Possibilities of determination of alteration degree of rocks by thermogravimetry View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2009-05

AUTHORS

P. Rózsa, S. Szakáll, Éva Balázs, A. Bartha

ABSTRACT

Rhyolite-rhyodacite tuff samples were analysed by X-ray powder diffraction, ICP-OES and thermogravimetric (TG) methods to determine mineral and major element composition as well as different types of bound water, respectively. Similarly to CIA values, some TG parameters (H2O[I] — water released up to ca. 200–220°C; H2O[III] — water loss above 500–550°C and H2O[I+III]) show positive correlation to the amount of secondary minerals. Moreover, these parameters are in close positive correlation to CIA values. Our results suggest that TG determination of different types of bound water may serve as a useful tool for estimation and characterisation of alteration degree of rocks. More... »

PAGES

433-438

References to SciGraph publications

  • 1988-03. Possibility of thermal analysis of different types of bonding of water in minerals in JOURNAL OF THERMAL ANALYSIS AND CALORIMETRY
  • 2008-07. Study of soils by thermal analysis in JOURNAL OF THERMAL ANALYSIS AND CALORIMETRY
  • 2008-04. Thermal characterization of the clay binder of heritage Sydney sandstones in JOURNAL OF THERMAL ANALYSIS AND CALORIMETRY
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    http://scigraph.springernature.com/pub.10.1007/s10973-008-9386-3

    DOI

    http://dx.doi.org/10.1007/s10973-008-9386-3

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