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Last modified
1/31/2019 6:59:17 PM
Creation date
1/31/2019 2:26:04 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0543429
PE
3528
FACILITY_ID
FA0005340
FACILITY_NAME
J C TRUCKING
STREET_NUMBER
1207
Direction
S
STREET_NAME
AURORA
STREET_TYPE
ST
City
STOCKTON
Zip
95206
APN
14734404
CURRENT_STATUS
02
SITE_LOCATION
1207 S AURORA ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
WNg
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EHD - Public
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f <br /> Methanol was detected in MW-8 at the low value of 62.µg/L. The compound 1,2 DBA was <br /> not detected in any of the monitor wells sampled. The fuel oxygenates DIPE, EtBE, TAME, <br /> TBA, and ethanol were not detected at or above the laboratory reporting limit in any of the <br /> groundwater samples collected and analyzed from the eight monitor wells. <br /> Results.of the analyses are summarized in Table 11. The analytical laboratory data sheets <br /> can be found in Appendix B. <br /> 3.3 Groundwater Flow Direction and Gradient <br /> h: JJW prepared a groundwater potentiometric surface map based on the'static groundwater <br /> elevations measured on June 23, 2009 in. the seven monitor wells screened across the <br /> groundwater table. During this first half of semi-annual groundwater sampling the <br /> groundwater level is approximately thirty-one feet below the ground surface. The <br /> groundwater elevations for this sampling event were approximately one foot higher than the <br /> last quarterly sampling event in December 2008. The shallow groundwater flow direction, in <br /> the vicinity of the former USTs, was calculated to flow toward the southeast with an average, <br /> relatively flat, groundwater gradient of approximately 0.0014 ft/ft. This is consistent with the <br /> data collected from previous quarters. ' Figure 3 illustrates the groundwater potentiometric <br /> surface and flow direction. <br /> Based on the analytical data from the monitor wells, the TPH-gasoline plume is inferred to be <br /> approximately 90 feet in length along its long axis. The plume is not inferred to extend down <br /> gradient very far due in part to the relatively flat groundwater gradient. Figure 4 illustrates the <br /> inferred limits of groundwater contamination at the top of the groundwater table for the June <br /> E r? 2009 sampling event. <br /> 4.0 OZONE SPARGE SYSTEM <br /> Lr <br /> The ozone sparging system was started, and ozone sparging was initiated on December 1, <br /> 2004. On 29 March 2009, sparge point SP-6 was taken of-line and SP-4 put on-line to focus <br /> on ozone remediation at the 125 foot bgs level near to monitor well MW-11. From the <br /> quarterly sampling event on 9 December 2008, to 30 May 2009, the system ran 60 days out <br /> of 172 days, for a total run time of 18,280 hours. From 30 May 2009 to the last time the <br /> system was checked, on 7 November 2009, the system:has run continuously for 161 days, <br /> and has a total run time of 21,384 hours since initial startup. The ozone generating stations <br /> on the ozone sparge system panel are currently plumbed to the following sparge points at the <br /> listed depths (feet below ground surface): <br /> Sparge Point Depth Sparge Point Depth Sparge Point Death <br /> SP-1 50 SP-5 50 SIP 50 <br /> SP-2 50 SP-6 SP-10 38 <br /> f SP-3 50 SP-7 50 SP-11 50 <br /> SP-4 125 SP-8 48 SP-12 50 <br /> All the sparge points at the 50 foot level are currently being utilized to maximize the <br /> + remediation efforts on the most contaminated zone, the shallow groundwater in the vicinity of <br /> the former USTs. One sparge point in each UST excavation pit (SP-6 and SP-10), installed <br /> at the top of the groundwater table, has been on-line to remediate soil contamination from <br /> ozone system initial startup to 29 March 2009, when SP-6 was taken off-line for the benefit of <br /> deeper remediation efforts. Sparge point SP710 is currently still on-line. The system is <br /> 4 <br /> JJW GEOSCIENCES Inc. <br />
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