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The chapter discusses effective stress under hydrodynamic conditions, focusing on the effects of pore water pressure changes within soil due to seepage. It highlights how hydraulic gradients influence effective stress differently during upward and downward flows, emphasizing conditions like quicksand. The implications of changes in total stress and pore water pressure on soil stability, particularly under different water table conditions, are examined.
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9.pdfClass Notes
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Term: Effective Stress
Definition: The concept that represents the stress carried by the soil skeleton, defined as total stress minus pore water pressure.
Term: Hydraulic Gradient
Definition: The change in pressure head per unit length along the flow path, which drives the movement of groundwater.
Term: Quicksand Condition
Definition: A state where upward flow reduces effective stress to zero, causing soil to behave like a liquid.