Nature © Macmillan Publishers Ltd. Geology: Neobium solutionAs the Earth's core separated from the mantle, elements were distributed according to their affinities for the metallic core and the silicate mantle. Hence the mystery of Earth's 'missing' niobium. Niobium, the thinking went, is a 'lithophile' (or 'rock-loving') element and so should be present in the mantle in proportions, relative to the other elements, similar to those seen in the stony meteorites that record the make up of the early Solar System. The fact that there is less niobium in the crust and upper mantle than expected led to the suggestion that there were niobium-rich reservoirs hidden deeper in the mantle. But a new look at niobium's properties reveals that at high pressure it partitions between liquid metal and silicate in just the same way as the siderophile (iron-loving) element vanadium. So the niobium may have been in the core all along.
4 January 2001 table of contents
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