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Mineral compositions and sources of the riverbed sediment in the desert channel of Yellow River

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Abstract

The Yellow River flows through an extensive, aeolian desert area and extends from Xiaheyan, Ningxia Province, to Toudaoguai, Inner Mongolia Province, with a total length of 1,000 km. Due to the construction and operation of large reservoirs in the upstream of the Yellow River, most water and sediment from upstream were stored in these reservoirs, which leads to the declining flow in the desert channel that has no capability to scour large amount of input of desert sands from the desert regions. By analyzing and comparing the spatial distribution of weight percent of mineral compositions between sediment sources and riverbed sediment of the main tributaries and the desert channel of the Yellow River, we concluded that the coarse sediment deposited in the desert channel of the Yellow River were mostly controlled by the local sediment sources. The analyzed results of the Quartz-Feldspar-Mica (QFM) triangular diagram and the R-factor models of the coarse sediment in the Gansu reach and the desert channel of the Yellow River further confirm that the Ningxia Hedong desert and the Inner Mongolian Wulanbuhe and Kubuqi deserts are the main provenances of the coarse sediment in the desert channel of the Yellow River. Due to the higher fluidity of the fine sediment, they are mainly contributed by the local sediment sources and the tributaries that originated from the loess area of the upper reach of the Yellow River.

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Authors and Affiliations

  1. Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Donggang West Road 260, Lanzhou, Gansu Province, 730000, People’s Republic of China

    Xiaopeng Jia & Haibing Wang

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  1. Xiaopeng Jia
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  2. Haibing Wang
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Correspondence to Xiaopeng Jia.

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Jia, X., Wang, H. Mineral compositions and sources of the riverbed sediment in the desert channel of Yellow River. Environ Monit Assess 173, 969–983 (2011). https://doi.org/10.1007/s10661-010-1438-z

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  • DOI: https://doi.org/10.1007/s10661-010-1438-z

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