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ARCHIVED REPORTS XR0006421
Environmental Health - Public
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2900 - Site Mitigation Program
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PR0519189
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ARCHIVED REPORTS XR0006421
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Last modified
8/21/2019 4:00:47 PM
Creation date
8/21/2019 2:47:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0006421
RECORD_ID
PR0519189
PE
2950
FACILITY_ID
FA0014347
FACILITY_NAME
CURRENTLY VACANT
STREET_NUMBER
6425
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95207
APN
09741031
CURRENT_STATUS
02
SITE_LOCATION
6425 PACIFIC AVE
P_LOCATION
01
QC Status
Approved
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EHD - Public
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Similar reductions can be seen when comparing SB2 with S135 and SB7, or 92% and 85% for TPI-Ig <br /> respectively While Benzene, Toluene and Ethylbenzene have been reduced to trace amounts <br /> Xylenes have been reduced to 54% and 13% of their original values respectively <br /> Confirmation soil boring S137 was converted into a two inch PVC well MW13 This well and MW I, <br /> MW2, MW3 and MW 10 are currently being used for vapor extraction <br /> MW2 and MW13 are also used for air sparging (commencing on October 9, 1997) Sparging of <br /> these wells introduces and make oxygen available for biodegradation of the down gradient wells <br /> MW8 and MW12 Prior to shutting off the air sparging vapor extraction system on December 8, <br /> 1997, MW2, MW8, MW9 MW12 and MW13 were tested for the amount of DO in the groundwater <br /> Sparging had saturated MW2 and MW13 with oxygen, they registered 9 1 and 7 6 mg/L <br /> respectively Upgradient well MW9 contained 4 1 mg/L while downgradient wells MW8 and <br /> MW12 contained 1 3 and 1 8 mg/L Once the sparging and vapor extraction is turned off, the DO in <br /> the groundwater is depleted almost immediately <br /> Natural Attenuation is occurring at this site Field groundwater analysis obtained December 16, <br /> 1997 for Dissolved Oxygen, Nitrate, Sulfate and Ferrous Iron demonstrate that the available oxygen <br /> is being used by microorganisms and a reducing environment has been established at MW2 with the <br /> onset of methogenisis, see Figures Appendix F <br /> Bacteria native to the soil at hydrocarbon contamination sites normally degrade hydrocarbons The <br /> most effective hydrocarbon degraders (eaters) are the aerobic (oxygen using) bacteria The amount <br /> of available dissolved oxygen is usually the factor controlling the rate that these bacteria degrade the <br /> gasoline <br /> A much slower degradation process starts when the dissolved oxygen is depleted The plume begins <br /> to become anaerobic and the bacterium commences to reduce nitrate, ferric iron, and sulfate to <br /> further degrade the hydrocarbons Eventually, as these compounds and the oxygen are used, the <br /> bacteria begin methogenesis, in which the hydrocarbons are converted to methane <br /> The prior bioremediation sampling results also indicate that natural attenuation/bioremediation is <br /> active at this site <br /> The presence of Ferrous iron in the wells indicates that biodegradation has progressed to the point <br /> that the system is oxygen deficient and the bacteria have started to reduce the iron to provide oxygen <br /> for the degradation <br /> Biodegradation in MW2, which is in the heart of the plume, has consumed all of the available <br /> electron acceptors <br /> The carbon dioxide (CO2) levels in the vapor extraction effluent stream indicate that a portion of the <br /> hydrocarbons have been degraded CO2 and water are the final byproducts of the biodegradation of <br /> hydrocarbons The carbon in CO2 results from the oxidation of the hydrocarbon radical CH2 and as <br /> such 1 mg of CO2= 0 41 mg of CH2 (CH2(12+1+1 = 14) /(CO2 (12+16+16=34) <br /> 8 8603 Update#54/CLOSURE 3 12/98 <br />
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