Uptake of elements from seawater by ferromanganese crusts: solid-phase associations and seawater speciation
Marine Fe–Mn oxyhydroxide crusts form by precipitation of dissolved components from seawater. Three hydrogenetic crust samples (one phosphatized) and two hydrothermal Mn-oxide samples were subjected to a sequential-leaching procedure in order to determine the host phases of 40 elements. Those host-p...
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Published in | Marine geology Vol. 198; no. 3; pp. 331 - 351 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
15.07.2003
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Subjects | |
Online Access | Get full text |
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