历史时期大清河南系的变迁研究——兼谈与白洋淀湖群的演变关系

发布时间：2018-01-19 03:21

本文关键词： 历史时期大清河南系水系变迁白洋淀湖群河湖关系　出处：《中国历史地理论丛》2012年02期 　论文类型：期刊论文

【摘要】：海河水系以"清"为名的大清河其实只是相对于位居其南、其北著名浊流滹沱河与永定河而言的"清"河。历史时期,随着上游水土流失的日益加剧,大清河南系各河含沙量不断增高,干流段决徙逐渐频繁。本文利用历史文献,对先秦以来在自然与人类活动共同影响下的大清河南系的变迁进行了探讨,揭示和总结了两千余年来水系格局变动的基本过程及主要特点。大清河南系又是白洋淀湖群地表径流补给最大的水源,上述研究结论还将是理解和分析这一著名湖群演变不可忽视的重要基础。
[Abstract]:In fact, the Daqing River in the name of "Qing" in the Haihe River system is only relatively situated in the south. The Hutuo River and the Yongding River in the north are known as the "Qing" River in the north. In the historical period, with the increasing water and soil loss in the upper reaches of the river. The sediment content of Henan River in the Qing Dynasty is increasing, and the decision and migration of the main stream are becoming more and more frequent. This paper discusses the changes of Henan system in the Qing Dynasty under the influence of the natural and human activities since the Pre-Qin Dynasty by using the historical documents. This paper reveals and summarizes the basic process and main characteristics of the change of water system pattern in the past 2,000 years. The Henan system is also the largest source of surface runoff recharge in Baiyangdian Lake Group. The above conclusions will also be an important basis for understanding and analyzing the evolution of this famous lake group.
【作者单位】：华东理工大学社会与公共管理学院;
【基金】：国家自然科学基金项目“明代以来海河水系变迁与河、湖关系及其人文驱动因素的研究”(40801073) 中央高校基本业务费专项基金项目“行政干预背景下的水资源配置及其社会影响——以海河流域为中心的实证探索”(WE1023001)
【分类号】：K928.6
【正文快照】： 大清河属海河水系五大支流之一,位于永定河系以南、子牙河系以北,由于处在著名浊流永定河与滹沱河之间,河水相对较清,故曰“清河”。①其实大清河的“清”只是相对于永定河与滹沱河而言的,事实上,现京广铁路线以西的支流多为沙质河床,纵坡较陡,河道宽浅多沙,加上南北浊流永定

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