Page 212 - Handbook of Thermal Analysis of Construction Materials
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Section 2.0 - Calcium Chloride                               195


                              a peak effect at about 13–14 hours. This peak occurs at lower temperatures
                              and is also sharper as the amount of added chloride is increased. At 20%
                              CaCl , a sharp peak occurs at about two hours.
                                  2
                                     By applying thermal analysis, XRD, and chemical methods, it has
                              been concluded that calcium chloride may exist in different states in the
                                                                          [5]
                              system tricalcium silicate-calcium chloride-water.  The chloride may be
                              in the free state, as a complex on the surface of the silicate during the
                              dormant period, as a chemisorbed layer on the hydrate surface, in the
                              interlayer spaces, and in the lattice of the hydrate. Figure 5 gives the
                              estimate of the states of chloride in the silicate hydrated for different
                                     [5]
                              periods.  The results show that the amount of free chloride drops to about
                              12% within 4 hours, becoming almost nil in about 7 days. At 4 hours, the
                              amount of chloride existing in the chemisorbed and/or interlayer positions
                              rises sharply and reaches about 75%. Very strongly held chloride that
                              cannot be leached, even with water, occurs to an extent of about 20% of the
                              initially added chloride. Since this will not be in a soluble state in water, it
                              would not be available for corrosion processes. The formation of com-
                              plexes may explain effects such as the acceleration of hydration, the
                              increase in surface area, morphological changes, and the inhibition of
                              formation of afwillite (a crystalline form of calcium silicate hydrate) in the
                              presence of calcium chloride.






























                              Figure 4. Influence of CaCl  on the heat evolution characteristics of hydrating C S.
                                                  2                                      3
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