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SR0084051 (4)
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SR0084051 (4)
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Last modified
10/26/2022 1:19:52 PM
Creation date
10/26/2022 1:17:47 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
SR0084051
PE
2903
FACILITY_ID
FA0024553
FACILITY_NAME
SHARPE ARMY DEPOT OFF SITE EXTRACTION WELL INSTALLATION
STREET_NUMBER
700
STREET_NAME
ROTH
STREET_TYPE
RD
City
LATHROP
Zip
94523
APN
19802001
ENTERED_DATE
8/10/2021 12:00:00 AM
SITE_LOCATION
700 ROTH RD
P_LOCATION
07
P_DISTRICT
003
QC Status
Approved
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EHD - Public
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Groundwater Well Installation Work Plan Sharpe Army Depot <br /> Lathrop, California <br />Ahtna Environmental, Inc. 12 <br />9. Run the data logger self-test routine (if available) to check that the data logger and transducers <br />are operating properly. If the self-test indicates that the instrument is not operating correctly, <br />the test will not be started, and a backup transducer will be installed. <br />10. Measure and record the water level in the pumped well and each observation well. Record <br />measurements taken as part of the test on an aquifer constant-rate test field data sheet <br />(Appendix A). Record water levels prior to the start of the test. Then record levels during the <br />pumping period at an interval of 5 to 10 minutes (depending on the rate of drawdown and using <br />professional judgment). Finally, record levels after the pump has stopped until the water level <br />in the test well is within 10 percent of its initial (pre-pumping) water level. <br />11. Check that the power supply or generator for the submersible pump is ready, piping is in place, <br />the discharge rate has been determined and set, and the data logging equipment is ready. The <br />initial discharge rate for the step-drawdown test is 5 gpm for the A Zone well and 40 gpm for the <br />C Zone well. The discharge rate for the constant rate test will be determined based on the <br />results of the step-drawdown test. <br />12. Turn on data loggers for all transducers before starting the pump in the test well. Record the <br />test start time. <br />13. Begin to measure water levels periodically using a manually operated water level meter to check <br />the accuracy of the transducer readings and to provide backup data if the data logger fails. <br />Check water levels more frequently at the beginning of the test when levels are changing rapidly <br />(i.e., every minute for the first 10 minutes, and every 2 minutes for the next 10 minutes, etc.). <br />14. Begin to check the pumping discharge rate periodically using the flow meter to check that the <br />well is being pumped at the appropriate discharge rate. Also, check the flow rate by comparing <br />it to the totalizer flow meter reading. Record the flow rate on the aquifer constant-rate test field <br />data sheet (Appendix A). <br />15. After pumping the well for the specified test duration, set the data logger to begin recording <br />recovery, and then shut off the pump. <br />16. After monitoring recovery until the water level in the test well is within 10 percent of its pre- <br />pumping water level, remove the pump and transducers from the wells. <br />17. Transfer the test data from the data logger to an appropriate data storage device (such as a <br />personal computer or tablet) using the downloading procedures from the data logger. <br />Pumping test data will be analyzed using AQTESOLV™, an industry-standard software package used for <br />the design and interpretation of aquifer tests. Analyses may include one or more of the following: <br />• Neuman type curves for delayed yield analysis (Neuman, 1975) <br />• Leaky Aquifer Method (Hantush, 1956), Distance-Drawdown (Jacob, 1963), or Residual Drawdown <br />Method (Jacob, 1950) for transmissivities and hydraulic conductivities <br />• Leaky Aquifer Method (Hantush, 1956) method for storativity values <br />• Other methods as applicable, based on site conditions and test results <br />Data from the constant rate tests will be used to calculate transmissivity and storativity.
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