Va. Trounova et al., SYNCHROTRON-RADIATION X-RAY FLUORESENCE STUDY OF THE COMPOSITIONAL HOMOGENEITY OF A SEDIMENT CORE FROM LAKE-BAIKAL, X-ray spectrometry, 25(2), 1996, pp. 55-59
The first 100 m core-drill sample which was obtained by drilling from
a boat frozen in the ice of Lake Baikal (BDP-93-1) was quantitatively
investigated by synchrotron radiation XRF to investigate the trace ele
ment contents. The ability to change the energy of the exciting monoch
romatic beam and the high intensity of the radiation allow the investi
gations to be performed with detection limits of 1-2 ppm for groups of
geochemically important elements, Rb-Nb, Ba-Nd, and for milligram sam
ples. The results showed geochemical inhomogeneity in the 61-65 m rang
e of the core-drill, characterized by higher ratios of Sr to Rb, Sr to
Y and Sr to Ce compared with other sections of the core.