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!

11 Other formulas that you can solve using the same Inputs

Time at which Steady-Shape Conditions Develop
time at which steady-shape conditions develop=(7200*Distance from Pumping Well to Observation Well^2*Storage Coefficient)/Transmissivity GO
Storage Coefficient when Time at which Steady-Shape Conditions Develop is Given
Storage Coefficient=Transmissivity*time at which steady-shape conditions develop/7200*Distance from Pumping Well to Observation Well^2 GO
Storage Coefficient from the Time-Drawdown Graphs
Storage Coefficient=(2.25*Transmissivity*Time at the Point of Intersection )/Distance from Pumping Well to Observation Well^2 GO
Equation for the Varying Dimensionless Group u in Theis Equation
Varying Dimensionless Group =(Distance from Pumping Well to Observation Well^2*Storage Coefficient)/4*Transmissivity*Time GO
Theis Equation to Determine Storage Coefficient
Storage Coefficient=(4*Transmissivity*Time*Varying Dimensionless Group )/Distance from Pumping Well to Observation Well^2 GO
Equation for Pumping Rate when Transmissivity derived from the Time-Drawdown Graphs is Given
Pumping Rate=(Transmissivity*4*pi*Drawdown Across One Log Cycle)/Pumping Rate GO
Quantity of Water when Transmissivity is Given
Quantity of water=Transmissivity*Large Width of Aquifer*Hydraulic Gradient GO
Theis Equation to Determine Transmissivity
Transmissivity=(Pumping Rate*Well Function of u)/4*pi*Storage Coefficient GO
Thickness of Aquifer when Transmissivity is Given
Aquifer Thickness at Midpoint =Transmissivity/Hydraulic Conductivity GO
Transmissivity Derived from the Time-Drawdown Graphs
Transmissivity=(2.3*Pumping Rate)/4*pi*Drawdown Across One Log Cycle GO
Equation for Drawdown Across One Log Cycle when Transmissivity is Given
Drawdown Across One Log Cycle=2.3*Pumping Rate/Transmissivity*4*pi GO

7 Other formulas that calculate the same Output

Storage Coefficient when Time at which Steady-Shape Conditions Develop is Given
Storage Coefficient=Transmissivity*time at which steady-shape conditions develop/7200*Distance from Pumping Well to Observation Well^2 GO
Storage Coefficient from Distance-Drawdown Graphs
Storage Coefficient=2.25*Transmissivity*Time at which the Drawdowns were Measured/Distance from Pumping Well to Point Intersection^2 GO
Storage Coefficient for Inconsistent Units from Distance-Drawdown Graphs
Storage Coefficient=Transmissivity*Time at which the Drawdowns were Measured/640*Distance from Pumping Well to Point Intersection^2 GO
Storage Coefficient from the Time-Drawdown Graphs
Storage Coefficient=(2.25*Transmissivity*Time at the Point of Intersection )/Distance from Pumping Well to Observation Well^2 GO
Modified Equation for Storage Coefficient from Time-Drawdown Graphs
Storage Coefficient=(Transmissivity*Time at the Point of Intersection )/640*Distance from Pumping Well to Observation Well^2 GO
Theis Equation to Determine Storage Coefficient
Storage Coefficient=(4*Transmissivity*Time*Varying Dimensionless Group )/Distance from Pumping Well to Observation Well^2 GO
Storage Coefficient when Distance from Pumping Well is Given
Storage Coefficient=2.25*Transmissivity*Time/Distance from Pumping Well to Point Intersection^2 GO

