Uncertainties in the relationship between atmospheric nitrogen deposition and forest carbon sequestration

被引:156
作者
Sutton, Mark A. [1 ]
Simpson, David [2 ,3 ]
Levy, Peter E. [1 ]
Smith, Rognvald I. [1 ]
Reis, Stefan [1 ]
van Oijen, Marcel [1 ]
de Vries, Wim [4 ]
机构
[1] Ctr Ecol & Hydrol, Edinburgh Res Stn, Penicuik EH26 0QB, Midlothian, England
[2] Norwegian Meteorol Inst, NO-0313 Oslo, Norway
[3] Chalmers Univ Technol, SE-41296 Gothenburg, Sweden
[4] Univ Wageningen & Res Ctr, NL-6700 AA Wageningen, Netherlands
基金
英国自然环境研究理事会;
关键词
atmospheric deposition models; biogeochemical models; carbon sequestration; chronosequences; forest growth; greenhouse gas budgets; net ecosystem productivity; nitrogen deposition; regression analysis; uncertainty;
D O I
10.1111/j.1365-2486.2008.01636.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
In a recent study, Magnani et al. report how atmospheric nitrogen deposition drives stand-lifetime net ecosystem productivity (NEPav) for midlatitude forests, with an extremely high C to N response (725 kg C kg(-1) wet-deposited N for their European sites). We present here a re-analysis of these data, which suggests a much smaller C : N response for total N inputs. Accounting for dry, as well as wet N deposition reduces the C : N response to 177 : 1. However, if covariance with intersite climatological differences is accounted for, the actual C : N response in this dataset may be < 70 : 1. We then use a model analysis of 22 European forest stands to simulate the findings of Magnani et al. Multisite regression of simulated NEPav vs. total N deposition reproduces a high C : N response (149 : 1). However, once the effects of intersite climatological differences are accounted for, the value is again found to be much smaller, pointing to a real C : N response of about 50-75 : 1.
引用
收藏
页码:2057 / 2063
页数:7
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