鸭绿江河口地区沉积物的粒度变化及影响因素

冉隆江, 石勇, 高建华, 刘月, 李富祥, 白凤龙, 李军. 鸭绿江河口地区沉积物的粒度变化及影响因素[J]. 海洋地质与第四纪地质, 2012, 32(2): 31-42. doi: 10.3724/SP.J.1140.2012.02031
引用本文: 冉隆江, 石勇, 高建华, 刘月, 李富祥, 白凤龙, 李军. 鸭绿江河口地区沉积物的粒度变化及影响因素[J]. 海洋地质与第四纪地质, 2012, 32(2): 31-42. doi: 10.3724/SP.J.1140.2012.02031
RAN Longjiang, SHI Yong, GAO Jianhua, LIU Yue, LI Fuxiang, BAI Fenglong, LI Jun. GAIN SIZE VARIATION AND ITS INFLUENCING FACTORS IN THE SEDIMENT CORES OF YALU RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2012, 32(2): 31-42. doi: 10.3724/SP.J.1140.2012.02031
Citation: RAN Longjiang, SHI Yong, GAO Jianhua, LIU Yue, LI Fuxiang, BAI Fenglong, LI Jun. GAIN SIZE VARIATION AND ITS INFLUENCING FACTORS IN THE SEDIMENT CORES OF YALU RIVER ESTUARY[J]. Marine Geology & Quaternary Geology, 2012, 32(2): 31-42. doi: 10.3724/SP.J.1140.2012.02031

鸭绿江河口地区沉积物的粒度变化及影响因素

  • 基金项目:

    国家自然科学基金项目(40976051,40871019,40906042)

详细信息
    作者简介: 冉隆江(1985-),男,硕士生,主要从事河口海岸研究,E-mail:ranlongjiang3050@126.com
  • 中图分类号: P736.2

GAIN SIZE VARIATION AND ITS INFLUENCING FACTORS IN THE SEDIMENT CORES OF YALU RIVER ESTUARY

  • 通过对比鸭绿江河口不同地区柱状样的粒度参数及敏感组分变化规律,分析了河口不同地区沉积动力环境和沉积特征的差异;结合代表性柱状样的210Pb测年,分析了柱状样在不同时期自然和人类活动影响下的沉积特征变化。结果表明,西水道主要受潮流作用而含有泥沙互层,粒度参数变化小;西岸潮滩受潮流和波浪作用含有贝壳碎屑,并在顶部出现粗化层。近几十年来,鸭绿江河口地区沉积特征的变化主要由于人类活动对水沙入海通量的影响:1941年以前柱状样的波动沉积特征反映了河流山溪性特征;1941-1970(1980)年随水沙入海通量减少而呈现砂含量降低、粉砂增加的特征;1970(1980)-1990年由于水沙入海通量变化较小,而呈现沉积物组成和敏感组分保持稳定的特征;但1990年后随水沙入海通量的进一步降低,邻近河口区域的沉积物出现明显的粗化。
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出版历程
收稿日期:  2011-06-30
修回日期:  2011-09-19

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