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地理学报  2012 

黄河三角洲岸线及现行河口区水下地形演变

DOI: 10.11821/xb201203008, PP. 368-376

Keywords: 黄河三角洲,岸线,河口,水下地形,演变

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Abstract:

根据实测的岸线和水深数据,利用Surfer和Mapinfo等软件进行数据处理,结合不同阶段利津站输沙量,分析了黄河三角洲岸线及现行河口区水下地形演变。结果表明1953-2000年,68%左右的入海泥沙淤积在口门和滨海区。由于入海流路变迁,不同岸段的岸线变化具有各自的特征。刁口河流路以西岸线基本稳定;刁口河流路以东—孤东油田以北岸线经历先淤后冲,属于强侵蚀岸段,但在防潮大堤的保护下得到人为控制下的稳定;清水沟流路形成的岸线整体向海淤进,但清8出汊后,清水沟老河口沙嘴南侧出现侵蚀。1976-1996年,现行河口(清水沟流路)水下地形总体上表现为淤积,顶坡段变缓,前坡段变陡。1996-2005年,清水沟老河口水下地形顶坡段和前坡段发生侵蚀,底坡段呈现淤积;出汊新河口水下地形继续淤积,但程度和范围都比1976-1996年的小。孤东油田近岸侵蚀加剧。

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