4.7 Article

A new LandscapeDNDC biogeochemical module to predict CH4 and N2O emissions from lowland rice and upland cropping systems

期刊

PLANT AND SOIL
卷 386, 期 1-2, 页码 125-149

出版社

SPRINGER
DOI: 10.1007/s11104-014-2255-x

关键词

Methane; Nitrous oxide; Paddy rice; Maize; Model

资金

  1. German Research Foundation (DFG) [FOR 1701, BU1173/13-1, KI1413]
  2. knowledge hub of the Joint Research Programming Initiative on Agriculture, Food Security and Climate Change (FACCE-JPI) within the project Modelling European Agriculture with Climate Change for Food Security (MACSUR)
  3. ECLAIRE project (Effects of Climate Change on Air Pollution and Response Strategies for European Ecosystems)
  4. EU's Seventh Framework Programme for Research and Technological Development (FP7)
  5. Climate Change, Agricultural and Food Security Programme (CCAFS) of CGIAR Institutes

向作者/读者索取更多资源

Replacing paddy rice by upland systems such as maize cultivation is an on-going trend in SE Asia caused by increasing water scarcity and higher demand for meat. How such land management changes will feedback on soil C and N cycles and soil greenhouse gas emissions is not well understood at present. A new LandscapeDNDC biogeochemical module was developed that allows the effect of land management changes on soil C and N cycle to be simulated. The new module is applied in combination with further modules simulating microclimate and crop growth and evaluated against observations from field experiments. The model simulations agree well with observed dynamics of CH (4) emissions in paddy rice depending on changes in climatic conditions and agricultural management. Magnitude and peak emission periods of N (2) O from maize cultivation are simulated correctly, though there are still deficits in reproducing day-to-day dynamics. These shortcomings are most likely related to simulated soil hydrology and may only be resolved if LandscapeDNDC is coupled to more complex hydrological models. LandscapeDNDC allows for simulation of changing land management practices in SE Asia. The possibility to couple LandscapeDNDC to more complex hydrological models is a feature needed to better understand related effects on soil-atmosphere-hydrosphere interactions.

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