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The Effect of Sediment Size and Face Slope on Breach Formation of Non-cohesive Homogeneous Embankments Failed by Overtopping

机译:沉积物大小和面部坡对突破形成非粘性均匀堤防的影响失败

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Previous research mainly focused on flood propagation and few works were done for dam breach formation. It is difficult because it relates to several branches of knowledge such as hydraulics, sedimentary dynamics and soil mechanics at the same time. Laboratory experi-ments for non-cohesive homogenous embankments failed by overtopping have been undertak-en to research the effects of sediment size and face slope on breach formation in Nanjing Hy-draulic Research Institute (NHRI). According to the results median diameter D50 has little effects on breach formation. Decreasing the downstream face slope has significant effects on it. It can delay the flood peak from dam breach and slow the speed of lateral extension of breach.
机译:以前的研究主要集中在洪水繁殖中,为坝突发形成完成了很少的作品。很难,因为它涉及同时液压,沉积动力学和土壤力学等几个知识分支。对于非凝聚性均匀堤防的实验室实验,通过拓展失败了,研究了沉积物大小和面部坡度对南京高级研究所(NHRI)的突破形成的影响。根据结果​​,中值D50对突发形成影响不大。减少下游面坡对其具有显着影响。它可以延迟坝漏洞的洪水峰值并减慢突发横向延伸的速度。

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