Change in Recharge in Groundwater Hydrology Formulas

Change in Recharge is the rate at which water moves downward from surface water to groundwater. And is denoted by ΔR. Change in Recharge is usually measured using the Cubic Meter per Second for Volumetric Flow Rate. Note that the value of Change in Recharge is always negative.

Groundwater Hydrology formulas that make use of Change in Recharge

fxEquation for rate of natural discharge when cone of depression ceases to expandGo

FAQ

What is the Change in Recharge?

Change in Recharge is the rate at which water moves downward from surface water to groundwater. Change in Recharge is usually measured using the Cubic Meter per Second for Volumetric Flow Rate. Note that the value of Change in Recharge is always negative.

Can the Change in Recharge be negative?

Yes, the Change in Recharge, measured in Volumetric Flow Rate can be negative.

What unit is used to measure Change in Recharge?

Change in Recharge is usually measured using the Cubic Meter per Second[m³/s] for Volumetric Flow Rate. Cubic Meter per Day[m³/s], Cubic Meter per Hour[m³/s], Cubic Meter per Minute[m³/s] are the few other units in which Change in Recharge can be measured.

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