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On Dehydration of Bound Water of Sepiolite
Abstract
Bound water of sepiolite dehydrates in two steps in the temperature range of 250-650°C, as shown in the TG-curve. These steps are described here as steps II and III. At step II, half of the bound water is removed; other half at step III. From step II to III, discontinuous changes are confirmed in such properties as activation energy of dehydration, a-dimension, axial ratio, and intensities and spacings of X-ray powder reflections. A structural state at step II may be recognized as a distinct phase in the dehydration process.
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Cited by
He, C., Osbaeck, B., & Makovicky, E. (1995) · Cement and Concrete Research · doi:10.1016/0008-8846(95)00165-4 · Cited by 503
Properties of adsorbents used for bleaching of vegetable oils and animal fats
Kuuluvainen, V., Mäki‐Arvela, P., Rautio, A., Kordas, K., Roine, J., Aho, A., Toukoniitty, B., Österholm, H., Toivakka, M., & Murzin, D. Y. (2015) · Journal of Chemical Technology & Biotechnology · doi:10.1002/jctb.4621 · Cited by 21
Metadata
- Authors
- Nagata, H., Shimoda, S., & Sudo, T.
- Venue
- Clays and Clay Minerals
- Publisher
- Cambridge University Press (CUP)
- Published
- 1974-06
- Volume
- 22
- Issue
- 3
- Pages
- 285-291
- ISSN
- 0009-8604 (ISSN-L)
- 1552-8367
- OpenAlex
- W2144166892
- Cited by
- 165
- References
- 0
- FWCI
- 2.94
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: On Dehydration of Bound Water of Sepiolite. https://app.cochat.ai/papers/10.1346/ccmn.1974.0220310
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- Nagata, H., Shimoda, S., & Sudo, T. (1974). On Dehydration of Bound Water of Sepiolite. Clays and Clay Minerals. https://doi.org/10.1346/ccmn.1974.0220310
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
