Influence of soil and water conservation measures on reducing in frequency of hyperconcentrated flows in the Wudinghe River basin
Xu J.
2011
关键词Hyperconcentrated flows Soil and water conservation Sand-dust storm Wudinghe River Loess Plateau of China loess plateau yellow-river china erosion example mountain
英文摘要Based on data of SSC, precipitation, sand-dust storms and area of soil and water conservation, a study has been made of the temporal variation in the frequency of hyperconcentrated flows in the Wudinghe River, a major tributary of the Yellow River, China. The results showed that the decreasing trend in the frequency of hyperconcentrated flows (F (h)) was significant. High-flow season precipitation (P (6-9)) decreased slightly, and annual number of sand-dust storm days (D (ss)) decreased markedly. Correlation analysis shows that the variation in P (6-9) had little influence on the decreasing F (h), but the decreasing D (ss) had significant influence on the decreasing F (h). The 5-year moving average of the frequency of hyperconcentrated flows (F (h,5m)) was closely correlated with the area of land terracing, the area of the land created by check dams, the area of tree planting and the area of grass planting. The results of the present study show that the frequency of hyperconcentrated flows can be significantly reduced by soil and water conservation measures. Thus, these results may be useful for decision making for the management of sediment-related disasters in the Wudinghe River basin and in the Yellow River basin.
出处Environmental Earth Sciences
62
7
1513-1520
收录类别SCI
语种英语
ISSN号1866-6280
内容类型SCI/SSCI论文
源URL[http://ir.igsnrr.ac.cn/handle/311030/22713]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Xu J.. Influence of soil and water conservation measures on reducing in frequency of hyperconcentrated flows in the Wudinghe River basin. 2011.
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