论文

人类活动对公元1194年以来黄河河口延伸速率的影响

展开
  • 中国科学院地理科学与资源研究所,北京100101
许炯心(1948-),男,研究员,博士生导师。从事河流地貌研究工作,共发表论文110余篇,出版专著4部(含合著)。

收稿日期: 2001-02-01

  修回日期: 2001-03-01

  网络出版日期: 2001-01-24

基金资助

中国科学院知识创新工程重要方向项目(KZCX2-20705);国家重点基础研究规划项目(G1999043604)

The Yellow River Mouth Extension Since 1194 as Influenced by Human Activities

Expand
  • Institute of Geographical Sciences and Natural Resources Research,CAS, Beijing 100101 China

Received date: 2001-02-01

  Revised date: 2001-03-01

  Online published: 2001-01-24

摘要

以近 50年来的观测资料和公元 1 1 94年以来苏北废黄河和现代黄河的历史文献资料为基础,在宏观时间尺度上 (1 0 2 ~ 1 0 3年 )研究了人类活动对黄河口延伸速率的影响。结果表明,废黄河口的延伸可以分为两个阶段,1 1 94~ 1 578年为第一阶段,河口延伸速率较慢 ;1 579~ 1 855年为第二阶段,河口延伸速率大大加快。 1 855年以来现代黄河河口延伸速率的变化曲线可以分为 3个阶段,分别用 3条斜率不同的直线来拟合。 3条直线之间的两个转折点可以代表人类活动的方式和强度发生改变的临界点。由此建立了人类活动影响下现代黄河三角洲河口延伸过程的三阶段模式。

本文引用格式

许炯心 . 人类活动对公元1194年以来黄河河口延伸速率的影响[J]. 地理科学进展, 2001 , 20(1) : 1 -9 . DOI: 10.11820/dlkxjz.2001.01.001

Abstract

Based on the instrument measured data in the past 50 years and the data extracted from historical documents, a study has been made of the human activities on the river mouth extension, at a time scale of 10 2~10 3 years. During the period studied, the Yellow River empties into the Yellow Sea and Bohai Sea, successively, and the deltas it has shaped are known as Abandoned and Modern Yellow River Deltas. The extension of the Abandoned Yellow River can be divided into 2 stages. The first is from 1194 to 1578, during which the extension rate of river mouth was rather slow. The second is from 1579 to 1855, during which the extension rate was greatly accelerated. The curve showing the temporal variation of the extension rate of the modern Yellow River Mouth can be fitted by 3 straight lines with different slopes. Accordingly, the change from 1855 to present can be divided into 3 stages, and the turning points between the 3 straight lines may be regarded as the threshold points that indicates the marked changes in the manner and degree of human activities. On this basis, a 3 stage model has been put forward to describe the process of river mouth extension as a response to the changing human activities.

参考文献

[1]  庞家珍,司书亨.黄河河口演变[J].海洋与湖沼,1979,10(2):136~141.

[2]  郭永盛.现代黄河三角洲变迁[J].海洋科学,1980(1):30~40.

[3]  尹学良.黄河口的河床演变[J].泥沙研究,1986(4):13~35.

[4]  叶青超,陆中臣,杨毅芬等.黄河下游河流地貌[M].北京:科学出版社,1990.40~51,155~170.

[5]  叶青超主编.黄河流域环境演变与水沙运行规律研究[M].济南:山东科技出版社,1994.108~115.

[6]  钱意颖,叶清超,周文浩.黄河干流水沙变化与河床演变[M].北京:中国建材工业出版社,1993.160~200.

[7]  曾庆华,胡春洪等.黄河口演变规律及整治[M].济南:黄河水利出版社,1998.

[8]  水利部黄河水利委员会黄河水利史述要编写组.黄河水利史述要[M].北京:水利出版社,1982.

[9]  中国科学院中国自然地理编辑委员会.中国自然地理(历史自然地理)[M].北京:科学出版社,1982.

[10]  尤联元.小浪底工程修建对黄河河口淤积的影响[J].地理科学进展,2000,19(2):142~148.

[11]  中国科学院黄土高原综合科学考察队.黄土高原地区自然环境及其演变[A].见:杨勤业主编.北京:科学出版社,1991.125~152.

[12]  杜瑜.甘肃、宁夏黄土高原历史时期农牧业发展研究[A].见:王守春主编.黄河流域环境演变与水沙运行规律研究文集[C].北京:海洋出版社,1993.102~155.
文章导航

/