Abstract
A white calcium bentonite (CaB) taken from Çamlıdere (Ankara, Turkey) region was heated at various temperatures between 100 and 1100 °C for 2 h. The mineralogy of the CaB was determined as calcium smectite (CaS), metahalloysite (MH), opal-A (OA), opal-CT (OCT), quartz (Q), feldspar (F), and calcite (C) using the X-ray diffraction patterns of the natural CaB and its heated samples. Besides the XRD patterns, the thermogravimetry, differential thermal analysis, and low-temperature nitrogen adsorption (N2-AD) data show that the CaS lose adsorbed and hydration water up to 300 °C, dehydroxylation takes place between 300 and 750 °C, and then the 2:1 layer structure completely collapses above 900 °C. The activation energies for the dehydration and dehydroxylation were calculated as 7636 and 48838 J mol−1, respectively, from the TG data using Coats and Redfern method. The specific surface area (S) and specific micro–mesopore volume (V) obtained from N2-AD data were 44 m2 g−1 and 0.100 cm3 g−1 for the natural CaB. S and V reach their maxima of 105 m2 g−1 and 0.155 cm3 g−1, respectively, at 300 °C, remain approximately constant as the temperature increases up to 700 °C and then decrease almost in parallel with each other, reaching their minima at 900 °C. This indicates that the S and V values increase gradually during dehydration and dehydroxylation of the CaS.
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Acknowledgements
The authors wish to thank to Scientific and Technical Research Council of Turkey (TÜBİTAK) and Ankara University Research Foundation for supporting this work under the project 107T622 and 2003.05.07.083.
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Bayram, H., Önal, M., Yılmaz, H. et al. Thermal analysis of a white calcium bentonite. J Therm Anal Calorim 101, 873–879 (2010). https://doi.org/10.1007/s10973-009-0626-y
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DOI: https://doi.org/10.1007/s10973-009-0626-y