Discussion
Flow through a 500 m wide section of that aquifer, at transmissivity 750 m\( ^2 \)/day and gradient 0.002, is
Answer: A
Correct answer: 750 m\( ^3 \)/day
The discharge through a width \( W \) of aquifer is
\[ Q = TiW = 750 \times 0.002 \times 500 = 750 \ \mathrm{m^3/day} \]which is the Darcy law written for the whole saturated thickness. Note that the transmissivity has already absorbed the thickness, so the aquifer depth must not be brought in again.
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