

FOLLOWUS
1.College of Marine Geoscience, Ocean University of China, Qingdao 266100, China
2.Key Lab of Submarine Geoscience and Prospecting Techniques, Ministry of Education, Ocean University of China, Qingdao 266100, China
Longhai ZHU, E-mail: zhulonghai@ouc.edu.cn
收稿:2019-11-12,
录用:2020-4-1,
网络首发:2020-05-13,
纸质出版:2021-02
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Origin and geochemistry of surface sediments in the mud deposit area offshore the Shandong Peninsula, China[J]. 海洋湖沼学报(英文), 2021,39(2):483-499.
Yingtao ZHU, Xiuli FENG, Longhai ZHU, et al. Origin and geochemistry of surface sediments in the mud deposit area offshore the Shandong Peninsula, China[J]. Journal of Oceanology and Limnology, 2021, 39(2): 483-499.
Origin and geochemistry of surface sediments in the mud deposit area offshore the Shandong Peninsula, China[J]. 海洋湖沼学报(英文), 2021,39(2):483-499. DOI: 10.1007/s00343-020-9300-9.
Yingtao ZHU, Xiuli FENG, Longhai ZHU, et al. Origin and geochemistry of surface sediments in the mud deposit area offshore the Shandong Peninsula, China[J]. Journal of Oceanology and Limnology, 2021, 39(2): 483-499. DOI: 10.1007/s00343-020-9300-9.
The waters offshore the Shandong Peninsula separate the North Yellow Sea from the South Yellow Sea
and receive a large amount of terrestrial material from Chinese and Korean rivers
making it an ideal area for studying land-sea interactions. However
little attention has been given to measuring sediment transportation in most previous studies. Based on an analysis in composition of major and trace elements and particle size characteristics from 62 surface sediment samples from the northeastern region off Shandong Peninsula
the type
element composition
and controlling factors of the surface sediments were investigated. In addition
the transportation of sediments from source to sink was described from measured thermohaline data. The results show two types of surface sediments: sandy silt and silt. The sediments were mainly terrestrial; and marine carbonate had little effect on sediment composition. Shown on a binary diagram of Rb/Sc to Co/Sc
the Huanghe (Yellow) and Changjiang (Yangtze) rivers are the main sources of surface sediments in the study area. The component mixing model showed that the relative contribution of sediment from the Huanghe River was up to 92%
followed by the Changjiang River (8%). The Yellow Sea Warm Current and the North Shandong Peninsula Coastal Current met at ~37.7°N in the study area
and were the main forces carrying sediment from the two main river sources. However
there was a deficit of transported material into the study area in summer. The secondary distribution of sediment from the two river sources was controlled by tidal currents and waves.
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