Two major factors influence the rate of water flow from the soil to the roots : the hydraulic conductivity of the soil and the magnitude of the pressure gradient through the soil.
32.
Among the natural controls on lavaka formation are the amount of seismic activity in the region, the topographic relief ( or slope ), and hydraulic conductivity of materials in the saprolite.
33.
The hydraulic conductivity of the underlying soils is about 2.6-4.5 * 10 ^-6 m / s with a mean bulk porosity of 0.34.
34.
The water content is very important in vadose zone hydrology, where the hydraulic conductivity is a strongly nonlinear function of water content; this complicates the solution of the unsaturated groundwater flow equation.
35.
Investigations to determine subsurface characteristics ( such as natural groundwater velocity during ambient conditions, hydraulic conductivity of the subsurface, and lithology of the subsurface ) are important in developing a successful biostimulation system.
36.
Probably because of the particular difficulty, cost of measurement, and availability of large databases, the most comprehensive research in developing PTFs has been for the estimation of water retention curve and hydraulic conductivity.
37.
If a rock unit of low porosity is highly fractured, it can also make a good aquifer ( via fissure flow ), provided the rock has a hydraulic conductivity sufficient to facilitate movement of water.
38.
The U . S . Department of Energy is funding another KGS project on the integrated use of surface and subsurface nuclear magnetic resonance ( NMR ) for measuring and mapping saturated hydraulic conductivity in three dimensions.
39.
Such geosynthetic aggregates replace conventional gravel while simultaneously increasing porosity, increasing hydraulic conductivity and eliminating the fine dust " fines " inherent to gravel aggregates which otherwise serve to clog and disrupt the operation of many drainage applications.
40.
In hydrology, the harmonic mean is similarly used to average hydraulic conductivity values for flow that is perpendicular to layers ( e . g ., geologic or soil )-flow parallel to layers uses the arithmetic mean.
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