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Liquifaction of soil by liju

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Sam Blackoutz
Sam Blackoutz
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‘Liquefaction is a phenomenon where in a mass of soil losses a large percentage of its shear resistance, when subjected to monotonic, cyclic, or shock loading, and flows in a manner resembling a liquid until the shear stresses acting on the mass are as low as the reducedshear resistance .’
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju
Liquifaction of soil by liju

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Liquifaction of soil by liju

  • 1.
  • 2.
  • 3. ‘Liquefaction is a phenomenon where in a mass of soil losses a large percentage of its shear resistance, when subjected to monotonic, cyclic, or shock loading, and flows in a manner resembling a liquid until the shear stresses acting on the mass are as low as the reducedshear resistance .’