This is the first report to show that the two Si-29-NMR signals (-86.3
, -87.1 ppm) of Q(2) of natural and synthetic xonotlites were clearly
split, which is in accord with the crystal structure study of Kudoh et
al.(1) The H-1-NMR spectra were deconvoluted into three lines at 2.19
, 1.86 and 5.26 ppm and assigned to structural Ca-OH, Si-OH and molecu
lar water, respectively. The signal intensities are in good agreement
with the thermogravimetric analysis.