A method for measuring and calculating the maximum scour depth of viscous debris flow gully bed and its application
A debris flow ditch and scour depth technology, applied in hydraulic engineering, hydraulic engineering equipment, construction, etc., can solve the problem of poor calculation accuracy, not considering the movement resistance of debris flow and scourable solid materials in the channel, and cannot meet the engineering foundation of viscous debris flow prevention and control. The needs of buried depth design and other issues, to achieve the effect of perfect calculation theory and accurate calculation results
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Embodiment 1
[0034] Jiangjiagou is located in the north of Dongchuan City, Yunnan Province, and the water flows into the small river from east to west. Jiangjiagou drainage area is 48.6km 2, the main ditch is 13.9km long, the highest altitude is 3269m, and the lowest altitude is 1042m. It is a famous viscous debris flow ditch. From June 12 to October 3, 1983, 21 mudslides broke out in the main ditch of Jiangjiagou. The debris flow gully bed was scoured violently, resulting in the general exposure of the 1404m diversion embankment block stone armor foundation and the collapse of 694m. At present, there are few debris flow prevention and control projects in the lower reaches of Jiangjiagou, and large areas of farmland and its supporting water conservancy facilities lack effective protection, which is greatly threatened by debris flow disasters.
[0035] In order to reduce the threat of mudslide hazards and protect the farmland in the lower reaches of Jiangjiagou, it is planned to build a p...
Embodiment 2
[0043] Hongchun Ditch is located in the northeast of Yingxiu Town, Wenchuan County, on the left bank of the Minjiang River. It is a viscous debris flow ditch. Coordinates of the mouth of the ditch: N31°04′01″, E103°29′33″; Area of the ditch: 5.35km 2 ; The length of the main ditch: 3.6km; the elevation of the highest point: 2168.4m; the elevation of the confluence: 880m; the relative height difference: 1288.4m; Before the Wenchuan Earthquake, two smaller debris flows occurred in Hongchungou. After the Wenchuan Earthquake, a large number of collapses and landslides were induced by the earthquake, which provided important loose materials for the formation of debris flows, and the Hongchungou debris flows tended to be active. On August 14, 2010, heavy rainfall caused a debris flow in Hongchungou, with a scale of 805,000 m 3 , of which more than 400,000 m 3 directly into the Minjiang River. The accumulation of mudslides in the Minjiang River blocked the main channel of the M...
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