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Grain-size distribution and subsurface mapping at the Setiu wetlands, Setiu, Terengganu

机译:登嘉楼Setiu湿地Setiu湿地的粒度分布和地下测绘

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摘要

A study was carried out around the lagoon and coastal area of Setiu wetlands to determine the general characteristics and grain-size distribution of their sediments. Sediment samples were collected from 39 stations of the lagoon area and 8 stations of the coastal area, and were analyzed for their sedimentological characteristics (mean, sorting, skewness and kurtosis). The sediment mean size ranged between 0.06-2.52 and 2.12-2.69 phi (?) for both lagoon and coastal sea-bottom sediments, respectively. Generally, the sediments in the study area consist mostly of coarse to fine particles. The major portions of the sediment are negatively skewed. This indicates that the study area is under the influence of the rather strong wave and current action. The study also encompassed the geophysical survey that was conducted near the coastal zone of the study area. The high-resolution seismic sub-bottom profiling technique is the standard method employed to map geological features and locate structures below the surface of the seafloor. Data obtained from seismic records were used to interpret the seismic reflectors. Three main reflectors (layers), which consist of the seabed and the seabed multiple, were traced using Sonar Web Pro software, and the results showed a uniform distribution pattern for all stations surveyed. It is envisaged that this method could be an effective way to image the marine subsurface structures; thus, its use is anticipated in the higher degrees of sedimentary research and marine resource exploration.
机译:在Setiu湿地的泻湖和沿海地区进行了一项研究,以确定其沉积物的一般特征和粒度分布。分别从泻湖地区的39个站点和沿海地区的8个站点收集了沉积物样本,并分析了它们的沉积学特征(平均,分类,偏斜和峰度)。泻湖和沿海海底沉积物的沉积物平均粒径分别在0.06-2.52和2.12-2.69 phi(?)之间。通常,研究区的沉积物主要由粗颗粒到细颗粒组成。沉积物的主要部分为负偏斜。这表明研究区域受到了相当大的波浪和潮流的影响。该研究还包括在研究区域沿海地区附近进行的地球物理调查。高分辨率地震子底部轮廓分析技术是用于绘制地质特征图并在海底表面以下定位结构的标准方法。从地震记录中获得的数据用于解释地震反射体。使用Sonar Web Pro软件追踪了三个主要的反射器(层),它们由海床和海床多重组成,并且结果显示所有被测站点的分布模式都是均匀的。可以设想,该方法可能是对海底结构成像的有效方法。因此,有望将其用于更高水平的沉积研究和海洋资源勘探。

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