黄土高原典型淤地坝溃决的界面促渗与水力激发促溃机制

    THE FAILURE MECHANISM OF TYPICAL CHECK DAMS ON THE LOESS PLATEAU INDUCED BY INTERFACE INFILTRATION AND HYDRAULIC EXCITATION

    • 摘要: 黄土高原极端暴雨下淤地坝溃决事件频发,查明淤地坝的防洪标准、显著的界面促渗效应、极端暴雨水力激发下的溃决机制至关重要。为此采用野外调查、现场监测、室内试验等手段开展典型治沟造地小流域淤地坝的水毁溃决机制研究,以揭示淤地坝水毁破坏模式、坝体渗流特征、渐进溃决机制。结果表明:(1)典型淤地坝水毁破坏可分为坝体变形与坝体破坏两类。其中坝体变形可分为坝顶沉降、坝坡滑塌两类,坝体破坏可分为管涌式溃坝、滑移式溃坝、漫顶式溃坝3类;(2)淤地坝特殊地质结构诱导了差异的坝坡渗流规律,导致了坝体差异的渐进式水毁破坏特征。疏松坝体易诱导强渗流浸润软化坝体,造成坝顶沉降及坝体渐进滑塌;挖填、堆填软弱界面易诱导优势渗流,造成坝体沿界面软弱带、软弱区产生渗透变形破坏;(3)极端暴雨短时激发了坝体强渗流、快速放大了界面优先流,导致坝体内孔隙水压力激增,渗透力沿界面带快速冲蚀土体使坝坡产生管涌破坏、沿界面区快速冲剪土体使坝坡产生滑移破坏。研究成果从界面促溃角度揭示了黄土高原淤地坝频繁溃决的水力激发机制,为淤地坝高防洪标准建设及关键防溃技术提出提供重要参考。

       

      Abstract: Frequent breaches of check dams occur on the Loess Plateau during extreme rainstorms. It is crucial to evaluate the low flood control standards of check dams, the significant infiltration enhancement at the interface, and the breach mechanisms triggered by hydraulic forces during such extreme rainfall events. This study employs field investigations, on-site monitoring, and laboratory experiments to examine water-induced damage and breach mechanisms in check dams within typical small watersheds used for gully control and land reclamation. The research aims to elucidate the failure modes of check dams, the seepage characteristics of the dam body, and the progressive breach mechanism. The results indicate that typical water-induced failure modes of check dams can be classified into two main categories: dam deformation and dam failure. Dam deformation includes crest settlement and slope collapse, while dam failure can be further subdivided into three types: piping-induced dam break, slope slip-induced dam break, and overtopping-induced dam break. The unique geological structure of check dams leads to distinct seepage behaviors within the dam body, resulting in progressive water-induced damage characteristics. The loose composition of the dam body facilitates intense seepage, leading to material softening, crest settlement, and progressive slope collapse. Additionally, weak interfaces between excavation and fill layers are prone to forming dominant seepage pathways, causing deformation and failure along these weak zones. During extreme rainstorms, intense seepage within the dam body and enhanced preferential flow at the interface sharply increase pore water pressure. The resulting seepage forces rapidly erode soil along the interface, triggering piping failure within the dam body. Furthermore, rapid shearing along the interface area leads to sliding failure of the dam structure. These findings clarify the hydraulic excitation mechanism responsible for the frequent collapse of check dams on the Loess Plateau due to interface-induced failure.

       

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