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Hydrodynamics and sediment flux of hoa in an Indian Ocean atoll

机译:印度洋环礁中a的水动力和泥沙通量

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摘要

Detailed hydrodynamic and sediment flux measurements are reported from 11 hoa (shallow cross-reef channels) in the Cocos (Keeling) Islands, Indian Ocean. All hoa exhibit unidirectional oceanside reef to lagoon fluxes. These currents are driven by tides, wave set-up and incident waves, and the presence of islands that generate alongshore gradients so that currents flow toward the topographic low points of hoa entrances in the reef rim. Two functional groups of hoa are identified that extend Chevalier's typology of hoa and possess different process signatures. Sediment-limited hoa (SLH) are efficient conduits of sediment transport. They are located close to the reef rim where incident wave energy propagates across the reef crest into the hoa and is able to entrain sediment. Transport-limited hoa (TLH) are characterized by low rates of sediment transport because incident wave energy is negligible as they are located much further from the reef edge than SLH. In the absence of an entrainment mechanism the oceanside reef flat is laden with sediment. Storm energy increases transport efficiency through hoa. However, the net sedimentation response differs between the two hoa types. Proximity to the reef edge means that frequent storms flush sediment from SLH increasing hoa depth and enhancing the potential for erosion of the conglomerate boundary. In contrast, the greater reef width fronting TLH means that sediment transport from reef flats to the lagoon is only activated during infrequent storms. The contrasting process signatures account for morphological differences between sediment-limited hoa (lagoonward decrease in depth and increase in width), and transport-limited hoa (lagoonward increase in depth). The number and type of functional hoa are found to have significant implications for the rate of lagoon sedimentation in enclosed atolls. In general, an increase in frequency of functional hoa and increased proportion of SLH will promote more rapid rates of lagoon infill.
机译:据报道,印度洋的科科斯(基林)群岛的11条珊瑚礁(浅礁礁通道)详细地测量了水动力和泥沙通量。所有的珊瑚都表现出单向的海边礁到泻湖通量。这些电流是由潮汐,波浪形波和入射波以及存在沿岸梯度产生的岛的存在所驱动的,因此,电流流向礁石边缘的珊瑚礁入口的地形低点。确定了两个功能组的hoa,它们扩展了Chevalier hoa的类型,并具有不同的过程签名。沉积物局限性清水(SLH)是沉积物输送的有效管道。它们位于礁石边缘附近,在这里入射波能量穿过礁石顶传播到珊瑚中,并能够夹带沉积物。输运受限的荷包油(TLH)的特点是泥沙输运速率低,因为入射波能量比SLH距礁石边缘远得多,因此可以忽略不计。在没有夹带机制的情况下,海边的礁滩上充满了沉积物。风暴能量通过居安思危提高了运输效率。但是,两种居留类型之间的净沉降响应有所不同。靠近礁石边缘意味着频繁的暴风雨冲刷了SLH的沉积物,从而增加了花a深度并增强了砾岩边界侵蚀的可能性。相反,朝向TLH的更大的礁石宽度意味着,只有在罕见的暴风雨期间才激活从礁滩到泻湖的沉积物传输。形成鲜明对比的过程特征说明了沉积物限制的hoa(深度向后减小并增加宽度)和运输限制的hoa(深度向后增大)之间的形态学差异。发现功能性居所的数量和类型对封闭环礁中泻湖的沉积速率有重要影响。通常,功能性居室频率的增加和SLH比例的增加将促进泻湖填充的更快速度。

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