The book is a detailed course on a new paradigm in soil mechanics, one solidly based on science (thermodynamics) and findings by Casagrande's group at Harvard University. The theory holds that soils when sheared reach a "steady-state" condition, a finding that is exactly in line with the thermodynamics of dissipative systems. From this, the theory is extended to show that soil deformation is the result of a simple friction based Poisson process in which particles move to their final position at random shear strains. The book introduces the reader to this concept, and unpacks it. It aims at both advanced undergraduates, as well as graduate and research students.
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