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dc.contributor.authorAndermann, Georgeen_US
dc.contributor.authorFujiwara, Francisen_US
dc.contributor.authorWorman, Jamesen_US
dc.contributor.authorOlson, Edwinen_US
dc.date.accessioned2006-07-19T19:53:26Zen_US
dc.date.available2006-07-19T19:53:26Zen_US
dc.date.issued1987-07en_US
dc.identifier.citationFuel 66N7 (1987) 932-934en_US
dc.identifier.issn0016-2361en_US
dc.identifier.urihttp://hdl.handle.net/1850/2210en_US
dc.description.abstractThe high resolution oxygen (O-K) and carbon (C-K) X-ray fluorescence spectra of coals were taken on a 5 metre grating X-ray spectrometer. A comparison of the C-K spectra of a North Dakota lignite (Beulah) and a Utah bituminous coal (Deer Creek) established that more diverse π-bond character was present in the lignite which is consistent with the large oxygen to carbon π-bonding component in the latter. The intensities of the oxygen K emissions on three coal samples gave excellent correlation to the per cent oxygen on a moisture free basis as determined by indirect methods and offers a potentially easy direct method for the determination of oxygen.en_US
dc.format.extent37365 bytesen_US
dc.format.mimetypeapplication/pdfen_US
dc.language.isoen_USen_US
dc.publisherElsevier: Fuelen_US
dc.titleHigh resolution X-ray fluorescence spectroscopy : A potentially useful technique for chemical bonding studies in fossil fuelsen_US
dc.typeAbstracten_US
dc.subject.keywordChemical bondingen_US
dc.subject.keywordFossil fuelsen_US
dc.subject.keywordXFSen_US
dc.identifier.urlhttp://dx.doi.org/10.1016/0016-2361(87)90332-2


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