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ARCHIVED REPORTS XR0006109
EnvironmentalHealth
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2900 - Site Mitigation Program
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PR0542421
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ARCHIVED REPORTS XR0006109
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Last modified
6/21/2019 12:55:13 PM
Creation date
6/21/2019 10:35:52 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0006109
RECORD_ID
PR0542421
PE
2950
FACILITY_ID
FA0024377
FACILITY_NAME
COUNTRY CLUB BLVD/295950
STREET_NUMBER
1876
STREET_NAME
COUNTRY CLUB
STREET_TYPE
BLVD
City
STOCKTON
Zip
95204
APN
12319101
CURRENT_STATUS
01
SITE_LOCATION
1876 COUNTRY CLUB BLVD
P_LOCATION
01
QC Status
Approved
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SJGOV\wng
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EHD - Public
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� 4 <br /> I <br /> PUMP TEST <br /> The presence of the two groundwater zones, A and B, and the presence of the monitor wells MW 1 <br /> through MW5 which are screened across both zones, complicated the performance of a pump test <br /> at this site Because of this MW 1 was destroyed prior to the test <br /> Of major concern was the location of MW1 in relation to RW1A and RW1B and the MW6 cluster <br /> With monitor wells completed across both zones pumping from one zone will cause flow up or <br /> down the cross zone well from the non-pumped zone <br /> Because the modeling was only preliminary a simple analog model of the interaction of pumping <br /> from RWOIA and the cross-zonal flow in MW1 was developed The flow up the well is driven by <br /> the difference in head between the two groundwater zones Even in two inch casing, the anticipated <br /> flow between the two zones is significant with even a slight difference in head <br /> From the Hazen-Williams Formula, for anticipated flow in a pipe <br /> Q=0 432C,D2 6354 54 <br /> Q-= ft3/S <br /> Ci= Coefficient dependent on surface roughness approximately 120 <br /> D= pipe diameter in feet <br /> S = head lose in feet per feet of pipe <br /> For a 2-inch pipe with a differential of 0 01 feet per the 3-foot clay layer that separates the zones <br /> the flow in the pipe would be 13830 gallons per day <br /> D=2/12=0 167 <br /> S= 0 1/3=0 033 <br /> Q=O 432*120*0 1672 63*0 0033°54=0 0214 ft3/sec=1 284 cfm = 9 604 gpm or 13830 gpd <br /> From the above it can be assumed that flow between zones in MW 1 would be sufficient to equalize <br /> the head between the two zone even in response to significant pumping at RWO1 <br /> The preliminary model used the distance drawdown equation to calculate the response to pumping <br /> The equation was solved for three instances <br /> 1 The response of the upper zone from pumping RWOIA <br /> 2 The response of the upper zone to the flow of water from the lower zone to upper zone at <br /> MW 1 <br /> 3 The drawdown of the lower zone in response to flow from the lower zone to the upper zone in <br /> MW I <br /> While running the model the flow parameter in MWI between the two zones was adjusted so that <br /> the groundwater elevation for both the A and B zone were equal, as the zones responded to <br /> pumping at RW 1 A <br /> In an analog model the resulting drawdowns are considered to be additive The model indicated <br /> that the flow at MW 1 would be great enough to significantly affect the response of the upper <br /> I <br /> Pump Test 1/20-27/03 <br />
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