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Soil Water
                                                                                             Soil Water  203

                                                                                          Figure 10.5
                                                                                          The finer the
                                                                                          particles the larger
                                                                                          the surface area.


















                  Every surface has unsatisfied bonds that adsorb water and other molecules.
                  Colloidal suspensions are highly surface-active, which means that they are
                  sensitive to the presence of chemicals that can act as either dispersing agents or
                  flocculating agents.


                  10.7.2   Double-Layer Theory
                  The stability of suspensions remained somewhat of a mystery prior to the
                  development of double-layer theory, which was proposed in the nineteenth
                  century by von Helmholtz and later modified independently by Guoy and
                  Chapman. The theory is based on a supposition that a surface carries a negative
                  charge. This can be attributed to the large size and larger surface exposure of
                  oxygen ions in minerals, and to net charge deficiencies in expansive clay minerals
                  that are balanced with interlayer cations. In a suspension, negative surfaces
                  attract positive ions that are accompanied by hydration water as illustrated in
                  Fig. 10.3(d), so they do not approach closely enough to neutralize the surface
                  charge on the colloid. The combination of negative surface charge balanced by
                  cations that can approach but do not attach constitutes a diffuse double layer.This
                  concept is illustrated in Fig. 10.6.

                  There also are weak attractive forces between particles or molecules that are called
                  van der Waals attractions. These forces are relatively constant while the diffuse
                  double layer changes depending on the hydration, concentration, and electrical
                  charges of the cations. Therefore by juggling cations in the diffuse double layer a
                  colloid can be ‘‘stabilized,’’ that is, remain dispersed, or it can become flocculated.
                  Flocculation is the preferred attribute in soils used for engineering purposes,
                  although dispersion is utilized in particle size analysis.


                  A high salt concentration or more highly charged positive ions such as Ca 2þ
                  compress the double layer and cause flocculation, whereas lower charged and

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