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Insights into mechanisms governing forest carbon response to nitrogen deposition: a model–data comparison using observed responses to nitrogen addition

机译:对控制森林碳对氮沉积响应的机制的见解:使用观察到的氮添加响应的模型与数据比较

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In many forest ecosystems, nitrogen (N) deposition enhances plant uptake ofcarbon dioxide, thus reducing climate warming from fossil fuel emissions.Therefore, accurately modeling how forest carbon (C) sequestration respondsto N deposition is critical for understanding how future changes in Navailability will influence climate. Here, we use observations of forest Cresponse to N inputs along N deposition gradients and at five temperateforest sites with fertilization experiments to test and improve a globalbiogeochemical model (CLM-CN 4.0). We show that the CLM-CN plant C growthresponse to N deposition was smaller than observed and the modeled responseto N fertilization was larger than observed. A set of modifications to theCLM-CN improved the correspondence between model predictions andobservational data (1) by increasing the aboveground C storage in responseto historical N deposition (1850–2004) from 14 to 34 kg C per additional kg N added through deposition and (2) by decreasing the aboveground net primaryproductivity response to N fertilization experiments from 91 to 57 g C m?2 yr?1. Modeled growth response to N deposition was mostsensitive to altering the processes that control plant N uptake and thepathways of N loss. The response to N deposition also increased with a moreclosed N cycle (reduced N fixation and N gas loss) and decreased whenprioritizing microbial over plant uptake of soil inorganic N. The net effectof all the modifications to the CLM-CN resulted in greater retention of Ndeposition and a greater role of synergy between N deposition and risingatmospheric CO2 as a mechanism governing increases in temperate forestprimary production over the 20th century. Overall, testing models with boththe response to gradual increases in N inputs over decades (N deposition)and N pulse additions of N over multiple years (N fertilization) allows forgreater understanding of the mechanisms governing C–N coupling.
机译:在许多森林生态系统中,氮(N)沉积会增加植物对二氧化碳的吸收,从而减少化石燃料排放引起的气候变暖。因此,准确模拟森林碳(C)的固存对氮沉降的响应方式对于了解未来可航行性的变化将如何影响至关重要气候。在这里,我们通过施肥实验,利用沿N沉积梯度和五个温带森林站点对N输入的森林Cresponse观测资料,进行施肥试验,以测试和改善全球生物地球化学模型(CLM-CN 4.0)。我们表明,CLM-CN植物C对N沉积的生长响应比观察到的要小,并且对N施肥的建模响应比观察到的要大。对CLM-CN的一系列修改改进了模型预测与观测数据之间的对应关系(1),通过将历史氮的沉积量(1850-2004)从地上每增加一千克N增加到14到34千克碳,增加了地上碳的储存,以及2)通过将氮肥试验的地上净初级生产力响应从91 g C m ?2 yr ?1 降低到57 g C m ?2 yr ?1 。对氮沉积的模拟生长响应对改变控制植物吸收氮和氮损失途径的过程最为敏感。对氮沉降的响应也随着更接近的氮循环而增加(减少了氮的固定和氮的损失),而当优先考虑微生物而不是植物吸收土壤无机氮时,氮的响应降低。所有对CLM-CN的修饰的净效应导致氮沉积的保留更大。 N沉积和大气CO 2 上升之间的协同作用在控制20世纪温带森林初级生产力增加的机制中起着更大的作用。总体而言,测试模型既可以响应数十年来N输入的逐渐增加(N沉积),也可以响应多年以来N的N脉冲添加(N施肥),从而可以更好地理解控制C–N耦合的机制。

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