Transmissivity given Storage Coefficient from Theis Equation Solution

STEP 0: Pre-Calculation Summary
Formula Used
Transmissivity = (Storage Coefficient (Theis Equation)*Distance from Pumping Well^2)/(4*Time*Varying Dimensionless Group)
T = (S*r^2)/(4*t*u)
This formula uses 5 Variables
Variables Used
Transmissivity - (Measured in Square Meter per Second) - Transmissivity is the rate at which groundwater flows horizontally through an aquifer or the degree to which a medium allows something, in particular electromagnetic radiation, to pass through it.
Storage Coefficient (Theis Equation) - Storage Coefficient (Theis Equation) is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer.
Distance from Pumping Well - (Measured in Meter) - Distance from Pumping Well to the point where drawdown occurs.
Time - (Measured in Second) - Time can be defined as the ongoing and continuous sequence of events that occur in succession, from the past through the present to the future.
Varying Dimensionless Group - Varying Dimensionless Group that varies with both the position of the observation well and the time.
STEP 1: Convert Input(s) to Base Unit
Storage Coefficient (Theis Equation): 0.101 --> No Conversion Required
Distance from Pumping Well: 3 Meter --> 3 Meter No Conversion Required
Time: 4 Second --> 4 Second No Conversion Required
Varying Dimensionless Group: 0.81 --> No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
T = (S*r^2)/(4*t*u) --> (0.101*3^2)/(4*4*0.81)
Evaluating ... ...
T = 0.0701388888888889
STEP 3: Convert Result to Output's Unit
0.0701388888888889 Square Meter per Second --> No Conversion Required
FINAL ANSWER
0.0701388888888889 0.070139 Square Meter per Second <-- Transmissivity
(Calculation completed in 00.004 seconds)

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4 Analysis of Aquifer-Test Data Calculators

Transmissivity given Storage Coefficient from Theis Equation
Go Transmissivity = (Storage Coefficient (Theis Equation)*Distance from Pumping Well^2)/(4*Time*Varying Dimensionless Group)
Theis equation to determine storage coefficient
Go Storage Coefficient (Theis Equation) = (4*Transmissivity*Time*Varying Dimensionless Group)/Distance from Pumping Well^2
Storage Coefficient from Theis Equation of Transmissivity
Go Storage Coefficient (Theis Equation) = (Pumping Rate*Well Function of u)/(Transmissivity*4*pi)
Theis equation to determine transmissivity
Go Transmissivity = (Pumping Rate*Well Function of u)/(4*pi*Storage Coefficient (Theis Equation))

Transmissivity given Storage Coefficient from Theis Equation Formula

Transmissivity = (Storage Coefficient (Theis Equation)*Distance from Pumping Well^2)/(4*Time*Varying Dimensionless Group)
T = (S*r^2)/(4*t*u)

What Theis equation?

The Theis equation describes radial confined groundwater flow in a uniformly thick horizontal, homogeneous, isotropic aquifer of infinite areal extent.

How to Calculate Transmissivity given Storage Coefficient from Theis Equation?

Transmissivity given Storage Coefficient from Theis Equation calculator uses Transmissivity = (Storage Coefficient (Theis Equation)*Distance from Pumping Well^2)/(4*Time*Varying Dimensionless Group) to calculate the Transmissivity, The Transmissivity given storage coefficient from Theis equation is the rate at which groundwater flows horizontally through an aquifer. Transmissivity is denoted by T symbol.

How to calculate Transmissivity given Storage Coefficient from Theis Equation using this online calculator? To use this online calculator for Transmissivity given Storage Coefficient from Theis Equation, enter Storage Coefficient (Theis Equation) (S), Distance from Pumping Well (r), Time (t) & Varying Dimensionless Group (u) and hit the calculate button. Here is how the Transmissivity given Storage Coefficient from Theis Equation calculation can be explained with given input values -> 0.070139 = (0.101*3^2)/(4*4*0.81).

FAQ

What is Transmissivity given Storage Coefficient from Theis Equation?
The Transmissivity given storage coefficient from Theis equation is the rate at which groundwater flows horizontally through an aquifer and is represented as T = (S*r^2)/(4*t*u) or Transmissivity = (Storage Coefficient (Theis Equation)*Distance from Pumping Well^2)/(4*Time*Varying Dimensionless Group). Storage Coefficient (Theis Equation) is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer, Distance from Pumping Well to the point where drawdown occurs, Time can be defined as the ongoing and continuous sequence of events that occur in succession, from the past through the present to the future & Varying Dimensionless Group that varies with both the position of the observation well and the time.
How to calculate Transmissivity given Storage Coefficient from Theis Equation?
The Transmissivity given storage coefficient from Theis equation is the rate at which groundwater flows horizontally through an aquifer is calculated using Transmissivity = (Storage Coefficient (Theis Equation)*Distance from Pumping Well^2)/(4*Time*Varying Dimensionless Group). To calculate Transmissivity given Storage Coefficient from Theis Equation, you need Storage Coefficient (Theis Equation) (S), Distance from Pumping Well (r), Time (t) & Varying Dimensionless Group (u). With our tool, you need to enter the respective value for Storage Coefficient (Theis Equation), Distance from Pumping Well, Time & Varying Dimensionless Group and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
How many ways are there to calculate Transmissivity?
In this formula, Transmissivity uses Storage Coefficient (Theis Equation), Distance from Pumping Well, Time & Varying Dimensionless Group. We can use 1 other way(s) to calculate the same, which is/are as follows -
  • Transmissivity = (Pumping Rate*Well Function of u)/(4*pi*Storage Coefficient (Theis Equation))
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