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首页> 外文期刊>Global change biology >Regional application of PnET-N-DNDC for estimating the N2O source strength of tropical rainforests in the Wet Tropics of Australia
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Regional application of PnET-N-DNDC for estimating the N2O source strength of tropical rainforests in the Wet Tropics of Australia

机译:PnET-N-DNDC在澳大利亚湿热带地区热带雨林N2O源强度估算中的区域应用

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摘要

In contrast to the significant importance of tropical rainforest ecosystems as one of the major sources within the global atmospheric N2O budget (2.2-3.7 Tg N yr(-1)), regional estimates of their N2O source strength are still limited and highly uncertain. To contribute toward more reliable estimates of the N2O source strength of tropical rainforest ecosystems on a regional scale, we modified a process-oriented biogeochemical model, PnET-N-DNDC, and parameterized it to simulate C and N turnover and associated N2O emissions in and from tropical rainforest ecosystems. Model modifications included: (1) new parameterizations associated with plant physiology and soil hydrology and the addition of algorithms relating daily leaf litterfall to water stress as well as to daily rainfall to account for the effects of heavy rainfall damage; (2) the development of a denitrifier activity index that depends on soil moisture conditions and influences N turnover by denitrification; and (3) the addition of a biological N fixation algorithm. Daily simulated N2O emissions based on site data were in good agreement (model efficiencies up to 0.83) with field observations in the Wet Tropics of Australia and Costa Rica. The model was even able to reproduce the highly dynamic pattern of N2O emissions with short-term increases during the wet season. Sensitivity analyses demonstrated that the PnET-N-DNDC model was sensitive to changes in soil properties such as pH, clay content, soil organic carbon and climatic factors such as rainfall and temperature. By linking the PnET-N-DNDC model to a geographic information systems database, tropical rainforests in a 9000 km(2) area of the Wet Tropics of Australia are estimated to emit 962 t N2O-N yr(-1) (2.4 kg N2O-N ha(-1) yr(-1)) between July 1997 and June 1998.
机译:与热带雨林生态系统作为全球大气N2O预算(2.2-3.7 Tg N yr(-1))中的主要来源之一的重要性相比,其区域N2O来源强度的估算仍然有限且高度不确定。为了在区域范围内更可靠地估算热带雨林生态系统的N2O来源强度,我们修改了以过程为导向的生物地球化学模型PnET-N-DNDC,并对其进行参数化以模拟C和N转换以及相关的N2O排放。来自热带雨林生态系统。模型的修改包括:(1)与植物生理学和土壤水文学有关的新参数设置,并增加了将每日落叶数与水分胁迫以及每日降雨相关的算法,以解决降雨对降雨造成的影响; (2)反硝化活性指数的发展取决于土壤水分条件并通过反硝化影响氮的转化; (3)增加了生物氮固定算法。根据现场数据得出的每日模拟N2O排放与澳大利亚和北非湿热带地区的实地观测结果吻合很好(模型效率高达0.83)。该模型甚至能够重现N2O排放的高度动态模式,并在雨季短期内增加。敏感性分析表明,PnET-N-DNDC模型对土壤性质的变化敏感,例如pH,粘土含量,土壤有机碳和气候因素(例如降雨和温度)的变化。通过将PnET-N-DNDC模型链接到地理信息系统数据库,估计澳大利亚湿热带9000 km(2)区域中的热带雨林排放962吨N2O-N yr(-1)(2.4 kg N2O在1997年7月至1998年6月之间-N ha(-1)yr(-1))。

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