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Erosion characteristics of loess tunnels on the Loess Plateau: A field investigation and experimental study

机译:黄土高原黄土隧道的侵蚀特点:田间调查与实验研究

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Loess tunnels are a common geo-hazard in the Loess Plateau and not only cause considerable soil and water loss, but also aggravate and even induce the occurrence and development of other disasters such as ground fissures, mudflows, collapses, and landslides. To date, research on the hydrological characteristics and erosion behaviour of loess tunnel systems has focused on field investigation data and limited river basin observation data, whereas field test information and data are very scarce. In this study, field surveys, observations, field scouring experiments, and laboratory-based sediment percentage tests were conducted to analyse the erosion characteristics, spatial distribution, and hydrological characteristics of a large-scale loess tunnel system in the hilly Loess Plateau southeast region of northern China. The results showed that the loess tunnel erosion exhibited periodicity. Tunnel erosion in each period shows a similar erosion process, that is, thin-layer water flow erosion and lateral expansion, tunnel wall collapse and deposit due to the loss of support from the lateral erosion, and erosion and transport of deposits by water flow. Waterfall erosion, lateral erosion, headward erosion, and the resulting collapses were the main forms of tunnel erosion. Besides this, the base level of erosion significantly affects the erosion characteristics of the loess tunnel. The hydrological characteristics during field scouring experiments exhibited three different stages: a lag effect, attributed to the temporary loss of water velocity in the first stage; small water flow fluctuations in the second stage; and an increase in total seepage loss with increased water injection flow in the third stage. The erosion rate was positively correlated with the flow quantity. The results of this study not only provide valuable reference data for research on the mechanism and velocity of erosion events in loess, but also provide a theoretical basis for the prevention of loess tunnel disasters in engineering construction. (c) 2020 John Wiley & Sons, Ltd.
机译:黄土隧道是黄土高原的常见地理危险,不仅引起了相当大的土壤和水分,而且加重甚至诱导了地下裂缝,泥流,坍塌等其他灾难的发生和发展。迄今为止,黄土隧道系统的水文特征和侵蚀行为的研究专注于现场调查数据和有限的河流流域观测数据,而现场测试信息和数据非常稀缺。在本研究中,进行了现场调查,观察,现场擦除实验和基于实验室的沉积物百分比试验,以分析丘陵黄土高原东南地区大型黄土隧道系统的侵蚀特性,空间分布和水文特征北方。结果表明黄土隧道侵蚀表现出周期性。每个时期的隧道侵蚀显示出类似的侵蚀过程,即薄层水流侵蚀和横向膨胀,隧道壁塌陷和沉积物由于横向侵蚀的支持,以及通过水流腐蚀和沉积物的腐蚀和运输。瀑布侵蚀,侧面侵蚀,前向侵蚀和所产生的坍塌是隧道侵蚀的主要形式。除此之外,侵蚀的基础水平显着影响黄土隧道的侵蚀特性。现场冲刷实验期间的水文特性表现出三个不同的阶段:滞后效应,归因于第一阶段的暂时损失的水速度;第二阶段的小水流量波动;并在第三阶段增加水注射流量的总渗流损失增加。侵蚀率与流量呈正相关。本研究的结果不仅为黄土侵蚀事件的机制和速度提供了有价值的参考数据,而且还为防止黄土隧道灾害的工程建设提供了理论依据。 (c)2020 John Wiley&Sons,Ltd。

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