Page 521 - Handbook of Thermal Analysis of Construction Materials
P. 521

492                  Chapter 12 - Clay-Based Construction Products


                                     The durability of clay bricks to freezing-thawing cycles is also
                              presented. Emphasis is placed on the use of thermal methods, e.g., dilatom-
                              etry to determine the factors that contribute to freezing-thawing resistance.
                              A method for determining the firing temperature characteristics of clay
                              brick is presented. The use of brick particulate additives to portland cement
                              concrete for enhancement of freezing-thawing resistance and the applica-
                              bility of thermal techniques to assess the bloatability of clays is also
                              described.




                              2.0    THERMAL BEHAVIOR AND
                                     IDENTIFICATION OF CLAYS AND
                                     ACCESSORY MINERALS



                              2.1    DTA of Clay Minerals


                                     Thermal methods (DTA, TG, TMA, and dilatometry) are well-
                              established investigative tools in clay science and related industrial applica-
                              tions. [1][2]  Clay brick manufacturers have employed these techniques to
                              optimize their plant production procedures.
                                     The successful firing of clays in industrial processes involves
                              considerations related to volume change, phase changes, and crystalliza-
                              tion phenomena. Drying shrinkage of clay minerals occurs due to pore
                              water loss in the temperature range of 100–150°C. The oxidation of any
                              organic material takes place in the range of 200–600°C. The oxidation of
                              sulfides begins between 400 and 500°C. The hydroxyl water is removed
                              from the clay minerals starting at temperatures somewhat below 500°C and
                              continuing to temperatures approaching 900°C. The nature of the clay
                              minerals in clays and the particle size influences the specific temperature
                              and rate of hydroxyl loss.
                                     Some of the general conclusions that can be drawn from the DTA
                                                                              [3]
                              studies of various clays may be summarized as follows.  An endothermic
                              reaction below about 200°C usually indicates the presence of montmoril-
                              lonite or illite. A clay containing these components will have high plasticity
                              and shrinkage, will probably be non-refractory, and will burn red. In
                              general, the larger this fraction the higher the plasticity and shrinkage.
                              Endothermic reactions between 300 and 500°C usually indicate a hydrox-
                              ide of alumina or iron. If the component is a hydroxide of alumina, the clay
   516   517   518   519   520   521   522   523   524   525   526