Carbon dioxide and methane production in small reservoirs flooding upland boreal forest
The FLooded Uplands Dynamics EXperiment (FLUDEX) was designed to assess the impact of reservoir creation on carbon cycling in boreal forests by (a) determining whether production of the greenhouse gases (GHG) carbon dioxide$({\rm CO}_{2})$and methane$({\rm CH}_{4})$in reservoirs is related to the am...
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Published in | Ecosystems (New York) Vol. 8; no. 3; pp. 267 - 285 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
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New York, NY
Springer Science+Business Media
01.04.2005
Springer Springer Nature B.V |
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Abstract | The FLooded Uplands Dynamics EXperiment (FLUDEX) was designed to assess the impact of reservoir creation on carbon cycling in boreal forests by (a) determining whether production of the greenhouse gases (GHG) carbon dioxide$({\rm CO}_{2})$and methane$({\rm CH}_{4})$in reservoirs is related to the amount of organic carbon (OC) stored in the flooded landscape, (b) examining temporal trends in GHG production during initial stages of flooding, and (c) considering the net difference between GHG fluxes before and after flooding to estimate the true effect of reservoir creation on atmospheric GHG levels. Three forested sites that varied in the amount of OC stored in soils and vegetation (30,870-45,860 kg C${\rm ha}^{-1}$) were experimentally flooded from June to September in 1999-2001. Throughout the study, net${\rm CO}_{2}$and${\rm CH}_{4}$production in all three reservoirs was not related to overall site OC storage. During the 1st flooding season, net${\rm CO}_{2}$production in the three reservoirs was 703-797 kg C${\rm ha}^{-1}$, but it decreased during the 2nd and 3rd flooding seasons to between 408 and 479 kg C${\rm ha}^{-1}$. However,${\rm CH}_{4}$production increased in all reservoirs with each flooding season, from about 3.2-4.6 kg C${\rm ha}^{-1}$in 1999 to 12.8-24.9 kg C${\rm ha}^{-1}$in 2000 and 29.7-35.2 kg C${\rm ha}^{-1}$in 2001. Over the long term, effects of boreal reservoir creation on atmospheric GHG levels may be largely due to net changes in${\rm CH}_{4}$cycling between the undisturbed and flooded ecosystems. |
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AbstractList | The FLooded Uplands Dynamics EXperiment (FLUDEX) was designed to assess the impact of reservoir creation on carbon cycling in boreal forests by (a) determining whether production of the greenhouse gases (GHG) carbon dioxide$({\rm CO}_{2})$and methane$({\rm CH}_{4})$in reservoirs is related to the amount of organic carbon (OC) stored in the flooded landscape, (b) examining temporal trends in GHG production during initial stages of flooding, and (c) considering the net difference between GHG fluxes before and after flooding to estimate the true effect of reservoir creation on atmospheric GHG levels. Three forested sites that varied in the amount of OC stored in soils and vegetation (30,870-45,860 kg C${\rm ha}^{-1}$) were experimentally flooded from June to September in 1999-2001. Throughout the study, net${\rm CO}_{2}$and${\rm CH}_{4}$production in all three reservoirs was not related to overall site OC storage. During the 1st flooding season, net${\rm CO}_{2}$production in the three reservoirs was 703-797 kg C${\rm ha}^{-1}$, but it decreased during the 2nd and 3rd flooding seasons to between 408 and 479 kg C${\rm ha}^{-1}$. However,${\rm CH}_{4}$production increased in all reservoirs with each flooding season, from about 3.2-4.6 kg C${\rm ha}^{-1}$in 1999 to 12.8-24.9 kg C${\rm ha}^{-1}$in 2000 and 29.7-35.2 kg C${\rm ha}^{-1}$in 2001. Over the long term, effects of boreal reservoir creation on atmospheric GHG levels may be largely due to net changes in${\rm CH}_{4}$cycling between the undisturbed and flooded ecosystems. The FLooded Uplands Dynamics EXperiment (FLUDEX) was designed to assess the impact of reservoir creation on carbon cycling in boreal forests by (a) determining whether production of the greenhouse gases (GHG) carbon dioxide (CO sub(2)) and methane (CH sub(4)) in reservoirs is related to the amount of organic carbon (OC) stored in the flooded landscape, (b) examining temporal trends in GHG production during initial stages of flooding, and (c) considering the net difference between GHG fluxes before and after flooding to estimate the true effect of reservoir creation on atmospheric GHG levels. Three forested sites that varied in the amount of OC stored in soils and vegetation (30,870-45,860 kg C ha super(-1)) were experimentally flooded from June to September in 1999-2001. Throughout the study, net CO sub(2) and CH sub(4) production in all three reservoirs was not