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ARCHIVED REPORTS_3RD QUARTER 2010 SITE STATUS REMEDIAL SUMMARY AND GROUNDWATER MONITORING REPORT
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ARCHIVED REPORTS_3RD QUARTER 2010 SITE STATUS REMEDIAL SUMMARY AND GROUNDWATER MONITORING REPORT
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Last modified
6/25/2020 5:01:40 AM
Creation date
6/24/2020 2:26:02 PM
Metadata
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EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
3RD QUARTER 2010 SITE STATUS REMEDIAL SUMMARY AND GROUNDWATER MONITORING REPORT
RECORD_ID
PR0519031
PE
2960
FACILITY_ID
FA0014239
FACILITY_NAME
PARCEL 2A - TIDEWATER STOCKTON
STREET_NUMBER
666
STREET_NAME
WEBER
STREET_TYPE
AVE
City
STOCKTON
Zip
95670
APN
13737002
CURRENT_STATUS
01
SITE_LOCATION
666 WEBER AVE
QC Status
Approved
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EHD - Public
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' Stanw <br /> L & M OPERABLE UNIT-THIRD QUARTER 2010 SITE STATUS, REMEDIAL SUMMARY, <br /> AND GROUNDWATER MONITORING REPORT <br /> Groundwater Monitoring and Sampling <br /> October 27, 2010 <br /> ' Validation issues with report number 73872: <br /> ' Matrix Spike and MSD results associated with samples MW-9 and MW-20 for the analyte MtBE <br /> ether were outside of the stated QC limits. This may indicate a possible bias for the reporting <br /> ' accuracy. The RPD values are within range indicating precision in reporting. The LCS <br /> recoveries were within QC limits indicating accuracy in reporting. Therefore, the reported <br /> values are considered valid. <br /> 2.4 THIRD QUARTER 2010 B-ZONE GROUNDWATER RESULTS <br /> 2.4.1 B-Zone Groundwater Gradient <br /> B-Zone groundwater elevations at the Site ranged from 7.19 ft below MSL in well MW-35 to <br /> ' 2.04 ft above MSL in well MW-44 (Table 3 and Figure 10). Groundwater flow during the third <br /> quarter 2010 in deeper zone (B-zone) was noticed in four separate sections of the site <br /> (northeast, southeast, central, and west). The highest B-Zone groundwater elevation (2.04 ft <br /> 1 above MSL) was reported in well MW-44, located in the southwest portion of the site east of <br /> Mormon Slough. Along the northeastern portion of the Site, groundwater flow direction was to <br /> the southeast with an approximate hydraulic gradient of 0.02 ft/ft. In the southeastern portion of <br /> ' the Site, groundwater flow direction was to the east-southeast with an approximate hydraulic <br /> gradient of 0.005 ft/ft. In the central part of the site, groundwater flow direction was to the <br /> northeast with an approximate hydraulic gradient of 0.01 ft/ft. In the western portion of the Site, <br /> ' groundwater flow direction was to the north-northwest with an approximate hydraulic gradient of <br /> 0.01 ft/ft (Figure 10). The overall historic trend of the B-Zone gradient is to the east-northeast. <br /> Historical groundwater flow direction and gradient data are summarized in Table 8, and vertical <br /> gradients summarized in Table 9. The B-Zone groundwater elevation contour map for the July <br /> 19, 2010 monitoring event is included as Figure 10. <br /> 2.4.2 B-Zone Groundwater Quality Data <br /> During the third quarter 2010, groundwater samples were collected from 15 deep zone wells <br /> between July 19 and 22, 2010 (Table 1). Groundwater analytical results are presented in <br /> Tables 4 through 7, and summarized below. TPHg, TPHd, TPHo, benzene, MtBE, and TBA <br /> isoconcentration contour maps are included as Figures 11 through 16, respectively. The <br /> ' certified laboratory analytical reports for the groundwater sampling event conducted for the L&M <br /> OU are included in Appendix C. <br /> o <br /> 1'17,dewlo61 SbAIon(ParceliA 15)\ReportsWMR120,,101013QIMSSRORSRQMRS'0d10n_FIN1 doo 2.8 <br />
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