The release behavior of inorganic nitrogen and phosphorus in sediment during disturbance

doi:10.1007/s00343-008-0197-y

	The release behavior of inorganic nitrogen and phosphorus in sediment during disturbance
	Wang Pibo 1,2; Song Jinming1 ; Guo Zhanyong 1; Li Pengcheng1
	2008-05-01
发表期刊	CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
ISSN	0254-4059
卷号	26 期号:2 页码:197-202
文章类型	Article
摘要	Sediments and surface water were sampled in a tide flat in the Huiquan Bay, Qingdao, China in January 2004 to simulate the exchange of NH(4)-N/NO(3)-N/PO(4)(3-) between sediments and surface water. A working system was designed with which samples were shaken at 60, 120 and 150 revolutions per minute (r/min). Experiment results show that NH(4)-N concentration in water at shaking rate of 60 r/min decreased gradually, while at 120 r/min increased gradually. In resuspension, fine-grained sediments contributed most NH(4)-N to the seawater, followed by medium-grained and coarse-grained sediments. The NO(3)-N concentration in water had a negative relation, with the shaking rate; the medium-grained sediments contributed more NO(3)-N to seawater than the coarse- and fine-grained sediments. The PO(4)(3-) concentration is positively related with the shaking rate, the fine-grained sediments were the main N and P contributor to the seawater, followed by medium- and coarse-grained sediments.; Sediments and surface water were sampled in a tide flat in the Huiquan Bay, Qingdao, China in January 2004 to simulate the exchange of NH4-N/NO3-N/PO43- between sediments and surface water. A working system was designed with which samples were shaken at 60, 120 and 150 revolutions per minute (r/min). Experiment results show that NH4-N concentration in water at shaking rate of 60 r/min decreased gradually, while at 120 r/min increased gradually. In resuspension, fine-grained sediments contributed most NH4-N to the seawater, followed by medium-grained and coarse-grained sediments. The NO3-N concentration in water had a negative relation, with the shaking rate; the medium-grained sediments contributed more NO3-N to seawater than the coarse- and fine-grained sediments. The PO43- concentration is positively related with the shaking rate, the fine-grained sediments were the main N and P contributor to the seawater, followed by medium- and coarse-grained sediments.
关键词	Resuspension Sediment Nh(4)-n No(3)-n Po(4)(3-)
学科领域	Limnology ; Oceanography
DOI	10.1007/s00343-008-0197-y
URL	查看原文
收录类别	SCI
语种	英语
WOS记录号	WOS:000256416000013
引用统计	被引频次：7[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/5394
专题	海洋生态与环境科学重点实验室海洋生物技术研发中心
作者单位	1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.State Ocean Adm, N China Sea Branch, Qingdao 266033, Peoples R China
第一作者单位	中国科学院海洋研究所
推荐引用方式 GB/T 7714	Wang Pibo,Song Jinming,Guo Zhanyong,et al. The release behavior of inorganic nitrogen and phosphorus in sediment during disturbance[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2008,26(2):197-202.
APA	Wang Pibo,Song Jinming,Guo Zhanyong,&Li Pengcheng.(2008).The release behavior of inorganic nitrogen and phosphorus in sediment during disturbance.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,26(2),197-202.
MLA	Wang Pibo,et al."The release behavior of inorganic nitrogen and phosphorus in sediment during disturbance".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 26.2(2008):197-202.

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