Ps. Fiske et Jf. Stebbins, THE STRUCTURAL OF MG IN SILICATE LIQUIDS - A HIGH-TEMPERATURE MG-25, NA-23, AND SI-29 NMR-STUDY, The American mineralogist, 79(9-10), 1994, pp. 848-861
We have studied the structural role of Mg in silicate liquids as a fun
ction of temperature and composition using high-temperature Mg-25, Na-
23, and Si-29 NMR. To establish the relationship between the isotropic
chemical shift (delta(iso)) and the coordination number for Mg-25 in
silicates, we have obtained high-resolution Mg-25 MAS NMR spectra on i
sotopically enriched akermanite ([4]Mg) and diopside ([6]Mg) using spi
n-echo pulse sequences and absolute-value Fourier-transform techniques
. The delta(iso) for akermanite is 49 +/- 3 ppm, and that for diopside
is 8 +/- 3 ppm, demonstrating that the chemical-shift range for Mg-25
in the silicates is similar to that established in oxides. The delta(
iso) for Mg-25 in (CaO)0.29 (MgO)0.14 (SiO2)0.57 liquid at 1400-degree
s-C is 8 ppm, suggesting that Mg resides in a structural environment s
imilar to that in diopside. The delta(iso) for Mg-25 in (Na2O)0.28(MgO
)0.18(SiO2)0.54 liquid shifts from 34 ppm at 1150-degrees-C to 29 ppm
at 1360 degrees-C, indicating smaller coordination numbers than in the
Ca liquid but a relatively large increase in the Mg-O bond length or
coordination number (or both) with increasing temperature. The delta(i
so) for Na-23 shows similar, but less pronounced, changes, whereas the
Si-29 delta(iso) is unchanged over this range of temperatures. This s
uggests that Mg undergoes the largest increases in bond distance or CN
(or both) of any of the cations in the liquid. Spin-lattice relaxatio
n times for Mg-25 and Na-23 were measured in liquid (Na2O)0.28-(MgO)0.
18(SiO2)0.54 over the same range of temperatures. The apparent activat
ion energy of the Mg-25 relaxation (related to Mg diffusional motion)
is 119 kJ/mol, intermediate between that of Na and Si. The apparent ac
tivation energy for Na-23 relaxation is 85 kJ/mol, which is higher tha
n that observed in sodium silicate liquids of similar polymerization b
ut comparable to that in mixed alkali silicate liquids, suggesting tha
t Na and Mg may show a mixed-cation effect.