Plutonium speciation in water from Mono Lake, California

J.M. Cleveland; T.F. Rees; K.L. Nash

doi:10.1126/science.222.4630.1323

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Plutonium speciation in water from Mono Lake, California

J.M. Cleveland·T.F. Rees·K.L. Nash

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Abstract

The solubility of plutonium in Mono Lake water is enhanced by the presence of large concentrations of indigenous carbonate ions and moderate concentrations of fluoride ions. In spite of the complex chemical composition of this water, only a few ions govern the behavior of plutonium, as demonstrated by the fact that it was possible to duplicate plutonium speciation in a synthetic water containing only the principal components of Mono Lake water.

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Source-reported bounding extent: 37.894106221864334° to 38.11956391803898° latitude; -119.23547883490315° to -118.82146949863339° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeX RIS

J.M. Cleveland, T.F. Rees, K.L. Nash. 1983. Plutonium speciation in water from Mono Lake, California. https://doi.org/10.1126/science.222.4630.1323

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