Department of Forest Ecology & Management, Swedish University of Agricultural Sciences (SLU), SE-901 83, Umeå, Sweden.
Nicholas School of the Environment, Duke University, Durham, North Carolina, 27708, USA.
Ecol Appl. 2017 Sep;27(6):1838-1851. doi: 10.1002/eap.1571. Epub 2017 Jul 10.
We report results from long-term simulated external nitrogen (N) input experiments in three northern Pinus sylvestris forests, two of moderately high and one of moderately low productivity, assessing effects on annual net primary production (NPP) of woody mass and its interannual variation in response to variability in weather conditions. A sigmoidal response of wood NPP to external N inputs was observed in the both higher and lower productivity stands, reaching a maximum of 65% enhancement regardless of the native site productivity, saturating at an external N input of 4-5 g N·m ·yr . The rate of increase in wood NPP and the N response efficiency (RE , increase in wood NPP per external N input) were maximized at an external N input of ~3 g N·m ·yr , regardless of site productivity. The maximum RE was greater in the higher productivity than the lower productivity stand (20 vs. ~14 g C/g N). The N-induced enhancement of wood NPP and its RE were, however, markedly contingent on climatic variables. In both of the higher and lower productivity stands, wood NPP increased with growing season precipitation (P), but only up to ~400 mm. The sensitivity of the response to P increased with increasing external N inputs. Increasing growing season temperature (T) somewhat increased the N-induced drought effect, whereas decreasing T reduced the drought effect. These responses of wood NPP infused a large temporal variation to RE , making the use of a fixed value unadvisable. Based on these results, we suggest that regional climate conditions and future climate scenarios should be considered when modeling carbon sequestration in response to N deposition in boreal P. sylvestris, and possibly other forests.
我们报告了在三个北方欧洲赤松森林中进行的长期模拟外部氮(N)输入实验的结果,其中两个森林生产力中等偏高,一个森林生产力中等偏低,评估了这些实验对木质生物量的年净初级生产力(NPP)及其对天气条件变化的年际变化的影响。在这两个生产力较高和较低的林分中,观察到木质 NPP 对外部 N 输入的 S 形响应,无论原生地点的生产力如何,外部 N 输入增加 4-5 g N·m ·yr 时,NPP 最大增加 65%,达到饱和。木质 NPP 增加的速率和 N 响应效率(RE,每外部 N 输入增加的木质 NPP)在外部 N 输入约 3 g N·m ·yr 时达到最大值,而与地点生产力无关。在较高生产力的林分中,RE 比较低生产力的林分更大(约 20 比 14 g C/g N)。然而,N 诱导的木质 NPP 增加及其 RE 显著取决于气候变量。在这两个生产力较高和较低的林分中,木质 NPP 随着生长季降水(P)增加,但最多增加约 400 mm。对 P 的响应敏感性随外部 N 输入的增加而增加。生长季温度(T)升高会略微增加 N 诱导的干旱效应,而 T 降低会减少干旱效应。这些木质 NPP 的响应为 RE 注入了很大的时间变化,因此不建议使用固定值。基于这些结果,我们建议在模拟北方欧洲赤松对 N 沉积的碳固存时,应考虑区域气候条件和未来气候情景,以及其他森林。