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黄河调水调沙影响下的现行三角洲叶瓣冲淤演化格局

龙跃 吴晓 毕乃双 张勇 王厚杰

海洋地质前沿2017,Vol.33Issue(3):7-11,5.
海洋地质前沿2017,Vol.33Issue(3):7-11,5.DOI:10.16028/j.1009-2722.2017.03002

黄河调水调沙影响下的现行三角洲叶瓣冲淤演化格局

EVOLUTION OF ACTIVE YELLOW RIVER (HUANGHE) DELTA UNDER THE WATER AND SEDIMENT REGULATION SCHEME (WSRS)

龙跃 1吴晓 1毕乃双 1张勇 2王厚杰1

作者信息

  • 1. 中国海洋大学海洋地球科学学院海底科学和探测技术教育部重点实验室,青岛 266100
  • 2. 中国地质调查局青岛海洋地质研究所,青岛 266071
  • 折叠

摘要

Abstract

Based on the datasets collected from Landsat images and the water and sediment data from the Lijin station in the period of 1996 to 2013,the evolution of the active Yellow River delta under the influence of the Water and Sediment Regulation Scheme (WSRS) are investigated.The result indicates that,after the WSRS,the subaerial delta accreted slowly due to the sediment accumulation in the nearshore area after the dam-regulation.Along with the continuous implementations of WSRS,however,the river bed sediments in the lower reaches are increasingly coarser than ever,resulting in the continuous increase in the critical energy for resuspension of the riverbed sediment.Thus the lower channel could no longer supply coarser sediment to the sea;therefore we speculate the critical sediment load for maintainance of the present delta lobe should increase in the future.

关键词

黄河/调水调沙/入海泥沙通量/三角洲演化

Key words

the Yellow River/Water and Sediment Regulation Scheme (WSRS)/sediment load/delta evolution

分类

海洋科学

引用本文复制引用

龙跃,吴晓,毕乃双,张勇,王厚杰..黄河调水调沙影响下的现行三角洲叶瓣冲淤演化格局[J].海洋地质前沿,2017,33(3):7-11,5.

基金项目

科技部国家重点研发计划(2016YFA0600903) (2016YFA0600903)

海洋地质前沿

OACSCDCSTPCD

1009-2722

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