The problem provides the following parameters for a confined aquifer system:
The discharge ($Q_0$) of a single tubewell operating independently in a confined aquifer is given by the Thiem equation (steady-state):
$ s_0 = \frac{Q_0}{2 \pi K b} \ln\left(\frac{R}{r_w}\right) $
Here, $s_0$ is the drawdown, $Q_0$ is the discharge, $K$ is hydraulic conductivity, $b$ is aquifer thickness, $R$ is the radius of influence, and $r_w$ is the well radius.
When multiple wells operate simultaneously, their cones of depression interfere. The total drawdown at the location of any well is the sum of the drawdown caused by its own pumping and the drawdowns caused by the other pumping wells (superposition principle).
Let $Q_{actual}$ be the discharge of each well when all three operate simultaneously. The drawdown at the location of the first well ($s_1$) is:
$ s_1 = \frac{Q_{actual}}{2 \pi K b} \ln\left(\frac{R}{r_w}\right) + \frac{Q_{actual}}{2 \pi K b} \ln\left(\frac{R}{d}\right) + \frac{Q_{actual}}{2 \pi K b} \ln\left(\frac{R}{d}\right) $
Simplifying this equation:
$ s_1 = \frac{Q_{actual}}{2 \pi K b} \left[ \ln\left(\frac{R}{r_w}\right) + 2 \ln\left(\frac{R}{d}\right) \right] $
Assuming the maximum drawdown at each well location remains the same ($s_1 = s_0 = 10$ m), we can find the ratio of the actual discharge ($Q_{actual}$) to the original discharge ($Q_0$).
From the single well equation: $10 = \frac{Q_0}{2 \pi K b} \ln\left(\frac{R}{r_w}\right)$
From the simultaneous operation equation: $10 = \frac{Q_{actual}}{2 \pi K b} \left[ \ln\left(\frac{R}{r_w}\right) + 2 \ln\left(\frac{R}{d}\right) \right]$
Equating the two expressions (since both equal 10):
$ \frac{Q_0}{2 \pi K b} \ln\left(\frac{R}{r_w}\right) = \frac{Q_{actual}}{2 \pi K b} \left[ \ln\left(\frac{R}{r_w}\right) + 2 \ln\left(\frac{R}{d}\right) \right] $
Solving for the ratio $\frac{Q_{actual}}{Q_0}$:
$ \frac{Q_{actual}}{Q_0} = \frac{\ln\left(\frac{R}{r_w}\right)}{\ln\left(\frac{R}{r_w}\right) + 2 \ln\left(\frac{R}{d}\right)} $
Now, substitute the values:
$ \frac{Q_{actual}}{Q_0} = \frac{9.2103}{9.2103 + 2 \times 1.2040} = \frac{9.2103}{9.2103 + 2.4080} = \frac{9.2103}{11.6183} \approx 0.79275 $
The percent loss in discharge is calculated as:
$ \text{Percent Loss} = \left(1 - \frac{Q_{actual}}{Q_0}\right) \times 100 $
$ \text{Percent Loss} = (1 - 0.79275) \times 100 = 0.20725 \times 100 \approx 20.73\% $
Water from a confined aquifer having transmissivity of 1000 $m^2 day^{-1}$ is pumped through a fully penetrating well of 300 mm diameter at a rate of 1200 $m^3 day^{-1}$. If the radius of influence is 400 m, the drawdown in the well under steady-state flow condition in meter is __________ [round off to two decimal places]
(Take $\pi = 3.14$)