地理学报 ›› 2003, Vol. 58 ›› Issue (2): 247-254.doi: 10.11821/xb200302012

• 河流环境 • 上一篇    下一篇

黄河下游2300年以来沉积速率的变化

许炯心1, 孙季2   

  1. 1. 中国科学院地理科学与资源研究所,北京 100101;
    2. 西南科学技术大学,四川 绵阳 621000
  • 收稿日期:2002-05-08 修回日期:2002-11-16 出版日期:2003-03-25 发布日期:2003-03-25
  • 作者简介:许炯心 (1948-), 男, 四川绵阳人。研究员, 博士生导师。长期从事河流地貌研究工作。共发表论文130余篇。E-mail:xujx@igsnrr.ac.cn
  • 基金资助:

    国家自然科学基金重大项目(59890200); 中国科学院地理科学与资源研究所知识创新工程领域前沿项目(CXIOG-A00-05-01)

Sedimentation Rate Change in the Lower Yellow River in the Past 2300 Years

XU Jiongxin1, SUN Ji2   

  1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China
  • Received:2002-05-08 Revised:2002-11-16 Online:2003-03-25 Published:2003-03-25
  • Supported by:

    National Natural Science Foundation of China, No.59890200; Knowledge Innovation Project of the Institute of Geographic Sciences and Natural Resources Research, CAS, No.CXIOG-A00-05-01

摘要:

采用沉积学方法提取沉积速率的记录,利用历史文献研究的方法提取气候与人类活动变化的信息,对黄河下游2300年以来的沉积速率的变化及其与气候、植被及人类活动的关系进行了研究,揭示黄河流域地貌系统对气候变化及人类活动所导致的土地覆被、土地利用方式变化的响应过程。研究表明,黄河流域地貌系统中的下游沉积带对于中游侵蚀带的响应是灵敏的,流域植被和土地利用方式的变化,是导致下游河道沉积加速的主导因素;这种变化主要取决于人类活动,同时与气候的变化也有一定关系。在沉积加速的过程中,公元7世纪至10世纪以及18世纪中叶以来,表现为两个突变时期。

关键词: 沉积速率, 人类活动, 气候变化, 黄河

Abstract:

Sedimentary method has been used to determine the historical sedimentation rate in this study, and historical literature has been studied to obtain information on climate change and human activities. Based on the data obtained in this way, the temporal variation in the sedimentation rate of the lower Yellow River in the past 2300 years has been studied in relation with climate change and human activities. The results indicate that the response of the sedimentation zone of the Yellow River system to the change in the erosion zone is sensible. The changes in vegetation and land use, both related to climate change and human activities, are two major controls for the acceleration of sedimentation rate. In addition, changes in strategies for the harnessing of the lower Yellow River are also responsible for such acceleration. During the process of accelerated sedimentation in the past 2300 years, the period of the 7th-10th centuries and the period since the mid-19th century have been identified as two periods with abrupt changes.

Key words: sedimentation rate, human activities, climate change, the lower Yellow River