Empirical electronic polarizabilities for use in refractive index measurements at 589.3 nm: Hydroxyl polarizabilities
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Robert D. Shannon
Abstract
Refractive indices of minerals and inorganic compounds can be calculated from their chemical compositions using the additivity rule for electronic polarizabilities and converting the sum of polarizabilities α using the Anderson-Eggleton relationship:
with the molar volume Vm solved for the mean refractive index nD at 589.3 nm. Whereas the polarizability of cations is a single parameter, the polarizability of anions is described by a two-parameter term
Thus, we find that these summed intrinsic polarizabilities for OH-bonds which are involved in H-bonding are significantly lower than the corresponding summed intrinsic polarizabilities for OH-bonds not involved in H-bonding. We attribute the reduction in polarizability of hydroxyl ions in clinometaborite, sassolite, archerite, kalicinite and metaborite, and the compound NaPO2(OH)2 to the presence of H-bonds and a reduction of Hirshfeld atomic charge on the O atom.
Acknowledgments
We thank Ruth Shannon for the tabulation of data, and Frank Hawthorne and an anonymous reviewer for improving the manuscript.
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- Experimental study of apatite-fluid interaction and partitioning of rare earth elements at 150 and 250 °C
- Assimilation of xenocrystic apatite in peraluminous granitic magmas
- Cathodoluminescence of iron oxides and oxyhydroxides
- The effect of elemental diffusion on the application of olivine-composition-based magmatic thermometry, oxybarometry, and hygrometry: A case study of olivine phenocrysts from the Jiagedaqi basalts, northeast China
- Characterization of nano-minerals and nanoparticles in supergene rare earth element mineralization related to chemical weathering of granites
- Atomic-scale interlayer friction of gibbsite is lower than brucite due to interactions of hydroxyls
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- The role of parent lithology in nanoscale clay-mineral transformations in a subtropical monsoonal climate
- Discovery of terrestrial andreyivanovite, FeCrP, and the effect of Cr and V substitution on the low-pressure barringerite-allabogdanite transition
- Microstructural changes and Pb mobility during the zircon to reidite transformation: Implications for planetary impact chronology
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