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Simulating carbon dioxide exchange in boreal ecosystems flooded by reservoirs

机译:模拟水库充斥的北方生态系统中的二氧化碳交换

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A process-based reservoir model of Flooded Forest Denitrification Decomposition (FF-DNDC) was developed to simulate carbon dioxide (CO2) exchange from flooded boreal landscapes. The reservoir model is based on Forest-DNDC, a terrestrial biogeochemistry model which supports detailed soil carbon (C) processes including redox chemistry, with modification to represent the disturbed soil and vegetation C dynamics due to the presence of an overlying water column on the ecosystems. Soil decomposition rates and temperature and oxygen profiles were changed, and sedimentation to the soil surface was added. FF-DNDC was evaluated using CO2 exchange measurements from the newly created Eastmain-1 reservoir in northern Quebec, Canada. For the first four years of the reservoir (2006 to 2009), simulated daily CO2 emissions averaged 1.42 g C m(-2) d(-1) (ranging from 0.75 to 3.24 g C m(-2) d(-1)) from the flooded forest and 0.74 g Cm-2 d(-1) (ranging from 0.51 to 1.09 gC m(-2) d(-1)) from the flooded peatland. The simulated emissions were smaller than the thin-filmed boundary layer exchanges based on measured partial pressure of carbon dioxide (pCO(2)) but were larger than the exchanges measured using an eddy covariance system. However, the temporal patterns of simulated and measured exchanges were similar. We simulated potential CO2 emissions over 100 years, the expected operating lifetime of the reservoir, with assuming no change in climate. Simulated CO2 emissions decreased with time since flooding especially for the first four decades. The 100-year cumulative emissions from the flooded peatland were larger than those from the flooded forest. Sensitivity analysis indicated that vegetation and soil inputs and parameters controlling the quality and/or quantity of decomposable soil C in flooded ecosystems (e.g. woody vegetation biomass, soil organic carbon in organic and mineral layers, and carbon:nitrogen ratio in woody vegetation and soil) were important to the reservoir CO2 emission. (C) 2016 Elsevier B.V. All rights reserved.
机译:建立了基于过程的水淹森林反硝化分解(FF-DNDC)储层模型,以模拟淹没的北方景观中的二氧化碳(CO2)交换。储层模型基于Forest-DNDC,这是一种陆地生物地球化学模型,支持详细的土壤碳(C)过程,包括氧化还原化学,并进行了修改以表示由于生态系统上存在水柱而扰动的土壤和植被C动态。 。改变土壤分解速率和温度和氧分布,并增加土壤表面的沉降。使用加拿大魁北克省北部新建的Eastmain-1油藏的CO2交换测量值对FF-DNDC进行了评估。在水库的前四年(2006年至2009年)中,模拟的每日平均CO2排放量平均为1.42 g C m(-2)d(-1)(范围为0.75至3.24 g C m(-2)d(-1) )和来自泥炭地的0.74 g Cm-2 d(-1)(范围从0.51到1.09 gC m(-2)d(-1))。模拟的排放量小于基于测量的二氧化碳分压(pCO(2))的薄膜边界层交换,但大于使用涡旋协方差系统测量的交换。但是,模拟和测量的交换的时间模式相似。我们在假设气候没有变化的情况下,模拟了100年内潜在的CO2排放量(水库的预期使用寿命)。自洪水以来,特别是在头四个十年中,模拟的CO2排放随时间减少。淹没泥炭地的100年累积排放量大于淹没森林的100年累积排放量。敏感性分析表明,植被和土壤的投入以及控制淹没生态系统中可分解土壤C的质量和/或数量的参数(例如木质植被生物量,有机层和矿物层中的土壤有机碳以及木质植被和土壤中的碳氮比)对储层二氧化碳排放很重要。 (C)2016 Elsevier B.V.保留所有权利。

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