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Natural Recharge in Groundwater Hydrology Formulas

The Natural Recharge is a process by which groundwater is replenished naturally when precipitation infiltrates the ground, moving through the soil and rock layers until it reaches the water table. And is denoted by R. Natural Recharge is usually measured using the Cubic Meter per Second for Volumetric Flow Rate. Note that the value of Natural Recharge is always negative.

Formulas to find Natural Recharge in Groundwater Hydrology

fxEquation for recharge when recharge exceeds discharge​Go
fxBalance equation when reduction in natural discharge equal rate of withdrawal​Go
fxEquation for recharge when discharge exceeds recharge​Go
fxRecharge when Maximum Height of Water Table​Go
fxNatural Recharge given Total Head​Go

Groundwater Hydrology formulas that make use of Natural Recharge

fxNatural discharge when discharge exceeds recharge​Go
fxNatural discharge when recharge exceeds discharge​Go
fxEquation for rate of natural discharge when cone of depression ceases to expand​Go
fxEquation for ground water storage when recharge exceeds discharge​Go
fxWater Table Profile Neglecting Depths of Water in Drains​Go
fxMaximum Height of Water Table​Go
fxLength when Discharge entering per Unit Length of Drain is Considered​Go
fxLength when Maximum Height of Water Table is Considered​Go
fxEquation of Head for Unconfined Aquifer on Horizontal Impervious Base​Go
fxEquation for Water Divide​Go
fxDischarge per Unit Width of Aquifer at any Location x​Go
fxDischarge at Downstream Water Body of Catchment​Go
fxDischarge Entering Drain per Unit Length of Drain​Go
fxCoefficient of Aquifer Permeability given Maximum Height of Water Table​Go
fxCoefficient of Aquifer Permeability given Water Table Profile​Go

List of variables in Groundwater Hydrology formulas

fx Natural Discharge ​Go
fx Change in Groundwater Storage ​Go
fx Reduction in Natural Discharge ​Go
fx Rate of Withdrawal ​Go
fx Maximum Height of Water Table ​Go
fx Length between Tile Drain ​Go
fx Coefficient of Permeability ​Go
fx Water Table Profile ​Go
fx Flow in 'x' Direction ​Go

FAQ

What is the Natural Recharge?
The Natural Recharge is a process by which groundwater is replenished naturally when precipitation infiltrates the ground, moving through the soil and rock layers until it reaches the water table. Natural Recharge is usually measured using the Cubic Meter per Second for Volumetric Flow Rate. Note that the value of Natural Recharge is always negative.
Can the Natural Recharge be negative?
Yes, the Natural Recharge, measured in Volumetric Flow Rate can be negative.
What unit is used to measure Natural Recharge?
Natural 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 Natural Recharge can be measured.
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