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Thermal diffusion of lanthanide chlorides

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TLDR
In this paper, the molar entropy of rare earth chlorides at 0.001, 0.01 and 0.1N were measured by the potentiometric method using the silver, silver chloride thermocell at a mean temperature of 25°C.
Abstract
The molar entropy (or heat) of transport of aqueous rare earth chlorides at 0.001, 0.01 and 0.1N have been measured by the potentiometric method using the silver, silver chloride thermocell at a mean temperature of 25°C. Our results indicate that the entropy of transport of rare earth chlorides exhibits a two-series, step function type of dependence on ionic radii. Although this is not the usual S-shaped dependence on ionic radii observed in many thermodynamic and transport properties, the Soret data do seem to show that hydration of the heavier rare earth ions may be rather different from the lighter rare earth ions. The concentration dependence of the entropy of transport have also been investigated for LaCl3, SmCl3, and YbCl3. In all cases the experimental limiting slopes agree well with that predicted by theory based on the electrostatic model.

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Thermal non-equilibrium transport in colloids

TL;DR: In this article, different transport mechanisms for charged colloids, and how a thermal gradient gives rise to companion fields, are discussed, with particular emphasis on the thermal response of the electrolyte solution: positive and negative ions diffuse along the temperature gradient and thus induce a thermoelectric field which in turn acts on the colloidal charges.
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Proportionality of Intrinsic Heat of Transport to Standard Entropy of Hydration for Aqueous Ions

TL;DR: In this paper, the authors evaluated the ionic entropies of 53 aqueous ions at infinite dilution at 25°C using the reduction rule proposed by the authors and the limiting laws of Agar, and of Helfand and Kirkwood.
Journal ArticleDOI

Thermoelectric effect on charged colloids in the Hückel limit

TL;DR: The thermophoretic coefficient DT of a charged colloid is studied, which consists of two contributions, a dielectrophoretic term proportional to the permittivity derivative d$ \varepsilon$/dT and a Seebeck term, i.e., the macroscopic electric field induced by the thermal gradient in the electrolyte solution.
Journal ArticleDOI

Thermal diffusion of dilute aqueous NH4Cl, Me4NCl, Et4NCl,n-Pr4NCl, andn-Bu4NCl solutions at 25°C

TL;DR: In this article, the Soret effect of dilute aqueous solutions of NH4Cl, Me4NCl, Et4Ncl, n-Pr4NCL, and n-Bu4Cl has been investigated potentiometrically using the silver, silver chloride thermocell.
Journal ArticleDOI

The Soret effect in dilute aqueous alkaline earth and nickel chloride solutions at 25°C

TL;DR: In this article, the Soret effect in dilute aqueous solutions of alkaline earth and nickel chlorides at 25°C has been investigated by the potentiometric method and the molar entropies of transport have been obtained from the measurements of the initial (homoheneous) and final (Soret steady-state) thermoelectric powers.
References
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Journal ArticleDOI

Free Volume and Entropy in Condensed Systems III. Entropy in Binary Liquid Mixtures; Partial Molal Entropy in Dilute Solutions; Structure and Thermodynamics in Aqueous Electrolytes

TL;DR: The first and second papers in this series, which make it possible to interpret entropy data in terms of a physical picture, are applied to binary solutions, and equations are derived relating energy and volume changes when a solution is formed to the entropy change for the process as discussed by the authors.
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The coordination (hydration) of rare earth ions in aqueous chloride solutions from x ray diffraction. I.TbCl3,DyCl3, ErCl3,TmCl3,and LuCl3

TL;DR: In this paper, the rare earth complex (RE(H3O)8]3+, has been identified in concentrated (3.2−3.6 m) aqueous TbCl3,DyCl3 and DyCl3 solutions from x ray diffraction measurements.
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The coordination (hydration) of rare earth ions in aqueous chloride solutions from x‐ray diffraction. III. SmCl3, EuCl3, and series behavior

TL;DR: In this paper, the inner sphere water coordination of rare earth ions in aqueous solutions decreases from nine to eight due to decreasing rare earth ionic radii, and the average water coordination is 8.8 for Sm3+ and 8.3 for Eu3+.
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Enthalpy of hydration of the proton

TL;DR: In this article, a simple model of aqueous solutions is used to estimate the absolute hydration enthalpy of the proton at infinite dilution and at 298 c-K. The value obtained is -260.7 kcal mole/sup -1/ with an estimated uncertainty of surface proces 2.
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