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Experiments research on anti-scourability of the big-sized samples from loess caves

机译:黄土溶洞大样品抗冲刷性试验研究

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摘要

Soil erosion resistant capacity is divided into the soil anti-erodibility and the soil anti-scouribility. Tunnel erosion belongs to one of specific soil erosions, which is largely distributed in loess areas. Tunnel erosion in the loess not only directly causes a large amount of materials loss, but also indirectly brings many engineering geological problems associated with landslides, road bases and dams. This paper, by means of field experiments of big-sized samples from loess cave, analyzing scouring process of big-sized original state loess, which divided into three periods: a period of rapid erosion, an erosion slow-down period and a period of steady erosion, discussing influence factors of loess erosion rates, and calculating the comprehensive index of soil anti-scourability, that is, loess erodible coefficient. Results of this study can play a significant role on quantizing analysis on the formation and evolution of loess caves, further understanding of tunnel erosion processes of loess, also have practical value to direct soil and water conservation.
机译:抗土壤侵蚀能力分为土壤抗侵蚀性和土壤抗冲蚀性。隧道侵蚀属于特定的土壤侵蚀之一,主要分布在黄土地区。黄土中的隧道侵蚀不仅直接造成大量材料损失,而且还间接带来许多与滑坡,路基和水坝有关的工程地质问题。本文通过对黄土溶洞大样品的田间试验,分析了大型原状黄土的冲刷过程,将其分为三个阶段:快速侵蚀期,侵蚀减缓期和侵蚀期。稳定侵蚀,讨论黄土侵蚀速率的影响因素,并计算土壤抗冲蚀性的综合指标,即黄土易蚀性系数。研究结果对定量分析黄土溶洞的形成和演化,进一步认识黄土的隧道侵蚀过程具有重要意义,对指导水土保持具有实用价值。

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