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Hydration Structure of Exchangeable Cu2+ in Vermiculite and Smectite

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Clays and Clay Minerals

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  1. Department of Agronomy, Cornell University, Ithaca, NY, 14853, U.S.A.

    Murray McBride

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  1. Murray McBride
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McBride, M. Hydration Structure of Exchangeable Cu2+ in Vermiculite and Smectite. Clays Clay Miner. 24, 211–212 (1976). https://doi.org/10.1346/CCMN.1976.0240410

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  • DOI: https://doi.org/10.1346/CCMN.1976.0240410

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