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ARCHIVED REPORTS_SEPARATE PHASE HYDROCARBON INVESTIGATION UNOCAL EXTRACTION WELL PILOT STUDY 2011
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ARCHIVED REPORTS_SEPARATE PHASE HYDROCARBON INVESTIGATION UNOCAL EXTRACTION WELL PILOT STUDY 2011
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Last modified
2/13/2020 6:26:46 PM
Creation date
2/13/2020 2:35:54 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
SEPARATE PHASE HYDROCARBON INVESTIGATION UNOCAL EXTRACTION WELL PILOT STUDY 2011
RECORD_ID
PR0009302
PE
2960
FACILITY_ID
FA0004002
FACILITY_NAME
MORTON-ALCO
STREET_NUMBER
55
Direction
S
STREET_NAME
LINCOLN
STREET_TYPE
ST
City
STOCKTON
Zip
95203
APN
13737004
CURRENT_STATUS
01
SITE_LOCATION
55 S LINCOLN ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Stantec <br /> Report of Findings for the Waterfront Towers Separate Phase Hydrocarbon Investigation <br /> and Unocal Extraction Well Pilot Study <br /> Waterfront Towers Parking Lot <br /> March 4, 2011 <br /> The total groundwater extracted from GWE-1 was 147.5 gallons, when averaged over time, this <br /> would be approximately <0.11 gpm. Groundwater extraction data can be viewed in Table 2. <br /> The total mass of TPHg removed during the pilot test from soil vapor was estimated using <br /> analytical results for TPHg as hexane, mass flow rates, and system runtime. The calculations <br /> are presented in Table 6. Similar calculations based on FID readings as hexane were not <br /> completed because of the scale of the difference between laboratory results and FID <br /> measurements. Other chemical constituents such as BTEX were not calculated individually <br /> because those laboratory results were all non-detect and are also assumed to be incorporated <br /> within the TPHg results as part of the applicable carbon range. <br /> During TPE on GWE-1, approximately 3.05 lbs of TPHg were removed by SVE. The removal <br /> rate was approximately 3.14 Ib/day. Calculations of mass removal by SVE are presented in <br /> Table 6. <br /> During TPE on GWE-2, the removal of chemical constituents is not directly calculated because <br /> groundwater analytical samples were not collected during TPE and also due to low groundwater <br /> production and flow rates. During the first half of the TPE test on GWE-2, the stinger tube orifice <br /> was lowered into the well casing approximately 13 feet bgs, which was approximately the level <br /> of the air/water interface inside the well. It was lowered to 17 feet bgs for the remainder of the <br /> test, but produced little groundwater. Despite lowering the stinger tube orifice to the bottom of <br /> the well little to no groundwater was produced following the deeper placement. <br /> Presentation of groundwater chemical constituent total removal and removal rates is reserved <br /> for the GWE test data and results sections below where the information collected is more viable <br /> and meaningful for such an analysis. <br /> 4.11 GWE-1 AND GWE-2 CONCLUSIONS <br /> The results of the GWE and TPE tests were evaluated with the following objective feasibility <br /> criteria: <br /> • Projected groundwater recovery rates <br /> • Projected SVE vapor flow rates <br /> • Projected GWE and SVE chemical mass removal rates <br /> • Projected information about GWE and SVE operational parameters <br /> • Conceptual design of GWE and SVE from GWE-1 and GWE-2 <br /> Groundwater extraction and treatment from GWE-1 and GWE-2 is considered a necessity <br /> because those activities may help to recover chemical mass from the UOU and maintain <br /> cleanliness of fill material placed there by the SRDA following excavation activities. GWE-1 <br /> (northernmost GWE well) and GWE-2 (the southernmost GWE well) are located in the GCT that <br /> was completed on the western boundary of the UOU excavation fill. The floor of the GCT slopes <br /> from north-to-south; thus when pumping from the GCT is initiated downstream, groundwater will <br /> tend to flow first through GWE-1 and then to GWE-2; this mimics the Site geology where, in <br /> general, groundwater has a tendency to flow from near Weber Avenue to the north through the <br /> 4.13 <br />
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