Matrix-bound phosphine in Ny-?lesund Area of Arctic

Phosphine, a ubiquitous trace gas in the atmosphere, acts as a carrier of gasous phosphorus in the biogeochemical cycle. The research of phosphine will show new light on the mechanisms of how the phosphorus supplement influence the biogeochemical cycle and global warming. In this paper, we detect th...

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Bibliographic Details
Main Authors: Feng, Ying, Wang, Qiang, Yao, Ziwei, Geng, Jinju
Other Authors: Wang, Q.(qwang@pku.edu.cn), Institute of Science and Technology Information of China, Beijing 100038, China, College of Environmental Science and Engineering, Peking University, Beijing 100871, China, National Marine Environmental Monitoring Center, Dalian 116023, China, State Key Laboratory of Pollution Control and Resource Reuse, School of Environment, Nanjing University, Nanjing 210093, China
Format: Journal/Newspaper
Language:English
Published: 高技术通讯英文版 2009
Subjects:
Online Access:https://hdl.handle.net/20.500.11897/407754
https://doi.org/10.3772/j.issn.1006-6748.2009.03.019
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Summary:Phosphine, a ubiquitous trace gas in the atmosphere, acts as a carrier of gasous phosphorus in the biogeochemical cycle. The research of phosphine will show new light on the mechanisms of how the phosphorus supplement influence the biogeochemical cycle and global warming. In this paper, we detect the phosphine in Arctic Pole area for the first time. The result shows that matrix-bound phosphine (MBP) exists in all the samplings. Phosphine distributions varied with different environmental origins. Average phosphine concentrations in tundra soil, lake sediments, sea sediments, seabird-droppings and deer guanos were 14.17 ng/kg dry, 35.44 kg dry, 67.20 kg dry, 32.9 ng/kg dry, and 25.52 ng/kg dry respectively. Correlation analysis shows that there is an obviously positive correlation between Porg and MBP. It could be concluded that anaerobic decomposition of Porg and the mechano-chemistry action of the rock probably are the possible reasons explaining the mechanism of MBP production in Arctic Pole area. Copyright ? by HIGH TECHNOLOGY LETTERS PRESS. EI 0 3 331-336 15