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Question

A fully penetrating tubewell of 0.2 m diameter is operational in a confined aquifer of 20 m thickness. The hydraulic conductivity of the formation (K) is 20 m per day and the radius of influence is 1000 m. Water table is 50 m above the bottom of screen and the maximum drawdown is 10 m. Subsequently two more tubewells of the same size are installed in such a way that the three tubewells form an equilateral triangle of side 300 m. All three tubewells have equal discharge when operated independently. If all tubewells are operated simultaneously, the percent loss in the discharge of the first well is

The correct answer is
20.73

Given Parameters

The problem provides the following parameters for a confined aquifer system:

  • Tubewell diameter: $D = 0.2 \text{ m}$
  • Aquifer thickness: $b = 20 \text{ m}$
  • Hydraulic conductivity: $K = 20 \text{ m/day}$
  • Radius of influence: $R = 1000 \text{ m}$
  • Distance between wells: $d = 300 \text{ m}$
  • Maximum drawdown: $s_0 = 10 \text{ m}$
  • Number of wells: 3
  • Well radius: $r_w = D/2 = 0.1 \text{ m}$

Single Well Discharge Calculation

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.

Simultaneous Well Operation Analysis

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] $

Calculating Actual Discharge and Loss

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:

  • $R/r_w = 1000 / 0.1 = 10000$
  • $R/d = 1000 / 300 = 10/3 \approx 3.333$
  • $\ln(R/r_w) = \ln(10000) \approx 9.2103$
  • $\ln(R/d) = \ln(10/3) \approx 1.2040$

$ \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 $

Percent Loss Calculation

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\% $

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Important Questions from Steady Flow Through Wells

  1. A well fully penetrates a $30\text{ m}$ thick confined aquifer. After a long period of pumping at a constant rate of $0.06\text{ m}^3\text{.s}^{-1}$, drawdowns of $3.6\text{ m}$ and $2.0\text{ m}$ are found at distances $60\text{ m}$ and $120\text{ m}$ away from the well, respectively. The hydraulic conductivity of the aquifer is $n \times 10^{-4}\text{ m.s}^{-1}$. The value of $n$ is ________ (Rounded off to two decimal places)
  2. A $40$ cm diameter tubewell is constructed in a $10$ m thick confined aquifer having hydraulic conductivity of $25$ m day$^{-1}$. The peizometric surface is observed to be $40$ m high from the impervious stratum at the radius of influence of $500$ m. The drawdown in the tubewell is $30$ m. If the thickness of aquifer is doubled and diameter of tubewell is reduced to half, keeping all other parameters and conditions same, the change in discharge from the well is [Take $ \pi = 3.14$]
  3. In an area, one tubewell of 15 cm diameter was operating such that groundwater table is 40 m above the bottom of screen. The groundwater formation has permeability (K) as 20 m.d$^{-1}$ and well has radius of influence of 980 m with a maximum drawdown of 12 m. After some time, a second tubewell of same size was installed at a distance of 500 m from the first tubewell. If both the tubewells are running simultaneously and have equal discharge, the loss of discharge in the first tubewell due to installation of the second tubewell, in %, is _________. (Rounded off to 2 decimal places)
  4. A $0.30$ m diameter well penetrates an unconfined aquifer with a saturated depth of $40$ m. After $8$ hours of pumping at a steady rate of $0.03$ $m^3$ $s^{-1}$, the drawdown in two observation wells located at $20$ m and $50$ m away from the pumping well are found to be $3$ m and $2$ m, respectively. The drawdown in the pumping well in m is ________ (rounded off to $1$ decimal place, Consider $\pi = 3.14$).
  5. 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 $\pi = 3.14$)

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