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  Nitrogen fixation and denitrification in a floodplain forest near Manaus, Brazil

Kreibich, H., & Kern, J. (2003). Nitrogen fixation and denitrification in a floodplain forest near Manaus, Brazil. Hydrological Processes, 17, 1431-1441. doi:10.1002/hyp.1294.

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資料種別: 学術論文

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kreibich_2003.pdf (出版社版), 444KB
 
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 作成者:
Kreibich, Heidi, 著者
Kern, Jürgen1, 著者           
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1Working Group Tropical Ecology, Max Planck Institute for Limnology, Max Planck Institute for Evolutionary Biology, Max Planck Society, ou_976549              

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キーワード: nitrogen fixation; denitrification; forest soil; floodplain; acetylene reduction assay; acetylene block method
 要旨: The Amazon floodplain (várzea) is seasonally affected by water level fluctuations of the Solimões/Amazon River. The drastic environmental changes that occur also include microbiological processes, such as nitrogen (N2) fixation and denitrification. Both processes were measured in the soil by the acetylene reduction assay and the acetylene block method in a várzea forest on Ilha de Marchantaria, Central Amazonia, Brazil. In the surface soil horizon (0-5 cm), N2 fixation was highest during the exposed period (0·04-0·26 nmolN h-1 g-1 dry weight (dw)). In contrast, denitrification varied from 0 to 1·40 nmolN h-1 g-1 dw, with high rates during the submerged and the transition periods. No significant difference between locations with legume trees, with non-legume trees and without trees could be observed. N2 fixation rates of incubations (litter down to 450 cm depth) for samples collected during the exposed period ranged from 0 to 0·11 nmolN h-1 g-1 dw, with highest rates in the surface soil horizon (0-5 cm). Denitrification ranged from 0 to 0·05 nmolN h-1 g-1 dw, with the highest rate at 250-300 cm depth, which was just below the water table. The maximum N2 fixation rate (0·89 nmolN h-1 g-1dw) and denitrification rate (0·09 nmolN h-1 g-1 dw) occurred in the litter layer. On average, at least three times as much N is lost from the surface soil horizon via denitrification than is gained by N2 fixation annually, but the rates are strongly influenced by the flood pulse. Copyright © 2003 John Wiley & Sons, Ltd.

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言語: eng - English
 日付: 2003
 出版の状態: 出版
 ページ: -
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 査読: 査読あり
 識別子(DOI, ISBNなど): eDoc: 39152
DOI: 10.1002/hyp.1294
その他: 2203/S 37935
 学位: -

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出版物名: Hydrological Processes
  出版物の別名 : Hydrol. Process.
種別: 学術雑誌
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出版社, 出版地: -
ページ: - 巻号: 17 通巻号: - 開始・終了ページ: 1431 - 1441 識別子(ISBN, ISSN, DOIなど): ISSN: 0885-6087