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Soil Consistency and Engineering Classification
                                                                  Soil Consistency and Engineering Classification  259

                  therefore is between 6 and 19 cm, depending on filling of the shrinkage cracks and
                  amount of lateral elastic compression of the soil.


                  12.8.9   Controlling Volume Change with a
                  Nonexpansive Clay (n.e.c.) Layer

                  One of the most significant discoveries for controlling expansive clay was by
                  Dr. R. K. Katti and his co-workers at the Indian Institute of Technology, Mumbai.
                  Katti’s group conducted extensive full-scale laboratory tests to confirm field
                  measurements, such as shown in Fig. 12.9, and found that expansion can be
                  controlled by a surficial layer of compacted non-expansive clay. A particularly
                  severe test for the design was the canal shown in Fig. 12.10. The most common
                  application of Katti’s method is to stabilize the upper meter (3 ft) of expansive
                  clay by mixing in hydrated lime, Ca(OH) 2 . If only the upper one-third, 30 cm
                  (1 ft), is stabilized, volume change will be (0.15 þ 0.08)   30 ¼ 7 cm (3 in.), a
                  reduction of about 60 percent. If the upper 60 cm (2 ft) is stabilized, the volume
                  change will be 0.08   30 ¼ 2.4 cm (1 in.), a reduction of over 85 percent.
                  Stabilization to the full depth has been shown to eliminate volume change
                  altogether. The next question is, why?

                  An answer may be in the curves in Fig. 12.8, as a loss of clay structure greatly
                  increases clay expandability. As a result of shrink-swell cycling and an increase in
                  horizontal stress, expansive clays are visibly sheared, mixed, and remolded, so by
                  destroying soil structure expansion probably begets more expansion. According to
                  this hypothesis, substituting a layer of nonexpansive clay for the upper highly
                  expansive layer may help to preserve the structure and integrity of the underlying
                  layer. It was found that using a sand layer or a foundation load instead of densely

                                                                                          Figure 12.10
                                                                                          The Malaprabha
                                                                                          Canal in India was
                                                                                          successfully built
                                                                                          on highly
                                                                                          expansive clay
                                                                                          using Katti’s
                                                                                          method, by
                                                                                          replacing the upper
                                                                                          1 m of soil with
                                                                                          compacted
                                                                                          nonexpansive clay
                                                                                          (n.e.c.) to
                                                                                          replicate the
                                                                                          conditions shown
                                                                                          in Fig. 12.9 for the
                                                                                          underlying soil.

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