期刊
GLOBAL CHANGE BIOLOGY
卷 14, 期 9, 页码 2057-2063出版社
WILEY
DOI: 10.1111/j.1365-2486.2008.01636.x
关键词
atmospheric deposition models; biogeochemical models; carbon sequestration; chronosequences; forest growth; greenhouse gas budgets; net ecosystem productivity; nitrogen deposition; regression analysis; uncertainty
资金
- Natural Environment Research Council [ceh010023] Funding Source: researchfish
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.
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