欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2011, Vol. 22 ›› Issue (02): 467-472.

• 研究报告 • 上一篇    下一篇

黄河改道以来黄河三角洲演变过程及其驱动机制

韩广轩1,栗云召1,2,于君宝1**,许景伟3,王光美1,张志东1,毛培利1,刘玉虹1   

  1. 1中国科学院烟台海岸带研究所滨海湿地生态实验室/山东省海岸带环境过程重点实验室, 山东烟台 264003;2中国科学院研究生院, 北京 100049; 3山东省林业科学院, 济南 250014
  • 出版日期:2011-02-18 发布日期:2011-02-18

Evolution process and related driving mechanisms of Yellow River Delta since the diversion of Yellow River.

HAN Guang-xuan1, LI Yun-zhao1,2, YU Jun-bao1, XU Jing-wei3, WANG Guang-mei1, ZHANG Zhi-dong1, MAO Pei-li1, LIU Yu-hong1   

  1. 1Laboratory of Coastal Wetland Ecology/Shandong Province Key Laboratory of Coastal Zone Environment Processes, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, Yantai 264003, Shandong, China|2Graduate University of Chinese Academy of Sciences, Beijing 100049, China|3Shandong Academy of Forestry, Ji’nan 250014, China
  • Online:2011-02-18 Published:2011-02-18

摘要: 基于1976—2009年的23期遥感影像,并结合1976—2008年利津站水沙数据以及黄河流域年均降水量数据,定量分析黄河入海水沙特征以及黄河三角洲演变过程及其驱动机制. 结果表明:1976—2008年间,黄河入海年径流量和年输沙量呈现出年际变化大和丰枯水(沙) 年交替的特征,但总体均呈下降趋势;清水沟流路河口三角洲岸线和面积变化总体呈淤积增长趋势,三角洲的发育过程大致分1976—1985年、1986—1995年和1996—2009年3个阶段,3 个阶段的增长速率逐阶段递减;黄河三角洲岸线和面积与利津站累积输沙量之间均呈显著的指数函数关系;黄河流域降水量的年际波动与利津站入海输沙量年际波动基本同步,并具有相关性,说明黄河流域降水量的年际波动是引起入海径流量和输沙量波动的重要原因.

关键词: 黄河三角洲, 岸线, 演变, 驱动机制

Abstract: Based on the 23 sheets of remote sensing images from 1976 to 2009, in combining with the water and sediment data from Lijin station and the annual precipitation data of Yellow River Basin from 1976 to 2008, this paper quantitatively analyzed the features of water and sediment discharge from Yellow River, and the evolution process of Yellow River Delta and related driving mechanisms. In 1976-2008, the annual runoff and the annual sediment discharge into sea changed largely and frequently, but overall, presented a decreasing trend. Since the course of the Yellow River changed its direction to Qingshui channel in 1976, the Delta coastline and area were generally in a silting-up state. The evolution process of the Delta could be approximately divided into three stages, i.e., 1976-1985, 1986-1995, and 1996-2009, and the increasing rate of the Delta decreased with the stages. The coastline and area of the Delta were significantly exponentially correlated to the sediment accumulated at Lijin station, and the inter-annual variation of the precipitation of the Yellow River Basin had a strong correlation with that of the sediment at Lijin station, suggesting that the annual variation of the precipitation in Yellow River Basin was the main factor affecting the runoff and sediment discharge into sea.

Key words: Yellow River Delta, coastline, evolution, driving mechanism