Method for measuring and calculating under-dam scouring maximum depth of window dam and application
A technology of maximum depth and window, which is applied in the design of debris flow and sand dams, and in the field of debris flow prevention and control engineering structures. It can solve the problems of limiting the actual reference value and inconsistency of the measurement results, and achieve the effect of simple parameter value and simple calculation process.
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Embodiment 1
[0031] In the design of a window dam, the method of the invention is used to calculate the maximum scouring depth h under a window dam d 。
[0032] A debris flow gully is located in Wenchuan County, Aba Tibetan and Qiang Autonomous Prefecture, Sichuan Province. It is a first-class tributary on the right bank of Minjiang River. The drainage area of the gully is 54.26km 2 The longitudinal length of the main ditch is 15.74km, and the average longitudinal ratio of the main ditch bed is 201 ‰. The plane shape of the basin is in the shape of "leaves". The upper reaches of the gully are narrow, mostly in the shape of "V", the middle and lower reaches are wide and gentle, in the shape of "U", with local width and width alternating. The mountains in the gully area are high and steep, and the longitudinal slope of the gully is large, which is conducive to the collection of rainfall and provides a foundation for the outbreak of debris flow. The national highway G213 and Duwen expressway proj...
Embodiment 2
[0044] The method of the invention is used to check the maximum scouring depth h under a window dam d 。
[0045] A debris flow gully is located in group 4, Xiaba village, Puji Town, Puge County, Liangshan Prefecture, Sichuan Province. The drainage area of the gully is 23.30km 2 The longitudinal length of the main ditch is 10.47km, and the average longitudinal ratio of the main ditch bed is 195 ‰. The overall shape of the basin is in the shape of "leaves". The mountain in the gully area is high and the slope is steep, and the longitudinal slope of the gully is large. The gully area is rich in debris flow deposits. There are many collapse points and loose slope deposits on both sides of the gully area, which provides material source conditions for the outbreak of debris flow. Goukou is a typical minority village. A large-scale debris flow broke out in the gully, which washed away the highway at the gully mouth and blocked the river, posing a serious threat to the villages at the gul...
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