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ARCHIVED REPORTS XR0001026
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3500 - Local Oversight Program
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PR0544236
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ARCHIVED REPORTS XR0001026
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Last modified
3/6/2019 8:03:07 PM
Creation date
3/6/2019 4:10:48 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0001026
RECORD_ID
PR0544236
PE
3526
FACILITY_ID
FA0024238
FACILITY_NAME
JM EQUIPMENT COMPANY
STREET_NUMBER
1245
Direction
W
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16323034
CURRENT_STATUS
02
SITE_LOCATION
1245 W CHARTER WAY
P_LOCATION
01
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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Geolog"'Technics Inc Page 3 <br /> 4''Quarter 2001 Groundwater Momtonng Report <br /> Project No 507 2 <br /> January 17,2002 <br />' <br /> Vertical Groundwater Gradients <br /> Under vertical groundwater flow conditions, the water level in a monitoring well is a <br /> function of the length of the well screen and its depth or vertical position in the aquifer As <br /> with horizontal flow conditions, the diameter of the well or piezometer is immaterial <br /> The following procedure is used to calculate vertical groundwater gradient <br /> • Determine vertical distance between the two measuring devices by the distance from the <br /> mid-point between the top and bottom seal of the deep well (MW-109) and the mid- <br /> point between the groundwater elevation and the bottom seal in the shallow well (MW- <br /> 9) <br /> • Measure the head in both wells used in the calculations <br /> • If the lateral distance between the well pair is greater than a few feet, then calculations <br />' must be made to correct the down-gradient piezometric head to account for the sloping <br /> water table between the wells The calculation considers the slope of the water table and <br /> the distance in a down-gradient direction between the two wells used in the calculations <br /> rFigure 2 shows the location of the well cluster used for calculating the vertical groundwater <br /> gradient in this report, MW-9 and MW-109 Table 1 shows Summary of Water Level and <br /> M Gradients Slope and Bearing, and Table 2 shows the calculated vertical gradients The <br /> information used in the calculations is shown below <br /> Vertical gradient calculation formulas are as follows <br /> G Vertical correction for gradient [(gw gradient slope) x (distance) = vertical correction] <br /> 0 Vertical head [(head of deep well) - (head of shallow+ correction) = vertical head] <br /> • Vertical gradient [(vertical head) /vertical distance) = vertical gradient] <br /> 1 For both of the December 2001 monitoring events a vertical gradient was calculated for the <br /> MW-9/MW-109 pair In both cases the vertical gradient was negative (a downward <br /> direction) and larger in magnitude than the horizontal gradient of the water table <br />' 1.2 Groundwater Sampling Procedure <br /> 1 On December 4, 2001, Don Light of Del-Tech mobilized to the site to conduct groundwater <br /> monitoring of the eleven existing monitoring wells <br /> Before sampling was attempted the wells were sounded for depth to water and then a clear <br /> disposable bailer was used to determine if floating product was present The wells were <br /> purged of at least three well volumes of stagnant water using a dedicated Waterra check-ball <br /> assembly and '/z inch tubing Purging continued until the temperature, conductivity, and pH <br /> of the groundwater stabilized (<10% variation between three readings), indicating that <br />
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