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huang he he kou san jiao zhou hai an de fa yu ji qi dui shang you he dao de ying xiang
Author(s): 
Pages: 211-219
Year: Issue:  3
Journal: Oceanologia et Limnologia Sinica

Keyword:  黄河河口上游河道三角洲海岸溯源冲刷小循环流路上游水位河口延伸溯源淤积黄河口;
Abstract: <正> 河口三角洲河床演变的特点主要是泥沙在河口区堆积而造成的河口延伸。各河口的河流及海洋条件差别很大,河口延伸的情况也迥异。河流输沙量小的河口三角洲,其延伸速度很慢,往往要数百年、甚至数千年才能表现出明显的变化。多沙的河口三角洲,情况则大为不同。亚马孙河、密西西比河、布拉马普特拉河及长江都是入海沙量较大的河流,
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