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首页> 外文期刊>Geomorphology >Littoral sediment transport and shoreline changes along Ennore on the southeast coast of India: Field observations and numerical modeling
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Littoral sediment transport and shoreline changes along Ennore on the southeast coast of India: Field observations and numerical modeling

机译:印度东南沿海恩诺尔河沿岸的沉积物输运和海岸线变化:实地观测和数值模拟

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摘要

The newly constructed port in 2001 at Ennore, on the southeast coast of India near Chennai, with breakwaters on either side (north and south) has been causing large-scale changes in nearshore morphology. Beach profiles and shoreline positions along 25 km coastline of Ennore were measured at regular intervals during 2001-06 to understand the sediment transport patterns in the region. At the same time the results of wave hind-casting and wave transformation modeling were incorporated in LITDRIFT model to compute the sediment transport rates along Ennore coast. The model results are compared with the sediment tiansport values obtained from beach profile measurements. The performance of the model at different locations within the study area with variable wave conditions has been examined. The annual net sediment loss ( ) versus accumulation (+) were estimated for two smaller study areas (cells) containing ten regularly spared beach profiles numbered from north to south, BP1-5 in cell I and BP6-10 in cell II. For the cell I region, which is protected by the Ennore shoals and where human interference is minimum, the annual net sediment supply is +0.02 × 10~6 m~3 as obtained from beach profile measurements while the model gave a value of + 0.014×10~6 m~3. For the cell II region where there is large human intervention by way of Ennore port development and breakwater construction, the annual net sediment movement as obtained by the beach measurements is - O.l4×10~6 m~3 while the model gave a value of -0.154×10~6 m~3. It is found that the performance of the model is satisfactory and the model may be used successfully to study sediment dynamics along any coastline provided one has detailed understanding of the coastline orientation, nearshore topography, cross-shore bathymetry and prevailing annual wave climate. Based on the sediment transport data and beach profile measurements the beach and shoreline changes for transect locations BP-1 to BP-10 are also critically examined in this paper.
机译:2001年在印度东南部钦奈附近的恩诺尔(Ennore)新建的港口,两侧(北部和南部)都有防波堤,已引起近岸形态的大规模变化。在2001-06年期间,定期测量了Ennore海岸线25公里处的海滩剖面和海岸线位置,以了解该地区的泥沙输送方式。同时,在LITDRIFT模型中结合了波后预报和波转换模型的结果,以计算沿Ennore海岸的泥沙输送速率。将模型结果与从海滩剖面测量获得的沉积物天体数值进行比较。已经研究了该模型在研究区域内具有波动条件的不同位置的性能。估计了两个较小的研究区域(单元)的年度净沉积物损失()对累积量(+)的变化,其中包含从北到南编号的十个定期备用海滩剖面,单元一中的BP1-5和单元二中的BP6-10。对于由Ennore浅滩保护且人为干扰最小的I区,通过海滩剖面测量获得的年净沉积物供应量为+0.02×10〜6 m〜3,而模型给出的值为+ 0.014 ×10〜6 m〜3。对于通过Ennore港口开发和防波堤建设而需要大量人为干预的II区,通过海滩测量获得的年净泥沙运动为-O.l4×10〜6 m〜3,而模型给出了一个值-0.154×10〜6 m〜3发现该模型的性能令人满意,并且只要对海岸线的方向,近岸地形,跨岸测深法和盛行的年波气候有详细的了解,该模型就可以成功地用于研究沿任何海岸线的沉积物动力学。基于沉积物传输数据和海滩剖面测量结果,本文还对BP-1至BP-10样线位置的海滩和海岸线变化进行了严格检查。

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