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ARCHIVED REPORTS_XR0002243
Environmental Health - Public
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3500 - Local Oversight Program
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PR0545205
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ARCHIVED REPORTS_XR0002243
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Last modified
1/27/2020 3:43:34 PM
Creation date
1/27/2020 3:20:24 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0002243
RECORD_ID
PR0545205
PE
3528
FACILITY_ID
FA0003164
FACILITY_NAME
NORTH POLE GAS & FOOD INC
STREET_NUMBER
574
Direction
W
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
TRACY
Zip
95376
CURRENT_STATUS
02
SITE_LOCATION
574 W GRANT LINE RD
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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SJGOV\sballwahn
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EHD - Public
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20 STEP DRAWDONVN TEST <br /> A three step, well performance test was performed in EW-1 On August 29, 2001 the first stem <br /> was performed at a nominal flow rate of 3 GPM On October 31 2001 two stepped rates were <br /> performed at a nominal flow rates of 6 and 12 GPM The three steps were conducted at mean <br /> flow rates as maintained by DOLETm Flow Regulators of the indicated nominal flow rates The <br /> following table lists the nominal flow rate, the mean flow rate, the end of step drawdown, and the <br /> duration for each step of the step drawdown test The sum of two nominal flow rates from two <br /> DOLE valves ar e indicated as appropriate <br /> Step Nominal Mean Drawdown Step <br /> Flow Rate Flow Rate (Ft ) Duration <br /> (GPM) (GPM) (minutes) <br /> 1 3 2 56 073 40 <br /> 2 6 5 65 279 30 <br /> . 3 12 11 01 11 10 90 <br /> The interpretation of the step drawdown test is provided in Figure 1 This graph is a double <br /> logarithmic plot showing the water level drawdown versus the discharge rate The step <br /> drawdown test data points are represented by the three filled circles <br /> Drawdown in a pumped well is made of two components aquifer loss (drawdown caused by <br /> resistance to laminar flow in the aquifer) and well loss Well loss is the drawdox n required to <br /> overcome the resistance to turbulent flow in the vicinity of the well through the screen and <br /> filterpack, and within the well if the pump is tightly fit Anisotropic aquifer stratification can <br /> also affect tlus relationship The total drawdown is represented by the following equation <br /> D = BQ } CQP <br /> where D = drawdown in the pumped well in YI <br /> Q = flow or discharge rate in GPM, <br /> BQ = aquifer loss, <br /> CQP = well loss, <br /> and B, C, and P are coefficients <br /> H 20GE01, A GROUNDWATER CONSULTANCY <br />
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