1. 中国地质大学(武汉)地质过程与成矿预测全国重点实验室
2. 煤炭工业规划设计研究院有限公司
纸质出版:2026
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李宇峰, 刘金存, 刘金华, 等. 长江口及邻近海域表层沉积物Sr、Nd同位素组成及意义[J]. 地质科技通报, 2026,45(2):262-273.
李宇峰, 刘金存, 刘金华, et al. 长江口及邻近海域表层沉积物Sr、Nd同位素组成及意义[J]. Bulletin of Geological Science and Technology, 2026, 45(2): 262-273.
李宇峰, 刘金存, 刘金华, 等. 长江口及邻近海域表层沉积物Sr、Nd同位素组成及意义[J]. 地质科技通报, 2026,45(2):262-273. DOI: 10.19509/j.cnki.dzkq.tb20240401.
李宇峰, 刘金存, 刘金华, et al. 长江口及邻近海域表层沉积物Sr、Nd同位素组成及意义[J]. Bulletin of Geological Science and Technology, 2026, 45(2): 262-273. DOI: 10.19509/j.cnki.dzkq.tb20240401.
长江口是连接陆地和海洋的重要枢纽,因其复杂的地形、丰富的陆源物质以及与人类活动的紧密联系,受到学者们的广泛关注。以长江口及其邻近海域海底表层沉积物为研究对象,系统分析了Sr、Nd同位素以及微量元素的地球化学行为。结果表明,长江口及邻近海域沉积物主要由陆源物质构成,源自长江流域的沉积物占据主导地位,部分物质来自古黄河三角洲。海陆交互区域的Nd元素由于胶体凝聚现象显著富集,而复杂的水动力条件导致该区域的沉积物粒径较细,Sr元素则表现出明显的贫化。通过基于R语言的稳定同位素混合模型(SIMMR)分析,发现长江中下游对海陆交互区域表层沉积物的贡献有所增加。长江上游的物质由于大坝建设被大量截留,导致中下游河道从沉积的“汇”转变为泥沙供应的“源”,从而增加了中下游物质对河口及邻近海域沉积物的贡献。尽管如此,长江上游物质仍在长江口沉积物中占据主导地位。研究成果揭示了长江口及邻近海域的沉积环境和源汇过程,为揭示地表物质循环过程、探究海洋环境演化提供重要信息。
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