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机构地区:[1]中国科学院海洋研究所
出 处:《海洋科学集刊》2001年第1期68-82,共15页Studia Marina Sinica
基 金:中国科学院重点资助项目;KZ952-SI-424号;山东省软科办重点资助项目;97-8号
摘 要:随着我国经济的快速发展,黄河三角洲已经成为重要的石油工业基地和重要的农业开发区,兴建了许多港口和养殖基地。历史证明,由人工控制的黄河尾闾段河道已处于相对稳定状态,在三角洲区的经济发展过程中起了重要的作用。1976年黄河改道由清水沟流路入海以来,该流路已行水20多年,为了保障该区的发展,有关部门提出了稳定流路多年不变的方针,并经专家论证,可以继续使用50—70年。Input of huge quantities of sediment discharged to the sea and change of the lower course of the Huanghe River cause great changes in coastal and submarine geomorphology and sand movement. The sand spit on the Huanghe River mouth extended 40 km to seaward from 1976-1996. The sand spits extending velocity is 2. 1 km/a at present, and its front is less than 50 km from the east and south coast of the Laizhou Bay. If it continuously extend for some ten years, this part of Laizhou bay will become a lagoon. By that time, the marine ecology environment will change largely and the Xiaoqinghe River mouth and adjacent harbor will be silted. Many ports have been built on the Huanghe River delta coast and adjacent areas. The continued extension of the river mouth spit, wrong choose of inlet position, untimely use of the rivers lower course, any and all of these will affect to construction of ports there. The Huanghe River changed its lower course and emptied into Laizhou Bay from the Qing 8 branch in Aug. 1996. When the lower course started to change, the inlets direction of the main axis was N81°30′E. However two months later, it extended NW. Sandy sediment discharged from the Huanghe River transported along shore to NW and turbidity water with fine sediment reached the vicinity of Dongying Harbor. In order to decrease the influence of sediment discharged from the Huanghe River on coastal ports in the adjacent coast, it is necessary to scientifically choose the position of the inlet, correctly control the use time of the rivers lower course, and change the direction of inlet in due course.
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