Transmissivity in Aquifer Analysis and Properties Formulas

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. And is denoted by T. Transmissivity is usually measured using the Square Meter per Second for Kinematic Viscosity. Note that the value of Transmissivity is always negative.

Formulas to find Transmissivity in Aquifer Analysis and Properties

fxTheis equation to determine transmissivityGo

fxTransmissivity given Storage Coefficient from Theis EquationGo

Aquifer Analysis and Properties formulas that make use of Transmissivity

fxTheis Equation to determine Storage CoefficientGo

fxStorage Coefficient from Theis Equation of TransmissivityGo

List of variables in Aquifer Analysis and Properties formulas

fx Pumping Rate Go

fx Well Function of U Go

fx Storage Coefficient (Theis Equation) Go

fx Storage Coefficient Go

fx Distance from Pumping Well Go

fx Pumping Time Go

fx Varying Dimensionless Group Go

FAQ

What is the Transmissivity?

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. Transmissivity is usually measured using the Square Meter per Second for Kinematic Viscosity. Note that the value of Transmissivity is always negative.

Can the Transmissivity be negative?

Yes, the Transmissivity, measured in Kinematic Viscosity can be negative.

What unit is used to measure Transmissivity?

Transmissivity is usually measured using the Square Meter per Second[m²/s] for Kinematic Viscosity. Square Meter per Hour[m²/s], Square Centimeter per Second[m²/s], Square Millimeter per Second[m²/s] are the few other units in which Transmissivity can be measured.

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