Water Table Depth 2 in Groundwater Hydrology Formulas

The Water Table Depth 2 refers to the vertical distance from the ground surface down to the water table, which is the upper surface of the zone of saturation where the soil or rock is fully saturated. And is denoted by H₂. Water Table Depth 2 is usually measured using the Meter for Length. Note that the value of Water Table Depth 2 is always positive.

Groundwater Hydrology formulas that make use of Water Table Depth 2

fxEquilibrium Equation for Well in Unconfined AquiferGo

fxCoefficient of Permeability when Equilibrium Equation for Well in Unconfined AquiferGo

FAQ

What is the Water Table Depth 2?

The Water Table Depth 2 refers to the vertical distance from the ground surface down to the water table, which is the upper surface of the zone of saturation where the soil or rock is fully saturated. Water Table Depth 2 is usually measured using the Meter for Length. Note that the value of Water Table Depth 2 is always positive.

Can the Water Table Depth 2 be negative?

No, the Water Table Depth 2, measured in Length cannot be negative.

What unit is used to measure Water Table Depth 2?

Water Table Depth 2 is usually measured using the Meter[m] for Length. Millimeter[m], Kilometer[m], Decimeter[m] are the few other units in which Water Table Depth 2 can be measured.

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