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  Winter wheat carbon exchange in Thuringia, Germany

Anthoni, P. M., Freibauer, A., Kolle, O., & Schulze, E.-D. (2004). Winter wheat carbon exchange in Thuringia, Germany. Agricultural and Forest Meteorology, 121(1-2), 55-67. doi:10.1016/S0168-1923(03)00162-X.

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資料種別: 学術論文

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BGC0692.pdf (出版社版), 255KB
 
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 作成者:
Anthoni, P. M.1, 著者           
Freibauer, A.1, 著者           
Kolle, O.2, 著者           
Schulze, E.-D.1, 著者           
所属:
1Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497751              
2Service Facility Field Measurements & Instrumentation, O. Kolle, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497769              

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キーワード: Winter wheat Net ecosystem exchange Eddy covariance Roth-c model Long-term experiments Soil organic-carbon Simulating trends Tall vegetation Climate-change Forest Sequestration Europe Model
 要旨: Eddy covariance measurements and estimates of biomass net primary production (NPP) in combination with soil carbon turnover modelled by the Roth-C model were used to assess the ecosystem carbon balance of an agricultural ecosystem in Thuringia, Germany, growing winter wheat in 2001. The eddy CO2 flux measurements indicate an annual net ecosystem exchange (NEE) uptake in the range from -185 to -245 g C m(-2) per year. Main data analysis uncertainty in the annual NEE arises from night-time u* screening, other effects (e.g. coordinate rotation scheme) have only a small influence on the annual NEE estimate. In agricultural ecosystems the fate of the carbon removed during harvest plays a role in the net biome production (NBP) of the ecosystem, where NBP is given by net ecosystem production (NEP = -NEE) minus non-respiratory losses of the ecosystem (e.g. harvest). Taking account of the carbon removed by the wheat harvest (290 g C m(-2)), the agricultural field becomes a source of carbon with a NBP in the order of -45 to -105 g C m(-2) per year. Annual carbon balance modelled with the Roth-C model also indicated that the ecosystem was a source for carbon (NBP -25 to -55 g C m(-2) per year). Based on the modelling most of carbon respired resulted from changes in the litter and fast soil organic matter pool. Also, the crop and management history, particularly the C input to soil in the previous year, significantly affect next year's CO2 exchange. (C) 2003 Elsevier B.V. All rights reserved. [References: 36]

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 日付: 2004
 出版の状態: 出版
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 識別子(DOI, ISBNなど): その他: BGC0692
DOI: 10.1016/S0168-1923(03)00162-X
PII: 414
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出版物 1

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出版物名: Agricultural and Forest Meteorology
種別: 学術雑誌
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出版社, 出版地: Amsterdam : Elsevier
ページ: - 巻号: 121 (1-2) 通巻号: - 開始・終了ページ: 55 - 67 識別子(ISBN, ISSN, DOIなど): CoNE: https://pure.mpg.de/cone/journals/resource/954928468040
ISSN: 0168-1923