Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 300+ more calculators!
Chandana P Dev
NSS College of Engineering (NSSCE), Palakkad
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11 Other formulas that calculate the same Output

Transmissivity when Storage Coefficient from Distance-Drawdown Graphs is Given
Transmissivity=(Storage Coefficient*Distance from Pumping Well to Point Intersection^2)/(2.25*Time at which the Drawdowns were Measured) GO
Transmissivity when Time at which Steady-Shape Conditions Develop is Given
Transmissivity=7200*Distance from Pumping Well to Observation Well^2*Storage Coefficient/time at which steady-shape conditions develop GO
Transmissivity When Storage Coefficient is Given from Theis Equation
Transmissivity=(Storage Coefficient*Distance from Pumping Well to Observation Well^2)/(4*Time*Varying Dimensionless Group ) GO
Transmissivity When Discharge Quantity is Known
Transmissivity=(Quantity of water/Large Width of Aquifer)*(Distance Between the Points/Change in Head Between the Points) GO
Transmissivity when First Estimate of the Pumping Rate is Given
Transmissivity=First Estimate of the Pumping Rate/2.7*Drawdown Across One Log Cycle GO
Theis Equation to Determine Transmissivity
Transmissivity=(Pumping Rate*Well Function of u)/4*pi*Storage Coefficient GO
Transmissivity of Aquifer
Transmissivity=Hydraulic Conductivity*Aquifer Thickness at Midpoint GO
Transmissivity Derived from the Time-Drawdown Graphs
Transmissivity=(2.3*Pumping Rate)/4*pi*Drawdown Across One Log Cycle GO
Transmissivity from Distance-Drawdown Graphs
Transmissivity=2.3*Pumping Rate/2*pi*Drawdown Across One Log Cycle GO
Transmissivity for Inconsistent Units from Distance-Drawdown Graphs
Transmissivity=70*Pumping Rate/Drawdown Across One Log Cycle GO
Modified Equation for Transmissivity from Time-Drawdown Graphs
Transmissivity=35*Pumping Rate/Drawdown Across One Log Cycle GO

Transmissivity when Distance from Pumping Well is Given Formula

Transmissivity=Distance from Pumping Well to Point Intersection^2*Storage Coefficient/2.25*Time
T=r<sub>o</sub>^2*S/2.25*T
More formulas
Distance from Pumping Well GO
Storage Coefficient when Distance from Pumping Well is Given GO
First Estimate of the Pumping Rate GO
Transmissivity when First Estimate of the Pumping Rate is Given GO
Drawdown across One Log Cycle when First Estimate of the Pumping Rate is Given GO

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 Transmissivity when Distance from Pumping Well is Given?

Transmissivity when Distance from Pumping Well is Given calculator uses Transmissivity=Distance from Pumping Well to Point Intersection^2*Storage Coefficient/2.25*Time to calculate the Transmissivity, The Transmissivity when Distance from Pumping Well is Given is the rate at which groundwater flows horizontally through an aquifer. Transmissivity and is denoted by T symbol.

How to calculate Transmissivity when Distance from Pumping Well is Given using this online calculator? To use this online calculator for Transmissivity when Distance from Pumping Well is Given, enter Distance from Pumping Well to Point Intersection (ro), Storage Coefficient (S) and Time (T) and hit the calculate button. Here is how the Transmissivity when Distance from Pumping Well is Given calculation can be explained with given input values -> 2.525E+14 = 50^2*1/2.25*63113904.

FAQ

What is Transmissivity when Distance from Pumping Well is Given?
The Transmissivity when Distance from Pumping Well is Given is the rate at which groundwater flows horizontally through an aquifer and is represented as T=ro^2*S/2.25*T or Transmissivity=Distance from Pumping Well to Point Intersection^2*Storage Coefficient/2.25*Time. Distance from Pumping Well to Point Intersection where the Straight Line Intersects the Zero-drawdown line, 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 and Time is used to calculate the amount that has a simple interest.
How to calculate Transmissivity when Distance from Pumping Well is Given?
The Transmissivity when Distance from Pumping Well is Given is the rate at which groundwater flows horizontally through an aquifer is calculated using Transmissivity=Distance from Pumping Well to Point Intersection^2*Storage Coefficient/2.25*Time. To calculate Transmissivity when Distance from Pumping Well is Given, you need Distance from Pumping Well to Point Intersection (ro), Storage Coefficient (S) and Time (T). With our tool, you need to enter the respective value for Distance from Pumping Well to Point Intersection, Storage Coefficient and Time 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 Distance from Pumping Well to Point Intersection, Storage Coefficient and Time. We can use 11 other way(s) to calculate the same, which is/are as follows -
  • Transmissivity=Hydraulic Conductivity*Aquifer Thickness at Midpoint
  • Transmissivity=(Quantity of water/Large Width of Aquifer)*(Distance Between the Points/Change in Head Between the Points)
  • Transmissivity=(Pumping Rate*Well Function of u)/4*pi*Storage Coefficient
  • Transmissivity=(Storage Coefficient*Distance from Pumping Well to Observation Well^2)/(4*Time*Varying Dimensionless Group )
  • Transmissivity=7200*Distance from Pumping Well to Observation Well^2*Storage Coefficient/time at which steady-shape conditions develop
  • Transmissivity=(2.3*Pumping Rate)/4*pi*Drawdown Across One Log Cycle
  • Transmissivity=35*Pumping Rate/Drawdown Across One Log Cycle
  • Transmissivity=2.3*Pumping Rate/2*pi*Drawdown Across One Log Cycle
  • Transmissivity=(Storage Coefficient*Distance from Pumping Well to Point Intersection^2)/(2.25*Time at which the Drawdowns were Measured)
  • Transmissivity=70*Pumping Rate/Drawdown Across One Log Cycle
  • Transmissivity=First Estimate of the Pumping Rate/2.7*Drawdown Across One Log Cycle
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