The following is an abstract for the selected article. A PDF download of the full text of this article is available here. Members may download full texts at no charge. Non-members may be charged a small fee for certain articles.
Application of Electron Emission Spectroscopy to Characterize Sulfur Bonds in Coal
Volume 27, Number 5 (Oct. 1973) Page 347-351
Schultz, Harry D.; Proctor, W.G.
Electron binding energies of minerals typically found in coal were measured by the induced electron emission method. The shift in binding energies for Fe and S atoms were correlated with different chemical environments. The iron 2p3/2 electron in pyrrhotite (Fe1-xS) is bound by 3.8 eV more than the Fe 2p3/2 electron in pyrite (FeS2), whereas the 2p sulfur electron is shifted by 0.8 eV. Chemical shift data for minerals and organic sulfides were determined and correlated with structure variations. Subsequently, multiple sulfur signals observed on raw coals were correlated with this IEE data. Thus, we have demonstrated that the modes of occurrence of sulfur (pyritic, sulfate, organic) can be determined on raw coal; this represents the first spectroscopic technique capable of performing this characterization.