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Natural ferromanganese sediments

Natural ferromanganese sediments are, of course, mixtures of several mineral phases, including a significant proportion of Fe oxyhydroxides. Therefore, it is possible that adsorption to manganese oxides is not the only way in which Mo is incorporated in oxic sediments. Koschinsky and Hein [28] conducted sequential leaching experiments to determine whether various metals are primarily associated with Mn or with Fe oxyhydroxide phases in ferromanganese cmsts and nodules. [Pg.326]

Nielsen SG, Rehkamper M, Norman MD, HaUiday AN, Harrison D (2006) Thallium isotopic evidence for ferromanganese sediments in the mantle source of Hawaiian basalts. Nature 439 314-317... [Pg.261]

See other pages where Natural ferromanganese sediments is mentioned: [Pg.320]    [Pg.324]    [Pg.326]    [Pg.343]    [Pg.344]    [Pg.409]    [Pg.3487]    [Pg.1994]   
See also in sourсe #XX -- [ Pg.326 ]



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Ferromanganese

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