Show simple item record

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


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record