Hostname: page-component-cd9895bd7-q99xh Total loading time: 0 Render date: 2024-12-25T10:05:20.256Z Has data issue: false hasContentIssue false
  • English
  • Français

Baseline Studies of the Clay Minerals Society Source Clays: Thermal Analysis

Published online by Cambridge University Press:  28 February 2024

Stephen Guggenheim  and
A. F. Koster van Groos
Stephen Guggenheim*
Affiliation:
Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, Illinois 60607, USA
A. F. Koster van Groos
Affiliation:
Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, Illinois 60607, USA
*
E-mail of corresponding author: xtal@uic.edu
Rights & Permissions [Opens in a new window]

Extract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Thermal analysis involves a dynamic phenomenological approach to the study of materials by observing the response of these materials to a change in temperature. This approach differs fundamentally from static methods of analysis, such as structural or chemical analyses, which rely on direct observations of a basic property of material (e.g. crystal structure or chemical composition) at a well-defined set of conditions (e.g. temperature, pressure, humidity). Clay minerals are highly susceptible to significant compositional changes in response to subtle changes in conditions. For example, changes in the fugacity of water affect the stability of interlayer H2O in a clay mineral (see below). Therefore, care must be taken that all experimental conditions are known with accuracy and precision

Type
Research Article
Information
Clays and Clay Minerals , Volume 49 , Issue 5 , October 2001 , pp. 433 - 443
Copyright
Copyright © 2001, The Clay Minerals Society

References

Chipera, S.J. and Bish, D., 2001 Baseline studies of the Clay Minerals Society Source Clays: powder diffraction analyses Clays and Clay Minerals 49 398–409 10.1346/CCMN.2001.0490507.CrossRefGoogle Scholar
Costanzo, P.M., 2001 Baseline studies of the Clay Minerals Society Source Clays: introduction Clays and Clay Minerals 49 372–373 10.1346/CCMN.2001.0490502.CrossRefGoogle Scholar
Guggenheim, S. and Koster van Groos, A.F., 1992 High-Pressure Differential Thermal Analysis (HP-DTA) I. Dehydration reactions at elevated pressures in phyllosilicates Journal of Thermal Analysis 38 1701–1728 10.1007/BF01979366.CrossRefGoogle Scholar
Guggenheim, S. and Koster van Groos, A.F., 1992 High-Pressure Differential Thermal Analysis (HP-DTA) II. Dehydroxylation reactions at elevated pressures in phyllosilicates Journal of Thermal Analysis 38 2529–2548 10.1007/BF01974630.CrossRefGoogle Scholar
Mackenzie, R.C., 1972 Differential Thermal Analysis, vol. 2. Applications London and New York Academic Press.Google Scholar
Mackenzie, R.C. and Callière, S. (1979) Thermal analysis, DTA, TG, DTG. Pp. 243–284 in: Data Handbook for Clay Materials and other Non-metallic Minerals (Olphen, H. van and Fripiat, J.J., editors). Pergamon, Oxford, UK.Google Scholar