A Calculation Method of Bulk Density of Debris Flow in Earthquake Area Based on the Size of Solid Particles of Debris Flow
A technology for solid particles and debris fluids, applied in calculation, computer-aided design, instruments, etc., can solve the problems of small actual bulk density value of debris flow, inability to meet the design of debris flow prevention and control engineering in earthquake areas, and low clay content, etc., and achieve the perfect calculation theory. Effect
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Embodiment 1
[0042] Niuquangou is located on the south side of Yingxiu Town, on the right bank of Minjiang River, about 1km upstream to Yingxiu New Town. The shape of the Niujuangou watershed is fan-shaped, with a longitudinal length of 5.4km, an average width of 2.0km, and a watershed area of 10.7km 2 . The highest point of the watershed is located on the west side of the survey area, with an elevation of about 2700m, and the lowest point is located at the mouth of the Minjiang River where Niuquangou joins, with an elevation of 858.3m and a relative elevation difference of about 1842m. The channel is generally deep-cut "V"-shaped valley, the main channel is 6124m long, the relative height difference is 1629m, and the average vertical slope of the main channel is 266‰.
[0043] In order to effectively prevent and control debris flow, prevent the Minjiang River from being blocked and threaten the downstream safety, the bulk density of the debris flow outbreak can be obtained in advance, ...
Embodiment 2
[0051] Gaojiagou is located on the north side of Ginkgo Township, on the right bank of the Minjiang River. The main ditch is 3.26km long vertically, 1.3km wide horizontally, and has an area of 3.79km 2 , the plane shape is approximately fan-shaped, and the relative height difference of the watershed is about 1807m. The longitudinal slope of Gaojiagou is generally steep, with an average vertical gradient drop of 523‰ in the whole valley. There are 4 tributary ditches developed in the gully domain, the length of the tributary ditches is relatively short, generally between 0.5 and 1.6 km, and the vertical gradient of the gully is relatively large, mostly above 500‰.
[0052] In order to effectively prevent and control debris flow, prevent the Minjiang River from being blocked and threaten the downstream safety, the bulk density of the debris flow outbreak can be obtained in advance, and the effective prediction can be made according to the gradation characteristics of the debri...
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