Инд. авторы:	Cherkashina T.Yu., Khudonogova E.V., Revenkoa A.G., Letnikova E.F.
Заглавие:	Application of the background standard method for the determination of Rb, Sr, Y, Zr, and Nb contents in phosphorites by x-ray fluorescence
Библ. ссылка:	Cherkashina T.Yu., Khudonogova E.V., Revenkoa A.G., Letnikova E.F. Application of the background standard method for the determination of Rb, Sr, Y, Zr, and Nb contents in phosphorites by x-ray fluorescence // X-ray Spectrometry. - 2009. - Vol.38. - Iss. 2. - P.144-151. - ISSN 0049-8246. - EISSN 1097-4539.
Внешние системы:	DOI: 10.1002/xrs.1122; SCOPUS: 2-s2.0-70350778486;
Реферат:	eng: The aim of the present work is to demonstrate the application of the x-ray fluorescence (XRF) technique to the determination of Rb, Sr, Y, Zr, and Nb contents in phosphorites. The effect of a chemical sample composition on fluorescence intensities of analytical lines has been taken into account using the background standard method. A novelty of the work is the detailed study of a background to choose the background position, free from the spectral line overlaps of the elements presented in the sample. The most suitable background position is the position at the angle 2Θ = 29{ring operator} whenusing the analyzing crystal LiF(200). Duringour investigationwefaced a problemof choice of Certified Reference Materials (CRMs) for the calibration of the phosphorites. To estimate interelement effects and to choose CRMs for the calibration the intensities were theoretically calculated. The statistical processing of analytical results of the technique is carried out. This technique may be applied to the determination of Rb, Sr, Y, Zr, and Nb contents in the phosphorites. Also, the possibility has been demonstrated to use the XRF technique for geochemical investigations of rocks. Phosphorites of Bokson-Khubsugul Basin were selected as an example. As a result of the investigation the genetic type of phosphorites was established, which corresponded to the present geodynamical depositional environment. The character of the distribution of Rb, Sr, Y, Zr, and Nb contents in the phosphorites was also studied. Copyright © 2008 John Wiley & Sons, Ltd.
Издано:	2009
Физ. характеристика:	с.144-151