Direct observation of tetravalent cerium in ferromanganese nodules and crusts by X-ray-absorption near-edge structure (XANES)

X-ray-absorption near-edge structure (XANES) was successfully applied for t he diner determination of Ce valence in hydrogenetic ferromanganese nodules (two samples) and crust tone sample). Rare earth element (REE) patterns of the hydrogenetic ferromanganese nodules and crust recovered from the Pacif ic Ocean show large positive Ce anomalies, especially when normalized to se awater. Despite some disadvantages in the spectroscopic analysis of Ce in n atural samples (e.g., low concentration and interference from other element s), intense synchrotron radiation and measurement of fluorescent XANES with semiconductor detectors having high energy resolution enabled us to detect XANES at Ce L-III edge in the ferromanganese nodule or crust. In the XANES spectra of the nodule or crust, large double peaks were observed, showing that the oxidation state of Ce in the nodule or crust is predominantly tetr avalent with little contribution from Ce(III). This is the first in-situ qu antitative analysis of Ce(IV) among total Ce in natural samples as a trace element as far as we know. The results obtained by XANES seem to be consist ent with the percentage of Ce(IV) estimated from seawater-normalized REE pa tterns, suggesting that seawater is a precursor of REE in the marine deposi ts. The present results also confirm that Ce enrichment relative to other R EEs in hydrogenetic ferromanganese deposits is due to oxidative removal of Ce from seawater to the ferromanganese nodules and crust in the marine envi ronment. Comparison of XANES spectra of Ce sorbed on synthetic manganese ox ide and CeO2 vs. those of the ferromanganese nodules and crust suggests tha t the initial reaction of Ce with the ferromanganese nodules and crust is t he sorption of dissolved Ce(III) to the manganese oxide surface. Copyright (C) 2000 Elsevier Science Ltd.