Time at which Steady Shape Conditions Develop Solution

STEP 0: Pre-Calculation Summary
Formula Used
Time at Which Steady-shape Conditions Develop = (7200*Distance from Pumping Well^2*Storage Coefficient)/Transmissivity
tc = (7200*r^2*S)/τ
This formula uses 4 Variables
Variables Used
Time at Which Steady-shape Conditions Develop - (Measured in Second) - Time at which Steady-Shape Conditions develop at the Outermost Observation Well.
Distance from Pumping Well - (Measured in Meter) - Distance from Pumping Well to the point where drawdown occurs.
Storage Coefficient - Storage Coefficient is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer.
Transmissivity - (Measured in Square Meter per Second) - The Transmissivity refers to the measure of how much water can be transmitted horizontally through an aquifer is the product of the hydraulic conductivity of the aquifer and its saturated thickness.
STEP 1: Convert Input(s) to Base Unit
Distance from Pumping Well: 3 Meter --> 3 Meter No Conversion Required
Storage Coefficient: 85 --> No Conversion Required
Transmissivity: 1.4 Square Meter per Second --> 1.4 Square Meter per Second No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
tc = (7200*r^2*S)/τ --> (7200*3^2*85)/1.4
Evaluating ... ...
tc = 3934285.71428571
STEP 3: Convert Result to Output's Unit
3934285.71428571 Second -->65571.4285714286 Minute (Check conversion ​here)
FINAL ANSWER
65571.4285714286 65571.43 Minute <-- Time at Which Steady-shape Conditions Develop
(Calculation completed in 00.004 seconds)

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Coorg Institute of Technology (CIT), Coorg
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Time Drawdown Analysis Calculators

Time at which Steady Shape Conditions Develop
​ LaTeX ​ Go Time at Which Steady-shape Conditions Develop = (7200*Distance from Pumping Well^2*Storage Coefficient)/Transmissivity
Storage Coefficient given time at which Steady Shape conditions develops
​ LaTeX ​ Go Storage Coefficient = Transmissivity*Time at Which Steady-shape Conditions Develop/7200*Distance from Pumping Well^2
Transmissivity derived from time drawdown graphs
​ LaTeX ​ Go Transmissivity = (2.3*Pumping Rate)/(4*pi*Drawdown Across One Log Cycle)
Equation for pumping rate of transmissivity from time drawdown graphs
​ LaTeX ​ Go Pumping Rate = (Transmissivity*4*pi*Drawdown Across Log Cycle)/2.3

Time at which Steady Shape Conditions Develop Formula

​LaTeX ​Go
Time at Which Steady-shape Conditions Develop = (7200*Distance from Pumping Well^2*Storage Coefficient)/Transmissivity
tc = (7200*r^2*S)/τ

What is Transmissivity?

Transmissivity describes the ability of the aquifer to transmit groundwater throughout its entire saturated thickness. Transmissivity is measured as the rate at which groundwater can flow through an aquifer section of unit width under a unit hydraulic gradient.

How to Calculate Time at which Steady Shape Conditions Develop?

Time at which Steady Shape Conditions Develop calculator uses Time at Which Steady-shape Conditions Develop = (7200*Distance from Pumping Well^2*Storage Coefficient)/Transmissivity to calculate the Time at Which Steady-shape Conditions Develop, Time at which Steady Shape Conditions Develop at the outermost observation well for practical purposes. Time at Which Steady-shape Conditions Develop is denoted by tc symbol.

How to calculate Time at which Steady Shape Conditions Develop using this online calculator? To use this online calculator for Time at which Steady Shape Conditions Develop, enter Distance from Pumping Well (r), Storage Coefficient (S) & Transmissivity (τ) and hit the calculate button. Here is how the Time at which Steady Shape Conditions Develop calculation can be explained with given input values -> 1092.857 = (7200*3^2*85)/1.4.

FAQ

What is Time at which Steady Shape Conditions Develop?
Time at which Steady Shape Conditions Develop at the outermost observation well for practical purposes and is represented as tc = (7200*r^2*S)/τ or Time at Which Steady-shape Conditions Develop = (7200*Distance from Pumping Well^2*Storage Coefficient)/Transmissivity. Distance from Pumping Well to the point where drawdown occurs, Storage Coefficient is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer & The Transmissivity refers to the measure of how much water can be transmitted horizontally through an aquifer is the product of the hydraulic conductivity of the aquifer and its saturated thickness.
How to calculate Time at which Steady Shape Conditions Develop?
Time at which Steady Shape Conditions Develop at the outermost observation well for practical purposes is calculated using Time at Which Steady-shape Conditions Develop = (7200*Distance from Pumping Well^2*Storage Coefficient)/Transmissivity. To calculate Time at which Steady Shape Conditions Develop, you need Distance from Pumping Well (r), Storage Coefficient (S) & Transmissivity (τ). With our tool, you need to enter the respective value for Distance from Pumping Well, Storage Coefficient & Transmissivity 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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