Abstract
IN work on the determination of trace elements in silicate rocks1, an attempt has been made to solve the inherent difficulties of achieving a rapid and efficient dissolution of large samples (up to 200 gm.) of silicate rocks and at the same time ensuring that the minimum quantities of reagents are used.
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References
Brooks, R. R., Ahrens, L. H., and Taylor, S. R., Geochim. et Cosmochim. Acta, 18, 3 (1960).
Edge, R. A., and Ahrens, L. H., (in the press).
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BROOKS, R. Dissolution of Silicate Rocks. Nature 185, 837–838 (1960). https://doi.org/10.1038/185837b0
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DOI: https://doi.org/10.1038/185837b0
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