The estimated average aquifer hydraulic conductivity, as determined from the <br /> pumping test, is 74 gpd/ft2 The average transmissivity was estimated as 738 <br /> gpd/ft The average storativity was estimated as 0 007 <br />' - The velocity of groundwater, using the estimated average aquifer hydraulic <br /> conductivity, groundwater gradient, and an assumed effective porosity of 26 percent, <br /> is 0 15 foot/day <br /> • The steady state groundwater capture zone of well EW-1, while pumping at 13 gpm, <br /> was determined to be 635 feet in width with a stagnation point 101 feet <br /> downgradient from well EW-1 <br /> • Hydraulic control around the impacted area can be achieved with a relatively low <br /> pumping rate from three groundwater recovery wells <br /> • The physical investigation concluded that the site geology is suitable to treatment by <br /> groundwater extraction and HVE <br /> • The groundwater capture zone of well EW-1 during combined HVE and groundwater <br /> pumping is expected to be enhanced because of greater potential pumping rates <br /> and drawdown as was observed during the pilot studies <br />' • Based on the Vent-ROI computer model, the HVE data analyses determined a radius <br /> of influence of approximately 18 feet at 15 scfm at 148 5 inches of water vacuum per <br /> extraction well <br /> The groundwater pumping test and subsequent computer modeling determined that <br /> a combined one-year capture zone of approximately 460 by 360 feet can be <br />' obtained from three extraction wells depending on the pumping rate of 2 2 gpm per <br /> well <br /> - Initial concentrations of hydrocarbons in the soil vapor was up to 280,000 JA g/I <br /> groundwater pumping and HVE test <br />' 2819Ra34 070 <br /> GROUNDWATER <br /> TECHNOLOGY, INC <br />
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