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海南海莲红树林土壤CH4的产生及其某些影响因素

卢昌义 叶勇 林鹏 黄玉山 谭凤仪

卢昌义, 叶勇, 林鹏, 黄玉山, 谭凤仪. 海南海莲红树林土壤CH4的产生及其某些影响因素[J]. 海洋学报, 1998, 20(6): 132-138.
引用本文: 卢昌义, 叶勇, 林鹏, 黄玉山, 谭凤仪. 海南海莲红树林土壤CH4的产生及其某些影响因素[J]. 海洋学报, 1998, 20(6): 132-138.
Lu Changyi, Ye Yong, Lin Peng, Wong Yushan, Tam Nora F Y. Methane production from soils of Bruguiera sexangula mangrove swamp in the Hainan and its several affecting factors[J]. Haiyang Xuebao, 1998, 20(6): 132-138.
Citation: Lu Changyi, Ye Yong, Lin Peng, Wong Yushan, Tam Nora F Y. Methane production from soils of Bruguiera sexangula mangrove swamp in the Hainan and its several affecting factors[J]. Haiyang Xuebao, 1998, 20(6): 132-138.

海南海莲红树林土壤CH4的产生及其某些影响因素

基金项目: 国家自然科学基金资助项目(编号49676298);香港科技大学资助

Methane production from soils of Bruguiera sexangula mangrove swamp in the Hainan and its several affecting factors

  • 摘要: 全球CH4预算的估算表明,湿地是大气CH4最大的生物排放源[1].旨在估算全球大气CH4湿地源强的工作大多集中在内陆淡水环境,因为在此环境的CH4通量较大[2].国外对海岸盐沼的CH4排放也有一些报道,发现其通量变化范围较大,并进而研究了温度、土壤湿度、盐度以及土壤有机碳含量等因素对CH4排放的影响[3].
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    Conrad H.Control of methane production in terrestrial ecosystems.In:Exchange of Trace Gases between Terrestrial Ecosysterns and the Atmosphere(Andreac M O and Schimel D S eds),Chichester,John Wiley & Sons Ltd.,1989,39~58
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出版历程
  • 收稿日期:  1997-05-13
  • 修回日期:  1997-08-04

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