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Editorial Honoring Pitzer

Editorial Honoring Pitzer 2 FANK J. MILLERO model to cover a wide range of temperatures (0 to 250 C) and pressure (0 to 1000 bars). These equations are now used to account for the ionic interactions of natural waters by most geochemists studying aqueous solutions. References Harvie, C. E. and Weare, J. H. (1980) The prediction of mineral solubilities in natural waters: The Na- K-Mg-Ca-SO -Cl-H O system from zero to high concentration at 25 C. Geochim. Cosmochim. 4 2 Acta 44, 981–997. Pitzer, K. S. (1975) Thermodynamics of electrolytes. V. Effects of higher order electrostatic terms. J. Solution Chem. 3, 249–265. Pitzer, K. S. (1991) Theory: Ion interaction approach: Theory and data collection, In: Activity Coefficients Pitzer, K. S. (1995) Thermodynamics. Third Edition. Series in Advanced Chemistry, McGraw-Hill, New York.. Pitzer, K. S. and Kim, J. J. (1974) Thermodynamics of electrolytes. IV. Activity and osmotic coefficients for mixed electrolytes. J. Am. Chem. Soc. 96, 5701–5707. Pitzer, K. S. and Mayorga, G. (1973) Thermodynamics of electrolytes. II. Activity and osmotic coefficients for strong electrolytes with one or both ions univalent. J. Phys. Chem. 77, 2300–2308. Pitzer, K. S. and Mayorga, G. (1974) Thermodynamics of electrolytes. III. Activity and osmotic coefficients for 2-2 http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Aquatic Geochemistry Springer Journals

Editorial Honoring Pitzer

Millero, Frank
Aquatic Geochemistry , Volume 4 (1) – Oct 15, 2004
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References (7)

Publisher
Springer Journals
Copyright
Copyright © 1998 by Kluwer Academic Publishers
Subject
Earth Sciences; Geochemistry; Hydrology/Water Resources; Hydrogeology; Water Quality/Water Pollution
ISSN
1380-6165
eISSN
1573-1421
DOI
10.1023/A:1009604730389
Publisher site
See Article on Publisher Site

Abstract

2 FANK J. MILLERO model to cover a wide range of temperatures (0 to 250 C) and pressure (0 to 1000 bars). These equations are now used to account for the ionic interactions of natural waters by most geochemists studying aqueous solutions. References Harvie, C. E. and Weare, J. H. (1980) The prediction of mineral solubilities in natural waters: The Na- K-Mg-Ca-SO -Cl-H O system from zero to high concentration at 25 C. Geochim. Cosmochim. 4 2 Acta 44, 981–997. Pitzer, K. S. (1975) Thermodynamics of electrolytes. V. Effects of higher order electrostatic terms. J. Solution Chem. 3, 249–265. Pitzer, K. S. (1991) Theory: Ion interaction approach: Theory and data collection, In: Activity Coefficients Pitzer, K. S. (1995) Thermodynamics. Third Edition. Series in Advanced Chemistry, McGraw-Hill, New York.. Pitzer, K. S. and Kim, J. J. (1974) Thermodynamics of electrolytes. IV. Activity and osmotic coefficients for mixed electrolytes. J. Am. Chem. Soc. 96, 5701–5707. Pitzer, K. S. and Mayorga, G. (1973) Thermodynamics of electrolytes. II. Activity and osmotic coefficients for strong electrolytes with one or both ions univalent. J. Phys. Chem. 77, 2300–2308. Pitzer, K. S. and Mayorga, G. (1974) Thermodynamics of electrolytes. III. Activity and osmotic coefficients for 2-2

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Aquatic Geochemistry – Springer Journals

Published: Oct 15, 2004

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