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首页> 外文期刊>Journal of earth system science >Seasonal impact on beach morphology and the status of heavy mineral deposition a€“ central Tamil Nadu coast, India
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Seasonal impact on beach morphology and the status of heavy mineral deposition a€“ central Tamil Nadu coast, India

机译:对印度泰米尔纳德邦中部海岸的海滩形态和重矿物沉积状况的季节性影响

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摘要

The aim of the present research was to investigate the seasonal impact on nearshore beach dynamics and the status of heavy mineral distribution along central Tamil Nadu coast, India. Beach profile measurements were made in 10 profiling sites between Thirukadaiyur and Velankanni on monthly and seasonal basis from January 2011 to July 2012. Using beach profile data, variation in beach width, slope and volumetric changes have been calculated. Beach slope and nearshore wave parameters were used to quantify the longshore sediment transport rate. Beaches between Thirukadaiyur and Karaikkal attained predominant transport rate in northern direction whereas, the rest of the beaches are in southern direction. The seasonal action of wind and wave currents create nearshore bar during northeast (NE) monsoon and frequent berms at tidal zone during southwest (SW) monsoon. Surface sediment samples were collected in each location for quantifying the heavy mineral weight percentage during the period of pre- and post-Thane cyclone. Sediments were also studied by X-ray diffraction (XRD) to evaluate the changes and occurrence of heavy minerals in beach sands. The XRD results show that sediments in the study area have enriched heavy mineral distribution even after strong cyclonic event. It confirms the redistribution of heavy mineral deposits present in the coast. The results suggested that monsoonal action has influenced the seasonal changes in beach morphology and it does not affect the heavy mineral distribution.
机译:本研究的目的是调查对印度泰米尔纳德邦中部沿海近岸海滩动力学的季节性影响以及重矿物分布的状况。从2011年1月至2012年7月,按月和季节在Thirukadaiyur和Velankanni之间的10个配置文件站点中进行海滩轮廓测量。使用海滩轮廓数据,计算了海滩宽度,坡度和体积变化的变化。使用海滩坡度和近岸波浪参数来量化近岸沉积物的传输速率。蒂鲁卡代尤尔(Thirukadaiyur)和卡拉伊卡尔(Karaikkal)之间的海滩在北部地区的运输率达到了主要水平,而其他海滩则在南部方向。风和波浪流的季节性作用在东北(NE)季风期间形成近岸海带,而在西南(SW)季风期间在潮汐带形成频繁的护堤。在Thane旋风之前和之后的每个位置收集表面沉积物样品,以定量重矿物重量百分比。还通过X射线衍射(XRD)研究了沉积物,以评估沙滩沙中重矿物的变化和发生。 X射线衍射结果表明,即使在强烈的气旋事件后,研究区的沉积物也丰富了重矿物分布。它证实了沿海重矿物矿床的重新分布。结果表明,季风作用影响了海滩形态的季节性变化,并且不影响重矿物的分布。

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