Abstract
The decomposition behaviour of dolomite samples has been carried out by simultaneous DTA-TG experiments. Dolomite samples could be classified broadly into two categories as regular and iron-bearing dolomites based on DTA decomposition temperatures. The mass% FeO of all the dolomite samples was identified by DTA and the results are confirmed by atomic absorption spectrophotometer experiments.
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Kök, M.V., Smykatz-Kloss, W. Thermal Characterization of Dolomites. Journal of Thermal Analysis and Calorimetry 64, 1271–1275 (2001). https://doi.org/10.1023/A:1011521802817
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DOI: https://doi.org/10.1023/A:1011521802817