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ARCHIVED REPORTS_XR0004053
Environmental Health - Public
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PR0545387
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ARCHIVED REPORTS_XR0004053
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Entry Properties
Last modified
3/5/2020 9:43:33 AM
Creation date
3/5/2020 8:28:36 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004053
RECORD_ID
PR0545387
PE
3528
FACILITY_ID
FA0005718
FACILITY_NAME
SINCLAIR TRUCKING
STREET_NUMBER
3780
Direction
W
STREET_NAME
LINNE
STREET_TYPE
RD
City
TRACY
Zip
95376
CURRENT_STATUS
02
SITE_LOCATION
3780 W LINNE RD
P_DISTRICT
005
QC Status
Approved
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SJGOV\sballwahn
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EHD - Public
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' Gealgtal cluics Inc.l�cPage 3 <br /> Sinclair Trucking <br /> Feasibility Study <br /> Project No. 1030.3 <br /> June 25,2003 <br /> A number of factors keep vapor extraction from being a promising technology at the site: <br /> • Shallow depth to groundwater — 9 to 12 feet bgs. Thin vadose zones are problematic to <br /> ' vapor extraction due to the tendency of the air to short circuit to the ground surface. <br /> The shallow groundwater would also cause a problem by mounding in and around the <br /> vapor extraction wells. <br /> ' • Low permeability of vadose zone materials. The vadose zone materials at the site are <br /> primarily composed of silts and clays, which have low penneability. Low permeability <br /> soils create problems for vapor extraction systems by limiting the radial influence of the <br /> ' extraction wells. A blower with high vacuum potential must be used which increases <br /> energy consumption. High vacuum would also cause a problem with mounding of the <br /> groundwater. <br /> • The majority of the contamination is tied up in the smear zone of the aquifer. It would <br /> ' be very difficult to target this zone as much of the year it is under the water table and the <br /> rest of the year it is within the capillary fringe zone. <br /> ' 2.2 Monitored Natural Attenuation <br /> Monitored natural attenuation (NINA) consists of long term monitoring of groundwater <br /> conditions. Attenuation of a groundwater plume can occur through physical processes such <br /> as advection and dispersion, or through biological processes. In theory, biological <br /> organisms that can degrade hydrocarbons are ubiquitous in the subsurface. These <br /> organisms metabolize the hydrocarbons in oxidation-reduction processes. Under NINA, the <br /> laboratory analyses include chemical parameters that indicate whether oxidation-reduction <br /> reactions are taking place and natural biological mechanisms are decreasing the mass of <br /> residual contamination at a site. The chemical parameters may include dissolved oxygen, <br /> sulfate, nitrate, oxidation-reduction potential, conductivity and pH. A decrease in residual <br /> mass can be monitored by measuring concentrations of these parameters, along with a <br /> demonstrated decrease in contaminant concentrations in the sites' wells. <br /> ' In essence, monitored natural attenuation involves monitoring the site over a period of <br /> several years to determine if the VOCs are degrading over time. Unenhanced <br /> bioremediation is not a viable option for the site because current] there is- <br /> bioloeical <br /> activityat the site The site has been under investigation for nearly 8 years and the <br /> groundwater concentrations remain relatively stable at the site. S { 3y2yp�51. <br /> ' 2.3 Enhanced Bioremediation <br /> Enhanced biodegradation is an option for the site because currently there is evidence <br /> biological activityat the site. The concept for this site would be tout Ey4fogen peroxide <br /> ' o t e excavation pit prior o ackfilling the pit. Tubing will be installed in the backfill to <br /> facilitate future injection of hydrogen peroxide. The hydrogen peroxide will immediately <br /> oxidize the hydrocarbon constituents while supplying oxygen to the subsurface. Dissolved <br /> oxygen measured at the site averages less than 1-ppm and needs to be enhanced to assist <br /> natural biodegradation. <br /> _ <br /> Soil samples collecte during the installation of MW-1 in June of 1995 indicated the �`''� <br /> ' presence of 13,600 mg/Kg TPH-G. Soil samples collected during the installation of MW- <br /> 101 in April of 2002 indicated the presence of 71.2 m /Kg TPH-G. Additional evidence of <br /> active biodegradation include: <br /> S�(,t csi �� <br />
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