黄河下游2300年以来沉积速率的变化

doi:10.11821/xb200302012

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

黄河下游2300年以来沉积速率的变化

许炯心¹, 孙季²

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

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/Abstract

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

许炯心,孙季. 黄河下游2300年以来沉积速率的变化[J]. 地理学报, 2003, 58(2): 247-254.

XU Jiongxin, SUN Ji. Sedimentation Rate Change in the Lower Yellow River in the Past 2300 Years[J]. Acta Geographica Sinica, 2003, 58(2): 247-254.

参考文献

[1] Schumm S A. The Fluvial System. New York: John Wiley, 1977. 338.

[2] Zhang Ren, Xie Shunan. A discussion of the main cause of the continuous aggradation of the lower Yellow River based on the sedimentation of the old channel of Yellow River from the Ming to Qing dynasties. Sediment Research, 1982, (2).
[张仁, 谢树楠. 废黄河的淤积形态与黄河下游持续淤积的主要原因. 泥沙研究, 1982, (2).]

[3] Xu Hailiang.. The historical sedimentation of the lower Yellow River and its tendency. Journal of Hydraulic Engineering, 1990, (7): 42-48.
[徐海亮. 黄河下游堆积历史与发展趋势. 水利学报, 1990, (7): 42-48.]

[4] Ye Qingchao, Lu Zhongchen, Yang Yifen et al. River Geomorphology of the Lower Yellow River. Beijing: Science Press, 1990.
[叶青超, 陆中臣, 杨毅芬等. 黄河下游河流地貌, 北京: 科学出版社, 1990.]

[5] Ye Qingchao, You Lianyuan, Xu Jiongxin et al. Tendency of the Lower Yellow River as a Hanging River and the Environmental Effects. Zhengzhou: Publishing House for the Yellow River Water Conservancy, 1998. 116-125.
[叶青超, 尤联元, 许炯心等. 黄河下游地上河发展趋势与环境后效. 郑州: 黄河水利出版社, 1998. 116-125.]

[6] Xu Fuling, Zhang Hongmo, Liu Chunxiang. Compilation of the map of old channels of the lower Yellow River using remote sensing images. In: Tian Guoliang (ed.), Remote Sensing Analyses of Rivers and Lakes in the Huang-Huai-Hai Plain. Beijing: Science Press, 1988. 42-50.
[徐福龄, 张洪模, 刘春祥. 应用遥感资料编制黄河下游古河道变迁图. 见: 田国良主编, 黄淮海平原水域动态演变遥感分析. 北京: 科学出版社, 1988. 42-50.]

[7] Ding Lianzhen. A study of river channel training in the lower Yellow River. In: Institute of Water Resources and Hydro-power Research (ed.), Collected Papers of Institute of Water Resources and Hydro-power Research, Sediment Volume, No.11, Beijing: Publishing House for Water Conservancy, 1986. 1-19.
[丁联臻. 黄河下游东坝头以下河道整治经验初步总结. 水利水电科学研究院论文集, 泥沙, No.11, 北京: 水利出版社, 1986. 1-19.]

[8] Xu Jinzhi. Historical large floods and droughts in the middle Yellow River Basin, Geographical Data, 1957, No.1. Beijing: Science Press, 1957.
[徐近之. 黄河中游历史上的大水与大旱, 地理学资料, 第一缉. 北京: 科学出版社, 1957.]

[9] Chen Baosong. On the Population of the Loess Plateau of China. Beijing: Science Press, 1990. 1-122.
[中国科学院黄土高原综合科学考察队, 黄土高原地区人口问题, 陈宝松主编, 北京: 中国经济出版社, 1990. 1-122.]

[10] Yang Pinglin. A study of historical population in the middle Yellow River basin. In: Wang, S (ed.), Collection of Researches on Environmental Changes of the Yellow River Basin and Laws of Water and Sediment Transportation, Vol.5. Beijing: Science Press, 1993. 20-30.
[杨平林. 历史时期黄河中游地区人口地理研究, 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, Vol.5. 北京: 海洋出版社, 1993. 20-30.]

[11] Langbein L B, Schumm S A. Yield of sediment in relation to mean annual precipitation. Transactions, American Geophysical Union, 1958, 39: 1076-1084.

[12] Xu Jiongxin. Zonal distribution of river basin erosion and sediment yield in China. Chinese Science Bulletin, 1994, 39(11): 1356-1361.
[许炯心. 我国流域侵蚀产沙的地带性特征. 科学通报, 1994, 39(11): 1019-1022.]

[13] Wu X, Niu Z, Wang S et al. Historical Changes in Environment and the Resultant Water and Sediment Changes in the Yellow River Basin. Beijing: Meteorological Press, 1994. 65-91.
[吴祥定, 钮仲勋, 王守春等. 历史时期黄土高原植被与人文要素的变化. 北京: 海洋出版社, 1994. 65-91.]

[14] Yang Qinye (ed.). Natural Environment and Its Evolution of the Loess Plateau of China. Beijing: Science Press, 1991. 125-152.
[杨勤业主编. 黄土高原地区自然环境及其演变. 北京: 科学出版社, 1991. 125-152.]

[15] Compilation Group for "A Brief History of Water Conservancy of Yellow River". A Brief History of Water Conservancy of Yellow River. Beijing: Publishing House for Water Conservancy, 1982.
[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. 北京: 水利出版社, 1982.]

黄河下游2300年以来沉积速率的变化

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

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