Abstract
Cation exchange reactions with participation of heavy metals Mn, Co, Ni, Cu, Zn, Cd, Ba, and Pb were studed in oceanic low-temperature hydrothermal deposits of various mineral compositions and in hydrogenic Fe-Mn crusts. Individual minerals and their assemblages differ significantly in absorptive capacity, which increases in the following order: hematite ≪ Si-protoferrihydrite < protoferrihydrite < geothite < nontronite ≪ Fe-vernadite + Mn-feroxyhyte < Fe-free vernadite < bernessite + Fe-free vernadite < bernessite; i.e., it successively increases from the mineral with a coordination type of lattice to minerals with a layer-type structure. The exchange complex of all minerals includes Na+, K+, Ca2+, and Mg2+, i.e., the main cations of seawater. In Mn minerals, Mn2+ is the main exchange component. The contribution of all the mentioned cations to the exchange capacity of minerals is as high as 90–98%. The highest absorptive capacity among the examined low-temperature oceanic deposits is characteristic of hydrothermal Mn minerals. Their capacity exceeds substantially that of hydrothermal oxides, hydroxides, Fe-aluminosilicates, and hydrogenic Fe-Mn minerals. The absorptive capacity of all examined Mn minerals relative to heavy metals increases in the same order: Ni < Zn < Cd < Mn < Co < Pb < Cu.
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Original Russian Text © G.V. Novikov, I.V. Vikent’ev, O.Yu. Bogdanova, 2006, published in Geologiya Rudnykh Mestorozhdenii, 2006, Vol. 48, No. 4, pp. 351–374.
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Novikov, G.V., Vikent’ev, I.V. & Bogdanova, O.Y. Sorption of heavy metal cations by low-temperature deposits of Pacific hydrothermal fields. Geol. Ore Deposits 48, 304–325 (2006). https://doi.org/10.1134/S1075701506040052
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DOI: https://doi.org/10.1134/S1075701506040052