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ARCHIVED REPORTS XR0001707
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ARCHIVED REPORTS XR0001707
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Last modified
5/17/2019 2:59:14 PM
Creation date
5/17/2019 2:32:13 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001707
RECORD_ID
PR0522479
PE
2957
FACILITY_ID
FA0015299
FACILITY_NAME
GEWEKE LAND DEVELOPMENT & MARKETING
STREET_NUMBER
16
Direction
S
STREET_NAME
CHEROKEE
STREET_TYPE
LN
City
LODI
Zip
95240
APN
04323013
CURRENT_STATUS
01
SITE_LOCATION
16 S CHEROKEE LN
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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' 11•August 1999 <br /> AGE-NC Project No. 95-0109 <br /> Page 7 of 10 <br /> Data collected as,early as February 1994 was'included in the calculations of the remaining mass of <br /> hydrocarbons at the:site. Additional remediation is.likely to, have occurred in these areas, which , <br /> would further reduce the total mass of hydrocarbons remaining'at the site. . ; <br />' AGE notes that the hydrocarbon masses calculated are not intended'to be precise, but are only <br /> .estimates;based on the assumptions listed above for•use io evaluate`the'effectiveness of the remedial i. <br /> effort. The mass calculations and formulas are:presented in.Appendix E. <br /> 3.5. GROUND WATER GRADIENT AND DIRECTION <br /> The depth io ground water'ranged from 49.72 feet-bsg north bf the site to 52.39 feet bsg south of the <br /> site during the March 1999 monitoring event. The data indicates an average 1.23 feet increase of. <br /> ground water elevation between December 1998 and March 1999.'Grourid water elevation contours, <br /> based upon data collected on 17.March 1999, are depicted in Figure 3. The inferred ground water <br />' flow.direction is toward the south. Ground water elevations for MW-1 through MW-5 were.higher <br /> than the surrounding wells: These wells exhibit poor recharge and do not appear to be in equilibrium <br /> with the surrounding ground water, therefore data from these wells was not used to determine the <br /> ground water flow direction. <br /> ' 'Ground water elevation decreased an average of 0.24 feet between March and June 1999,•and <br /> decreased and average of 0.74 feet between June and July 1999. Ground water contours, based upon <br /> data collected on 30 July,1999 are depicted in,Figure 4.•A depression appears to be.located west of <br /> _ MW-14, while a localized high is located near,MW-9: Data,fro'm the,.June 1999.monitoring eyent51"s <br /> was.not plotted, but appears to be similar to the July 1999-data. Ground water elevations are-, <br /> summarized on Table 3. <br /> 3.6.' MICROBIOLOGICAL ACTIVITY'1N GROUNDWATER. <br /> Concentrations of-dissolved oxygen•variably increased and'decreased between-theDecember 1998 <br /> and March 1999 monitoring events and between'the Marchand-June 1999�'moriitoring &vents.in <br />' water samples collected from the wells.Only low general, <br /> microbiological activity was detected-in <br /> 'samples from both MW-9 and MW- `the "March •1999 sampling ^event. Selective <br /> 1 , • . , n...,.. - <br /> s'ubpopulations were not detected in the March 1999 samples: The laboratory report (.A. Keith <br /> Kaufman,March 30, 1999) and chain-of-custody form�are.included in Appendix D. <br /> Advanced GeoEnvironmental,Inc.' <br />
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