4.7 Article

Anthropogenic impacts on the decreasing sediment loads of nine major rivers in China, 1954-2015

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 739, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.scitotenv.2020.139653

关键词

Chinese rivers; Sediment load; Human activities; Climate change; Quantitative assessment

资金

  1. National Natural Science Foundation of China [41830540, 41906069]
  2. Scientific Research Fund of the Second Institute of Oceanography, MNR [SZ2002, JG2005]

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Over the past 60 years, because of the combined impacts of human activities and climate change, the sediment load of the nine major rivers (the Yellow, Yangtze, Pearl, Songhuajiang, Liaohe, Haihe, Huaihe, Qiantangjiang, and Minjiang rivers) in China has dropped by 85%, which had caused serious environmental problems such as reservoir siltation and estuary erosion. However, quantitatively evaluating the impact of different human activities on this decline is still an unsolved and complex problem. Based on a big new data set from 27 gauge stations and 469 meteorological stations, we established five methods to assess sediment loss of China's nine major rivers. During 1954-2015, the sediment load into the marginal seas via these nine rivers was characterized by a marked decline, from 1.95 Gt/yr (1954-1968) to 1.40 Gt/yr (1969-1985), 890 Mt/yr (1986-1998), 450 Mt/yr (1999 2003), and 310 Mt/yr (2004-2015), reflecting an 85% decrease between 1954-1968 and 2004 2015. The cumulative sediment load into the marginal seas was similar to 71.0 Gt, constituting similar to 7% of the global sediment load. The Yellow River, Yangtze River, Pearl River, and other six major rivers contributed 40.9 (58%), 22.9 (32%), 4.1 (6%), and 2.96 Gt (4%), respectively. We estimate that -53.0 Gt of terrestrial sediment has been retained on the mainland China because of human activities, with reservoir trapping, water resource utilization, and water-soil conservation measures accounting for 45.5%, 29%, and 25.5% of the total, respectively. The contribution of climatic factors was assessed to be secondary. This drastic reduction in river sediment load could lead to a series of negative effects on deltas: decreased sediment delivery, coastal erosion, aggravated reaction to storm disasters, and most importantly, loss of new land for human use. In addition, the large amounts of sediment trapping by reservoirs over long periods will cause siltation that could reduce reservoir water storage capacity. (C) 2020 Elsevier B.V. All rights reserved.

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