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Density and liquefaction During an earthquake, large bodies sink down due to the fact that due to vibration, small fractions of soil with low friction slip one below the other and become soil-like. Such soil is like suction sand. The global coefficient of voidness for sandy soil liquefaction is as follows: e = V empty / V sand Where '' V sand '' is the total volume of the sand particles and 'V V' is the total volume between the particles. dilution occurs during earthquakes when the coefficient f exceeds the critical value of 0.80 | available. What would be the '' P sand '' density? The density of silicon dioxide (the main ingredient in the sand) is 2,600x105 kg / m3.
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