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ARCHIVED REPORTS_XR0012693
Environmental Health - Public
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EHD Program Facility Records by Street Name
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3500 - Local Oversight Program
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PR0545039
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ARCHIVED REPORTS_XR0012693
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Last modified
12/10/2019 2:43:32 PM
Creation date
12/10/2019 10:35:44 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012693
RECORD_ID
PR0545039
PE
3528
FACILITY_ID
FA0010186
FACILITY_NAME
DEL MONTE FOODS PLNT #33 - DISCO WH
STREET_NUMBER
110
Direction
N
STREET_NAME
FILBERT
STREET_TYPE
ST
City
STOCKTON
Zip
95205
APN
15702009
CURRENT_STATUS
02
SITE_LOCATION
110 N FILBERT ST
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Tracer Research Corporation <br /> SHALLOW SOIL GAS INVESTIGATION- METHODOLOGY <br /> Shallow soil gas investigation refers to a method developed by TRC for investigating <br /> underground contamination from volatile organic chemicals (VOCs) such as industrial <br /> solvents,cleaning fluids and petroleum products by looking for their vapors in the shallow <br /> soil gas. The method involves pumping a small amount of soil gas out of ii;, ground <br /> through a hollow probe driven into the ground and analyzing the gas for the presence of <br /> volatile contaminants. The presence of VOCs in shallow soil gas indicates the observed <br /> compounds may either be in the vadose zone near the probe or in groundwater below the <br /> Probe. The snil <br /> gas technology is most effective in mapping low molecular weight ' <br /> halogenated solvent chemicals and petroleum hydrocarbons possessing high vapor pressures <br /> and low aqueous solubilities. These compounds readily partition out of the groundwater and <br /> i <br /> into the soil gas as a result of their high gas/liquid partitioning coefficients. Once in the soil <br /> gas, VOCs diffuse vertically and horizontally through the soil to the ground surface where <br /> they dissipate into the atmosphere. The contamination acts as a source and the above <br /> ground atmosphere acts as a sink,and typically a concentration gradient develops between <br /> the two. The concentration gradient in soil gas between the source and ground surface may <br /> r. <br /> be locally distorted by hydrologic and geologic anomalies (e.g. clays, perched water); <br /> however, soili <br /> gas mapping generally remains effective because distribution of the <br /> contamination is usually broader in areal extent than the local geologic barriers and is J <br /> �r <br /> deflined using a large database. The presence of geologic obstructions on a small scale tends <br /> to create anomalies in the soil gas-groundwater correlation, but generally does not obscure <br /> the broader areal picture of the contaminant distribution. <br /> Soil gas contaminant mapping helps to reduce the time and cost required to delineate_ <br /> underground contamination by volatile contaminants. The soil gas investigation does this <br /> by outlining the general areal extent of contamination. Conventional bore holes or <br /> observation wells are used to verify both the presence and extent of the subsurface w <br /> moll a <br /> ➢ire <br />
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