Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Figures Only Full Text Full Text (PDF) Supplementary Data Info Alert me when this article is cited Alert me if a correction is posted Citation Map Services Email this article to a friend Similar articles in this journal Similar articles in ISI Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via ISI Web of Science (1) Citing Articles via Google Scholar Google Scholar Articles by Bertoldi, C. Articles by Appel, P. Search for Related Content GeoRef GeoRef Citation

Heat-pulse calorimetry measurements on natural chlorite-group minerals

¹ Universität Salzburg, Fachbereich Materialwissenschaften, Abteilung Mineralogie, Hellbrunner Strasse 34, A-5020 Salzburg, Austria
² Universität Kiel, Institut für Geowissenschaften, Abteilung Mineralogie, Ohlshausenstrasse 40, D-24098 Kiel, Germany

Correspondence: ^* E-mail: christian.bertoldi{at}sbg.ac.at

Low- and high-temperature heat capacities of five natural chlorite-group samples were measured using the heat-capacity option of the Physical Properties Measurement System (Quantum Design), which is based on the principles of heat-pulse calorimetry, and by differential scanning calorimetry. Comprehensive chemical analyses were performed on these samples by electron microprobe analysis, by inductively coupled plasma mass spectrometry, and by Karl-Fischer titration (for H₂O). The natural chlorites span a range in X_Fe from 0.052 to 0.885 with increasing Al-content due to the Tschermak substitution with increasing X_Fe.

The measured heat capacities were extrapolated to the end-member compositions of chamosite and clinochlore. Integration of heat-capacity data yields the calorimetric standard entropies of chamosite (Fe₅Al)[Si₃AlO₁₀](OH)₈ and clinochlore (Mg₅Al)[Si₃AlO₁₀](OH)_8, with values of 572.0 ± 0.2 and 425.6 ± 0.4 J/(mol·K), respectively. The C_P-polynomial for end-member chamosite is C_P = 1151.7 – 8.4564 x 10³·T^–0.5 – 13.206 x 10⁶·T^–2 + 15.233 x 10⁸·T^–3 [J/(mol·K)], valid in the temperature range of 298.15–900 K, and that for end-member clinochlore is C_P = 1160.5 – 9.9819 x 10³·T^–0.5 – 5.9534 x 10⁶·T^–2 + 3.8677 x 10⁸·T^–3 [J/(mol·K)], valid in the temperature range of 298.15–1000 K.

The Fe-rich chlorites exhibit an asymmetric distribution of the excess heat capacity in a plot of C^ex_P vs. T, with a maximum at about 52 K. By analogy to annite, we interpret this peak to represent the magnetic ordering temperature.

Based on our standard entropy value for chamosite, the enthalpy of formation of berthierine (Fe_2.5Al_0.5)[Si_1.5Al_0.5O₅](OH)₄ was estimated as –3570.30 kJ/mol using a reported onset temperature of 70 °C at 16 MPa for the berthierine-chamosite polymorphic transition.

Key Words: Clinochlore • chamosite • heat pulse calorimetry • heat capacity • excess heat capacities • standard entropy • chlorite group minerals

This article has been cited by other articles:

				J. A. Schuessler, R. E. Botcharnikov, H. Behrens, V. Misiti, and C. Freda Amorphous Materials: Properties, structure, and Durability: Oxidation state of iron in hydrous phono-tephritic melts American Mineralogist, October 1, 2008; 93(10): 1493 - 1504. [Abstract] [Full Text] [PDF]