Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-23T15:34:16.484Z Has data issue: false hasContentIssue false

Influence of Citric Acid and Glycine on the Adsorption of Mercury (II) by Kaolinite under Various pH Conditions

Published online by Cambridge University Press:  28 February 2024

J. Singh
Affiliation:
Department of Soil Science, University of Saskatchewan, Saskatoon, Saskatchewan, S7N 5A8
P. M. Huang
Affiliation:
Department of Soil Science, University of Saskatchewan, Saskatoon, Saskatchewan, S7N 5A8
U. T. Hammer
Affiliation:
Department of Biology, University of Saskatchewan, Saskatoon, Saskatchewan, S7N 5E2
W. K. Liaw
Affiliation:
Saskatchewan Fisheries Laboratory, Department of Parks and Renewable Resources, Saskatoon Saskatchewan, S7N 2X8, Canada
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

This investigation was carried out to study the effect of different concentrations of citric acid and glycine, which are common in freshwaters, on the kinetics of the adsorption of Hg by kaolinite under various pH conditions. The data indicate that Hg adsorption by kaolinite at different concentrations of citric acid and glycine obeyed multiple first order kinetics. In the absence of the organic acids, the rate constants of the initial fast process were 46 to 75 times faster than those of the slow adsorption process in the pH range of 4.00 to 8.00. Citric acid had a significant retarding effect on both the fast and slow adsorption process at pHs of 6.0 and 8.0. It had a significant promoting effect on the fast and slow adsorption process at pH 4.00. Glycine had a pronounced enhancing effect on the rate of Hg adsorption by kaolinite during the fast process. The rise in pH of the system further increased the effect of glycine on Hg adsorption. The magnitude of the retarding/promoting effect upon the rate of Hg adsorption was evidently dependent upon the pH, structure and functionality of organic acids, and molar ratio of the organic acid/Hg. The data obtained suggest that low-molecular-weight organic acids merit close attention in studying the kinetics and mechanisms of the binding of Hg by sediment particulates and the subsequent food chain contamination.

