中国水利水电科学研究院学报Issue(2)：113-121,9.DOI:10.13244/j.cnki.jiwhr.2014.02.001
13至19世纪黄淮间运河自然史研究
Study on natural history of The Grand Canal between the Yellow River and Huai River during 13th and 19th century
摘要
Abstract
In 1128AD, the Yellow River changed its course from the Sishui River to the Huai River, which changed the relationship between the canal and other natural rivers since Warring States. The Huitong River and the Canal south of Xuzhou section, which was excavated in the Yuan dynasty, formed a special structure between the Canal and the Yellow River:in term of advantage, the Yellow River served both as the water source and as the waterway for the Canal, however, the Yellow River also brought the Canal a big distraction as its frequent burst. The paper studied the process of reconstruction of the Canal between the Yellow River and the Huai River as weel as the evolution of the regional water envi-ronment. The processes are listed as follows:(1)The waterway north of Xuzhou, the Nailaopo River, which was created by the flood of the Yellow River, has played a crucial role in the evolution of the waterway in south of Jining section and the Sishui basin. (2)The breach of the Yellow River, north of Xuzhou sec-tion had a direct impact on the yield of the Canal water between the Huitong caral and the Yellow River. In early Ming dynasty,with much effort of taking the water from the Bianhe River and Qinhe River to the Yellow River, the navigation between the Huitong canal and the Yellow River had been maintained for nearly 200 years. However,it was interrupted because of the siltation of the Xuzhou Hong channel and the Lvliang Hong Channel at last. (3)The silting of the Huitong River from Jining to Xuzhou section, was the main cause of regional water environmental change,and also the major reason for forming of the Jiahe Riv-er, the Middle Canal, Weishan Lake and other Lakes. Since these lakes could regulate the water as well as water tanks,the waterway of the Grand Canal finally separated from the Yellow River,and then naviga-tion became more unimpeded in the later 200 years. Therefore,the thesis conclusion are summarized as fol-lows: during the period of 700 years, the natural environment of the Huaibei Plain had changed drastically under the combined action of silt accumulation by the flood of the Yellow River, and the application of the Canal engineering system, which becomes an inconvenient natural historical characteristic of the Canal heritage system.关键词
自然史/黄河/运河/会通河/中运河Key words
natural history/Yellow River/Sishui River/Grand Canal/Huitong Canal/Middle Canal分类
水利科学引用本文复制引用
谭徐明,陈方舟,李云鹏,万金红..13至19世纪黄淮间运河自然史研究[J].中国水利水电科学研究院学报,2014,(2):113-121,9.基金项目
科技部基础性工作专项 （）