Storage Coefficient From Theis Equation of Transmissivity Formula

Storage Coefficient=(Pumping Rate*Well Function of u)/Transmissivity*4*pi
S=(Q*u)/T*4*pi
More formulas
Quantity of Water in Steady-State Unsaturated Flow in the Direction of Downward Movement GO
Quantity of Water in Steady-State Unsaturated Flow in the Direction of Upward Movement GO
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
Transmissivity When Discharge Quantity is Known GO
Natural Discharge when Discharge Exceeds Recharge GO
Natural Discharge When Recharge Exceeds Discharge GO
Equation for Recharge When Recharge Exceeds Discharge GO
Balance Equation When Reduction in Natural Discharge Equals the Rate of Withdrawal GO
Equation for Rate of Natural Discharge When the Cone of Depression Ceases to Expand GO
Reduced Ground-water When Discharge Exceeds Recharge GO
Equation for Recharge When Discharge Exceeds Recharge GO
Theis Equation to Determine Transmissivity GO
Theis Equation to Determine Storage Coefficient GO
Transmissivity When Storage Coefficient is Given from Theis Equation GO
Equation for Ground-water Storage When Recharge Exceeds Discharge GO
Equation for the Varying Dimensionless Group u in Theis Equation GO
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
Specific Capacity GO
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 the 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 Storage Coefficient From Theis Equation of Transmissivity?

Storage Coefficient From Theis Equation of Transmissivity calculator uses Storage Coefficient=(Pumping Rate*Well Function of u)/Transmissivity*4*pi to calculate the Storage Coefficient, Storage Coefficient From Theis Equation of transmissivity is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer. Storage Coefficient and is denoted by S symbol.

How to calculate Storage Coefficient From Theis Equation of Transmissivity using this online calculator? To use this online calculator for Storage Coefficient From Theis Equation of Transmissivity, enter Pumping Rate (Q), Well Function of u (u) and Transmissivity (T) and hit the calculate button. Here is how the Storage Coefficient From Theis Equation of Transmissivity calculation can be explained with given input values -> 0 = (2*(0))/0.00277777777777778*4*pi.

FAQ

What is Storage Coefficient From Theis Equation of Transmissivity?
Storage Coefficient From Theis Equation of transmissivity is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer and is represented as S=(Q*u)/T*4*pi or Storage Coefficient=(Pumping Rate*Well Function of u)/Transmissivity*4*pi. Pumping Rate is the actual volumetric pumping rate, Well Function of u is the data plot of drawdown versus time (or drawdown versus t/rz) is matched to the type curve of W(u) versus 1/u and Transmissivity is the rate at which groundwater flows horizontally through an aquifer.
How to calculate Storage Coefficient From Theis Equation of Transmissivity?
Storage Coefficient From Theis Equation of transmissivity is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer is calculated using Storage Coefficient=(Pumping Rate*Well Function of u)/Transmissivity*4*pi. To calculate Storage Coefficient From Theis Equation of Transmissivity, you need Pumping Rate (Q), Well Function of u (u) and Transmissivity (T). With our tool, you need to enter the respective value for Pumping Rate, Well Function of u and Transmissivity 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 Storage Coefficient?
In this formula, Storage Coefficient uses Pumping Rate, Well Function of u and Transmissivity. We can use 7 other way(s) to calculate the same, which is/are as follows -
  • Storage Coefficient=(4*Transmissivity*Time*Varying Dimensionless Group )/Distance from Pumping Well to Observation Well^2
  • Storage Coefficient=Transmissivity*time at which steady-shape conditions develop/7200*Distance from Pumping Well to Observation Well^2
  • Storage Coefficient=(2.25*Transmissivity*Time at the Point of Intersection )/Distance from Pumping Well to Observation Well^2
  • Storage Coefficient=(Transmissivity*Time at the Point of Intersection )/640*Distance from Pumping Well to Observation Well^2
  • Storage Coefficient=2.25*Transmissivity*Time at which the Drawdowns were Measured/Distance from Pumping Well to Point Intersection^2
  • Storage Coefficient=Transmissivity*Time at which the Drawdowns were Measured/640*Distance from Pumping Well to Point Intersection^2
  • Storage Coefficient=2.25*Transmissivity*Time/Distance from Pumping Well to Point Intersection^2
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