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EHD Program Facility Records by Street Name
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GRANT LINE
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2200 - Hazardous Waste Program
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PR0505941
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Last modified
12/17/2024 2:39:30 PM
Creation date
4/5/2019 8:21:03 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2200 - Hazardous Waste Program
File Section
COMPLIANCE INFO
RECORD_ID
PR0505941
PE
2220
FACILITY_ID
FA0006033
FACILITY_NAME
PG&E: Tracy Service Center
STREET_NUMBER
502
Direction
E
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
250-020-05
CURRENT_STATUS
01
SITE_LOCATION
502 E GRANT LINE RD
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\HW\HW_2220_PR0505941_502 E GRANT LINE_.tif
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EHD - Public
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4.4.2 Calculate the hydraulic conductivity of the uppermost aquifer <br />Field slug tests will be performed on two water table wells and one deep <br />well to provide data for the calculation of the hydraulic conductivity of <br />the uppermost aquifer. Hydraulic conductivity (K) will be determined using <br />calculations developed from the Thiem equation of steady state flow to <br />completely or partially penetrating wells in unconfined or leaky aquifers. <br />In addition, permeability, porosity, and grain size distribution analyses <br />will be performed on selected soil samples collected from the deep well <br />boring and representative of the aquifer matrices encountered. These data <br />will be used to verify slug test results and aid in the calculation of <br />groundwater flow velocity. <br />4.4.3 Calculate the groundwater flow velocity of the uppermost aquifer <br />Hydraulic gradient, porosity, and hydraulic conductivity calculations will <br />be used to estimate the groundwater flow velocity of the uppermost aquifer, <br />using the equation: <br />V K dh <br />n dl <br />(1) <br />where v is the groundwater flow velocity, dh/dl is the hydraulic gradient <br />' (change in hydraulic head per horizontal distance), and n is the effective <br />porosity of the aquifer matrix. <br />I I <br />it <br />n <br />J <br />4.5 Analyze the Potential for Historic Migration of Gas Plant Residues <br />Offsite <br />The groundwater flow velocity represents the fastest rate (ignoring <br />adsorption to soil particles) at which gas plant residues may be moving <br />through the aquifer. After calculating the groundwater flow velocity of the <br />uppermost aquifer and identifying the distribution and chemical composition <br />of the gas plant residues encountered onsite, an analysis of the potential <br />for historic migration of gas plant residues offsite will be performed <br />(taking into account such factors as the age of the residues and the rate of <br />infiltration). <br />3542a/BAV102 24 <br />
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