Answers are grounded in this paper and cite their sources.
Infrared spectra of two minerals; Urkut quartz (Hungary) and a Swedish feldspar, of different origin with different physical characteristics and crystallinity were studied. Samples were taken after appropriate grinding, and infrared spectra, X-ray powder diffraction and water vapor absorption measurements were made along with electronmicrographs. Quantitative conclusions were drawn from changes of particle size and the ratio of bands of the Si—O groups and also the degree of crystallinity and changes of the particle size, respectively.
No takes yet. Share an insight, caveat, or question.
Hlavay et al. (1978) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: