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Carbon cost of plant nitrogen acquisition: a mechanistic, globally applicable model of plant nitrogen uptake, retranslocation, and fixation

机译:植物氮素获取的碳成本:一种机制化,全球适用的植物氮素吸收,再转运和固定模型

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摘要

Nitrogen (N) generally limits plant growth and controls biosphere responses to climate change. We introduce a new mathematical model of plant N acquisition, called Fixation and Uptake of Nitrogen (FUN), based on active and passive soil N uptake, leaf N retranslocation, and biological N fixation. This model is unified under the theoretical framework of carbon (C) cost economics, or resource optimization. FUN specifies C allocated to N acquisition as well as remaining C for growth, or N-limitation to growth. We test the model with data from a wide range of sites (observed versus predicted N uptake r² is 0.89, and RMSE is 0.003 kg Nm-2yr-1). Four model tests are performed: (1) fixers versus nonfixers under primary succession; (2) response to N fertilization; (3) response to CO2 fertilization; and (4) changes in vegetation C from potential soil N trajectories for five DGVMs (HYLAND, LPJ, ORCHIDEE, SDGVM, and TRIFFID) under four IPCC scenarios. Nonfixers surpass the productivity of fixers after ~150-180 years in this scenario. FUN replicates the N uptake response in the experimental N fertilization from a modeled CO2 fertilization from a modeled CO2 fertilization; nonetheless, the correct response is obtained when differences in root biomass are included. Finally, N-limitation decreases biomass by 50 Pg C on average globally for the DGVMs. We propose this model as being suitable for inclusion in the new generation of Earth system models that aim to describe the global N cycle.
机译:氮通常会限制植物的生长,并控制生物圈对气候变化的反应。我们基于主动和被动土壤氮素吸收,叶片氮素重新分配和生物固氮作用,介绍了一种新的植物氮素吸收数学模型,称为固氮吸收法(FUN)。该模型在碳(C)成本经济学或资源优化的理论框架下是统一的。 FUN指定分配给N采集的C,以及剩余的C用于增长,或N限制增长。我们使用来自广泛站点的数据测试该模型(观察到的氮吸收与预测的氮吸收r²为0.89,RMSE为0.003 kg Nm-2yr-1)。进行了四个模型测试:(1)主继承下的固定器与非固定器; (2)对氮肥的响应; (3)对二氧化碳施肥的反应; (4)在四种IPCC情景下,五个DGVM(HYLAND,LPJ,ORCHIDEE,SDGVM和TRIFFID)的潜在土壤N轨迹中植被C的变化。在这种情况下,约150-180年后,非定影剂的生产率超过了定影剂的生产率。 FUN在模拟的CO2施肥中从模拟的CO2施肥中复制了实验氮施肥中的氮吸收响应。但是,当包括根生物量的差异时,可以获得正确的响应。最后,对于DGVM,N限制使全球平均生物量减少50 PgC。我们认为此模型适合包含在旨在描述全球N周期的新一代地球系统模型中。

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