Unoccupied states of pyrite probed by electron energy-loss spectroscopy (EELS)

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11 Scopus citations


Electron energy-loss spectra (EELS) of pyrite (FeS2) were acquired and include the Fe K, L2.3, M2.3, and M1 edges, and the S K, L2.3, and L1 edges. The core-loss edges exhibit a range of shapes and different theories are required to understand the spectra. In the process a clear picture of the conduction-band states as a function of energy above the band gap is obtained. This analysis reveals the extent of mixing of unoccupied states and thus provides an understanding of the limits of interpreting core-loss edges in light of the optical dipole limit. A unified picture of the unoccupied states is obtained by aligning the spectra on a common energy scale relative to the published Bremsstrahlung isochromat spectrum (BIS) and with the results of band structure calculations. This alignment allows similarities between the spectra of different atoms to be related to mixing of local conduction-band states. The coincidence of the Fe K and S L2.3 spectral features attests to the strong hybridization of the Fe p-S 3d states. The main Fe L2.3 edges are followed by structures that confirm an Fe-S bond with a substantial degree of mixing between Fe d6 and d7 states. The aligned EELS spectra clearly divide the unoccupied states into two regions. The first region is dominated by the intense d-like component of the Fe L3 edge and p-like components of the S K and L1 edges. A small pre-peak at the Fe K edge aligned with the Fe L2.3 edge peak maximum is indicative of Fe 4p + 3d eg and S 3p mixing. Similarly, the pre-peak to the S L2.3 edge arises from transitions to states with mixed S s + p + Fe 3d eg character.

Original languageEnglish (US)
Pages (from-to)485-491
Number of pages7
JournalAmerican Mineralogist
Issue number4
StatePublished - Apr 2004

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology


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