Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8047101 | Applied Clay Science | 2014 | 6 Pages |
Abstract
In the FT-IR spectra, the observed bands attributed to carbonate in the range of 1430-1550 cmâ 1 were singlets (for the natural and thermally exfoliated vermiculites) or split (for the heated vermiculite). This effect is likely due to structural breakdown and increased amorphisation created by heating and mechanical activation.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
E. Turianicová, A. Obut, Ľ. TuÄek, A. Zorkovská, İ. Girgin, P. Baláž, Z. Németh, M. Matik, D. Kupka,