The Capability Analysis of Flood Discharge in Ningmeng of Yellow River

Abstract:

the amount of water and sediment reduce obviously in Ning Meng reach because of the influence of the regulation of Long-Liu reservoir in upper of Yellow River、rainfall and production and living use water, especially the time reduce of large flows and the growth of small flow duration time, resulting main channel siltation and atrophy severe in the Inner Mongolia Reach, lower bankfull discharge, the main channel flooding capacity decreased when the great flood of water level rise, resulting in the increase of the river's ice flood control pressure. The study will provide technical support for flood control decision-making.

• Periodical: Applied Mechanics and Materials (Volumes 212-213)
• Pages: 705-709
• DOI: https://doi.org/10.4028/www.scientific.net/AMM.212-213.705
• Online since: October 2012
• Authors: Xin Ai Jing, Xiu Zhi Lin, Su Zhen Hou, Gen Li Liu
• Keywords: Bankfull Discharge, Flood Discharging Capacity, Reaches of Ningmeng, Yellow River

References

[1] C.H. Hu: Journal of Hydraulic Engineering, 2006, 37 (11): 1283 -1289. In Chinese

[2] W.Y. Yao, W.X. Li, S.Z. Hou: Journal of Hydraulic Engineering, 2005,36 (3): 0257 - 0 264. In Chinese

[3] X.X. Xue: Yellow River, 2003, (2): 8 - 9. In Chinese

[4] Y.C. Wang, X.W. Ping:Yellow River, 1996, (1): 5 - 10. In Chinese

[5] S.Z. Hou, P. Wang: Yellow River, 2007, (4): 21 - 22. In Chinese

[6] Lanzhou Institute of Desert: Yellow River, 1988, (1):14 - 19. In Chinese

[7] S.Z. Hou: Yellow River, 2007, (1): 25 - 26. In Chinese