In connection with pumping, or in this case with confined conditions, one receives data about the permeability coefficient in half the aquifer.
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can see the principles of this technique of the operation. By that technique
one can receive very exact results about the position and depths of the
ground water effective zone. The thickness of this zone you get the distribution
of the ground water within the saturated zone, further the degree of homogeneity
of the aquifer, the vertical distribution of the aquifer's field, further
the answer if an exchange between different formations can happen. In this
case you have an exchange of the lower aquifer which is under pressure with
the upper aquifer which is under lower pressure, therefore you have an upstream
and exchange of the two aquifers. In connection with pumping, or in this case with confined conditions, one receives data about the permeability coefficient in half the aquifer. |
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