首页> 外文会议>International conference on coastal engineering >RAPID FORMATION OF SAND BODY AT SHOREWARD EDGE OF OFFSHORE DREDGING HOLE AND RESULTING LARGE CHANGE IN SAND SPIT
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RAPID FORMATION OF SAND BODY AT SHOREWARD EDGE OF OFFSHORE DREDGING HOLE AND RESULTING LARGE CHANGE IN SAND SPIT

机译:海上疏浚孔的岸边的沙子身体的快速形成,并导致沙子唾液变化

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The influences of offshore sand mining on the surrounding beach topography were investigated at the Sumiyoshi-hama sand spit extending into Moriye Bay in Oita Prefecture, Japan. It was found that sand bars could develop above the MSL on the steep shoreward slope of the dredging hole in the tide and wave height ranges obtained from the predicted probability of wave occurrence at the Sumiyoshi-hama sand spit. As a result of the numerical simulation of wave height and nearshore currents given a predominant wave direction, wave height in the nearshore zone was found to be enhanced by the formation of the offshore dredging hole, and longshore currents toward the tip of the sand spit and counterclockwise currents on the lee side of the spit were accelerated by this wave intrusion. It was concluded that sand thrown up from the steep slope of the dredging hole by wave action was transported to the tip of the sand spit, causing large changes of the spit.
机译:在日本大分县的伦伊湾延伸到森林湾的Sumiyoshi-Hama沙滩吐对周围沙滩地形上的影响。发现砂杆可以在潮汐和波浪高度范围内的疏浚孔的陡峭横向斜面上方显影,并且从Sumiyoshi-hama砂吐的预测概率获得的波浪高度范围内。由于赋予主要波浪方向的波浪高度和近孔电流的数值模拟,发现近船区域中的波高通过形成海上疏浚孔,朝向沙子唾液尖端的龙头电流增强通过该波侵入加速吐的李侧的逆时针电流。得出结论是,从疏浚孔的陡坡通过波动作用抛出的沙子被运输到砂唾液的尖端,导致唾液的大变化。

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