Radius of Influence given Discharge for Partially Penetrating Well Solution

STEP 0: Pre-Calculation Summary
Formula Used
Radius of Influence = (Radius of Well*exp((2*pi*Coefficient of Permeability*Aquifer Thickness*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/Discharge for Partially Penetrating Well))
R = (r*exp((2*pi*K*b*(H-hw)*G)/Qv))
This formula uses 1 Constants, 1 Functions, 8 Variables
Constants Used
pi - Archimedes' constant Value Taken As 3.14159265358979323846264338327950288
Functions Used
exp - n an exponential function, the value of the function changes by a constant factor for every unit change in the independent variable., exp(Number)
Variables Used
Radius of Influence - (Measured in Meter) - The radius of influence is the distance from a pumping well to the point where the drawdown, or lowering of the water table, becomes negligible.
Radius of Well - (Measured in Meter) - The radius of well refers to the horizontal distance from the center of the well to its inner wall, essentially the well’s radius.
Coefficient of Permeability - (Measured in Meter per Second) - Coefficient of Permeability refers to the ease with which water can flow through the aquifer's pore spaces.
Aquifer Thickness - (Measured in Meter) - Aquifer Thickness (at Midpoint between Equipotential lines) or otherwise is the thickness of aquifer in which the pore spaces of rock forming the aquifer may or may not be with water.
Initial Piezometric Surface - (Measured in Meter) - The initial piezometric surface refers to the level at which groundwater naturally stands in a confined aquifer before any pumping or external influence.
Depth of Water - (Measured in Meter) - Depth of Water is the depth in the well measured above the impermeable layer.
Correction Factor - Correction Factor refers to the reduced efficiency and altered flow patterns due to the well not extending through the entire aquifer thickness.
Discharge for Partially Penetrating Well - (Measured in Cubic Meter per Second) - Discharge for Partially Penetrating Well refers to the volume of water extracted from an aquifer when the well does not extend through the entire thickness of the aquifer.
STEP 1: Convert Input(s) to Base Unit
Radius of Well: 2.94 Meter --> 2.94 Meter No Conversion Required
Coefficient of Permeability: 0.105 Centimeter per Second --> 0.00105 Meter per Second (Check conversion ​here)
Aquifer Thickness: 15 Meter --> 15 Meter No Conversion Required
Initial Piezometric Surface: 20 Meter --> 20 Meter No Conversion Required
Depth of Water: 2.44 Meter --> 2.44 Meter No Conversion Required
Correction Factor: 0.83 --> No Conversion Required
Discharge for Partially Penetrating Well: 5.08 Cubic Meter per Second --> 5.08 Cubic Meter per Second No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
R = (r*exp((2*pi*K*b*(H-hw)*G)/Qv)) --> (2.94*exp((2*pi*0.00105*15*(20-2.44)*0.83)/5.08))
Evaluating ... ...
R = 3.90528888788538
STEP 3: Convert Result to Output's Unit
3.90528888788538 Meter --> No Conversion Required
FINAL ANSWER
3.90528888788538 3.905289 Meter <-- Radius of Influence
(Calculation completed in 00.020 seconds)

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Created by Suraj Kumar
Birsa Institute of Technology (BIT), Sindri
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Meerut Institute of Engineering and Technology (MIET), Meerut
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Partially Penetrating Artesian Well Calculators

Coefficient of Permeability given Discharge for Partially Penetrating Well
​ LaTeX ​ Go Coefficient of Permeability = Discharge for Partially Penetrating Well/((2*pi*Aquifer Thickness*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/(log((Radius of Influence/Radius of Well),e)))
Aquifer Thickness given Discharge for Partially Penetrating Well
​ LaTeX ​ Go Aquifer Thickness = Discharge for Partially Penetrating Well/((2*pi*Coefficient of Permeability*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/(log((Radius of Influence/Radius of Well),e)))
Thickness of Aquifer given Discharge for Partially Penetrating Well
​ LaTeX ​ Go Initial Piezometric Surface = Depth of Water+(Discharge for Partially Penetrating Well*(log((Radius of Influence/Radius of Well),e)))/(2*pi*Coefficient of Permeability*Aquifer Thickness*Correction Factor)
Discharge for Partially Penetrating Well
​ LaTeX ​ Go Discharge for Partially Penetrating Well = (2*pi*Coefficient of Permeability*Aquifer Thickness*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/(log((Radius of Influence/Radius of Well),e))

Radius of Influence given Discharge for Partially Penetrating Well Formula

​LaTeX ​Go
Radius of Influence = (Radius of Well*exp((2*pi*Coefficient of Permeability*Aquifer Thickness*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/Discharge for Partially Penetrating Well))
R = (r*exp((2*pi*K*b*(H-hw)*G)/Qv))

What is Discharge for Partially Penetrating Well?

