The rate of which water goes into the soil is related to the soil's hydraulic conductivity.

Where hydraulic conductivity has the capability to be measured at any state.

The hydraulic conductivity can be found from an aquifer test.

The soil's hydraulic conductivity plays an important role in drainage design.

The hydraulic conductivity can vary for each side of the polygons.

Plants also increase soil or other root-bed medium hydraulic conductivity.

The hydraulic conductivity of aquifers is often anisotropic for the same reason.

There are also in-situ methods for measuring the hydraulic conductivity in the field.

It is related to the saturated hydraulic conductivity of the near-surface soil.

In general, the aquifer medium will determine hydraulic conductivity.

Possible causes of falling hydraulic conductivity include water stress and the freeze-thaw cycle.

It is a function of the soil suction head, porosity, hydraulic conductivity and time.

Saturated hydraulic conductivity, K, describes water movement through saturated media.

To calculate hydraulic conductivity, Darcy's law is used.

It is mainly used to provide estimates of the hydraulic conductivity of the soil near saturation.

There is a clear proportionality between pore throat radii and hydraulic conductivity.

There are two broad categories of determining hydraulic conductivity:

It is an indicator of other engineering properties such as compressibility, shear strength, and hydraulic conductivity.

It is necessary to have a higher porosity in the subsoil in order to improve the hydraulic conductivity.

Aquitards comprise layers of either clay or non-porous rock with low hydraulic conductivity.

Flow through porous media with multifractal hydraulic conductivity.

Transmissivity is directly proportional to horizontal hydraulic conductivity and thickness .

The apparent horizontal hydraulic conductivity of the aquifer is:

This has a significant effect on the overall hydraulic conductivities (water permeabilities) and molecular diffusion coefficients.

Hydraulic conductivity (K) is a property of soil that describes the ease with which water can move through pore spaces.