Abstract
The ultrasonic velocities, densities, viscosities, and electrical conductivities of aqueous solutions of magnesium nitrate and magnesium acetate have been measured from dilute to saturation concentrations at 0 <= t/degrees C <= 50. The temperature derivative of the isentropic compressibility, K-s, became zero at 2.28 and 2.90 mol kg(-1) for Mg(OAc)(2) and Mg(NO3)(2) solutions, respectively, at 25 ...
Abstract
The ultrasonic velocities, densities, viscosities, and electrical conductivities of aqueous solutions of magnesium nitrate and magnesium acetate have been measured from dilute to saturation concentrations at 0 <= t/degrees C <= 50. The temperature derivative of the isentropic compressibility, K-s, became zero at 2.28 and 2.90 mol kg(-1) for Mg(OAc)(2) and Mg(NO3)(2) solutions, respectively, at 25 degrees C. The total hydration numbers of the dissolved ions were estimated to be, respectively, 24.3 and 19.2 at these concentrations. Differences in K, for various M2+ salts, using the present and literature data, correlated with reported M2+ -OH2 bond lengths and to a lesser extent with cationic charge densities (ionic radii). The influence of anions on K, appears to follow the Hofmeister series and also correlates approximately with the anionic charge density. Substantial differences between Mg(OAc)(2)(aq) and Mg(NO3)(2)(aq) occur with respect to their structural relaxation times (derived from compressibility and viscosity data) and their electrical conductivities. These differences were attributed to a much greater ion association in Mg(OAc)(2) Solutions. Raman spectra recorded at 28 degrees C confirmed the presence of various types of contact ion pairs including mono- and bidentate complexes in Mg(OAc)(2)(aq). In Mg(NO3)(2)(aq), only noncontact ion pairs appear to be formed even at high concentrations. The experimental results are supported by molecular dynamics simulations, which also reveal the much stronger tendency of OAc- compared to NO3- to associate with Mg2+ in aqueous solutions. The simulations also allow an evaluation of the ion-ion and ion-water radial distribution functions and cumulative sums and provide a molecular picture of ion hydration in Mg(OAc)(2)(aq) and Mg(NO3)(2)(aq) at varying concentrations.
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