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Bounded Aquifers
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AQTESOLV Home > Tour > Bounded Aquifers

Bounded Aquifers

AQTESOLV now incorporates a powerful tool for analyzing pumping tests in bounded aquifers. Not only can you simulate simple problems with single boundaries, but you also can evaluate up to four boundaries!

The method of images is a well-known technique for mathematically incorporating the effect of boundaries in the calculation of drawdown in a bounded aquifer. For single boundaries such as a stream or a fault, it is straightforward to introduce an image well to represent the boundary; however, when two parallel boundaries are involved (e.g., a channel aquifer), the number of image wells required becomes infinite. Manual generation of these image wells becomes extremely tedious.

Fortunately, AQTESOLV has simplified the evaluation of these complex boundary problems by introducing a tool that automatically computes the location and number of image wells necessary to compute drawdowns correctly for a specified set of boundaries.

 
bulletrecharge and no-flow boundaries
bulletchannel aquifers
bulletclosed channel aquifers
bulletclosed aquifers
 

Channel (Strip) Aquifers

Aquifers often occur in long narrow valleys or buried channels. Simulating the two parallel no-flow boundaries of these channel aquifer configurations requires the use of an infinite array of image wells.

AQTESOLV simplifies the analysis by automatically generating the required image wells for you as shown in the example below.

 
Drawdown measured during a constant-rate pumping test in a buried channel aquifer near Estevan, Saskatchewan (Walton 1970).
 
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