SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 52:1566-1570 (1988)
© 1988 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Essington, M. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Essington, M. E.
Agricola
Right arrow Articles by Essington, M. E.

Solubility of Barium Arsenate

M. E. Essington*

Division of Waste Characterization and Chemistry, Western Res. Inst., Univ. of Wyoming Res. Corp., P.O. Box 3395, Laramie, WY 82071

*Corresponding author.

ABSTRACT

Current thermodynamic data suggest barium arsenate [Ba3(AsO4)2(c)] to be a highly stable phase. However, sufficient evidence is available to question the validity of the current data. In order to determine the solubility (pKsp) and calculate the standard free energy of formation ({Delta}f) of Ba3(AsO4)2(c), an equilbrium solubility study was conducted. The equilibrium experiments were carried out under three different ionic strength conditions for reaction times up to 45 d. Equilibrium was approached from both undersaturated and supersaturated initial conditions. The pKsp for the dissolution of Ba3(AsO4)2(c) was calculated to be 21.62. Correspondingly, a {Delta}f of – 3101.2 ± 2.0 kJ mol–1 was calculated. This value is 166.9 kJ mol–1 more positive than the current literature value. Reevaluation of the solubility data from a previous work suggests that the pKsp for the dissolution of BaHAsO4 · H2O(c) is 24.64 and the corresponding {Delta}f is – 1587.0 ± 2.5 kJ mol–1.


NOTES

Contribution of the Division of Waste Characterization and Chemistry. Support by the U.S. Dep. of Energy, as part of Cooperative Agreement no. DE-FC21-86MC11076, is gratefully acknowledged.

Received for publication January 25, 1988.


This article has been cited by other articles:


Home page
Soil Sci.Home page
R. B. Johnston and P. C. Singer
Solubility of Symplesite (Ferrous Arsenate): Implications for Reduced Groundwaters and Other Geochemical Environments
Soil Sci. Soc. Am. J., January 1, 2007; 71(1): 101 - 107.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1988 by the Soil Science Society of America.