| Description
| Solutions of groundwater flow to wells rank highest in importance. The objective of this course is to introduce how to determine the storage coefficients and transmissivities of aquifers by pumping tests of wells ; furthermore, well flow equations for steady and unsteady condition, for various types of aquifers, and for several special boundary conditions are also introduced. With these aquifer characteristics known, future declines in groundwater levels associated with pumpage can be calculated and as a basis for groundwater resource management.
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