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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