Author/Authors :
Zolotarev، نويسنده , , K.V. and Goldberg، نويسنده , , E.L. and Kondratyev، نويسنده , , V.I and Kulipanov، نويسنده , , G.N. and Miginsky، نويسنده , , E.G. and Tsukanov، نويسنده , , V.M. and Phedorin، نويسنده , , M.A. and Kolmogorov، نويسنده , , Yu.P.، نويسنده ,
Abstract :
The XRF beamline at the VEPP-3 (Budker INP, Novosibirsk, Russia) storage ring was modified for the performance of scanning analysis. A description and parameters of this facility are presented in the current paper. The initial results of testing of scanning analysis of bottom sediments from Lake Baikal are also presented. A spatial resolution of the scanning analysis is 0.1–1 mm which corresponds to 2–50 years of resolution. Such a scanning analysis of lake sediments provides high quality data as a requirement for paleoclimate reconstructions.
Keywords :
Microscanning , Trace elements , paleoclimate , SR-XRF , LAKE BAIKAL
