| dc.contributor.author |
Hovis, Guy L. |
|
| dc.contributor.author |
Harlov, D. E. |
|
| dc.date.accessioned |
2012-01-13T18:59:08Z |
|
| dc.date.available |
2012-01-13T18:59:08Z |
|
| dc.date.issued |
2010 |
|
| dc.identifier.citation |
Hovis, G. L. and D. E. Harlov. (2010) "Solution calorimetric investigation of fluor-chlorapatite crystalline solutions." American Mineralogist 95 (7): 946-952. |
en_US |
| dc.identifier.uri |
http://hdl.handle.net/10385/884 |
|
| dc.description.abstract |
Solution calorimetric measurements have been made on 17 synthetic fluorapatite-chlorapatite crystalline solutions at 50 degrees C in 20.0 wt% HCl under isoperibolic conditions. Analysis of the calorimetric data indicates that heats of mixing across the series may reach values as high as 8.3 kJ/mol. Normally such a high degree of thermodynamic nonideality would be associated with immiscibility, yet no such miscibility gap is indicated by either synthetic or natural fluor-chlorapatite specimens. Based on full chemical analyses, all Cl-rich samples (X(Cl) > 0.65) of this study have halogen deficiencies that imply the presence of 4-11 mol% vacancies in the anion sites, which are interpreted to be associated with oxyapatite substitution. Separate analysis of data for the vacancy-free samples produces a linear fit for enthalpy of solution vs. composition, which yields an alternative interpretation of thermodynamic ideality. Together these models define the limits of enthalpy behavior for the fluor-chlorapatite system. |
en_US |
| dc.publisher |
American Mineralogist |
en_US |
| dc.subject |
enthalpies of mixing |
en_US |
| dc.subject |
fluorapatite |
en_US |
| dc.subject |
chlorapatite |
en_US |
| dc.subject |
thermodynamics |
en_US |
| dc.title |
Solution calorimetric investigation of fluor-chlorapatite crystalline solutions |
en_US |
| dc.type |
Article |
en_US |
| dc.identifier.doi |
10.2138/am.2010.3485 |
|