中国工程科学
中國工程科學
중국공정과학
ENGINEERING SCIENCE
2013年
6期
20-24
,共5页
长江口%河口格局%亚三角洲
長江口%河口格跼%亞三角洲
장강구%하구격국%아삼각주
Yangtze estuary%estuary pattern%sub delta
受到第三驱动力的作用,长江河口发育模式由两侧岬角控制转变为中间依靠工程建筑向外突出的格局。这种格局的转变及利用航道疏浚土吹填,使得横沙东滩不断淤涨成陆。长江口南港南槽与北港之间的长兴岛、九段沙、横沙岛及横沙东滩组成串珠状岛链,形成长江口亚三角洲体系。横沙东滩新形成的约400 km2的土地和18 km深水岸线,加上远期建筑人工岛,可开发河口深水港区,与两侧河口湿地保护区相兼容,为上海提供城市发展的新空间。
受到第三驅動力的作用,長江河口髮育模式由兩側岬角控製轉變為中間依靠工程建築嚮外突齣的格跼。這種格跼的轉變及利用航道疏浚土吹填,使得橫沙東灘不斷淤漲成陸。長江口南港南槽與北港之間的長興島、九段沙、橫沙島及橫沙東灘組成串珠狀島鏈,形成長江口亞三角洲體繫。橫沙東灘新形成的約400 km2的土地和18 km深水岸線,加上遠期建築人工島,可開髮河口深水港區,與兩側河口濕地保護區相兼容,為上海提供城市髮展的新空間。
수도제삼구동력적작용,장강하구발육모식유량측갑각공제전변위중간의고공정건축향외돌출적격국。저충격국적전변급이용항도소준토취전,사득횡사동탄불단어창성륙。장강구남항남조여북항지간적장흥도、구단사、횡사도급횡사동탄조성천주상도련,형성장강구아삼각주체계。횡사동탄신형성적약400 km2적토지화18 km심수안선,가상원기건축인공도,가개발하구심수항구,여량측하구습지보호구상겸용,위상해제공성시발전적신공간。
The natural evolution pattern of the Yangtze estuary was changed by human activities. The estuary is not controlled by the sides’cape as it did in the past. In the middle of the estuary,a beaded island chain was formed by the Changxing Island,the Jiuduansha mudflat,the Hengsha Island and the Hengsha east shoal,and a new sub estuarine delta is coming into being. This sub delta keeps expanding outward relying on the engineering constructions. The Hengsha east shoal will become land due to mudflat enclosure and siltation with waterway dredging soil. The new reclaimed land area could reach 400 km2 and more than 18 km deep-water shoreline exists along the north coast of the mudflat edge. The plenty resources of the new sub estuarine delta and an artificial island outside the estuary could become a new space for Shanghai City development and a suitable lo-cation of deep-water harbor site.