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地理学报  2007 

长江口表层沉积物分布特征及动力响应

DOI: 10.11821/xb200701009, PP. 81-92

Keywords: 长江口,沉积物,中值粒径,潮流

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Abstract:

基于长江口2003年2月采集的58个表层沉积物样品及以同步水动力资料的分析表明,表层沉积物中值粒径自江阴—口外逐渐变细,由江阴附近的217.8μm减少到南槽口外的12.1μm;浑浊带海域表层沉积物中值粒径北港最大,平均为126.2μm,北槽其次,平均为48.4μm,南槽最小,平均为14.2μm;口外海域则北槽最大,为22.4μm,北港其次,为16.5μm,南槽最小,为12.1μm。沉积物分选性大多为中等—很差,中值粒径越大,分选系数越小;沉积物偏度大多是近对称—极正偏;峭度表现为中等峭度—很窄尖。横沙以上区域表层沉积物类型以砂为主,口外海域沉积物类型以粘土质粉砂为主,浑浊带海域表层沉积物类型复杂多样。长江口主槽表层沉积物中值粒径与落潮历时、Ve/Vf值和余流值等动力参数呈正相关关系,落潮动力条件是决定长江口表层沉积物中值粒径大小的主要动力因素。

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