Page 346 - Handbook of Thermal Analysis of Construction Materials
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Section 6.0 - Metakaolinite                                  323


                              6.0    METAKAOLINITE


                                     Soils and clays, in general, when calcined give off adsorbed,
                              interlayer, and hydrated types of water. These effects produce endothermal
                              peaks or loss of weight in DTA and TG, respectively. The endothermal
                              peaks are followed by exothermal peaks that are caused by re-crystalliza-
                              tion. Although many types of clay minerals such as montmorillonite, illite,
                              and some shales show these effects, they are not suitable as pozzolans in
                              concrete. Metakaolin, formed by heating kaolinite, seems to be the most
                              suitable additive material for cement. Heating of kaolinite involves removal
                              of adsorbed water at about 100°C and dehydroxylation at above 600°C,
                              followed by the formation of metakaolinite, an almost amorphous product.
                              The sequence of reactions is as follows: [60]


                                            Al Si O (OH)  (Kaolinite) at 600°C
                                              2
                                                 2
                                                         4
                                                   5
                                                   forms Al Si O  (Metakaolinite) + 2H O
                                                           2  2  7                   2
                              At higher temperatures, metakaolinite transforms to crystalline compounds
                              as follows:
                                     • Metakaolin at 925°C forms silicon spinel

                                     • Silicon spinel at 1100°C produces pseudo-mullite

                                     • Pseudo-mullite at 1440°C forms mullite + cristobalite
                                     Metakaolin (MK) is not cementitious by itself, but, having a high
                                                    2
                              surface area of about 20 m /g, it reacts with calcium, sodium and potassium
                              hydroxides, and gypsum/cement. The hydrated lime + MK reaction yields
                              gehelinite hydrate (C ASH ) and C-S-H. The C/S ratios of the calcium
                                                 2
                                                      8
                              silicate hydrate vary between 0.8 and 1.5. At higher hydration temperatures,
                              gehelinite is the stable phase. The hydration reaction at 50°C produces a
                              hydrogarnet phase of approximate composition C AS H . When MK is
                                                                         3   0.3  5.3
                              mixed with portland cement and hydrated, the lime formed as a hydration
                              product of cement is consumed by MK and the C-S-H product is formed. At
                              higher MK contents, gehlenite may form. The C/S ratio of the product may
                              vary between 1.0 (at 50% MK) and 1.6 (at 20% MK). [61]  The addition of MK
                              to portland cement results in the increased strength of the product. For
                              example, at 10% MK addition, the compressive strengths at 1, 3, and 28
                              days are 25, 33, and 40 MPa respectively, compared to the corresponding
                              values of 21, 25.5, and 36.4 MPa for the reference samples. [62]
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