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Practical implications of tidal flat shape

机译:潮汐平面形状的实际意义

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Arising from high precision empirical measurements of whole shore shape involving determination of incremental areas in narrow height bands undertaken during the 1980s, now confirmed by physical and mathematical models and theoretical studies, it has been established that accretion-dominated mudshores tend to be high and convex in cross-sectional shape, whereas their erosion-dominated counterparts tend to be low and concave. High and convex mudshores are preferable in coastal defence, port engineering and conservation terms to low and concave ones. In this paper the practical implications of these contrasted shapes are drawn out. The natural shapes of mudshores contrast with what might be anticipated from the well-established Bruun Rule for sandy shores. Accordingly, a new mudshore conceptual model, the Mehby Rule, is proposed which embraces all aspects of mudshore behaviour and will stand alongside the Bruun Rule. A new mudshore management tool, a top-down model, called S-factor analysis, is proposed and developed to a semi-quantitative state by way of a demonstration of its possibilities. It can be applied to quantifying the stability of mudshores. Mudshores with an S close to zero are stable in shape and approaching one type of equilibrium condition. As S departs progressively from zero in the negative direction shores become more accretion-dominated and, similarly, as they depart from zero in the positive direction they become more erosion dominated. A new mudshore management technology, tidal hat regeneration, is also proposed. The Mehby Rule shows that, to be stable and self-sustaining, whole shore profile manipulation is required, whilst S-factor analysis indicates these will have an S close to zero. By simultaneously placing a minimal wave attenuator and feeding with dense muddy dredge material, a low and concave mudshore can be converted into a more desirable high and convex one. The technology is proved from physical model tests and by analogy with the natural response of low and concave mudshores to a sudden change in the degree of wave protection. Thus, the new method seeks deliberately to copy accidentally induced shape change. The next stage will be to undertake full-scale field trials. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 35]
机译:由于对整个海岸形状进行高精度的经验测量,包括确定1980年代在狭窄的高度带中增加的面积,现在已通过物理和数学模型以及理论研究得到证实,现已确定以增生为主导的泥岸往往是高而凸的。横截面形状,而腐蚀占主导的对应部分往往较低且呈凹形。在沿海防御,港口工程和保护方面,高低洼的泥岸比低洼低洼的泥岸更好。在本文中,提出了这些对比形状的实际含义。泥岸的自然形态与公认的沙质海岸布鲁恩法则所预期的形成鲜明对比。因此,提出了一种新的泥岸概念模型,即Mehby规则,该模型涵盖了泥岸行为的所有方面,并将与Bruun规则并肩作战。提出了一种新的泥岸管理工具,称为S因子分析的自上而下的模型,并通过演示其可能性将其开发为半定量状态。它可以用于量化泥岸的稳定性。 S接近零的泥岸形状稳定,并接近一种平衡状态。当S在负方向上逐渐从零开始偏离时,海岸变得更受固结支配,并且类似地,当它们在正方向上从零开始偏离时,它们变得更受侵蚀支配。还提出了一种新的泥岸管理技术,即潮帽再生。梅比定律表明,要保持稳定和自我维持,就需要对整个岸坡剖面进行操纵,而S因子分析表明,它们的S值将接近于零。通过同时放置最小波衰减器并注入稠密的泥沙疏material材料,可以将低凹的泥岸转换成更理想的高凹的泥岸。该技术已通过物理模型测试以及与低凹凹岸对波浪防护等级突然变化的自然响应进行了证明。因此,新方法试图刻意复制意外引起的形状变化。下一阶段将进行全面的现场试验。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:35]

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