Wlodzimierz Derski, Ryszard Izbicki, Igor Kisiel, Zenon Mroz ... 738 pages - Publisher: Elsevier Science; (January, 1989) ... Language: English - ISBN-10: 0444564381 - ISBN-13: 978-0444564382.
Although theoretical in character, this book provides a useful source of
information for those dealing with practical problems relating to rock
and soil mechanics - a discipline which, in the view of the authors,
attempts to apply the theory of continuum to the mechanical
investigation of rock and soil media. The book is in two separate parts.
The first part, embodying the first three chapters, is devoted to a
description of the media of interest. Chapter 1 introduces the main
argument and discusses the essence of the discipline and its links with
other branches of science which are concerned, on the one hand, with
technical mechanics and, on the other, with the properties, origins, and
formation of rock and soil strata under natural field conditions.
Chapter 2 describes mechanical models of bodies useful for the purpose
of the discourse and defines the concept of the limit shear resistance
of soils and rocks. Chapter 3 gives the actual properties of soils and
rocks determined from experiments in laboratories and in situ. Several
tests used in geotechnical engineering are described and
interconnections between the physical state of rocks and soils and their
rheological parameters are considered. The second part of the book
considers the applications of various theories which were either first
developed for descriptive purposes in continuum mechanics and then
adopted in soil and rock mechanics, or were specially developed for the
latter discipline. Chapter 4 discusses the application of the theory of
linear viscoelasticity in solving problems of stable behaviour of rocks
and soils. Chapter 5 covers the use of the groundwater flow theory as
applied to several problems connected with water movement in an
undeformable soil or rock skeleton. Chapter 6 is a natural expansion of
the arguments put forward in the previous chapter. Here the movement of
water is regarded as the cause of deformation of the rock or soil skeleton.