Citation: | WANG Qing, WANG Jia, DONG Jie, ZOU Liang, WANG Rujie, XIE Yongjian, XU Meijun, XIE Xiaodong, ZHOU Xiaoxue. Geochemical characteristics and controlling factors of surface sediments in Jiaozhou Bay[J]. Marine Geology Frontiers, 2023, 39(8): 8-19. doi: 10.16028/j.1009-2722.2023.130 |
Based on the correlation analysis and factor analysis of grain size and geochemical compositions of 150 surface sediments from Jiaozhou Bay, Qingdao, East China, the spatial distribution, element correlation, and element combination were studied, and the sedimentary environmental implication of geochemical characteristics of the in-bay sediments was revealed. The results show that the surface sediments are rich in types, mainly sandy silts in Jiaozhou Bay. The major elements of the sediments are predominated by SiO2 and Al2O3, and the high value area of SiO2 is mainly distributed in the northeast and west-central areas, and the content of Al2O3 is higher in the estuaries of the north and northeast of the bay and near the coast, indicating that the sediments are mainly terrigenous detrital sediments. The highest trace elements is V, followed by Li and Ni, and the content distribution is similar to that of Al2O3. Except for CaO, the spatial variation coefficients of the elements in the bay are small, indicating that the distribution of the elements was relatively uniform. The results of the correlation analysis and factor analysis suggest that the grain size is the main factor controlling the distribution of most major and trace elements (Al2O3, MgO, CaO, TiO2, MnO, Fe2O3, Ni, Co, Li, W, V, etc.) in the bay. The contents of CaO and P2O5 are mainly affected by weathering and human activities.
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Deployment of sampling sites for surface sediment in Jiaozhou Bay
Distribution of surface sediment types in Jiaozhou Bay
Distribution of major elements in surface sediments from Jiaozhou Bay
Distribution of trace elements in surface sediments from Jiaozhou Bay
Correlation between the content of major elements and particle size
Correlation between the content of trace elements and particle size