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

被引:156
作者
Fisher, J. B. [1 ]
Sitch, S. [4 ]
Malhi, Y. [1 ]
Fisher, R. A. [2 ]
Huntingford, C. [3 ]
Tan, S. -Y. [1 ]
机构
[1] Univ Oxford, Environm Change Inst, Sch Geog & Environm, Oxford OX1 3QY, England
[2] Los Alamos Natl Lab, Los Alamos, NM 87545 USA
[3] Ctr Ecol & Hydrol, Wallingford OX10 8BB, Oxon, England
[4] Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England
基金
英国自然环境研究理事会;
关键词
TERRESTRIAL CARBON; SOIL-NITROGEN; ROOT BIOMASS; NUTRIENT RETRANSLOCATION; FOREST PRODUCTIVITY; ATMOSPHERIC CARBON; CYCLE FEEDBACKS; NET PRIMARY; CLIMATE; GROWTH;
D O I
10.1029/2009GB003621
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
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 r(2) is 0.89, and RMSE is 0.003 kg N m(-2).yr(-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 similar to 150-180 years in this scenario. FUN replicates the N uptake response in the experimental N fertilization from a modeled N fertilization. However, FUN cannot replicate the N uptake response in the experimental 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.
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页数:17
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