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The chapter discusses the principles of Terzaghi's one-dimensional consolidation theory, focusing on the assumptions that the soil medium is saturated, isotropic, and homogeneous while following Darcy's law. It explains the concept of volume change in soil due to consolidation and outlines limitations of the one-dimensional model such as constant permeability and assumptions of three-dimensional flow. The chapter concludes with Terzaghi's solution indicating consolidation progress with time and depth, emphasizing the importance of average degree of consolidation in practical applications.
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Term: OneDimensional Consolidation
Definition: A theory describing how compressible soil deposits consolidate over time due to vertical loading and how this process is affected by pore water expulsion.
Term: Degree of Consolidation
Definition: The ratio of the volume of pore water expelled to the original volume of voids, indicating how much of the consolidation process has occurred at a certain time and depth.
Term: Terzaghi’s Consolidation Equation
Definition: An equation that provides the mathematical framework for predicting the consolidation behavior of saturated soils under applied stress over time.