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ARCHIVED REPORTS XR0001365
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3500 - Local Oversight Program
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PR0544188
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ARCHIVED REPORTS XR0001365
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Last modified
2/27/2019 3:15:14 PM
Creation date
2/27/2019 11:42:30 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001365
RECORD_ID
PR0544188
PE
3526
FACILITY_ID
FA0006698
FACILITY_NAME
FERNANDOS PLACE
STREET_NUMBER
1201
Direction
S
STREET_NAME
CENTER
STREET_TYPE
ST
City
STOCKTON
Zip
95209
APN
14716003
CURRENT_STATUS
02
SITE_LOCATION
1201 S CENTER ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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WNg
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EHD - Public
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" - _ y <br /> i13 July 2004 <br /> s AGE-NC Project No 00-0769 <br /> Page 3 of 7 - <br /> 3 1 ' GROZJND WATER ELEVATION AND GRADIENT <br /> Depth to ground water was between 25 92 feet (MW-4D) and 30 12 feet (MW-5E) below the tops <br />' r ' of the well casings (BTOC)on 24 February 2004 Ground water elevations ranged from 15,34 feet ' <br /> (MW-4D)to 19 11 feet(MW--7D)below mean sea level(MSL) However,well casing elevation data <br /> for well MW-4D recorded during the February 2004 site survey appears to be erroneous' The well <br />' casing elevation data for well MW-4D was not utilized in plotting ground water elevation data <br /> Ground water elevation data collected from the site and wells off-site were plotted for the informal <br />' HU-1 through HU-4 hydrogeologic flow,units Ground water elevation data is presented in Table 1 <br /> and contoured ground water elevation data is presented in Figures 3 through 6 The elevation and <br /> gradient for each"unit is described below <br /> HU-1 <br /> Based on ground water elevation data collected in HU-1 Upper Zane(25 to 51 feet bsg),the ground <br /> water flow is generally toward the east and east--southeast with an average gradient of approximately <br /> • 0 003 ft/ft (Figure 3) <br /> HU-2 _ <br />' Based on ground water elevation data collected in HU-1(112 to 125 feet bsg),the ground water flow <br /> resembled an easterly trending ridge with the southern limb flowing toward the southeast at a <br /> gradient of approximately 0 002 ft/ft The northwest limb was inferred to be flowing north-northeast <br />' (Figure 4) <br /> r <br /> HU-3 <br /> Based on ground water elevation data collected in HU-3(140 to 160 feet bsg),the ground water flow <br /> Idirection is generally toward the east with an average gradient of approximately 0 001 ft/ft r <br /> (Figure 5) N <br /> HU-4 <br /> I the ground water <br /> Based on ground water elevation data collected in HU-4 (160 to 175 feet bsg}, <br /> • flow direction was generally toward the north at an approximate gradient of 0 007 ft/ft (Figure 6) <br /> rAdvanced GeoEnv ronmental,Inc <br /> rr ' r <br /> n s <br />
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