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Experimental study on impact behavior of submarine landslides on undersea communication cables

机译:海底滑坡对海底通信电缆撞击行为的实验研究

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AbstractSubmarine landslides, which are characterized by large scale and long run-out distance, could destroy undersea communication cables, thus resulting in a great number of economic losses. In this work, an experimental apparatus is designed to simulate the relative motion between the submarine landslide and undersea communication cable, and investigate the impact behavior of a submarine landslide. The test results show that submarine landslide with larger thickness and larger particle size can generate larger impact force on the communication cables. With an increase of the sliding velocity, the evolution of the flow behavior and impact force of the soil-water mixture can be divided into three stages: 1) landslide stage, the mixture consists a water layer and a sand layer, the impact force increases with the sliding velocity and reaches a peak value at this stage; 2) transforming stage, sand particles start to be eroded by water, and result into a turbidity current layer above the soil-water interface. At this stage, the impact force decreases to a minimum value; 3) turbidity current stage, all of the sand particles are eroded by water, and the impact force increases again when increasing the velocity continuously.HighlightsA test apparatus was developed to simulate the motion of a submarine landslide.Effective stress generated by landslide mass is a key factor to influence the impact behavior.The evolution of the impact force with the velocity could be divided into three stages.The impact force of a turbidity current is in proportion to the square of the velocity.Submarine landslides with larger particle size could act larger impact force on the cables.
机译: 摘要 海底滑坡具有规模大,跳动距离长的特点,可能破坏海底通信电缆,因此导致大量海底滑坡经济损失。在这项工作中,设计了一种实验设备来模拟海底滑坡和海底通信电缆之间的相对运动,并研究海底滑坡的撞击行为。测试结果表明,厚度较大,粒径较大的海底滑坡对通信电缆产生较大的冲击力。随着滑动速度的增加,土壤-水混合物的流动行为和冲击力的演化可分为三个阶段:1)滑坡阶段,混合物由水层和沙层组成,冲击力增大在此阶段以滑动速度达到峰值。 2)转化阶段,沙粒开始被水侵蚀,并在土壤-水界面上方形成浑浊流层。在这一阶段,冲击力减小到最小值。 3)在浑浊阶段,所有砂粒都被水侵蚀,并且当连续增加速度时,冲击力会再次增加。 突出显示 开发了一种测试设备来模拟海底滑坡的运动。 由滑坡体产生的有效应力是关键因素影响冲击行为。 冲击力随速度的变化可以分为三个阶段。 浊流的冲击力与速度的平方成比例。 粒径较大的海底滑坡可以对电缆施加更大的冲击力。

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