用熔丝塞模型进行土坝溃坝试验研究

D. Verma, B. Setia, V. K. Arora
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引用次数: 7

摘要

大坝的破坏是堤防破坏中最常见的形式之一。由于大坝溃坝会对建筑物造成大规模和广泛的破坏,并造成人员伤亡,这一问题引起了科学家们的注意。研究结果对堤防灾害评估和堤防下游居民预警系统的建立具有重要意义。土堤防因溢流而溃决的速度取决于土壤和水流的特性。不同的输入参数有助于理解这一现象,包括溃决的起始、溃决的宽度、溃决的深度、溃决的强度和到达峰值的时间。本文给出了用木制保险丝插头和五种不同土壤进行的实验室研究结果。所有试验的水力条件保持一致。黏结度和压实度是影响侵蚀过程的关键因素。对于纯非粘性土,表面侵蚀是逐渐发生的,而对于粘性土,则是头部侵蚀。溃口的行为取决于熔断器塞的尺寸、填充物的类型、水库容量和流入。对不同土壤的归一化决口水流线序列拟合了一个通用方程。方程的相关系数r2等于0.8,表明拟合良好。堤岸上游水库空间有限,水槽宽度有限是研究的局限性。
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Experimental Study of Breaching of an Earthen Dam using a Fuse Plug Model
Failure of dams due to overtopping is among the most frequent forms of embankment failures. Owing to massive and wide spread damage to structures and loss of lives associated with a dam failure, the subject has drawn the attention of scientists. The study also becomes essential for damage assessment and for development of early warning system of people downstream of the embankment. The rate of breaching of earthen embankments due to overtopping depends upon the soil and flow characteristics alike. Different input parameters that help in understanding the phenomenon are the temporal variation of initiation of the breach, breach width, breach depth, intensity of discharge and its time-to-peak. Present paper gives the results of laboratory investigation conducted using a wooden fuse plug and five different soils. The hydraulic conditions were kept same for all the experiments. It was observed that cohesiveness and degree of compaction were key factors in the erosion process. While for pure non-cohesive soils, surface erosion occurred gradually, but for the cohesive soils, headcut erosion was observed. The behaviour of breach depends upon dimensions of fuse plug, type of fill material, reservoir capacity and inflow. A common equation has been fitted to the series of normalized breach flow hydrographs of different soils. The equation has a coefficient of correlation r2 equal to 0.8 indicating a good fit. Limited space of the storage reservoir on the upstream of the embankment, and width of the flume are the limitations of the study.
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