related to overall site OC storage. During the 1st flooding season, net CO sub(2) production in the three reservoirs was 703-797 kg C ha super(-1), but it decreased during the 2nd and 3rd flooding seasons to between 408 and 479 kg C ha super(-1). However, CH sub(4) production increased in all reservoirs with each flooding season, from about 3.2-4.6 kg C ha super(-1) in 1999 to 12.8-24.9 kg C ha super(-1) in 2000 and 29.7-35.2 kg C ha super(-1) in 2001. Over the long term, effects of boreal reservoir creation on atmospheric GHG levels may be largely due to net changes in CH sub(4) cycling between the undisturbed and flooded ecosystems. The FLooded Uplands Dynamics EXperiment (FLUDEX) was designed to assess the impact of reservoir creation on carbon cycling in boreal forests by (a) determining whether production of the greenhouse gases (GHG) carbon dioxide (CO^sub 2^) and methane (CH^sub 4^) in reservoirs is related to the amount of organic carbon (OC) stored in the flooded landscape, (b) examining temporal trends in GHG production during initial stages of flooding, and (c) considering the net difference between GHG fluxes before and after flooding to estimate the true effect of reservoir creation on atmospheric GHG levels. Three forested sites that varied in the amount of OC stored in soils and vegetation (30,870-45,860 kg C ha^sup -1^) were experimentally flooded from June to September in 1999-2001. Throughout the study, net CO^sub 2^ and CH^sub 4^ production in all three reservoirs was not related to overall site OC storage. During the 1st flooding season, net CO^sub 2^ production in the three reservoirs was 703-797 kg C ha^sup -1^, but it decreased during the 2nd and 3rd flooding seasons to between 408 and 479 kg C ha^sup -1^. However, CH^sub 4^ production increased in all reservoirs with each flooding season, from about 3.2-4.6 kg C ha^sup -1^ in 1999 to 12.8-24.9 kg C ha^sup -1^ in 2000 and 29.7-35.2 kg C ha^sup -1^ in 2001. Over the long term, effects of boreal reservoir creation on atmospheric GHG levels may be largely due to net changes in CH^sub 4^ cycling between the undisturbed and flooded ecosystems.[PUBLICATION ABSTRACT] |
Author | Hall, B.D St. Louis, V.L Beaty, K.G Venkiteswaran, J.J Matthews, C.J.D Schiff, S.L Bodaly, R.A Joyce, E.M |
Author_xml | – sequence: 1 fullname: Matthews, C.J.D – sequence: 2 fullname: Joyce, E.M – sequence: 3 fullname: St. Louis, V.L – sequence: 4 fullname: Schiff, S.L – sequence: 5 fullname: Venkiteswaran, J.J – sequence: 6 fullname: Hall, B.D – sequence: 7 fullname: Bodaly, R.A – sequence: 8 fullname: Beaty, K.G |
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Cites_doi | 10.1021/es034424f 10.1029/97JD02233 10.1029/97JD00239 10.1641/0006-3568(2000)050[0766:RSASOG]2.0.CO;2 10.1006/jema.1998.0222 10.1029/1998GB900015 10.1017/S0376892900038194 10.1023/A:1012971715668 10.1021/es0205838 10.1038/348232a0 10.1061/(ASCE)0733-9372(1984)110:1(1) 10.1021/es9604931 10.1029/91GB02466 10.1029/94EO00987 10.1017/S0376892900034020 10.1139/x94-233 10.1029/1999JC000280 10.1021/es001924p 10.1029/94GB02651 10.1029/95GB02202 10.1029/92JC00188 10.1111/j.1752-1688.1981.tb02593.x 10.1029/1999GB900047 10.1139/a97-001 10.4319/lo.1998.43.4.0647 10.2134/jeq1998.00472425002700030017x 10.1017/S0376892997000118 10.1029/97GB01625 |
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Keywords | Methane Organic carbon Boreal forest Landscape Carbon dioxide Reservoir Decomposition Freshwater environment Canada Flood Ecosystem Greenhouse gas Artificial lake greenhouse gases; carbon dioxide; methane; reservoirs; decomposition; landscape organic carbon storage; FLooded Uplands Dynamics Experiment (FLUDEX); Ontario Taiga |
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Snippet | The FLooded Uplands Dynamics EXperiment (FLUDEX) was designed to assess the impact of reservoir creation on carbon cycling in boreal forests by (a) determining... |
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StartPage | 267 |
SubjectTerms | Animal and plant ecology Animal, plant and microbial ecology biogeochemical cycles Biological and medical sciences Boiling boreal forests Carbon Carbon dioxide carbon sequestration flooded conditions Flooded soils Floods forest ecosystems Forest soils Fresh water ecosystems Fundamental and applied biological sciences. Psychology gas production (biological) General aspects Greenhouse gases Methane montane forests reservoirs Soil air Surface water Synecology temporal variation Vegetation Watersheds |
Title | Carbon dioxide and methane production in small reservoirs flooding upland boreal forest |
URI | https://www.jstor.org/stable/25053825 https://www.proquest.com/docview/733070022/abstract/ https://search.proquest.com/docview/16192664 |
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