| Analysis of the Sediment Development and Trend In Jinshajiang River Drainage Area |
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| 作者姓名： | HUANG Chuan LOU Xiao peng LIU Yuan yuan |
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| 摘 要： | Jinshajiang River, which has a drainage area of 485,100 Km 2, average flux of 142.9 billion m 3, and soil conveyance of 247 million t/a, is the largest branch of Changjiang river. It is also the largest soil resource of the Three Gorges reservoir and upper reach of Changjiang River. To research the development and trend of Jinshajiang sediment not only has a relation to Jinshajiang water resource strategy, but also has important meaning to control the silt in Three Gorges reservoir and the Changjiang water resource development. The paper statistically analyses the flux and sediment conveyance of the Pingshan station, which is the primary hydrological station in the Jinshajiang River Drainage Area. Through several non-parameter statistical methods such as Spearman order correlativity check, Kendell order correlativity check, and linear regression check, the paper concludes that the sediment evolvement trend of Pingshan station is not distinct.
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| 关 键 词： | sediment trend analysis correlativity check |
| 修稿时间： | 2001/10/24 0:00:00 |
Analysis of the Sediment Development and Trend In Jinshajiang River Drainage Area |
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| HUANG Chuan,LOU Xiao peng,LIU Yuan yuan.Analysis of the Sediment Development and Trend In Jinshajiang River Drainage Area[J].Storage & Process,2002(1):21-23. |
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| Authors: | HUANG Chuan LOU Xiao peng LIU Yuan yuan |
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| Abstract: | Jinshajiang River, which has a drainage area of 485,100 Km 2, average flux of 142.9 billion m 3, and soil conveyance of 247 million t/a, is the largest branch of Changjiang river. It is also the largest soil resource of the Three Gorges reservoir and upper reach of Changjiang River. To research the development and trend of Jinshajiang sediment not only has a relation to Jinshajiang water resource strategy, but also has important meaning to control the silt in Three Gorges reservoir and the Changjiang water resource development. The paper statistically analyses the flux and sediment conveyance of the Pingshan station, which is the primary hydrological station in the Jinshajiang River Drainage Area. Through several non-parameter statistical methods such as Spearman order correlativity check, Kendell order correlativity check, and linear regression check, the paper concludes that the sediment evolvement trend of Pingshan station is not distinct. |
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| Keywords: | sediment trend analysis correlativity check |
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