Sediment distribution and transport pattern in the nearshore region, southeast coast of India

IF 1.6 Q4 ENVIRONMENTAL SCIENCES
Umakanta Pradhan, Subrat Naik, Pravakar Mishra, Uma Sankar Panda, M. V. Ramana Murthy
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Abstract

The present paper aimed to assess the sediment distribution pattern, mode of transport, and its interaction with hydrodynamic and topographic conditions at different depths and regions along the east coast of India. About 900 surficial sediment samples were collected and analysed on a monthly basis for the Chennai coastal region at 32 stations from 2013 to 2015. The study region is classified into four types, such as beach, inlet, 5 m, and 10 m depth. Sediment textural and grain size trend analyses were conducted to achieve the objectives. Sediment characteristics for the region were recorded as sandy, equally dominated by unimodal and bimodal at the beach, while unimodal at shallow depths (5 and 15 m). The sediments were medium sand to coarse sand at the beach, mostly fine followed by medium at 5 and 15 m depths. The sediment sorting is dominated by moderately well-sorted sediments; the skewness of beach sediments was negative, while nearshore sediments were found positive; average kurtosis values of sediments were noticed to be mesokurtic. The CM plot depicts that the sediments were mostly derived by tractive current, and the modes of transport are “bottom suspension and rolling” and “graded suspension no rolling” at beach locations and shallow water depths, respectively. The GSTA analysis reveals the annual average sediment transport pattern is northerly. The numerical hydrodynamic study confirms the GSTA and CM plot analysis. The study reveals a stable sedimentary environment south of the Chennai port and instability in the northern part. The study includes large spatiotemporal nearshore sediment data with hydrodynamic conditions, immensely helpful to coastal stakeholders and researchers.

印度东南海岸近岸地区的沉积物分布和迁移模式
本文旨在评估印度东海岸不同深度和区域的沉积物分布模式、迁移方式及其与水动力和地形条件的相互作用。从 2013 年到 2015 年,在钦奈沿海地区的 32 个站点每月收集并分析约 900 个表层沉积物样本。研究区域分为四种类型,如海滩、入海口、5 米和 10 米深度。为实现目标,进行了沉积物质地和粒度趋势分析。根据记录,该区域的沉积物特征为沙质,在海滩同样以单模和双模为主,而在浅水区(5 米和 15 米)则以单模为主。海滩上的沉积物为中砂至粗砂,在 5 米和 15 米深处大部分为细砂,其次为中砂。沉积物分选以中度良好分选沉积物为主;海滩沉积物的偏度为负,而近岸沉积物的偏度为正;沉积物的平均峰度值为中度偏度。CM图显示,沉积物主要由牵引流推移而来,在海滩和浅水区的推移模式分别为 "底部悬浮和滚动 "和 "分级悬浮无滚动"。GSTA 分析表明,年平均沉积物运移模式为偏北运移。水动力数值研究证实了 GSTA 和 CM 图分析。研究显示,钦奈港以南的沉积环境稳定,而北部则不稳定。该研究包括大量的近岸沉积物时空数据和水动力条件,对沿海利益相关者和研究人员大有帮助。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
3.80
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0.00%
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