4.5 Article

Temperature dependence of Raman shifts and line widths for Q0 and Q2 crystals of silicates, phosphates, and sulfates

Journal

AMERICAN MINERALOGIST
Volume 103, Issue 6, Pages 966-976

Publisher

MINERALOGICAL SOC AMER
DOI: 10.2138/am-2018-6314

Keywords

Raman shifts in crystals; Raman line widths in crystals; temperature dependence of Raman shifts; temperature dependence of Raman line widths

Ask authors/readers for more resources

The temperature dependence of Raman shifts and line widths (full-width at half maxima or FWHM) for the A I symmetric stretch of 10(4) (T = Si, P, S) have been analyzed for nine alkali and alkaline earth silicates, phosphates, and sulfates. In crystalline silicates, the Q(0) and Q(2) species Raman shifts decrease with temperature, whereas FWHM increase. The strikingly similar behavior of Q(0) and Q(2) in silicates and Q(0) in phosphates makes it possible to estimate to within +/- 4 cm(-1) Raman shifts up to similar to 1000 K. Similarly systematic increases in FWHM with temperature can be estimated to within +/- 5 cm(-1) up to similar to 1400 K. The type of element centering 10(4) (i.e., Si, P, or S) has no appreciable effect on the temperature dependence of Raman shifts or line widths; the local environment of the Q(0) and Q(2) tetrahedra is the primary determinant of the temperature dependence. The type of cation in the first coordination sphere of the tetrahedron may have a secondary effect by affecting Heisenberg lifetimes of Raman virtual states. Previous theoretical considerations have been modified to include the effect of the Heisenberg (or natural) lifetime on Raman FWHM. This contribution is required to explain the anomalous FWHM of Li2SiO3 relative to the FWHM of isostructural Na2SiO3 and the large Li2SO4 and Li3PO4 FWHM (relative to Ba and Sr phosphates). The theoretically based expressions dictate a necessary, simple relationship among temperature, Raman shift, and FWHM. The relationship is developed and it allows, with one measurement of Raman shift and FWHM (e.g., measured at 298 K), prediction of Raman shifts and FWHM of Q(0) and Q(2) crystals to within 5 cm(-1) up to similar to 1500 K. The properties of the 10(4) moiety (T = Si, P, S) are mostly responsible for the striking regularity of Raman shifts and FWHM, although alkali and alkaline earth cations affect to varying extent Heisenberg lifetimes, hence FWHM.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.5
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available