relative density 1.59 equal to
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The specific gravity, G, of a soil particle is defined as the ratio of its mass to the mass of an equal volume of water at 4°C. Many terrestrial soils have a specific gravity of 2.7; that is, the density of the individual particles is 2.7 g/cm3, or 2.7 times that of water (1 g/cm3).
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1000kg/m cube is the relative density of 1.59
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