Long-range order model of aqueous electrolyte solutions

4Citations
Citations of this article
5Readers
Mendeley users who have this article in their library.

Abstract

A partial long-range order model for aqueous electrolyte solutions is proposed to avoid contradictions present in the Debye-Huckel theory. The partial long-range order increases with increasing salt concentration because, as the ions are closer together, the coulombic energy of interaction which generates a quasi-lattice increases. Furthermore, the order decreases with increasing temperature because the thermal energy increases relative to the coulombic attraction of the ions. The long-range order parameter L and a parameter v which results from fluctuations and other effects are obtained for LiCl, NaCl and KC1 by comparing the theoretical configurational free energy to the electrical free energy obtained from the experimental activity coefficients. The specific interaction and the cluster integral models are discussed briefly at the end of this work. © 1977, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved.

Cite

CITATION STYLE

APA

Pytkowicz, R. M., Johnson, K., & Curtis, C. (1977). Long-range order model of aqueous electrolyte solutions. Geochemical Journal, 11(1), 1–7. https://doi.org/10.2343/geochemj.11.1

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free