Show simple item record

dc.contributor.author Petit S.
dc.date.accessioned 2024-09-22T02:54:09Z
dc.date.available 2024-09-22T02:54:09Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=17806987
dc.identifier.citation Developments in Clay Science, 2006, 1, C, 909-918
dc.identifier.issn 1572-4352
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/45312
dc.description.abstract Fourier transform infrared (FTIR) spectroscopy is a rapid, economical, easy, and non-destructive technique. The IR spectrum of a clay mineral is sensitive to its chemical composition, isomorphous substitution, layer stacking order, or structural modifications. This makes FTIR spectroscopy the most informative single technique not only for clay mineral composition and structure but also for interactions of the clay minerals with inorganic or organic compounds. After a brief presentation of the principles of the technique, the chapter gives an overview of the potential of FTIR for mineralogical identification of clay minerals samples, and for studying reactions with water and organic molecules. This chapter includes data from all three infrared regions, that is, far, middle, and near.
dc.title CHAPTER 12.6 FOURIER TRANSFORM INFRARED SPECTROSCOPY
dc.type Статья
dc.identifier.doi 10.1016/S1572-4352(05)01032-9


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