Hydraulic Conductivity

Hydraulic conductivity, symbolically represented as, is a property of vascular plants, soil or rock, that describes the ease with which a fluid (usually water) can move through pore spaces or fractures. It depends on the intrinsic permeability of the material and on the degree of saturation, and on the density and viscosity of the fluid. Saturated hydraulic conductivity, Ksat, describes water movement through saturated media.

Read more about Hydraulic ConductivityMethods of Determination, Determination By Experimental Approach, Anisotropy, Relative Properties, Ranges of Values For Natural Materials

Other articles related to "hydraulic conductivity":

Hydraulic Conductivity - Ranges of Values For Natural Materials
... Table of saturated hydraulic conductivity (K) values found in nature. ...
Permeability (earth Sciences) - Description - Relation To Hydraulic Conductivity
... water through a porous media is called the hydraulic conductivity permeability is a portion of this, and is a property of the porous media only, not the fluid ... Given the value of hydraulic conductivity for a subsurface system, the permeability can be calculated as where is the permeability, m2 is the hydraulic conductivity, m/s is ...
Characterisation Of Pore Space In Soil - Pore Space Relations - Hydraulic Conductivity
... Hydraulic conductivity (K) is a property of soil that describes the ease with which water can move through pore spaces ... Saturated hydraulic conductivity, Ksat, describes water movement through saturated media ... Where hydraulic conductivity has the capability to be measured at any state ...