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Physical model investigation of mid-scale mangrove effects on flow hydrodynamics and pressures and loads in the built environment

机译:中型红树林对内部流体动力学和压力和荷载作用的物理模型调查

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Large (km-scale) mangrove forests can provide protection to shorelines and near-coast structures during extreme coastal flood events, including tsunamis and tropical cyclones. However, little is known about the effects of mangroves with a modest cross-shore thickness (similar to 10-50 m), on flow hydrodynamics and resulting inland pressures and forces on near-coast structures. We constructed a 1:16 geometric-scale physical model of a Rhizophora mangle (red mangrove) fringe with modest cross-shore thickness to measure the effects of a mangrove forest's cross-shore thickness on wave attenuation and subsequent load reduction on near-coast structures, idealized during experiments with an array of cubes. Three configurations, one baseline with zero mangroves and two with mangrove cross-shore thicknesses corresponding to prototype-scale forest widths of 8.2 m and 19.0 m, were considered in front of an array of idealized slab-on-grade residential buildings. Transient wave conditions with varying incident parameters (wave amplitude, wave representative time scale, water level/mangrove emergence, and presence of a background current) were considered. Water surface elevations, water velocities, cross-shore forces, and pressures measured near and against the building array indicate that mangroves affected inland flow hydrodynamics and forces. The presence of mangroves was associated with elevated water levels and reduced peak velocities between the mangroves and inland structures. Increasing the mangrove cross-shore thickness reduced the cross-shore force on a structure by 11%-65% compared to the baseline case without mangroves. The force reduction by the mangrove configurations varied with incident wave representative time scale; waves with longer representative time scales required larger cross-shore thicknesses to provide similar force reductions to those observed for shorter waves. Further investigation into a wider range of mangrove crossshore thicknesses, trunk densities, and wave conditions is needed to inform engineering performance of natural and nature-based features for resilient coastal design.
机译:大型(公里规模)红树林森林可以在极端沿海洪水事件(包括海啸和热带旋风)期间为海岸线和近海岸结构提供保护。然而,关于红树林的影响很少,在流动流体动力学和近海岸结构上产生内陆压力和力量,对着跨岸厚度(类似于10-50米)的混合厚度(类似于10-50米)而闻名。我们建造了一个1:16的根毛细血管(红色红树林)边缘的物理模型,具有适度的交叉岸厚度,以测量红树林林的交叉侧厚度对波浪衰减的影响和随后的近海岸结构的负荷减少,在具有多维数据集阵列的实验期间理想化。在一个理想的平板对级住宅建筑物的前面,考虑了三种配置,具有与原型森林宽度相对应的红树林和两种具有混合的红细胞厚度的一个基线,并考虑了8.2米和19.0米的原型林宽度。考虑了具有不同事件参数的瞬态波条件(波浪幅度,波浪代表时间尺度,水位/红树林出现和背景电流的存在)。水面升高,水速度,跨岸动力和压力在附近和建筑物阵列中测量的压力表明,红树林影响内陆流动流体动力学和力。红树林的存在与水平升高的水平相关,并减少了红树林和内陆结构之间的峰值速度。与没有红树林的基线盒相比,增加红树林交叉截岸厚度将横腹力降低11%-65%。红树林配置的力减少因事件波代表时间尺度而变化;具有更长的代表性时间尺度的波需要更大的交叉横截面厚度,以提供与观察到的较短波的那些相似的力减少。需要进一步调查更广泛的红树林十字厚度,树干密度和波条件,以便为有弹性的沿海设计提供自然和自然的特征的工程性能。

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