ION-PAIRING IN AQUEOUS MGSO4 SOLUTIONS ALONG AN ISOCHORE TO 500-DEGREES-C AND 11 KBAR USING RAMAN-SPECTROSCOPY IN CONJUNCTION WITH THE DIAMOND-ANVIL CELL
Jd. Frantz et al., ION-PAIRING IN AQUEOUS MGSO4 SOLUTIONS ALONG AN ISOCHORE TO 500-DEGREES-C AND 11 KBAR USING RAMAN-SPECTROSCOPY IN CONJUNCTION WITH THE DIAMOND-ANVIL CELL, Chemical geology, 116(3-4), 1994, pp. 181-188
A high-temperature diamond-anvil cell is used in conjunction with micr
o-Raman spectrometer in the study of aqueous fluids containing 0.5 m M
gSO4 along an isochore from room conditions to 500-degrees-C and 11 kb
ar. Gaskets lined with platinum are used to contain the chemically-rea
ctive fluid. Ion-pairing of MgSO4 is shown to increase with increasing
pressure along an isochore with a density of approximately 1 g cm-3.
Mass-action constants for the reaction Mg2+ + SO4(2-) reversible MgSO4
range from 3.5 . 10(1) at 20-degrees-C, 1 bar to 1.25.10(4) at 500-de
grees-C, 11.4 kbar. The results agree favorably with those obtained th
rough electrical conductance measurements by V.G. Ritzert and E.U. Fra
nck. The relative abundances of the species are shown as a function of
temperature and pressure along the isochore.