Skip to content Skip to navigation
University of Warwick
  • Study
  • |
  • Research
  • |
  • Business
  • |
  • Alumni
  • |
  • News
  • |
  • About

University of Warwick
Publications service & WRAP

Highlight your research

  • WRAP
    • Home
    • Search WRAP
    • Browse by Warwick Author
    • Browse WRAP by Year
    • Browse WRAP by Subject
    • Browse WRAP by Department
    • Browse WRAP by Funder
    • Browse Theses by Department
  • Publications Service
    • Home
    • Search Publications Service
    • Browse by Warwick Author
    • Browse Publications service by Year
    • Browse Publications service by Subject
    • Browse Publications service by Department
    • Browse Publications service by Funder
  • Statistics
  • Help & Advice
University of Warwick

The Library

  • Login

Lattice energies of apatites and the estimation of Delta H-f(circle)(PO4(3-), g)

Tools
- Tools
+ Tools

UNSPECIFIED. (2004) Lattice energies of apatites and the estimation of Delta H-f(circle)(PO4(3-), g). INORGANIC CHEMISTRY, 43 (7). pp. 2340-2345. ISSN 0020-1669

Full text not available from this repository.
Official URL: http://dx.doi.org/10.1021/ic030255o

Abstract

Experimentally based lattice energies are calculated for the apatite family of double salts M-5(PO4)(3)X, where M is a divalent metal cation (Ca, Sr, Ba) and X is hydroxide or a halide. These values are also shown to be estimable, generally to within 4%, using the recently derived Glasser-Jenkins equation, U-POT = Al(2l/V-m)(1/3), where A = 121.39 kJ mol(-1). The apatites exhibiting greater covalent character (e.g., M = Pb, Cd, etc.) are less well reproduced but are within 8% of the experimentally based value. The lattice energy for ionic apatites having identical lattice ionic strengths, takes the particularly simple form U-POT/kJ mol(-1) = 26680/(V-m/nm(3))(1/3), reproducing cycle values Of U-POT well when V-m is estimated by ion volume summation and employing a volume for the PO43- ion (not previously quantified with an associated error) of 0.063 +/- 0.003 nm(3). A value for the enthalpy of formation of the gaseous phosphate ion, DeltaH(f)degrees(PO43-, g), is absent from current thermochemical tabulations. Examination of solution and solid state thermochemical cycles for apatites, however, leads us to a remarkably consistent value of 321.8 +/- 1.2 kJ mol(-1). Experimental and estimated lattice energies were used along with other thermodynamic data to determine enthalpies, entropies, and free energies of dissolution for apatites of uncertain stabilities. These dissolution values are compared with the corresponding values for stable apatites and are used to rationalize the relative instability of certain derivatives.

Item Type: Journal Article
Subjects: Q Science > QD Chemistry
Journal or Publication Title: INORGANIC CHEMISTRY
Publisher: AMER CHEMICAL SOC
ISSN: 0020-1669
Date: 5 April 2004
Volume: 43
Number: 7
Number of Pages: 6
Page Range: pp. 2340-2345
Identification Number: 10.1021/ic030255o
Publication Status: Published
URI: http://wrap.warwick.ac.uk/id/eprint/8578

Data sourced from Thomson Reuters' Web of Knowledge

Request changes to a record

Actions (login required)

View Item View Item
twitter

Email us: publications@warwick.ac.uk
Contact Details
About Us