Page 552 - Handbook of Thermal Analysis of Construction Materials
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522                  Chapter 12 - Clay-Based Construction Products


































                              Figure 24. Relation between one hour cold absorption and the saturation coefficient of
                              laboratory and plant-fired clay brick specimens. [31]



                                     Length changes for a Canadian brick fired at various temperatures
                              between 900 and 1100°C are shown in Fig. 25. All curves show a marked
                              hysteresis and a length anomaly around 575°C (due to α-quartz - β-quartz
                              inversion). These parameters have a magnitude that is inversely propor-
                              tional to the temperatures at which the specimens had originally been fired.
                                     Residual length changes produced by the temperature cycle are
                              plotted in Fig. 26 as a function of firing temperature. Values range from
                              0.4% shrinkage (900°C firing temperature) to 0.06% expansion (1100°C
                              firing temperature). Clay brick shrinks during firing and undergo additional
                              shrinkage during the refiring test. The previously well-fired brick (1100°C)
                              expanded slightly instead of shrinking as a result of re-heating.
                                     The integral of the peak in the length change curve (at approxi-
                              mately 575°C) was shown to decrease systematically with firing tempera-
                              ture. This peak suggests the α-quartz to β-quartz inversion. This inversion,
                              unlike the quartz-tridymite conversion, is rapid and instantaneously revers-
                              ible. A decrease in the anomaly with increased firing temperature is likely
                              a result of a more complete conversion of quartz to tridymite above 870°C.
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