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The water content, w, is defined in geotechnical literature as the ratio of the mass of the pore water, mw, to the mass of the dry solid particles, ms, given as a percentage. The pore water is the bulk water in the voids between the solid particles. The oven-drying method (BSI, 1990a; ASTM, 1998) is the preferred method for laboratory determination of the water content, calculated as the ratio of the reduction in the total mass of the test specimen to its equilibrium oven-dried mass mD, given as a percentage:...

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