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Water content : ウィキペディア英語版
Water content

Water content or moisture content is the quantity of water contained in a material, such as soil (called soil moisture), rock, ceramics, fruit, or wood. Water content is used in a wide range of scientific and technical areas, and is expressed as a ratio, which can range from 0 (completely dry) to the value of the materials' porosity at saturation. It can be given on a volumetric or mass (gravimetric) basis.
==Definitions==

Volumetric water content, θ, is defined mathematically as:
:\theta = \frac = V_h + V_w + V_a is the volume of wet material, that is, host material (e.g., soil particles, vegetation tissue) volume + water volume + air space.
Gravimetric water content is expressed by mass (weight) as follows:
:u = \frac
where m_w is the mass of water and m is the mass of the substance. Normally the latter is taken before drying:
:u' = \frac{m_\text{dry}}
To convert gravimetric water content to volumetric water content, multiply the gravimetric water content by the bulk specific gravity of the material.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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