Työväentutkimus Vuosikirja · 2024 · 86 citations · 23 references
AgricultureEnvironmental SciencesSoil SciencesSoil Carbon DynamicsSoil Organic MatterSoil ScienceCarbon CycleCarbon SequestrationGreenhouse Gas FluxesNitrogen CycleOrganic Matter TurnoverSoil Carbon LossesCarbon Flux In SoilsEmission FluxesGreenhouse Gas EmissionsGreenhouse Gas Emissions From SoilsSoil Carbon Dioxide FluxSoil Gas FluxesSoil Greenhouse Gas EmissionsSoil Organic Carbon
The effects of land-use and land-use change on soil greenhouse gas (GHG) fluxes are of concern due to Kyoto Protocol requirements. To quantify the soil GHG-fluxes of afforested organic soils in Finland, chamber measurements of soil CO 2 , CH 4 and N 2 O fluxes were made during the years 2002 to 2005 on twelve organic soil cropland and six cutaway peatland sites afforested 9 to 35 years ago. The annual soil CO 2 effluxes were statistically modelled using soil temperature as the driving variable and the annual CH 4 and N 2 O fluxes were estimated using the average fluxes during the measurement period. Soil CO 2 effluxes on afforested organic soil croplands varied from 207 to 539 g CO 2 -C m -2 a -1 and on cutaway peatlands from 276 to 479 g CO 2 -C m -2 a -1 . Both the afforested organic soil cropland and cutaway peatland sites acted mainly as small sinks for CH 4 ; the annual flux ranged from 0.32 to 0.61 g CH 4 -C m -2 . Afforested organic croplands emitted more N 2 O (from 0.1 to over 3.0 g N 2 O-N m -2 a -1 ) than cutaway peatland sites (from 0.01 to 0.48 g N 2 O-N m -2 a -1 ). Due to the decrease in soil CO 2 efflux, and no change in CH 4 and N 2 O fluxes, afforestation of organic croplands appears to decrease the greenhouse impact of these lands.
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On the Temperature Dependence of Soil Respiration
Jon Lloyd, John Taylor · Functional Ecology · 1994 · 4.2K citations
Methane flux from Minnesota Peatlands
Patrick Crill, Karen B. Bartlett, Robert C. Harriss et al. · Global Biogeochemical Cycles · 1988 · 431 citations
Natural Sciences, Environmental Sciences, Biogeochemistry +14