Transmissivity at Edge of Zone of Influence in Groundwater Hydrology Formulas

Transmissivity at Edge of Zone of Influence is the capacity of the aquifer to transmit water at the boundary of the area influenced by the pumping well. And is denoted by T_iz. Transmissivity at Edge of Zone of Influence is usually measured using the Square Meter per Second for Kinematic Viscosity. Note that the value of Transmissivity at Edge of Zone of Influence is always negative.

Formulas to find Transmissivity at Edge of Zone of Influence in Groundwater Hydrology

fxTransmissivity when Discharge at Edge of Zone of InfluenceGo

List of variables in Groundwater Hydrology formulas

fx Steady Flow in a Confined Aquifer Go

fx Radial Distance at Observation Well 2 Go

fx Radial Distance at Observation Well 1 Go

fx Possible Drawdown in Confined Aquifer Go

FAQ

What is the Transmissivity at Edge of Zone of Influence?

Transmissivity at Edge of Zone of Influence is the capacity of the aquifer to transmit water at the boundary of the area influenced by the pumping well. Transmissivity at Edge of Zone of Influence is usually measured using the Square Meter per Second for Kinematic Viscosity. Note that the value of Transmissivity at Edge of Zone of Influence is always negative.

Can the Transmissivity at Edge of Zone of Influence be negative?

Yes, the Transmissivity at Edge of Zone of Influence, measured in Kinematic Viscosity can be negative.

What unit is used to measure Transmissivity at Edge of Zone of Influence?

Transmissivity at Edge of Zone of Influence 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 at Edge of Zone of Influence can be measured.

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