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• W125958498 abstract "River water major element chemistry and isotopic ratios are generally controlled by mixtures of waters with differing end-member compositions such as surface runoff, groundwater and rain water. The compositions of such end-members are either inherited from heterogeneity in the original lithological sources (e.g. carbonate, silicate) or from process-related fractionation of elemental or isotopic ratios during weathering. Distinguishing process-related variations from lithological mixing trends is a problem fundamental to partitioning weathering fluxes between different sources, and understanding the underlying mechanisms that control chemical weathering. In many studies, distinguishing chemical signatures in river waters related to lithology from those related to weathering processes is complex because of heterogeneous lithology in most catchments." @default.
• W125958498 created "2016-06-24" @default.
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• W125958498 date "2010-05-01" @default.
• W125958498 modified "2023-09-23" @default.
• W125958498 title "Weathering processes revealed by seasonal variations in stable isotope ratios in rivers: The example of Mg" @default.
• W125958498 hasPublicationYear "2010" @default.
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