Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 500+ more calculators!
Chandana P Dev
NSS College of Engineering (NSSCE), Palakkad
Chandana P Dev has verified this Calculator and 500+ more calculators!

1 Other formulas that you can solve using the same Inputs

Quantity of Water when Transmissivity is Given
Quantity of water=Transmissivity*Large Width of Aquifer*Hydraulic Gradient GO

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 Distance from Pumping Well is Given
Transmissivity=Distance from Pumping Well to Point Intersection^2*Storage Coefficient/2.25*Time 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 Discharge Quantity is Known Formula

Transmissivity=(Quantity of water/Large Width of Aquifer)*(Distance Between the Points/Change in Head Between the Points)
T=(Q/W)*(dl/dh)
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Flow Through any Square from Darcy's law for Ground Water Flow Nets GO
Total Flow through any Set or Group of Equipotential Lines GO
Number of Squares Through Which the Flow occurs when Total Flow is given GO
Flow Through any Square when Total Flow is Given GO
Velocity Equation of Hydraulics GO
The Rate of Movement Through an Aquifer and a Confining Bed GO
Transmissivity of Aquifer GO
Thickness of Aquifer when Transmissivity is Given GO
Quantity of Water when Transmissivity is Given GO
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Natural Discharge When Recharge Exceeds Discharge GO
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Balance Equation When Reduction in Natural Discharge Equals the Rate of Withdrawal GO
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Equation for Recharge When Discharge Exceeds Recharge GO
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Theis Equation to Determine Storage Coefficient GO
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Transmissivity When Storage Coefficient is Given from Theis Equation GO
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Observed Drawdown in the Unconfined Aquifer GO
Time at which Steady-Shape Conditions Develop GO
Transmissivity when Time at which Steady-Shape Conditions Develop is Given GO
Storage Coefficient when Time at which Steady-Shape Conditions Develop is Given GO
Transmissivity Derived from the Time-Drawdown Graphs GO
Storage Coefficient from the Time-Drawdown Graphs GO
Equation for Pumping Rate when Transmissivity derived from the Time-Drawdown Graphs is Given GO
Equation for Drawdown Across One Log Cycle when Transmissivity is Given GO
Distance from the Pumping Well to the Observation Well when Storage Coefficient is Given GO
Modified Equation for Transmissivity from Time-Drawdown Graphs GO
Modified Equation for Storage Coefficient from Time-Drawdown Graphs GO
Transmissivity from Distance-Drawdown Graphs GO
Storage Coefficient from Distance-Drawdown Graphs GO
Pumping Rate from Distance-Drawdown Graphs when Transmissivity is Given GO
Drawdown across One Log Cycle from Distance-Drawdown Graphs when Transmissivity is Given GO
Transmissivity when Storage Coefficient from Distance-Drawdown Graphs is Given GO
Time at which the Drawdowns were Measured when Storage Coefficient is Given GO
Transmissivity for Inconsistent Units from Distance-Drawdown Graphs GO
Storage Coefficient for Inconsistent Units from Distance-Drawdown Graphs GO
Pumping Rate when Transmissivity is Given for Inconsistent Units from Distance-Drawdown Graphs GO
Drawdown across One Log Cycle when Transmissivity is Given for Inconsistent Units GO
Total Drawdown in a Pumping Well GO
Total Drawdown in a Pumping Well expressed in terms of Factors related to Hydraulic Characteristics GO
Drawdown in the Aquifer when Total Drawdown is Given GO
Well Loss when Total Drawdown is Given GO
Drawdown in an Aquifer caused by Pumping at any Point in the Aquifer GO
Distance from the Observation Well to the Image Well GO
Distance from the Observation Well to the Real Well GO
Time at which Drawdown is caused by Real Well at the Observation Well GO
Time at which Drawdown is Caused by Image Well at Observation Well GO
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Pumping Rate when Specific Capacity is Given GO
Drawdown when Specific Capacity is Given GO
Well Efficiency GO
Drawdown in the Aquifer when Well Efficiency is Given GO
Drawdown Inside the Well when Well Efficiency is Given GO
Distance from Pumping Well GO
Storage Coefficient when Distance from Pumping Well is Given GO
Transmissivity 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
Ghyben-Herzberg Relationship for Depth of Freshwater Below Sea Level GO
Height of the Water Table above Sea Level GO

What is Transmissivity?

The Capacity of an aquifer to transmit water of the prevailing Kinematic Viscosity is referred to as its Transmissivity. The Transmissivity (T) of an aquifer is equal to the hydraulic conductivity of the aquifer multiplied by the saturated thickness of the aquifer.

How to Calculate Transmissivity When Discharge Quantity is Known?

Transmissivity When Discharge Quantity is Known calculator uses Transmissivity=(Quantity of water/Large Width of Aquifer)*(Distance Between the Points/Change in Head Between the Points) to calculate the Transmissivity, Transmissivity When Discharge Quantity is Known is defined as the capacity of an aquifer to transmit water of the prevailing kinematic viscosity. Transmissivity and is denoted by T symbol.

How to calculate Transmissivity When Discharge Quantity is Known using this online calculator? To use this online calculator for Transmissivity When Discharge Quantity is Known, enter Quantity of water (Q), Large Width of Aquifer (W), Distance Between the Points (dl) and Change in Head Between the Points (dh) and hit the calculate button. Here is how the Transmissivity When Discharge Quantity is Known calculation can be explained with given input values -> 7.5 = (0.00833333333333333/40)*(10/1).

FAQ

What is Transmissivity When Discharge Quantity is Known?
Transmissivity When Discharge Quantity is Known is defined as the capacity of an aquifer to transmit water of the prevailing kinematic viscosity and is represented as T=(Q/W)*(dl/dh) or Transmissivity=(Quantity of water/Large Width of Aquifer)*(Distance Between the Points/Change in Head Between the Points). The quantity of water required to extinguish the fire, Large Width of Aquifer to determine Quantity of Water, Distance Between the Points Contributing to the change in Head and Change in Head Between the Points separated by Small distance dl.
How to calculate Transmissivity When Discharge Quantity is Known?
Transmissivity When Discharge Quantity is Known is defined as the capacity of an aquifer to transmit water of the prevailing kinematic viscosity is calculated using Transmissivity=(Quantity of water/Large Width of Aquifer)*(Distance Between the Points/Change in Head Between the Points). To calculate Transmissivity When Discharge Quantity is Known, you need Quantity of water (Q), Large Width of Aquifer (W), Distance Between the Points (dl) and Change in Head Between the Points (dh). With our tool, you need to enter the respective value for Quantity of water, Large Width of Aquifer, Distance Between the Points and Change in Head Between the Points 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 Quantity of water, Large Width of Aquifer, Distance Between the Points and Change in Head Between the Points. We can use 11 other way(s) to calculate the same, which is/are as follows -
  • Transmissivity=Hydraulic Conductivity*Aquifer Thickness at Midpoint
  • 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=Distance from Pumping Well to Point Intersection^2*Storage Coefficient/2.25*Time
  • Transmissivity=First Estimate of the Pumping Rate/2.7*Drawdown Across One Log Cycle
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