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The combined effect of short-term hydrological and N-fertilization manipulation of wetlands on CO2, CH4, and N2O emissions.
Bonetti, Giuditta; Limpert, Katy E; Brodersen, Kasper Elgetti; Trevathan-Tackett, Stacey M; Carnell, Paul E; Macreadie, Peter I.
Afiliación
  • Bonetti G; Deakin University, Centre for Integrative Ecology, School of Life and Environmental Sciences, Burwood Campus, Victoria, 3125, Australia. Electronic address: gbonetti@deakin.edu.au.
  • Limpert KE; Deakin University, Centre for Integrative Ecology, School of Life and Environmental Sciences, Burwood Campus, Victoria, 3125, Australia. Electronic address: klimpert@deakin.edu.au.
  • Brodersen KE; Marine Biological Section, Department of Biology, University of Copenhagen, 3000, Helsingør, Denmark. Electronic address: kasper.elgetti.brodersen@bio.ku.dk.
  • Trevathan-Tackett SM; Deakin University, Centre for Integrative Ecology, School of Life and Environmental Sciences, Burwood Campus, Victoria, 3125, Australia. Electronic address: s.trevathantackett@deakin.edu.au.
  • Carnell PE; Centre for Integrative Ecology, School of Life and Environmental Sciences, Deakin University, Geelong, Queenscliff Campus, Queenscliff, Victoria, 3225, Australia. Electronic address: paul.carnell@deakin.edu.au.
  • Macreadie PI; Deakin University, Centre for Integrative Ecology, School of Life and Environmental Sciences, Burwood Campus, Victoria, 3125, Australia. Electronic address: p.macreadie@deakin.edu.au.
Environ Pollut ; 294: 118637, 2022 Feb 01.
Article en En | MEDLINE | ID: mdl-34875268
ABSTRACT
Freshwater wetlands are natural sinks of carbon; yet, wetland conversion for agricultural uses can shift these carbon sinks into large sources of greenhouse gases. We know that the anthropogenic alteration of wetland hydrology and the broad use of N-fertilizers can modify biogeochemical cycling, however, the extent of their combined effect on greenhouse gases exchange still needs further research. Moreover, there has been recent interest in wetlands rehabilitation and preservation by improving natural water flow and by seeking alternative solutions to nutrient inputs. In a microcosm setting, we experimentally exposed soils to three inundation treatments (Inundated, Moist, Drained) and a nutrient treatment by adding high nitrogen load (300 kg ha-1) to simulate physical and chemical disturbances. After, we measured the depth microprofiles of N2O and O2 concentration and CO2 and CH4 emission rates to determine how hydrological alteration and nitrogen input affect carbon and nitrogen cycling processes in inland wetland soils. Compared to the Control soils, N-fertilizer increased CO2 emissions by 40% in Drained conditions and increased CH4 emissions in Inundated soils over 90%. N2O emissions from Moist and Inundated soils enriched with nitrogen increased by 17.4 and 18-fold, respectively. Overall, the combination of physical and chemical disturbances increased the Global Warming Potential (GWP) by 7.5-fold. The first response of hydrological rehabilitation, while typically valuable for CO2 emission reduction, amplified CH4 and N2O emissions when combined with high nitrogen inputs. Therefore, this research highlights the importance of evaluating the potential interactive effects of various disturbances on biogeochemical processes when devising rehabilitation plans to rehabilitate degraded wetlands.
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Texto completo: 1 Bases de datos: MEDLINE Asunto principal: Dióxido de Carbono / Humedales Idioma: En Revista: Environ Pollut Asunto de la revista: SAUDE AMBIENTAL Año: 2022 Tipo del documento: Article

Texto completo: 1 Bases de datos: MEDLINE Asunto principal: Dióxido de Carbono / Humedales Idioma: En Revista: Environ Pollut Asunto de la revista: SAUDE AMBIENTAL Año: 2022 Tipo del documento: Article