Page 14 - Geotechnical Engineering Soil and Foundation Principles and Practice
P. 14

Introduction
                                                                                              Introduction  9

                  Also in 1856, two other concepts were introduced that play an important role in
                  soil engineering. These are Darcy’s Law defining gravitational flow of water
                  through porous media such as soils, and Stokes’ Law describing the equilibrium
                  velocity of solid particles settling in liquids. Stokes’ Law is used for measurement
                  of fine soil particle sizes from their settlement rates.

                  Another important contribution in the field of soil pressures is that of
                  Sir Benjamin Baker in 1881. Baker observed that the slip surface for a bank
                  failure is not planar as indicated by the Rankine and Coulomb analyses, but
                  incorporates vertically oriented cracks at the upper end. Decades earlier, in 1846,
                  the internal structure of landslides was investigated in the field by Alexandre
                  Collin, whose detailed cross-sections showed a curved instead of a flat slip
                  surface. Collin’s work unfortunately escaped the attention or was ignored by later
                  workers, who perhaps were more taken with the classical theory, and was
                  rediscovered only in recent years.

                  In 1871, Otto Mohr devised a simple graphical means for presentation and
                  analysis of stress data, and ‘‘Mohr’s circle’’ has become an invaluable tool for
                  the modern geotechnical engineer. Mohr later confirmed and generalized the
                  Coulomb failure criterion by relating to experimental findings, and Coulomb’s
                  earlier description of components of shearing strength sometimes is referred to as
                  the ‘‘Mohr-Coulomb failure envelope.’’

                  Another nineteenth-century contribution that was destined to become extremely
                  useful in modern soil engineering was the solution by a mathematician,
                  Boussinesq (pronounced Boo-sin-esk). By use of elastic analysis, in 1885 he
                  showed that stresses from a point load on the surface of soil should dissipate in
                  three-dimensional space much like ripples from a stone thrown in water. Although
                  soil is far from being an ideal elastic material, pressure measurements indicate that
                  the Boussinesq solution is appropriate for determining pressures from founda-
                  tions and for computing lateral pressures on retaining walls from loads applied at
                  the surface of the soil backfill.


                  1.11 SOIL MOISTURE STUDIES



                  Early in the twentieth century soil scientists employed by the U.S. Depart-
                  ment of Agriculture were active in the study of the mechanics of soil moisture.
                  Among these was Briggs, who suggested a classification of soil moisture.
                  Concurrently Buckingham proposed the concept of capillary potential and
                  conductivity, which has led to a better understanding of the forces responsible for
                  the retention and movement of capillary water in soils. Haines and Fisher
                  developed an important concept of soil cohesion resulting from capillary forces
                  or suction of water in soils that tends to pull soil grains together and increase
                  friction.

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