Equivalent Permeability in Groundwater Hydrology Formulas

The Equivalent Permeability is referred as when the flow is parallel to stratification. And is denoted by K_e. Equivalent Permeability is usually measured using the Centimeter per Second for Speed. Note that the value of Equivalent Permeability is always negative.

Formulas to find Equivalent Permeability in Groundwater Hydrology

fxEquivalent Permeability when Transmissivity of Aquifer is ConsideredGo

Groundwater Hydrology formulas that make use of Equivalent Permeability

fxTransmissivity of Aquifer when Equivalent Permeability is ConsideredGo

fxAquifer Thickness when Transmissivity of Aquifer is ConsideredGo

List of variables in Groundwater Hydrology formulas

fx Transmissivity Go

fx Aquifer Thickness Go

FAQ

What is the Equivalent Permeability?

The Equivalent Permeability is referred as when the flow is parallel to stratification. Equivalent Permeability is usually measured using the Centimeter per Second for Speed. Note that the value of Equivalent Permeability is always negative.

Can the Equivalent Permeability be negative?

Yes, the Equivalent Permeability, measured in Speed can be negative.

What unit is used to measure Equivalent Permeability?

Equivalent Permeability is usually measured using the Centimeter per Second[cm/s] for Speed. Meter per Second[cm/s], Meter per Minute[cm/s], Meter per Hour[cm/s] are the few other units in which Equivalent Permeability can be measured.

Let Others Know

✖

Facebook

Twitter

Copied!