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The top documents tagged [unconfined aquifer slide]
Steady Flow to Wells Groundwater Hydraulics Daene C. McKinney
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Unit 04 : Advanced Hydrogeology Hydraulic Testing
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Groundwater and Wells Well is a hole bored into the zone of saturation and is the most common way of removing groundwater. Two types of wells: 1) Surface
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Stream Function Definitions Discharge Potential U is aquifer flux. It is a vector. U = qb, where q is flux per unit depth and b is aquifer thickness For
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Aquifers are typically saturated regions of ground water which produce an economically feasible quantity of water to a well or spring
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