According to the chemical composition of samples collected along the Niangqu main channel (N06, N09, N14, N20, and N23), Ca 2+ and Mg 2+ show a decreasing trend from upstream to downstream.
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Chemical weathering rates and controlling mechanisms of glacial catchments within different climate regimes in the Tibetan Plateau.
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The sentences
The chemical weathering rates of the glacier areas in the YTRB show an increasing trend from upstream to downstream.