The response of sedimentary record to catchment changesinduced by human activities in the western intertidal flat ofYalu River Estuary, China

SHI Yong LIU Zhishuai GAO Jianhua YANG Yang WANG Yaping

石勇, 刘治帅, 高建华, 杨旸, 王亚平. 鸭绿江河口西岸潮滩沉积对流域人类活动的响应[J]. 海洋学报英文版, 2017, 36(4): 54-63. doi: 10.1007/s13131-016-0941-7
引用本文: 石勇, 刘治帅, 高建华, 杨旸, 王亚平. 鸭绿江河口西岸潮滩沉积对流域人类活动的响应[J]. 海洋学报英文版, 2017, 36(4): 54-63. doi: 10.1007/s13131-016-0941-7
SHI Yong, LIU Zhishuai, GAO Jianhua, YANG Yang, WANG Yaping. The response of sedimentary record to catchment changesinduced by human activities in the western intertidal flat ofYalu River Estuary, China[J]. Acta Oceanologica Sinica, 2017, 36(4): 54-63. doi: 10.1007/s13131-016-0941-7
Citation: SHI Yong, LIU Zhishuai, GAO Jianhua, YANG Yang, WANG Yaping. The response of sedimentary record to catchment changesinduced by human activities in the western intertidal flat ofYalu River Estuary, China[J]. Acta Oceanologica Sinica, 2017, 36(4): 54-63. doi: 10.1007/s13131-016-0941-7

鸭绿江河口西岸潮滩沉积对流域人类活动的响应

doi: 10.1007/s13131-016-0941-7

The response of sedimentary record to catchment changesinduced by human activities in the western intertidal flat ofYalu River Estuary, China

  • 摘要: 对潮滩柱状沉积物粒度的垂向分布进行分析,结合流域水文资料和人类活动,可得出鸭绿江河口西岸潮滩沉积环境如何响应流域变化。可获取年份的水文资料显示:鸭绿江入海输沙量及径流量呈阶段性减小,可划分为1958-1970、1971-1990和1991-2009三个阶段,流域水库建设及植被覆盖率是其主控因素。1940-2010年间的柱状沉积物中敏感组分的变化可分为四个时期:1940-1950、1951-1980、1981-1990和1991-2010。潮滩沉积物的垂向粒径变化在1960-1980年间主要受流域植被覆盖率及水库建设控制,而1981-1990年间则与降雨量及土壤侵蚀强度直接相关。1990-2009年间入海径流量及输沙量的进一步减少,导致河口潮间带沉积物的粒径逐渐增大,及敏感组分中泥质成分含量的增加。
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  • 收稿日期:  2015-12-19
  • 修回日期:  2016-05-05

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