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Sorting and sedimentology character of sandy beach under wave action

机译:波浪动作下沙滩的分类和沉积物特征

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To explore the sandy beach sorting and sedimentary characteristic induced by wave action, a set of 2D wave flume experiments on a sandy beach were performed. The initial beach slope with non-uniform sand of combination of 1/10 and 1/20 was exposed to regular waves, random waves, cnoidal waves and solitary waves respectively. The evolution of cross-shore beach profiles and the grain size of sediments in different locations were measured and recorded. Experimental results show that the sediments of sandy beach under wave action produced obvious sorting phenomenon. The intense turbulence generated by breaking waves leads to the sediment-transporting, and provides the impetus for the movement of fine sands. Course sands deposited in intense turbulence deposition area because of carrying capacity of the flow is not enough due to turbulence effect. Fine sands were carried by the flow induced by breaking waves, and separately deposited in the area of weak turbulence.
机译:为了探索波动诱导的沙滩分类和沉积特征,进行了一组沙滩上的2D波水槽实验。具有1/10和1/20组合的非均匀沙子的初始海滩斜率分别暴露于常规波,随机波,Cnoidal波和孤立波。测量并记录了交叉岸海滩曲线的演变和不同地点沉积物的粒度。实验结果表明,波浪动作下沙滩的沉积物产生了明显的排序现象。通过破坏波产生的强烈湍流导致沉积物运输,并为细砂运动提供动力。由于湍流效应,由于流动的承载能力,沉积在强烈的湍流沉积区域中沉积在强烈的湍流沉积区域。通过破碎波引起的流动携带细砂,并分开沉积在弱湍流面积。

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