摘要
Through the analysis of macro- and micro-elements and their variations with XRF at the CCY loess-soil site, Ningxia, the authors obtain a number of geochemical parameters. There is a comparison between these chemical parameters and magnetic susceptibility, frequency dependent susceptibility, which indicates that during the paleosol formation, the climate was warm and humid with abundant precipitation and greater eluviation, while during the loess accumulation, the climate was relatively cold and arid with weak pedogenesis. The variation of elements can indirectly reflect the change of climate and pedogenic environment during the process of loess chemical weathering.