Dynamic Changes of Sediment Discharge and the Influencing Factors in the Yellow River, China, for the Recent 90 Years
Mu, Xingmin2,3; Zhang, Xiuqin2; Shao, Hongbo1,4; Gao, Peng2,3; Wang, Fei2,3; Jiao, Juying2,3; Zhu, Jingliang3
刊名CLEAN-SOIL AIR WATER
2012-03-01
卷号40期号:3页码:303-309
关键词Anomaly Accumulation Method Double Mass Curve Human Activities Rainfall Water Quality
ISSN号1863-0650
通讯作者Shao, HB (reprint author), Qingdao Univ Sci & Technol, Inst Life Sci, Qingdao 266042, Peoples R China. shaohongbochu@126.com
产权排序[Shao, Hongbo] Qingdao Univ Sci & Technol, Inst Life Sci, Qingdao 266042, Peoples R China; [Mu, Xingmin; Zhang, Xiuqin; Gao, Peng; Wang, Fei; Jiao, Juying] NW A&F Univ, Yangling, Shaanxi Provinc, Peoples R China; [Mu, Xingmin; Gao, Peng; Wang, Fei; Jiao, Juying; Zhu, Jingliang] Chinese Acad Sci, Inst Soil & Water Conservat, Yangling, Shaanxi Provinc, Peoples R China; [Shao, Hongbo] Chinese Acad Sci, CAS Shandong Prov Key Lab Coastal Environm Proc, Yantai Inst Costal Zone Res, Yantai, Peoples R China
文献子类Article
英文摘要The dynamic changes in the sediment discharge over 90 years from 1919 to 2008 in the Yellow River in China were assessed on the basis of annual rainfall series and annual sediment series in Shan County hydrological station. The key factors affecting sediment discharge, such as rainfall, and human activities were studied. Anomaly accumulation method and double mass curve were employed to test the stage changes of sediment discharge, and to determine the main factors of sediment decline. Results showed that the annual average sediment discharge under natural conditions was about 16 x 10(8) t, but the measured annual average sediment during 1919-2008 was 12.71 x 10(8) t. The highest annual average during the study period was 39.10 x 10(8) t in 1933 while the lowest was 1.77 x 10(8) t in 2008. Sediment discharge in the Yellow River experienced two low sediment stages (1924-1931 and 1979-2008) and a high sediment stage (1932-1971), respectively. Since 1979, there was a significant decreasing trend in the sediment discharge, and the main influencing factor was fierce human activities. Annual average sediment discharge in the post-development period (1979-2008) was 69.7% lower than that in the pre-development period (1919-1978), with average reduction of 81 and 19% caused by human activities and rainfall, respectively. These results provide important evidence for making protecting policy for water resources quality and environmental safety of the Yellow River.; The dynamic changes in the sediment discharge over 90 years from 1919 to 2008 in the Yellow River in China were assessed on the basis of annual rainfall series and annual sediment series in Shan County hydrological station. The key factors affecting sediment discharge, such as rainfall, and human activities were studied. Anomaly accumulation method and double mass curve were employed to test the stage changes of sediment discharge, and to determine the main factors of sediment decline. Results showed that the annual average sediment discharge under natural conditions was about 16 x 10(8) t, but the measured annual average sediment during 1919-2008 was 12.71 x 10(8) t. The highest annual average during the study period was 39.10 x 10(8) t in 1933 while the lowest was 1.77 x 10(8) t in 2008. Sediment discharge in the Yellow River experienced two low sediment stages (1924-1931 and 1979-2008) and a high sediment stage (1932-1971), respectively. Since 1979, there was a significant decreasing trend in the sediment discharge, and the main influencing factor was fierce human activities. Annual average sediment discharge in the post-development period (1979-2008) was 69.7% lower than that in the pre-development period (1919-1978), with average reduction of 81 and 19% caused by human activities and rainfall, respectively. These results provide important evidence for making protecting policy for water resources quality and environmental safety of the Yellow River.
学科主题Environmental Sciences & Ecology ; Marine & Freshwater Biology ; Water Resources
URL标识查看原文
WOS关键词QUALITY ; IMPACTS
WOS研究方向Environmental Sciences & Ecology ; Marine & Freshwater Biology ; Water Resources
语种英语
WOS记录号WOS:000300972600014
资助机构Chinese Academy of Sciences[KZCX2-XB2-05-03]; 973 Plan of China[2007CB407203]
公开日期2012-06-13
内容类型期刊论文
源URL[http://ir.yic.ac.cn/handle/133337/5464]  
专题烟台海岸带研究所_滨海湿地实验室
作者单位1.Qingdao Univ Sci & Technol, Inst Life Sci, Qingdao 266042, Peoples R China
2.NW A&F Univ, Yangling, Shaanxi Provinc, Peoples R China
3.Chinese Acad Sci, Inst Soil & Water Conservat, Yangling, Shaanxi Provinc, Peoples R China
4.Chinese Acad Sci, CAS Shandong Prov Key Lab Coastal Environm Proc, Yantai Inst Costal Zone Res, Yantai, Peoples R China
推荐引用方式
GB/T 7714
Mu, Xingmin,Zhang, Xiuqin,Shao, Hongbo,et al. Dynamic Changes of Sediment Discharge and the Influencing Factors in the Yellow River, China, for the Recent 90 Years[J]. CLEAN-SOIL AIR WATER,2012,40(3):303-309.
APA Mu, Xingmin.,Zhang, Xiuqin.,Shao, Hongbo.,Gao, Peng.,Wang, Fei.,...&Zhu, Jingliang.(2012).Dynamic Changes of Sediment Discharge and the Influencing Factors in the Yellow River, China, for the Recent 90 Years.CLEAN-SOIL AIR WATER,40(3),303-309.
MLA Mu, Xingmin,et al."Dynamic Changes of Sediment Discharge and the Influencing Factors in the Yellow River, China, for the Recent 90 Years".CLEAN-SOIL AIR WATER 40.3(2012):303-309.
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