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 you can solve using the same Inputs

Concentration of the reactant in second-order reaction (only one reactant)
Concentration of reactant (first)=1/(1/(Initial concentration of reactant (first))+Rate Constant*Time) GO
Concentration of the reactant in first-order reaction
Concentration of reactant (first)=e^(-Rate Constant*Time)*Initial concentration of reactant (first) GO
Concentration of the reactant in zero-order reaction
Concentration of reactant (first)=Initial concentration of reactant (first)-Rate Constant*Time GO
Growth of Current in LR Circuit
Growth of current in LR circuit=(e/Resistance)*(1-e^(-Time/(Inductance/Resistance))) GO
Electro Discharge Machining
Electro Discharge Machining=Voltage*(1-e^(-Time/(Resistance*Capacitance))) GO
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Rate of interest=(Simple Interest*100)/(Principal Investment Amount*Time) GO
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Principal Investment Amount=(Simple Interest*100)/(Rate of interest*Time) GO
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Simple Interest=(Principal Investment Amount*Rate of interest*Time)/100 GO
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Current Value for Alternating Current
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Resistance Welding
Resistance Welding=Current Magnitude^2*Resistance*Time 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
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
Storage Coefficient=(Pumping Rate*Well Function of u)/Transmissivity*4*pi GO

Theis Equation to Determine Storage Coefficient Formula

Storage Coefficient=(4*Transmissivity*Time*Varying Dimensionless Group )/Distance from Pumping Well to Observation Well^2
S=(4*T*T*u)/r^2
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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
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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
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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 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.

How to Calculate Theis Equation to Determine Storage Coefficient?

Theis Equation to Determine Storage Coefficient calculator uses Storage Coefficient=(4*Transmissivity*Time*Varying Dimensionless Group )/Distance from Pumping Well to Observation Well^2 to calculate the Storage Coefficient, Theis Equation to Determine Storage Coefficient is the equation in transient groundwater hydraulics and the solution in terms of drawdown. Storage Coefficient and is denoted by S symbol.

How to calculate Theis Equation to Determine Storage Coefficient using this online calculator? To use this online calculator for Theis Equation to Determine Storage Coefficient, enter Transmissivity (T), Time (T), Varying Dimensionless Group (u) and Distance from Pumping Well to Observation Well (r) and hit the calculate button. Here is how the Theis Equation to Determine Storage Coefficient calculation can be explained with given input values -> 175316.4 = (4*0.00277777777777778*63113904*1)/2^2.

FAQ

What is Theis Equation to Determine Storage Coefficient?
Theis Equation to Determine Storage Coefficient is the equation in transient groundwater hydraulics and the solution in terms of drawdown and is represented as S=(4*T*T*u)/r^2 or Storage Coefficient=(4*Transmissivity*Time*Varying Dimensionless Group )/Distance from Pumping Well to Observation Well^2. Transmissivity is the rate at which groundwater flows horizontally through an aquifer, Time is used to calculate the amount that has a simple interest, Varying Dimensionless Group that varies with both the position r of the observation well and the time t and Distance from Pumping Well to Observation Well.
How to calculate Theis Equation to Determine Storage Coefficient?
Theis Equation to Determine Storage Coefficient is the equation in transient groundwater hydraulics and the solution in terms of drawdown is calculated using Storage Coefficient=(4*Transmissivity*Time*Varying Dimensionless Group )/Distance from Pumping Well to Observation Well^2. To calculate Theis Equation to Determine Storage Coefficient, you need Transmissivity (T), Time (T), Varying Dimensionless Group (u) and Distance from Pumping Well to Observation Well (r). With our tool, you need to enter the respective value for Transmissivity, Time, Varying Dimensionless Group and Distance from Pumping Well to Observation Well 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 Transmissivity, Time, Varying Dimensionless Group and Distance from Pumping Well to Observation Well. We can use 7 other way(s) to calculate the same, which is/are as follows -
  • Storage Coefficient=(Pumping Rate*Well Function of u)/Transmissivity*4*pi
  • 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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