摘要
黄浦江水系是太湖流域的一个有机组成部分，其发育的过程与太湖流域水文环境变化密切相关。由于北宋开始的海平面上升，太湖地区水文环境发生重要变化，湖群扩张，三路排水格局转为吴淞江一路，吴淞江曲流发育。这个变化是黄浦江水系开始发育的动力。13世纪末海平面下降，又导致了太湖地区的水文环境发生相应改变。吴淞江的迅速淤浅，推动黄浦江水系的全面成熟和发展。
Huangpu River system is a component part of the Taihu Lake valley- Its developing proccss is closely related to the hydrologic enviroment of the Taihu Lake valley- Because of the rising of sea level from the beginning of the Song dynasty,the hudrologic environment in Taihu region went through great changes f including expansion of lake-groups, change from three drainage systems to one (Wusongjiang drainage system ), and the meander channeling of Wusongjiang River. These changes became the root cause of the development of Huangpu River system. In the end of the 13th century,the descending of sea 1evel led to a corresponding change of the hydrologic environment in Taihu region. The rapid deposition of Wusongjiang River and the resultant shallowing of it have brought about all-round maturation and development of Huangpu River system.
出处
《复旦学报（社会科学版）》
CSSCI
北大核心
1997年第6期54-59,111,共7页
Fudan Journal（Social Sciences）
基金
国家自然科学基金!9471072
