The coupling of the sedimentary records in the Yalu River estuary and the adjacent western coasts

Liu Yue; Cheng Yan; Li Hongjun; Gao Jianhua; Zheng Jinhua; Zhang Chunpeng; Zhang Liang; Liu Jingwei

doi:10.3969/j.issn.0253-4193.2017.01.008

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Liu Yue, Cheng Yan, Li Hongjun, Gao Jianhua, Zheng Jinhua, Zhang Chunpeng, Zhang Liang, Liu Jingwei. The coupling of the sedimentary records in the Yalu River estuary and the adjacent western coasts[J]. Haiyang Xuebao, 2017, 39(1): 76-88. doi: 10.3969/j.issn.0253-4193.2017.01.008

Citation:

Liu Yue, Cheng Yan, Li Hongjun, Gao Jianhua, Zheng Jinhua, Zhang Chunpeng, Zhang Liang, Liu Jingwei. The coupling of the sedimentary records in the Yalu River estuary and the adjacent western coasts[J]. Haiyang Xuebao, 2017, 39(1): 76-88. doi: 10.3969/j.issn.0253-4193.2017.01.008

Citation:

Liu Yue, Cheng Yan, Li Hongjun, Gao Jianhua, Zheng Jinhua, Zhang Chunpeng, Zhang Liang, Liu Jingwei. The coupling of the sedimentary records in the Yalu River estuary and the adjacent western coasts[J]. Haiyang Xuebao, 2017, 39(1): 76-88. doi: 10.3969/j.issn.0253-4193.2017.01.008

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The coupling of the sedimentary records in the Yalu River estuary and the adjacent western coasts

doi: 10.3969/j.issn.0253-4193.2017.01.008

1.
Urban Construction College, Eastern Liaoning University, Dandong 118003, China
2.
Key Laboratory for Coast and Island Development of Ministry of Education, Nanjing University, Nanjing 210093, China
3.
Water Affairs and Resource Management Office, Water Conservancy Bureau of Liaozhong County, Shenyang 110200, China

Received Date: 2016-04-06
Rev Recd Date: 2016-07-10

Abstract

Abstract

New evidence of the geomorphic evolution in the Yalu River estuary and coupling effects between water, sand, estuarine deposit and coastal development were explored, based on the analysis of ²¹⁰Pb and ¹³⁷Cs dating and the granularity of the 5 sediment cores collected from the Main Branch of the Yalu River estuary and the formerly studied 4 sediment cores collected in the tidal flat of western coasts and the West Branch. The results indicated that the fluvial action and the tidal action individually dominated the different sedimentary periods in the Main Branch;and the deposit dominated by the tidal action in the Main Branch was in accord with those in the West Branch and the adjacent western coasts in the Yalu River estuary. The material sources in the Main Branch were different from the West Branch and the western coasts. For the sedimentary records in the Main Branch, West Branch and the western coasts were all coupled with the environmental changes, the human activities, and the watershed events like the floods, and the responding time was basically synchronous. 5 obvious "event signals" appeared the sedimentary records, and the year of 1960 was the most important time when the estuarine geomorphy changed greatly.
- sedimentary record,
- Yalu River estuary,
- coupling

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References(31)

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