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- W2393315061 abstract "Research purposes: A large mud-stone flow suddenly happened in the Qingshuiwan section of Hainan east ring railway to be open for traffic soon and the eastern speedway.The mud-stone flow flowed over the railway embankment and passed through the space under the bridge and then flowed over the speedway surface into the South China Sea.By observing the forming process of mud-stone flow and using the various means,such as geologic survey,aerial photography,exploration and field test,the analysis of the formation cause for giant landslide,the mechanism of turning landslide into mud-stone flow and the runoffing and accumulating characteristics of the mud-stone flow was made. Research conclusions:(1)The appearance of the giant landslide in fluidity area reflected the features of the suddenness and the high-level and high-speed movement of gaint mud-stone flow.(2)The broken weathered granite rock mass and the unfavorable structural plane were the basic condition for landslide.(3)The effects of the heavy rainfall,loading and water softening along the steep under structural plane were the direct cause for the landslide.(4)After the landslide was rapidly gliding,the landslide disintegrated quickly and turned into mud-stone flow with water.Then the mud-stone flow constantly scoured the ditch bed to cause increasement of the water content gradually and quickly moved for about 4 kilometers.(5)The Qingshuiwan section of Hainan east ring railway and the eastern speedhway were located in the outside edge of the accumulating area of the mud-stone flow.When the mud-stone flow arrived at this place,its intensity was much weakened with less destroy degree." @default.
- W2393315061 created "2016-06-24" @default.
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- W2393315061 date "2012-01-01" @default.
- W2393315061 modified "2023-09-24" @default.
- W2393315061 title "Analysis of Formation Cause and Movement Characteristics of Mud-stone Flow in Mengshuiling of Hainan Province" @default.
- W2393315061 hasPublicationYear "2012" @default.
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