The land-ocean transfer process of Pb

	The land-ocean transfer process of Pb
	Yang, Dongfang 1,4; Zhang, Yinjiang 1; Qui, Xiancheng 1; Yang, Danfeng 2; Chen, Yu 3; Zhang, L ; Xu, D
	2016
关键词	Pb Distribution Seasonal variation Vertical variation Jiaozhou Bay
卷号	88
页码	1974-1977
英文摘要	This paper analyzed the seasonal variations and land-ocean transfer process of Pb in Jiaozhou Bay based on investigation data in surface waters in different seasons during 1979-1983. Results showed that during 1979-1983, both stream flow and marine current were the major Pb sources in Jiaozhou Bay. However, the inputs of Pb from atmosphere deposition and the top of the island were not beginning until 1981, and the inputs of Pb from marine traffic was not beginning until 1983. The seasonal variations of Pb contents in this bay were mainly determined by the inputs of Pb by anthropogenic activities, particularly the variations of the sources strengths. The land-ocean transfer of Pb could be expressed by a block diagram model, which indicated that Pb contents in the marine bay were mainly determined by the strength and frequency of Pb inputs from anthropogenic activities, and meanwhile, Pb was moving from high content areas to low content areas in the ocean interior.
会议录	PROCEEDINGS OF THE 2016 6TH INTERNATIONAL CONFERENCE ON MACHINERY, MATERIALS, ENVIRONMENT, BIOTECHNOLOGY AND COMPUTER (MMEBC)
会议录出版者	ATLANTIS PRESS
会议录出版地	29 AVENUE LAVMIERE, PARIS, 75019, FRANCE
语种	英语
WOS研究方向	Engineering ; Science & Technology - Other Topics
WOS记录号	WOS:000390720000397
内容类型	会议论文
源URL	[http://ir.fio.com.cn/handle/2SI8HI0U/5048]
专题	自然资源部第一海洋研究所
作者单位	1.Shanghai Ocean Univ, China Coll Life Sci, Shanghai 201306, Peoples R China; 2.Fudan Univ, Coll Informat Sci & Engn, Shanghai 200433, Peoples R China; 3.Shanghai Ocean Univ, Coll Informat, Shanghai 201306, Peoples R China; 4.SOA, North China Sea Environm Monitoring Ctr, Qingdao 266033, Peoples R China
推荐引用方式 GB/T 7714	Yang, Dongfang,Zhang, Yinjiang,Qui, Xiancheng,et al. The land-ocean transfer process of Pb[C]. 见:.