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首页> 外文期刊>Bulletin of engineering geology and the environment >Study on the destruction of backfilled loess slopes by short?term extreme rainfall erosion
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Study on the destruction of backfilled loess slopes by short?term extreme rainfall erosion

机译:短期极端降雨侵蚀对回填黄土边坡破坏研究

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This paper investigates the damage of loess slopes under the influence of short-term extreme rainfall. The experiment took the loess soil of Yan’an City, Shaanxi Province, as the research object, and the backfill loess slopes were prepared with different slope gradient (45°, 60°, and 75°). Artificial rainfall model experiments with a rainfall intensity of 120 mm/h and a rainfall duration of 4 h were carried out on three slopes. The experiments monitored the wet front migration pattern, rainfall infiltration characteristics, water content variation, pore water pressure variation and slope damage pattern. The experimental results show that the infiltration characteristics of rainwater are similar for slopes with different gradients. As the depth of the infiltration increases, the velocity of infiltration will decrease. In the early stages of rainfall, the degree of intrusion can reach 70–80, then decreases exponentially to around 20 as the duration of the rainfall increases. The main failure patterns for the 45° and 60° slopes are splash and scouring erosion failure. For the 75° slope, the main failure pattern is spalling. Short-term extreme rainfall and gradient have obvious effects on the slope failure pattern, especially for slopes with small gradients, and the splash effect and erosion will seriously damage the slope.
机译:本文研究了短期极端降雨影响下黄土边坡的破坏情况。试验以陕西省延安市黄土为研究对象,制备不同坡度(45°、60°、75°)的回填黄土边坡。在3个斜坡上开展了降雨强度为120 mm/h、降雨持续时间为4 h的人工降雨模式试验。试验监测了湿锋迁移模式、降雨渗透特征、含水量变化、孔隙水压力变化和边坡破坏模式。试验结果表明,不同坡度边坡的雨水入渗特性相似。随着渗透深度的增加,渗透速度会降低。在降雨的早期阶段,侵入程度可以达到70-80%,然后随着降雨时间的增加,侵入程度呈指数下降至20%左右。45°和60°斜坡的主要破坏模式是飞溅和冲刷侵蚀破坏。对于75°斜坡,主要的破坏模式是剥落。短期极端降雨和坡度对边坡破坏模式有明显影响,特别是对于坡度较小的边坡,飞溅效应和侵蚀会严重破坏边坡。

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