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广东省茂名市典型河流沉积物粒度特征及分布规律

Grain Size Characteristics and Distribution of Typical Fluvial Sediments in Maoming City, Guangdong Province

  • 摘要: 为了研究河流沉积物粒度参数空间分布规律,根据茂名市地理环境以及河流走向,在茂名市8条典型河流里采集115个表层沉积物样品并用激光粒度仪进行粒度分析。本次研究均只检测出砂、粉砂和黏土3种粒级组分。粉砂是主要的组分,砂和黏土含量相似但呈现出相反的分布特征。研究区表层沉积物平均粒径为4.37~7.3φ,变化范围较小;分选系数1.53~2.48,总体上分选性较差;偏度值-0.09~0.73,沉积物大多数处于正偏;峰度值0.70~1.17,峰态总体上平坦。鉴江和罗江表层沉积物样品呈现分选系数小而平均粒径大的规律,小东江和黄华江表层沉积物样品呈现分选系数大而平均粒径小的规律。鉴江干流平均粒径,中游>下游>上游,呈现先增大后减小的趋势。黄华江干流粒径呈现减小的趋势,沉积物趋向于粗端。罗江干流平均粒径呈现减小的趋势,河流流速大不易于细粒沉积。研究的粒度参数与粒级分布特征结论,为相关的研究提供数据支持和理论参考。

     

    Abstract: To investigate the spatial distribution characteristics of sediment grain size parameters in the surface sediments of rivers, this study collected 115 surface sediment samples from eight typical rivers in Maoming City, based on the geographical environment and the course of the rivers in the city. The collected samples were analyzed using a laser particle size analyzer. The study revealed that only three particle size components, namely sand, silt, and clay, were detected in the surface sediments of rivers in the research area. Silt was identified as the predominant component, with all eight rivers exhibiting silt content exceeding 50%. The content of sand and clay was similar, both registering below 20% in the studied rivers; however, they displayed contrasting distribution patterns within the river systems. The average grain size of surface sediments in the study area falls within the range of 4.37 to 7.3φ, indicating a relatively small variation. The sorting coefficients range from 1.53 to 2.48, suggesting overall poor sorting. Skewness values range from-0.09 to 0.73, with most sediments exhibiting positive skewness. Kurtosis values range from 0.70 to 1.17, indicating a generally flat peak. Specifically, sediments from the Jianjiang River and Luojiang River demonstrate a trend of low sorting coefficients and large average grain sizes. In contrast, sediments from the Xiaodong River and Huanghua River exhibit a pattern of high sorting coefficients and small average grain sizes. The average grain size of the main stream of the Jianjiang River, midstream > downstream > upstream, showed a trend of increasing and then decreasing. The main stream of Huanghua River showed a decreasing trend in particle size, and the sediment tended to be coarse-end. The average particle size of Luojiang River main stream showed a decreasing trend, and the river flow was not easy for fine grain deposition. The conclusions of this study on the characteristics of particle size parameters and grain size distribution provide data support and theoretical reference for related studies.

     

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