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3500 - Local Oversight Program
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PR0545372
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Last modified
2/14/2020 4:38:30 AM
Creation date
2/13/2020 9:38:07 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
WORK PLANS
RECORD_ID
PR0545372
PE
3528
FACILITY_ID
FA0003871
FACILITY_NAME
UPS Freight - Lathrop
STREET_NUMBER
1444
STREET_NAME
LATHROP
STREET_TYPE
Rd
City
Lathrop
Zip
95330
CURRENT_STATUS
02
SITE_LOCATION
1444 Lathrop Rd
P_LOCATION
07
P_DISTRICT
003
QC Status
Approved
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EHD - Public
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Di salvo Truddng-WP <br /> July 25,1995 <br /> Page-3- <br /> *f 3.4 PROPOSED SCOPE OF WORK <br /> Condor recommends pumping MW1 in an at empt to evaluate the lateral extent of <br /> groundwater contamination associated with the former UST's located at the site. MW is <br /> located in the estimated down gradient direction approximately 10 feet northwest of the former <br /> east end of TK4. Based on aquifer parameters discussed in section 3.1, Condor estimates that <br /> in a time period of 14 days at least one pore volume can be extracted from a cylindrical area <br /> surrounding MW1 with a circumference of approximately 10 feet. One groundwater sample will <br /> be collected from MW1 following extraction of one ore volume. If hydrocarbon constituents <br /> are detected at or above the reported laboratory det ction limits in the groundwater sample, <br /> pumping will continue until 14 days has elapsed or 10,000-gallons have been pumped. A final <br /> groundwater sample will be collected from MW1 at he end of pumping. The extracted <br /> groundwater will be stored on site ina 10,000-gallon frac tank. <br /> 3.1 Aquifer Parameters <br /> The site geology generally consists of medium sand from 10.5 feet to 16 feet bgs and silt <br /> from 16 feet to 18.5 feet. The hydraulic conductivity of silt is on the order of 100 times lower <br /> than the hydraulic conductivity of sand. In June, 1995, the static water level in MW1 was <br /> approximately 11.90 feet below the ground surface. ondor assumes the thickness of the <br /> aquifer is governed by the top of the water column (11.90 ft. bgs in June, 1995) and the top of <br /> the silt at 16.0 feet bgs. Therefore, the thickness of he shallow aquifer is approximately 4 feet. <br /> Based on an estimated aquifer porosity of 40%, the volume of groundwater present in a <br /> cylindrical area 10 feet from MW1 is approximately 3,800 gallons. A minimum hydraulic <br /> conductivity value for sandy material of 8.2 ft/day ( odd, Groundwater Hydrology, 1980) was <br /> used to evaluate the effects of pumping from MW1. The groundwater parameters were <br /> simulated using the Quickflow groundwater modeling program. Modeling indicated that <br /> pumping MW1 at 1 gpm would cause a 3 foot drawl Dwn and create a cone of depression of <br /> approximately 120 feet. If 1 gpm is achieved, one pc re volume of groundwater will be extracted <br /> within 3 days. Figure 3, Appendix A'shows results of the modeling program. <br /> 3.2 Pumping <br /> A submersible pump will be placed in MW1 t 16 feet bgs to allow for maximum draw <br /> down. The pump will be fitted with a high-low shut off switch to insure the water table does <br /> not drop 'below the pump inlet during pumping. All hoses and fittings will be securely attached <br /> to prevent rupture and potential surface discharge. Tbe groundwater will be pumped from <br /> tr= <br /> MW1 to a 10,000-gallon frac tank located on site. Following installation and setup, a Condor <br /> 1 - <br /> " CONDOR <br />
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