三门湾表层沉积物黏土矿物特征及来源分析

    Clay mineral assemblages and provenance in the surface sediment of the Sanmen Bay

    • 摘要: 利用XRD方法分析了三门湾表层沉积物中的黏土矿物组成和含量,结合沉积物粒径趋势分析及长江和三门湾流域中小河流的黏土矿物组合特征,开展了三门湾沉积物的来源分析。结果表明,三门湾表层沉积物中黏土矿物以伊利石为主,其次为高岭石和绿泥石,蒙脱石含量最低。其中,伊利石高值区位于海湾中部,高岭石和绿泥石高值区分布在港汊附近,蒙脱石则在近岸呈斑块状分布。三门湾现代表层沉积物主要来源于长江入海物质,海湾周边短源山溪性河流带来的物质仅影响了河口近岸区。

       

      Abstract: The content and composition of clay minerals from 83 surface samples in the Sanmen Bay were analyzed with XRD. Through grain size trends analysis and clay minerals assemblages characteristics of related rivers, the provenance of clay minerals and sediments resources of the Sanmen Bay were discussed. The results show that the majority of clay mineral in surface sediment in Sanmen Bay are illite, followed by kaolinite and chlorite, and the minority is smectite. The higher abundance of illite is distributed in the middle of the Sanmen Bay, and the higher kaolinite and chlorite located at the upper bay area either near the river estuaries or bay branches, and smectite displayed patchy distributions along the coast. The surface sediment in Sanmen Bay mainly comes from the Changjiang River, while sediments from small local mountainous rivers only affect the estuary area.

       

    /

    返回文章
    返回