Type
Research Article
Copyright
Copyright © 1996, The Clay Minerals Society

References

Davis, J.A. and Leckie, J.O.. 1978. Effect of adsorbed complexing ligands on trace metal uptake by hydrous oxides. Environ Sci Technol 12: 13091315.CrossRefGoogle Scholar
Fox, T.R. and Comerford, N.B.. 1990. Low-molecular weight organic acids in selected forest soils of southeastern USA. Soil Sci Soc Am J 54: 11391144.CrossRefGoogle Scholar
Gardner, L.R.. 1974. Organic vs inorganic metal complexes in sulfide marine waters. Speculative calculations based on available stability constants. Geochim Cosmochim Acta 38: 12971302.CrossRefGoogle Scholar
Genrich, D.A. and Bremner, J.M.. 1972. A reevaluation of ultrasonic-vibration method of dispersing soils. Soil Sci Soc Am Proc 38: 944947.CrossRefGoogle Scholar
Gjessing, E.T.. 1976. Physical and Chemical Characteristics of Aquatic Humus. Ann Arbor, Michigan: Ann Arbor Science Publ. 120p.Google Scholar
Grim, R.E.. 1968. Clay Mineralogy, 2nd Edition. New York, N.Y.: McGraw-Hill Publ. Co. 596p.Google Scholar
Jackson, M.L.. 1979. Soil Chemical Analysis—Advanced Course. Madison, Wisconsin: Published by the author, University of Wisconsin. 895p.Google Scholar
Johanssen, G.. 1971. On the structures of the hydrolysis complexes of mercury (II) in the solution. Acta Chem Scand 25: 27992806.CrossRefGoogle Scholar
Kudo, A., Miller, D.R. and Townsend, D.R.. 1977. Mercury transport interacting with bed sediment movements. Progr Water Technol 9: 923935.Google Scholar
Lehninger, A.L.. 1980. Biochemistry. New York.Worth Pub. Inc. 1104 p.Google Scholar
Lindberg, S.E., Andren, A.W. and Harriss, R.C.. 1975. Geochemistry of mercury in the estuarine environment. Estuarine Res 1: 6497.Google Scholar
Lindqvist, O.. 1991a. Mercury in the Swedish Environment. Water Air and Soil Pollution 55 (Special Issue). Dordrecht: Kluwer Academic Publishers. 261p.Google Scholar
Lindqvist, O.. 1991b. Mercury as Environmental Pollutant. Water Air and Soil Pollution 56 (Special Issue). Dordrecht: Kluwer Academic Publishers. 365p.Google Scholar
Martell, A.E. and Smith, R.M.. 1979. Critical Stability Constants. Vol. 4. New York: Plenum Press. 394p.Google Scholar
Moore, J.W. and Ramamoorthy, S.. 1984. Heavy Metals in Natural Waters. New York: Springer-Verlag. 268p.CrossRefGoogle Scholar
Mortland, M.M.. 1986. Mechanisms of adsorption of nonhumic organic species by clays. In: Huang, P.M., Schnitzer, M., editors. Interactions of Soil Minerals with Natural Organics and Microbes. SSSA Special Publication No. 17. Madison, WI: Soil Sci Soc Am. 5976.Google Scholar
Newton, D.W. and Ellis, R.. 1974. Loss of mercury (II) from solution. J Environ Qual 3: 2023.CrossRefGoogle Scholar
Oscarson, D.W., Rogers, J.S., Huang, P.M. and Liaw, W.K.. 1981. The nature of selected prairie lake and stream sediments. Int Rev Ges Hydrobiol 66: 95107.CrossRefGoogle Scholar
Parker, D.R., Zelazny, L.W. and Kinaraide, T.B.. 1987. Improvements to the program “GEOCHEM”. Soil Sci Soc Am J 51: 488491.CrossRefGoogle Scholar
Ramamoorthy, S. and Kushner, D.J.. 1975. Mercury metal binding sites in river water. Nature 256: 399401.CrossRefGoogle Scholar
Ramamoorthy, S. and Rust, B.R.. 1976. Mercury sorption and desorption characteristics of some Ottawa river sediments. Can J Earth Sci 13: 530536.CrossRefGoogle Scholar
Reeder, S.W., Demayo, A. and Taylor, M.C.. 1979. Guidelines for Surface Water Quality, 1. Mercury. Ottawa: Inland Water Directorate. 116.Google Scholar
Reid, R.S. and Podanyi, B.. 1988. A proton NMR study of the glycine-mercury(II) system in aqueous solution. J Inorg Biochem 32: 183195.CrossRefGoogle ScholarPubMed
Rogers, J.S., Huang, P.M. and Hammer, U.T.. 1984. Dynamics of desorption of mercury adsorbed on poorly crystalline oxides of manganese, iron, aluminium and silicon. Verh Int Verein Limnol 22: 283288.Google Scholar
Solomons, W. and Forstner, U.. 1984. Metals in the Hydrocycle. New York: Springer-Verlag. 349p.CrossRefGoogle Scholar
Sposito, G. and Mattigod, S.V.. 1979. GEOCHEM: A Computer Program for the Calculations of Chemical Equilibria in Soil Solution and Other Natural Water System. Riverside, CA: University of California.Google Scholar
Stevenson, F.J. and Fitch, A.. 1986. Chemistry of complexation of metal ions with soil solution organics. In: Huang, P.M., Schnitzer, M., editors. Interactions of Soil Minerals with Natural Organics and Microbes. SSSA Special Publication No. 17. Madison, WI: Soil Sci Soc Am. 2958.Google Scholar
Stumm, W.. 1987. Aquatic Surface Chemistry. New York: John Wiley & Sons. 780p.Google Scholar
Stumm, W. and Morgan, J.J.. 1981. Aquatic Chemistry. New York: Wiley. 781 p.Google Scholar
U.S. Environmental Protection Agency. 1974. Method of Chemical Analysis of Water and Waste. Office of Technol. Transfer, EPA-62576-74-003, Washington, D.C.Google Scholar
Wang, J.S., Huang, P.M., Hammer, U.T. and Liaw, W.K.. 1985. Influence of chloride on kinetics of the adsorption of mercury (II) by poorly crystalline Al, Fe, Mn, and Si oxides. Water Poll Res J Can 20: 6874.CrossRefGoogle Scholar
Wang, J.S., Huang, P.M., Liaw, W.K. and Hammer, U.T.. 1991. Kinetics of the desorption of mercury from selected freshwater sediments as influenced by chloride. Water, Air Soil Poll 56: 533542.CrossRefGoogle Scholar