Greenhouse Gas Emissions from Subtropical Agriculture Fields Decrease Over Time

T. Fall, Katie Heiden, A. Smyth, Z. Brym
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引用次数: 2

Abstract

Abstract Expansion of cultivated lands and field management impacts greenhouse gas (GHG) emissions from agriculture soils. Soils naturally cycle GHGs and can be sources or sinks depending on physical and chemical properties affected by cultivation and management status. We looked at how cultivation history influences GHG emissions from subtropical soils. We measured CO2, N2O, and CH4 fluxes, and soil properties from newly converted and continuously cultivated lands during the summer rainy season in calcareous soils from south Florida. Newly converted soils had more soil organic matter (OM), more moisture, higher porosity, and lower bulk density, leading to more GHG emissions compared to historically cultivated soils. Although more nutrients make newly converted lands more desirable for cultivation, conversion of new areas for agriculture was shown to release more GHGs than cultivated lands. Our data suggest that GHG emissions from agricultural soils may decrease over time with continued cultivation.
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亚热带农田温室气体排放随时间减少
耕地扩张和农田管理影响农业土壤温室气体排放。土壤自然循环温室气体,根据受种植和管理状况影响的物理和化学性质,可以是源或汇。我们研究了种植历史如何影响亚热带土壤的温室气体排放。在夏季雨季,我们测量了南佛罗里达钙质土壤中新转化和连续耕地的CO2、N2O和CH4通量以及土壤性质。新转化土壤具有更多的土壤有机质(OM)、更多的水分、更高的孔隙度和更低的容重,与历史上耕作的土壤相比,导致更多的温室气体排放。虽然更多的营养物质使新转化的土地更适合耕种,但研究表明,将新转化为农业的地区释放的温室气体比耕地更多。我们的数据表明,农业土壤的温室气体排放可能随着时间的推移而减少。
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