A thermodynamic analysis of the decrepitation process

M. S. Celik*, F. Suner

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

28 Citations (Scopus)

Abstract

The decrepitation properties of the two typical boron minerals colemanite and ulexite reveal that, whereas colemanite undergoes decrepitation, ulexite shows no sign of significant fragmentation upon heating. This process enables separation of colemanite from ulexite at temperatures above 400°C. A thermodynamic evaluation of 14 boron minerals has shown that only colemanite exhibits decrepitation. A mechanism involving the temperature differential at the onset of dehydration and decomposition and the resultant enthalpy change is proposed as being responsible for this intriguing phenomenon.

Original languageEnglish
Pages (from-to)167-174
Number of pages8
JournalThermochimica Acta
Volume254
Issue numberC
DOIs
Publication statusPublished - 15 Apr 1995

Keywords

  • Boron mineral
  • Calcination
  • Colemanite
  • Decrepitation
  • Thermodynamics

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