首页> 外文期刊>Arabian journal of geosciences >Distribution of grain size, clay mineralogy and organic matter of surface sediments from Tirumalairajanar Estuary, Tamilnadu, east coast of India
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Distribution of grain size, clay mineralogy and organic matter of surface sediments from Tirumalairajanar Estuary, Tamilnadu, east coast of India

机译:印度东海岸泰米尔纳德邦Tirumalairajanar河口的地表沉积物的粒度,粘土矿物学和有机质分布

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摘要

The aim of this study is to understand the various sources and factors controlling the abundance and distribution of clay minerals, sand, silt, clay and organic matter of the surface sediments of Tirumalairajanar Estuary in two different seasons. The study was undertaken for two seasons, based on ten selected stations all along the estuary, mouth and freshwater zone. Furthermore, along the estuary region, clay and silt were observed and also at few stations in the upstream end. Organic matters in the sediments appeared to be the main mechanisms for the distribution of clay minerals in estuary indicated that the distributions of clay minerals were comparatively higher during postmonsoon than in premonsoon season. The clay mineral assemblage consists mainly of chlorite, kaolinite, montmorillonite, illite and very scarce gibbsite. The clay from the sediments has been separated and studied for mineral identification using X-ray diffraction analysis. The present study also reveals that sediment texture is one of the main controlling factors for the distribution of organic matter.
机译:这项研究的目的是了解在两个不同季节中控制Tirumalairajanar河口表层沉积物的粘土矿物,沙子,粉砂,粘土和有机物的丰度和分布的各种来源和因素。该研究基于河口,河口和淡水区的十个选定站点进行了两个季节的研究。此外,在河口区域,在上游端的几个站点也观察到粘土和淤泥。沉积物中的有机物似乎是河口黏土矿物分布的主要机制,这表明季风后黏土矿物的分布比季风前季节要高。粘土矿物组合主要包括绿泥石,高岭石,蒙脱石,伊利石和非常稀少的菱铁矿。已经从沉积物中分离出粘土,并使用X射线衍射分析进行了矿物鉴定研究。本研究还表明,沉积物质地是有机质分布的主要控制因素之一。

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