Transmissivity of an Unconfined Aquifer in Groundwater Hydrology Formulas

The Transmissivity of an Unconfined Aquifer refers to the ability of the aquifer to transmit groundwater throughout its entire saturated thickness. And is denoted by T. Transmissivity of an Unconfined Aquifer is usually measured using the Square Meter per Second for Kinematic Viscosity. Note that the value of Transmissivity of an Unconfined Aquifer is always negative.

Formulas to find Transmissivity of an Unconfined Aquifer in Groundwater Hydrology

fxTransmissivity when Discharge at Drawdown is ConsideredGo

Groundwater Hydrology formulas that make use of Transmissivity of an Unconfined Aquifer

fxDischarge when Drawdown at Pumping Well is ConsideredGo

fxDrawdown when Steady Flow of Unconfined AquiferGo

fxChange in Drawdown given DischargeGo

List of variables in Groundwater Hydrology formulas

fx Steady Flow of an Unconfined Aquifer Go

fx Radius at the Edge of Zone of Influence Go

fx Radius of the Pumping Well Go

fx Drawdown at the Pumping Well Go

FAQ

What is the Transmissivity of an Unconfined Aquifer?

The Transmissivity of an Unconfined Aquifer refers to the ability of the aquifer to transmit groundwater throughout its entire saturated thickness. Transmissivity of an Unconfined Aquifer is usually measured using the Square Meter per Second for Kinematic Viscosity. Note that the value of Transmissivity of an Unconfined Aquifer is always negative.

Can the Transmissivity of an Unconfined Aquifer be negative?

Yes, the Transmissivity of an Unconfined Aquifer, measured in Kinematic Viscosity can be negative.

What unit is used to measure Transmissivity of an Unconfined Aquifer?

Transmissivity of an Unconfined Aquifer 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 of an Unconfined Aquifer can be measured.

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