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Internal characterization of embankment dams using ground penetrating radar (GPR) and thermographic analysis: A case study of the Medau Zirimilis Dam (Sardinia, Italy)

机译:使用地面穿透雷达(GPR)和热成像分析的堤坝内部表征 - 以达里米尔大坝(撒丁岛,意大利)为例

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摘要

The stability of embankment dams without an impermeable core depends on the characteristics of the face slab that prevents internal erosion, piping and eventual collapse of the structure. Under a Mediterranean climate, the impermeable asphaltic face slab is subjected to high solar radiation and consequent temperature changes, which can generate the creation of cracks and joints. The Medau Zirimilis Dam, located in the Casteddu River (Sardinia), is an embankment dam that has undergone seepage and continuous repairs in its asphalt face slab. These reparations have been conducted because of the occurrence of cracks and relative movement of different segments of the slab. To evaluate if seepage endangers the integrity of the dam, GPR was used, with different antennas (100, 250 and 500 MHz), along its crest and upstream and downstream faces, and the data were integrated with infrared thermographic images. Although geophysical data do not show structural changes affecting the main dam structure, deformation structures at shallow levels and in particular in the upstream face and along the crest of the dam have been identified. Such deformation affects the road atop the crest, the face slab and underlying levels, resulting in landslides that include material from several meters below the surface. The analysis permitted the identification of the origin of surficial cracks and their effects on the face slab. These sectors, independent of current movement, define the most unstable areas against water level changes that can affect the darn integrity. GPR analysis at the embankments usually has the handicap of high clay content that precludes electromagnetic wave penetration; however, in this case, the obtained resolution and extent of penetration using the different antennas was sufficient, due to the absence of an inner waterproof unit, and permitted the evaluation of the inner structure of the dam and the application of GPR for construction quality surveillance, internal structural characterization and dam monitoring.
机译:没有不可渗透的核心的堤坝坝的稳定性取决于防止内部侵蚀,管道和最终坍塌结构的面板的特性。在地中海气候下,不透水的助擦性面板经受高的太阳辐射和随后的温度变化,这可以产生裂缝和关节的产生。位于Casteddu River(Sardinia)的Medau Zirimilis Dam是一座堤防大坝,在其沥青脸部板块中经过渗漏和持续修复。由于裂缝和平板的不同段的裂缝和相对运动的发生,已经进行了这些赔偿。为了评估渗透延迟抑制大坝的完整性,使用GPR,沿着其峰值和上游和下游面使用不同的天线(100,250和500MHz),并且数据与红外热成像集成。尽管地球物理数据不显示影响主坝结构的结构变化,但已经识别出浅水平的变形结构,并且尤其在上游面和沿着大坝的峰值。这种变形影响了顶部的道路,面板平板和底层水平,导致山体滑坡,其包括从表面下方几米的材料。分析允许识别曲面裂缝的起源及其对面板的影响。这些扇区独立于当前的运动,定义了可能影响DARN完整性的水位变化的最不稳定的区域。堤坝的GPR分析通常具有高粘土含量的障碍,可以排除电磁波渗透;然而,在这种情况下,由于没有内部防水单元,所获得的分辨率和使用不同天线的渗透程度就足够了,并且允许评估大坝内部结构以及GPR用于施工质量监测的应用,内部结构表征和水坝监测。

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