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ARCHIVED REPORTS_XR0003876
Environmental Health - Public
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3500 - Local Oversight Program
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PR0545428
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ARCHIVED REPORTS_XR0003876
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Last modified
3/9/2020 7:23:22 PM
Creation date
3/9/2020 10:46:53 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0003876
RECORD_ID
PR0545428
PE
3528
FACILITY_ID
FA0005487
FACILITY_NAME
MARCIS DIESEL SERVICE
STREET_NUMBER
2969
STREET_NAME
LOOMIS
STREET_TYPE
RD
City
STOCKTON
Zip
95205
CURRENT_STATUS
02
SITE_LOCATION
2969 LOOMIS RD
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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' eolo ccal? <br /> G g eclucccs!nc Page 3 <br /> Groundwater Monitonng Report <br /> Project No 770 2 <br /> June 15, 2004 <br /> the site The deep well gradient directions for the same events are illustrated in Figures 213, <br /> 3B and 4B,respectively <br /> The historical water table gradients are illustrated in Figure 5A & 5B Groundwater <br /> Gradient Rose Diagrams for Water Table and Deep Wells, respectively The site's shallow <br />' aquifer displays highly variable shifts in groundwater direction It is noted that groundwater <br /> direction has been predominantly to the southeast since additional wells were installed in <br /> May 2002 The deeper aquifer flow had been consistently to the east for the previous seven <br /> sounding events But on April 28 and May 23, 2003, the gradient reversed ISO'from an <br /> easterly direction to a westerly direction The direction reversed again to the east for the <br /> remainder of the sounding events <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-105) and the mid- <br /> point between the groundwater elevation and the bottom seal in the shallow well (MW- <br /> 5) <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 /> tFigures 2A & 2B show the location of the well clusters, MW-51105 and MW-6/106, used <br /> for calculating vertical groundwater gradient in this report Table I includes Summary of <br /> ' Water Level and Gradients Water Table Wells, Table 2 includes Summary of Water Level <br /> and Gradients Deep Wells, Table 3 shows the calculated vertical gradients, and Table 6 <br /> contains the well construction details The information used in the calculations is shown <br /> ' below <br /> ' Vertical gradient calculation formulas are as follows <br /> • Vertical correction for gradient [(gw gradient slope) x (distance) = verticaI correction) <br /> • Vertical head [(head of deep well) - (head of shallow + correction) = vertical head] <br /> I0 Vertical gradient [(vertical head) /vertical distance) = vertical gradient] <br />
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