Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary

被引:5
|
作者
Jiang Siyi [1 ]
Xu Fangjian [2 ]
Li Yan [3 ]
Liu Xiling [4 ]
Zhao Yongfang [5 ]
Xu Wei [4 ]
机构
[1] State Ocean Adm, South China Sea Informat Ctr, Guangzhou 510300, Guangdong, Peoples R China
[2] China Univ Petr, Sch Geosci, Qingdao 266580, Peoples R China
[3] State Ocean Adm, Yantai Ocean Environm Monitoring Cent Stn, Yantai 264006, Peoples R China
[4] CNOOC Res Inst, Overseas Evaluat Ctr, Beijing 100027, Peoples R China
[5] Chinese Acad Sci, Inst Oceanol, Jiaozhou Bay Marine Ecosyst Res Stn, Qingdao 266071, Peoples R China
基金
中国国家自然科学基金;
关键词
grain size; Zhujiang River; sediment; transport trend; PEARL RIVER; CARBON; CHINA;
D O I
10.1007/s13131-014-0462-1
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Distributions of the parameters of sedimentary grain sizes and their correlations were studied to trace the sources of silts and their movement trends in the Zhujiang River Estuary based on the analyses of grain sizes from more than 1080 sedimentary samples. The distributions of the median diameter, public value, quartile deviation, and skewness of sediments were complex in the Zhujiang River Estuary mainly because of the impact of the matter source regions, distances from the source regions, and hydrodynamic conditions, such as waves, tidal currents, and coastal currents. Analyses of the parameters of the grain sizes for the various types of sediments showed that the distributions of the surface sediments in the Zhujiang River Estuary were controlled by many factors. Their matter sources were mainly the sediments discharged from the runoffs and ebb tidal currents, and from the open sea. The sediments mainly moved by suspension movement. The silts formed a large area of sediments with suspended fine silts in the Zhujiang River Estuary by internal adjustment transportation in the area, and moved toward the western coast of the Zhujiang River Estuary under the effect of Coriolis forces and coastal currents.
引用
收藏
页码:30 / 36
页数:7
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