The coefficient of transmissibility T for a confined aquifer can be determined by a pumping-out test together with other relevant observations. The applicable formula is (where Q = Discharge, and ΔS = Difference in drawdowns in two wells)

Question

TuteeHUB · Accepted Answer

$\frac{Q}{{1.72\;\sqrt {{\rm{\Delta }}S} }}$

TuteeHUB · Answer

$\frac{Q}{{2.72\;{\rm{\Delta }}S}}$

TuteeHUB · Answer

$\frac{Q}{{2.72}}{\rm{\Delta }}S$

TuteeHUB · Answer

$\frac{Q}{{2.72}}\sqrt {{\rm{\Delta }}S} $

1.	The coefficient of transmissibility T for a confined aquifer can be determined by a pumping-out test together with other relevant observations. The applicable formula is (where Q = Discharge, and ΔS = Difference in drawdowns in two wells)
A.	\(\frac{Q}{{2.72\;{\rm{\Delta }}S}}\)
B.	\(\frac{Q}{{1.72\;\sqrt {{\rm{\Delta }}S} }}\)
C.	\(\frac{Q}{{2.72}}{\rm{\Delta }}S\)
D.	\(\frac{Q}{{2.72}}\sqrt {{\rm{\Delta }}S} \)
Answer» B. \(\frac{Q}{{1.72\;\sqrt {{\rm{\Delta }}S} }}\)

The coefficient of transmissibility T for a confined aquifer can be determined by a pumping-out test together with other relevant observations. The applicable formula is (where Q = Discharge, and ΔS = Difference in drawdowns in two wells)

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