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Published in J Environ Qual 4:515-519 (1975)
© 1975 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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The Time Stability of Dissolved Mercury in Water Samples-II. Chemical Stabilization1

Peter Avotins and E. A. Jenne2

ABSTRACT

Bacteria were found to be the principal cause of instability of mercury in laboratory solutions. The volatilization loss rate increased rapidly after a variable lag period and then leveled off with increasing time. The marked reduction in the loss rate of mercury is a result of its combination with bacterial cells and metabolites. Reagents which either oxidize or solubilize organics removed mercury most effectively from sample containers in which mercury-bearing water had been stored. A small amount of mercury was found to have diffused into the polyethylene bottles. Solute mercury was most effectively stabilized in laboratory solutions and water samples with 0.05% KMnO4 without acidification.

Key Words: volatilization • sample preservation • organic forms • acids • oxidizing agents • bacteria • Pseudomonas sp. • Flavobacterium sp.


NOTES

1 Publication authorized by the Director, Geological Survey, U. S. Dep. of the Interior.

2 Soil Scientist and former Chemist, respectively, Water Resour. Div., U. S. Dep. of the Interior, Menlo Park, CA 94025.

Received for publication January 27, 1975.





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Copyright © 1975 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.