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One way to calculate water content would be to take a sample of the matter in question, weigh it, evaporate off the water component, and then weigh it again. The difference in weight divided by the original weight would be the portion of it which was water, I believe.

As I understand, the method geotechnical engineers use involves a machine squeezing water out of a sample. I haven't the slightest clue how that method works, if I'm even correct on that bit. I do know that their measurements for water saturation are volumetric in nature. Degree of saturation is given:

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15y ago

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