Subtopic: Steady and unsteady flow in confined and unconfined aquifers
Question Statement:
In an unsteady pumping test in a confined aquifer, drawdown is plotted against time on semi-logarithmic paper (Cooper-Jacob method). The drawdown per log cycle of time is $\Delta s = 1.20\text{ m}$. The constant pumping discharge is $Q = 3456\text{ m}^3\text{/day}$ ($= 0.040\text{ m}^3\text{/s}$). Using Cooper-Jacob's relation $T = \frac{2.303 Q}{4 \pi \Delta s}$, the aquifer transmissivity $T$ in $\text{m}^2\text{/day}$ is ________ (round off to 1 decimal place). Take $\pi = 3.1416$.