Most soils have a water content less than porosity, which is the definition of unsaturated conditions, and they make up the subject of vadose zone hydrogeology.
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Moniz said that on a trip to Hanford in January he had explored the problem and found that " the vadose zone is intellectually virgin territory ."
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Parts of the major caves emerged from the saturated phreatic zone into the vadose with temporary periods of repose during which additional solutional excavation occurred in the phreatic zone.
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"' SESOIL "'( SEasonal SOIL ) is a one-dimensional vertical transport screening-level model for the unsaturated ( vadose ) zone.
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The phreatic zone, below the phreatic surface where rock and soil is saturated with water, is the counterpart of the vadose zone, or unsaturated zone, above.
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In speleology, cave passages formed in the vadose zone tend to be canyon-like in shape, as the water dissolves bedrock on the floor of the passage.
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The codes generally use climate and soil data to arrive at a recharge estimate and use the Richards equation in some form to model groundwater flow in the vadose zone.
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Movement of water within the vadose zone is studied within soil physics and hydrology, particularly hydrogeology, and is of importance to agriculture, contaminant transport, and flood control.
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One of the main complications which arises in studying the vadose zone, is the fact that the unsaturated hydraulic conductivity is a function of the water content of the material.
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At any point above the water table, in the vadose zone, the effective stress is approximately equal to the total stress, as proven by Terzaghi's principle.
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