Xu, Ben and Poduska, Kristin M. (2014) Linking crystal structure with temperaturesensitive vibrational modes in calcium carbonate minerals. Physical Chemistry Chemical Physics, 16 (33). pp. 17634-17639. ISSN 1463-9084
- Published Version
Available under License Creative Commons Attribution Non-commercial.
We demonstrate a correlation between how an IR-active vibrational mode responds to temperature changes and how it responds to crystallinity differences. Infrared (IR) spectroscopy was used to track changes in carbonate-related vibrational modes in three different CaCO3 polymorphs (calcite, aragonite, and vaterite) and CaMg(CO3)2 (dolomite) during heating. Of the three characteristic IR-active carbonate modes, the in-plane bending mode (n4) shows the most pronounced changes with heating in polymorphs that have planar carbonate arrangements (calcite, aragonite, and dolomite). In contrast, this mode is virtually unchanged in vaterite, which has a canted arrangement of carbonate units. We correlate these trends with recent studies that identified the n4 mode as most susceptible to changes related to crystallinity differences in calcite and amorphous calcium carbonate. Thus, our results suggest that studies of packing arrangements could provide a generalizable approach to identify the most diagnostic vibrational modes for tracking either temperature-dependent or crystallinity-related effects in IR-active solids.
|Additional Information:||Memorial University Open Access Author's Fund|
|Department(s):||Science, Faculty of > Physics and Physical Oceanography|
|Date:||8 July 2014|
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