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IT <br /> • Shallow aquifers receive recharge by precipitation , <br /> crop irrigation , leakage from lagoons, and leakage <br /> from Stanislaus River <br /> • Vertical groundwater flow between the D Sand and <br /> underlying sediments is minimal and insignificant <br /> • Streambed of Stanislaus River has a uniform <br /> hydraulic conductivity and thickness <br /> • Stanislaus River has a uniform water depth <br /> • Water-supply wells and groundwater extraction wells <br /> fully penetrate the aquifers in which they are <br /> screened <br />