Darcy's law
Darcy's Law is a phenomologically derived constituative equation that describes the flow of a fluid through a porous medium (typically water through an aquifer). The law was formulated by Henry Darcy based on the results of 1855 and 1856 experiments on the flow of water through beds of sand. It, along with the conservation of mass, comprises the groundwater flow equation, which is one the basic building relationships of hydrogeology.
See also
~ Table of Content ~
| ► | Introduction |
| ► | Additional forms of Darcy's Law |
| ► | See also |
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