The discharge for a partially penetrating well refers to the volume of water extracted from an aquifer when the well does not extend through the entire thickness of the aquifer. This discharge is affected by factors like the hydraulic conductivity of the aquifer, the length of the well screen, the drawdown, and the well's radius. In partially penetrating wells, flow towards the well is more complex due to the incomplete interaction with the entire aquifer thickness, leading to potential reductions in efficiency and increased head losses compared to fully penetrating wells.

How to Calculate Radius of Influence given Discharge for Partially Penetrating Well?

Radius of Influence given Discharge for Partially Penetrating Well calculator uses Radius of Influence = (Radius of Well*exp((2*pi*Coefficient of Permeability*Aquifer Thickness*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/Discharge for Partially Penetrating Well)) to calculate the Radius of Influence, Radius of Influence given Discharge for Partially Penetrating Well formula is defined as the maximum radial distance from the well at which the influence of the well's discharge is felt, and is a critical parameter in evaluating the impact of pumping on groundwater flow in partially penetrating wells. Radius of Influence is denoted by R symbol.

How to calculate Radius of Influence given Discharge for Partially Penetrating Well using this online calculator? To use this online calculator for Radius of Influence given Discharge for Partially Penetrating Well, enter Radius of Well (r), Coefficient of Permeability (K), Aquifer Thickness (b), Initial Piezometric Surface (H), Depth of Water (hw), Correction Factor (G) & Discharge for Partially Penetrating Well (Qv) and hit the calculate button. Here is how the Radius of Influence given Discharge for Partially Penetrating Well calculation can be explained with given input values -> 3.905289 = (2.94*exp((2*pi*0.00105*15*(20-2.44)*0.83)/5.08)).

FAQ

What is Radius of Influence given Discharge for Partially Penetrating Well?
Radius of Influence given Discharge for Partially Penetrating Well formula is defined as the maximum radial distance from the well at which the influence of the well's discharge is felt, and is a critical parameter in evaluating the impact of pumping on groundwater flow in partially penetrating wells and is represented as R = (r*exp((2*pi*K*b*(H-hw)*G)/Qv)) or Radius of Influence = (Radius of Well*exp((2*pi*Coefficient of Permeability*Aquifer Thickness*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/Discharge for Partially Penetrating Well)). The radius of well refers to the horizontal distance from the center of the well to its inner wall, essentially the well’s radius, Coefficient of Permeability refers to the ease with which water can flow through the aquifer's pore spaces, Aquifer Thickness (at Midpoint between Equipotential lines) or otherwise is the thickness of aquifer in which the pore spaces of rock forming the aquifer may or may not be with water, The initial piezometric surface refers to the level at which groundwater naturally stands in a confined aquifer before any pumping or external influence, Depth of Water is the depth in the well measured above the impermeable layer, Correction Factor refers to the reduced efficiency and altered flow patterns due to the well not extending through the entire aquifer thickness & Discharge for Partially Penetrating Well refers to the volume of water extracted from an aquifer when the well does not extend through the entire thickness of the aquifer.
How to calculate Radius of Influence given Discharge for Partially Penetrating Well?
Radius of Influence given Discharge for Partially Penetrating Well formula is defined as the maximum radial distance from the well at which the influence of the well's discharge is felt, and is a critical parameter in evaluating the impact of pumping on groundwater flow in partially penetrating wells is calculated using Radius of Influence = (Radius of Well*exp((2*pi*Coefficient of Permeability*Aquifer Thickness*(Initial Piezometric Surface-Depth of Water)*Correction Factor)/Discharge for Partially Penetrating Well)). To calculate Radius of Influence given Discharge for Partially Penetrating Well, you need Radius of Well (r), Coefficient of Permeability (K), Aquifer Thickness (b), Initial Piezometric Surface (H), Depth of Water (hw), Correction Factor (G) & Discharge for Partially Penetrating Well (Qv). With our tool, you need to enter the respective value for Radius of Well, Coefficient of Permeability, Aquifer Thickness, Initial Piezometric Surface, Depth of Water, Correction Factor & Discharge for Partially Penetrating Well and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
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