%0 Journal Article
%T Constructing Huaihe River channels separated from Hongze Lake flowing into Yellow Sea
与洪泽湖分离的淮河入海水道可行性分析
%A XUE Chun-ting
%A ZHOU Liang-yong
%A
薛春汀
%A 周良勇
%J 地理研究
%D 2010
%I
%X The Huaihe River was an independent river directly flowing into the Yellow Sea before 1128. It became a tributary of the Yellow River in 1128~1851. The lower Yellow River channel shifted to north and entered the Bohai Sea in 1855. Actually, the Huaihe River has been a tributary of the Yangtze River since 1851. At present, after going into the Hongze Lake, the Huaihe River water flows into the sea by four routes. By constructing a channel separated from the Hongze Lake along the northern coast of the lake, and deeply excavating the present Huaihe River Channel to Sea and the Huaishu River-Beiliutang River-New Yihe River channels, water would directly flow into the Yellow Sea and no longer to the Yangtze River. An annual 1000×104 t of suspended sediments (increasing by 860×104 t more than present) would deposit on the coast from Lianyungang to the Sheyang River mouth. The coastal erosion from Lianyungang to the Sheyang River mouth would be ended: the northern section would be stable and the southern section would slowly prograde, forming a new Huaihe River delta. Meanwhile, the sediments would not accumulate on the middle Huaihe River channel and Hongze Lake, and would effectively reduce inundation in the middle Huaihe River reaches.
%K Huaihe River
%K Hongze Lake
%K sedimentation in channel
%K channel separated from lake
%K coastal erosion
淮河
%K 洪泽湖
%K 河道淤积
%K 河湖分离
%K 海岸侵蚀
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=869B153A4C6B5B85&jid=C0C75E88BA2EE501C8298896F64A711F&aid=2302E80842FD79E9ABB16DDE0FEA881D&yid=140ECF96957D60B2&vid=771469D9D58C34FF&iid=708DD6B15D2464E8&sid=3967641A4A35D81D&eid=77EAE2F82592C167&journal_id=1000-0585&journal_name=地理研究&referenced_num=0&reference_num=0