Journal of the American Ceramic Society · 1967 · 112 citations · 4 references
Natural SciencesChemistryMaterials ScienceInorganic ChemistryPhase TransformationsPhysical ChemistryCrystal ChemistryCrystal SystemsInorganic MaterialsPolymorphic TransformationsX-ray CrystallographyX-ray DiffractionCrystal Chemistry Of SilicatesDisplacive TransformationsPolymorphism In SilicatesSilicate ChemistrySilicate Crystal StructuresSilicate TransformationSolid Solution In SilicatesTransformations
In tricalcium silicate and its solid solutions six modifications were established: one rhombohedral ( R ), two monoclinic ( M I , M II ), and three triclinic ( T I , T II , T III ). All these forms are rhombohedral or pseudorhombohedral and extremely similar; the variations in the X‐ray diagrams and the transformation enthalpies are minute. Only three of the five transitions were observed by both X rays and DTA: T I ‐ T II (600°), T III – M I (980°), and M I – M II (990°); one was established by DTA ( T II – T III , 920°) and one by X rays only ( M II – R , 1050°C). This scheme of polymorphism is compared critically with results of other authors, and the nature of the various displacive transformations is discussed. X‐ray and DTA investigations of solid solutions of Ca 3 SiO 5 with Al 2 O 3 and ZnO established the phase relations as functions of temperature and composition. With Al 2 O 3 , two modifications ( T I and T II ) were stabilized; and with ZnO, five polymorphs ( T I T II , M I , M II , and R ). With both pure C 3 S and the solid solutions, the results are consistent and have a close bearing on the constitution of alites in portland cement clinker.
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The crystal structure of tricalcium silicate
J. W. Jeffery · Acta Crystallographica · 1952 · 135 citations