Saturated Thickness of the Aquifer in Groundwater Hydrology Formulas

The Saturated Thickness of the Aquifer refers to the vertical height of the aquifer in which the pore spaces are completely filled with water. And is denoted by H. Saturated Thickness of the Aquifer is usually measured using the Meter for Length. Note that the value of Saturated Thickness of the Aquifer is always negative.

Formulas to find Saturated Thickness of the Aquifer in Groundwater Hydrology

fxSaturated Thickness of Aquifer when Steady Flow of Unconfined Aquifer is ConsideredGo

Groundwater Hydrology formulas that make use of Saturated Thickness of the Aquifer

fxDischarge at Edge of Zone of InfluenceGo

fxDepth of Water in Pumping Well when Steady Flow in Unconfined Aquifer is ConsideredGo

fxDrawdown at Pumping WellGo

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 Coefficient of Permeability Go

fx Depth of Water in the Pumping Well Go

FAQ

What is the Saturated Thickness of the Aquifer?

The Saturated Thickness of the Aquifer refers to the vertical height of the aquifer in which the pore spaces are completely filled with water. Saturated Thickness of the Aquifer is usually measured using the Meter for Length. Note that the value of Saturated Thickness of the Aquifer is always negative.

Can the Saturated Thickness of the Aquifer be negative?

Yes, the Saturated Thickness of the Aquifer, measured in Length can be negative.

What unit is used to measure Saturated Thickness of the Aquifer?

Saturated Thickness of the Aquifer is usually measured using the Meter[m] for Length. Millimeter[m], Kilometer[m], Decimeter[m] are the few other units in which Saturated Thickness of the Aquifer can be measured.

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