T233 Apatite, from Magma to Medicine: In Honor of John M. Hughes
Wednesday, 7 November 2018
8:00 AM - 12:00 PM
Room 242
INSIGHT INTO THE CL-OH APATITE BINARY FROM FTIR SPECTROSCOPY
Paper number: T233-6
Program: Technical Sessions
Time: 9:10 AM – 9:25 AM
Authors
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John RakovanMiami University, Oxford, OH
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Daniel HarlovDeutsches GeoForschungsZentrum-GFZ, Potsdam
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Sean R. KellyMiami University, Oxford, OH
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John M. HughesUniversity of Vermont, Burlington, VT
Abstract
Hydrogen bonding is governed by the distance between hydrogen donor and hydrogen acceptor, as well as the electronegativity of the acceptor. Inter-oxygen distances for O(H)-O are linearly related to wavenumber in the OH stretching domain, and compare well with previous studies. O(H)-Cl distances form a similar linear array in that space, but with a different slope as compared to O(H)-O. Libowitzky (1999, Monatshefte Für Chemie) determined, for silicates, empirical relationships between wavenumber and O(H)-O distance. This relationship is very different for phosphates and for O(H)-Cl pairs in apatite group minerals. Conclusions garnered through research into silicate minerals should be extrapolated to phosphate minerals with prudence.
Spectral fitting is improved by recognition of a low-wavenumber feature in the OH stretching region as an OH-O pair. Although previously assigned as an OH-Cl pair, this peak is found in synthetic apatites that exclude chlorine. Oxyapatite is inferred in plasma-sprayed apatite on prosthetics. These data offer a means to recognize and measure O(H)-O pairs, in synthetic and in natural apatite group minerals. The presence of oxygen as a columnar anion also provides a means to reverse anionic ordering sequences along the c-axis, and preserve hexagonal symmetry.
Geological Society of America Abstracts with Programs. Vol. 50, No. 6
doi: 10.1130/abs/2018AM-320558
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