- Groundwater discharge
Groundwater discharge is the
volumetric flow rate ofgroundwater through anaquifer .Groundwater discharge, "Q"
Total groundwater discharge, as reported through a specified area, is similarly expressed as::Q = frac{dh}{dl}KAwhere:"Q" is the total groundwater discharge ( [L³T−1] ; m³/s), and:"A" is the area which the groundwater is flowing through ( [L²] ; m²)
For example, this can be used to determine the flow rate of water flowing along a plane with known geometry.
Conservation principle
The conservation principle shows that the mass or volume water flowing into a system is equal to that flowing out, with storage holding or releasing water in the system. Mathematically, this simple concept can be expressed as::Q_{mathrm{in-Q_{mathrm{out=frac{Delta S}{Delta t}where:Q_{mathrm{in and Q_{mathrm{out are the
volumetric flow rate s in and out the system (such as wells, rivers, etc.),:Delta S is the change of water volume that enters/leaves the system, and:Delta t is the change oftime If the system issteady state , then the right-hand side of the equation is 0.ee also
*
Groundwater flow equation
*Groundwater energy balance
*Submarine groundwater discharge
*Discharge (hydrology) – forriver s
*volumetric flow rate
*flux (transport definition)
*Darcy's Law References
* Freeze, R.A. & Cherry, J.A., 1979. "Groundwater", Prentice-Hall. ISBN 0-13-365312-9
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