CHAPTER 12.3 X-RAY ABSORPTION SPECTROSCOPY
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dc.contributor.author | Gates W.P. | |
dc.date.accessioned | 2024-09-22T02:54:11Z | |
dc.date.available | 2024-09-22T02:54:11Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=17811219 | |
dc.identifier.citation | Developments in Clay Science, 2006, 1, C, 789-864 | |
dc.identifier.issn | 1572-4352 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/45320 | |
dc.description.abstract | This chapter describes X-ray absorption spectroscopy (XAS). XAS corresponds to a range of X-ray spectroscopic techniques based on scattering, absorption, and emission (fluorescence, auger) of X-rays by matter. Synchrotron-based X-ray sources produce an intense X-ray emission with total fluxes and flux densities several orders of magnitude greater than conventional X-ray tubes. As a result, a nearly flat spectral distribution is produced over a large range of mineralogically important elements. This and recent advances in X-ray optics, detectors, insertion, and focusing devices as well as modeling of scattering processes made XAS a valuable tool for obtaining atomic-level information not previously attainable by conventional X-ray sources. The chapter reviews synchrotron-based studies of clays and clay minerals, focusing on the application of XAS to elucidating the structure and reactivity of 2:1 phyllosilicates, with particular emphasis on smectites. | |
dc.title | CHAPTER 12.3 X-RAY ABSORPTION SPECTROSCOPY | |
dc.type | Статья | |
dc.identifier.doi | 10.1016/S1572-4352(05)01029-9 |
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