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Soil Consistency and Engineering Classification
                254   Geotechnical Engineering

                 Figure 12.5
                 Linear relations
                 between PI and
                 percent clay.
                 Ratios were
                 defined by
                 Skempton (1953)
                 as activity indices,
                 which are shown
                 in parentheses.
                 The Shellhaven
                 soil clay probably
                 is smectite.


















                                       þ
                 Table 12.1         Na smectite (montmorillonite)               3–7
                 Activity indices of  Ca 2þ  smectite (montmorillonite)         1.2–1.3
                 selected clay                 Illite                           0.3–0.6
                 minerals (after Grim,  Kaolinite, poorly crystallized          0.3–0.4
                 1968)                Kaolinite, well crystallized              50.1


                                    is applied to the data in Fig. 12.6 with k ¼ 10, then A ¼ 1.23   0.04 where
                                    the   value is the standard error for a number of determinations n ¼ 81.
                                    This identifies the clay mineral as calcium smectite, which is confirmed by X-ray
                                    diffraction.


                12.7 LIQUID LIMIT AND COLLAPSIBILITY


                                    12.7.1   Concept

                                    A simple but effective idea was proposed in 1953 by a Russian geotechnical
                                    engineer, A. Y. Denisov, and later introduced into the U.S. by Gibbs and Bara of

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