H. Cho et Gr. Rossman, SINGLE-CRYSTAL NMR-STUDIES OF LOW-CONCENTRATION HYDROUS SPECIES IN MINERALS - GROSSULAR GARNET, The American mineralogist, 78(11-12), 1993, pp. 1149-1164
A detailed solid-state proton NMR study has been performed on garnets
containing low levels of OH (0.2-0.3 wt% as H2O), including a colorles
s and a pale orange grossular sample from Asbestos, Quebec, and a colo
rless grossular sample from Lelatema Hills, Tanzania. Synthetic hydrog
rossular powder, Ca3Al2(O4H4)3, has been investigated as well. The NMR
spectra of the three natural crystals have a broad line (40 kHz) with
a weak sharper feature superimposed. Multiple-quantum spectra indicat
e that in the Tanzanian garnet the dominant cluster size is two proton
s; in the colorless grossular from Asbestos a mixture of two proton an
d four proton clusters is in evidence; In the hydrogrossular powder, t
he cluster size is four protons. Solid echo envelope decay experiments
show that for all the natural samples a two-step decay process occurs
, implying the existence of two distinct proton environments. The area
ratios,indicate that the spectrum of each of the natural crystals is
dominated by a broad line with a Gaussian shape and a line width that
differs from the line width of the synthetic hydrogrossular. In the ca
se of the Tanzanian sample, the broad band constitutes approximately 8
5% of the area in the NMR spectrum. Moment analysis shows that althoug
h the synthetic hydrogrossular has an average interproton separation o
f 216 angstrom in the interacting cluster, it is 1.69 angstrom in the
grossular.