NiK-edge EXAFS and XANES and optical absorption spectroscopy experiments have been performed on a CaNiSi2O6 glass. The data are consistent with the presence of [5]Ni in a trigonal bipyramidal symmetry site, a previously unknown surrounding. Minor amounts of [4]Ni are also present. This environment explains why the Ni-O distances derived from EXAFS in the glass are shorter than in the crystalline equivalent and provides a rationale for the high olivine/liquid partition coefficients of Ni that govern its preferential location in mafic and ultramafic rocks.

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