| 近50 a来辽河口水下三角洲演变特征研究 |
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| 引用本文： | 韩志远,谢华亮,强海洋,李怀远.近50 a来辽河口水下三角洲演变特征研究[J].海洋学研究,2019,37(3):64-72. |
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| 作者姓名： | 韩志远 谢华亮 强海洋 李怀远 |
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| 作者单位： | 交通运输部天津水运工程科学研究所工程泥沙交通行业重点实验室,天津300456;中国自然资源经济研究院,北京101149 |
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| 基金项目： | 国家重点研发计划项目资助(2016YFC0402602);中央级公益性科研院所基本科研业务费项目资助(TKS170202) |
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| 摘 要： | 本文基于近50 a来的辽河口海域的水下地形资料,采用GIS技术手段研究了辽河口水下三角洲的演变特征。研究结果表明:近50 a来辽河水下三角洲外缘(蛤蜊岗子滩西缘和南缘、西滩西缘和南缘)出现较大幅度的侵蚀后退;蛤蜊岗子滩东缘淤积外移,南部滩尾东部有北移东偏趋势;近岸浅滩由淤涨变为基本稳定,局部有所侵蚀后退;受蛤蜊岗子滩向东淤进的影响,蛤蜊岗子滩东侧深槽有所缩窄;蛤蜊岗子滩和西滩之间深槽水域出现拓宽变浅的变化趋势。流域来水来沙减少是近年来辽河口水下三角洲外缘侵蚀后退的主要原因,外缘侵蚀泥沙在波流作用下向河口搬运是蛤蜊岗子滩东侧淤积、深槽缩窄的主要原因,近岸边滩人工围垦对水下三角洲演变的影响值得关注。
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| 关 键 词： | 辽河口 水下三角洲 地貌演变 GIS 蛤蜊岗子滩 |
| 收稿时间： | 2018-11-14 |
Evolution research on subaqueous delta of Liaohe Estuary in recent 50 years |
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| HAN Zhi-yuan,XIE Hua-liang,QIANG Hai-yang,LI Huai-yuan.Evolution research on subaqueous delta of Liaohe Estuary in recent 50 years[J].Journal of Marine Sciences,2019,37(3):64-72. |
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| Authors: | HAN Zhi-yuan XIE Hua-liang QIANG Hai-yang LI Huai-yuan |
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| Affiliation: | 1. Key Laboratory of Engineering Sediment, Tianjin Research Institute for Water Transport Engineering,Ministry of Transport,Tianjin 300456, China; 2. Chinese Academy of Natural Resources Economics, Beijing 101149, China |
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| Abstract: | Based on the topographical data of Liaohe Estuary in recent 50 years, the subaqueous delta evolution of Liaohe Estuary was studied by using GIS methods. The research results are showed as follows:The outer edge of the subaqueous delta of Liaohe Estuary(the western and southern edges of Geligangzi Shoal, the western and southern edges of Xitan Shoal) experienced a relatively erosion progress and the eastern edges of Geligangzi Shoal experienced a accumulation progress and the eastern head of the southern part of Geligangzi Shoal had moved northward and eastward.The Nearshore Shoal between the two river mouths experienced a process from accumulation to stability, and the shoal had eroded partially north of East Trough. Because of Geligangzi Shoal moving eastward, East Trough at east of Geligangzi Shoal had became narrow, and the deep water between Geligangzi Shoal and Xitan Shoal appeared a trend of widening and becoming shallow. The decrease of incoming sediments from Liaohe River was the main cause for the erosion of the outer edges of the subaqueous delta. The erosive sediment transport up to the estuary under the action of wave and flow was the main cause for the siltation of east edge of Geligangzi Shoal and East Trough became shallow and narrow. The impact of the artificial reclamation of the nearshore beach on the evolution of the underwater delta was worthy of attention. |
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| Keywords: | Liaohe Estuary subaqueous delta geomorphologic evolution GIS Geligangzi Shoal |
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