Titlebook: Differential Thermal Analysis; Application and Resu Werner Smykatz-Kloss Book 1974 Springer-Verlag Berlin · Heidelberg 1974 Differentialthe

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Development of Identification Diagrams all runs have been made under comparable heating conditions. The following consequence is: such an introductory diagram temperature versus . of a peak can be only valid for one set of investigation conditions. If you vary the heating rate, for example, you will get a shifting of the data. Therefore

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Influence of the Chemical Composition on the Decomposition Temperatures of Carbonates and Hydroxidespure crystal, the DTA curve of the same mineral that is impure or disordered only shows a broad deflection of lower intensity without a distinct endothermic minimum. The . (.) of a decomposition peak therefore indicates if substitutions or crystal physical defects are present or absent in a crystal

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Identities Welcome and Unwelcome in College,ents (., . and .). Meanwhile only the . of a deflection in the DTA curve is regarded as a measure for the amount of a reacting substance during the heating process (. and .; . and .; . and .; . et al.; ., . et al. and others).

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Reading as a Social Practice: Race Talk,ts with peaks at 380 and 580° C. Shape and temperatures of these peaks are dependent on the grain size (.), and on some other factors (.). A weak endothermic effect at 680° C points out the Curie point of Fe.O. (.); the temperature of this peak varies with different contents of titanium and manganes

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Steven R. Yussen,Randall L. Glyschtransformation behaviour of some pyroxenes. . published the data of the mineral ilvaite, and garnets can also be investigated by means of DTA if they contain some (OH) instead of (SiO.); e.g. see . and ., who reported on the data of hydrogrossular. Thermogravimetric investigations of . and of . (196

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The Spelling-Sound Code in Readinglty results from disorder of the structure which lowers the thermal effects, from differences in grain or particle size, from strongly varying chemical compositions of the minerals and from the fact that sheet silicate minerals scarcely occur in a pure form. However, they only occur in mixtures of s

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