Pl. Brown et al., HYDROLYSIS OF MAGNESIUM(II) AT ELEVATED-TEMPERATURES, Journal of the Chemical Society. Dalton transactions, (14), 1996, pp. 3071-3075
A potentiometric titration technique utilising a a hydrogen-electrode
concentration cell was applied to study the hydrolytic behaviour of th
e magnesium(II) ion in 0.10 and 1.0 mol kg(-1) sodium chloride at 60,
100, 150 and 200 degrees C. Data analysis indicates the presence of Mg
2+ (aq) and the solid species Mg(OH)(2), (s), only. Independent measur
ements have confirmed that [Mg(OH)](+) (aq) is a negligible ionic spec
ies under the prevailing experimental conditions. Experimental evidenc
e indicated that the solid species formed both rapidly and reversibly.
The equilibrium quotients for brucite formation were determined for e
ach temperature and ionic strength investigated and the corresponding
enthalpy and entropy of formation calculated. Formation constants have
also been calculated at zero ionic strength using the Debye-Huckel eq
uation, and these data, together with some other literature data, comp
ly with the equation log beta(12s)degrees = 2.49-(5847/T) where log be
ta(12s)degrees is the logarithm of the formation constant of brucite a
t zero ionic strength and T is the temperature in Kelvin.