首页> 外文会议>International conference on ocean, offshore and arctic engineering;OMAE2009 >CALCULATION OF WAVE-INDUCED SHALLOW STRATUM SEABED SLIDES IN THE SUBAQUEOUS YELLOW RIVER DELTA
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CALCULATION OF WAVE-INDUCED SHALLOW STRATUM SEABED SLIDES IN THE SUBAQUEOUS YELLOW RIVER DELTA

机译:黄河三角洲波浪诱发的浅层海底滑坡的计算

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Wave-induced seabed slide could happen even at very gently sloping silty seabed. Based on the wave-seabed interaction, the safety coefficient calculation model of wave-induced gentle seabed slides in the seabed instability was carried out using limit equilibrium method, Bishop Method, in this paper. The calculated results shows that the effective internal cohesion c and the effective internal friction angle 9 affect the location of slip surface and the magnitude of the safety coefficient significantly. The safety coefficient rises linearly with the increases of c and Φ at a fixed depth. The results fit reasonable well with the slide calculation results from a wave flume experiment in laboratory. Additionally, it was concluded that the silty seabed tended to slide under wave actions at the depth less than 5 meters in the Yellow River Subaqueous Delta.
机译:即使在非常缓慢倾斜的粉质海底也可能发生波浪诱发的海底滑坡。基于波浪-海床相互作用,本文采用极限平衡法Bishop法建立了波浪诱发海床不稳定区平缓海床滑坡的安全系数计算模型。计算结果表明,有效内聚力c和有效内摩擦角9显着影响滑移面的位置和安全系数的大小。在固定深度处,安全系数随c和Φ的增加而线性增加。结果与实验室波浪槽实验的玻片计算结果非常吻合。此外,得出的结论是,在黄河水下三角洲小于5米的深度处,粉质海床在波浪作用下趋于滑动。

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