Article ID Journal Published Year Pages File Type
8047101 Applied Clay Science 2014 6 Pages PDF
Abstract
In the FT-IR spectra, the observed bands attributed to carbonate in the range of 1430-1550 cm− 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
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