CHAPTER 12.6 FOURIER TRANSFORM INFRARED SPECTROSCOPY

dc.contributor.authorPetit S.
dc.date.accessioned2024-09-22T02:54:09Z
dc.date.available2024-09-22T02:54:09Z
dc.date.issued2006
dc.description.abstractFourier 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.identifierhttps://www.elibrary.ru/item.asp?id=17806987
dc.identifier.citationDevelopments in Clay Science, 2006, 1, C, 909-918
dc.identifier.doi10.1016/S1572-4352(05)01032-9
dc.identifier.issn1572-4352
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/45312
dc.titleCHAPTER 12.6 FOURIER TRANSFORM INFRARED SPECTROSCOPY
dc.typeСтатья

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