Page 485 - Handbook of Thermal Analysis of Construction Materials
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Section 5.0 - Simultaneous TG - DTG - DTA                    459


                                                           [8]
                                     Khalil and Gad’s results  indicate that heating gypsum continu-
                              ously at a constant rate of 10°C/min results in a loss of one and a half
                              molecules of its water of crystallization or about 15.3%. This leads to
                              hemihydrate formation between 180 and 220°C. The γ-anhydrite formed
                              between 220 and 300°C with a total loss of nearly all the combined water
                              of crystallization amounting to about 20.4%. Complete hemihydrate forma-
                              tion occurs when gypsum is heated at relatively lower temperatures for
                              longer periods. Heating at temperatures ranging between 100 and 130°C
                              causes the loss of nearly all of the two molecules of water forming the γ-
                              anhydrite with varying amounts of hemihydrate. Longer periods at these
                              temperatures favor the formation of γ-anhydrite. Heating at higher tempera-
                              tures causes the conversion of γ-anhydrite to the β-form at 360°C. The latter
                              changes to the α- modification at about 1230°C. Further heating up to
                              1300°C shows insignificant loss in mass other than that due to the loss of
                              the water of crystallization.




                              5.0    SIMULTANEOUS TG-DTG-DTA


                                     Isa and Oruno describe a method that enables identification of
                              intermediates (in the gypsum dehydration process) more easily. [10]  The
                              method involves the use of simultaneous TG-DTG-DTA under various
                              sealed atmospheres corresponding to three systems—open completely,
                              sealed, and quasi-sealed. Endothermic DTA peaks appear earlier (129 and
                              133°C) than the point of decreasing TG. This technique, resembling the
                              quasi-isothermal and isobaric thermogravimetry (Q-TG), is superior to the
                              latter in that it needs less of the sample.
                                     Typical results for the open system are shown in Fig. 10. The first
                              endothermic peak from the DTA, due to dehydration, begins at 102°C. The
                              TG and DTG curves begin at 107°C and 102°C respectively (for the
                              simultaneous technique) indicating the coincidence of the thermal and
                              thermogravimetric behaviors of hydration. This temperature is, however,
                              dependent on the sample amount, heating rate, the sensitivity of the TG,
                              DTG, and DTA, and the signal to noise ratio. The DTA exhibits two
                              endotherms (at 122 and 130°C), and there are considered to be two reaction
                              steps.
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