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On the tracks of Nitrogen deposition effects on temperate forests at their southern European range - an observational study from Italy

机译:氮沉积对南欧温带森林的影响-来自意大利的一项观测研究

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We studied forest monitoring data collected at permanent plots in Italy over the period 2000-2009 to identify the possible impact of nitrogen (N) deposition on soil chemistry, tree nutrition and growth. Average N throughfall (N-NO3+N-NH4) ranged between 4 and 29kg ha(-1)yr(-1), with Critical Loads (CLs) for nutrient N exceeded at several sites. Evidence is consistent in pointing out effects of N deposition on soil and tree nutrition: topsoil exchangeable base cations (BCE) and pH decreased with increasing N deposition, and foliar nutrient N ratios (especially N:P and N:K) increased. Comparison between bulk openfield and throughfall data suggested possible canopy uptake of N-,N- levelling out for bulk deposition >4-6kgha(-1)yr(-1). Partial Least Square (PLS) regression revealed that - although stand and meteorological variables explained the largest portion of variance in relative basal area increment (BAI(rel) 2000-2009) - N-related predictors (topsoil BCE, C:N, pH; foliar N-ratios; N deposition) nearly always improved the BAI(rel) model in terms of variance explained (from 78.2 to 93.5%) and error (from 2.98 to 1.50%). N deposition was the strongest predictor even when stand, management and atmosphere-related variables (meteorology and tropospheric ozone) were accounted for. The maximal annual response of BAI(rel) was estimated at 0.074-0.085% for every additional kgN. This corresponds to an annual maximal relative increase of 0.13-0.14% of carbon sequestered in the above-ground woody biomass for every additional kgN, i.e. a median value of 159 kgC per kgN ha(-1)yr(-1) (range: 50-504 kgC per kgN, depending on the site). Positive growth response occurred also at sites where signals of possible, perhaps recent N saturation were detected. This may suggest a time lag for detrimental N effects, but also that, under continuous high N input, the reported positive growth response may be not sustainable in the long-term.
机译:我们研究了2000-2009年期间在意大利永久性土地上收集的森林监测数据,以确定氮(N)沉积对土壤化学,树木营养和生长的可能影响。平均N穿透量(N-NO3 + N-NH4)介于4到29kg ha(-1)yr(-1)之间,并且在多个地点超过了营养物N的临界负荷(CLs)。指出氮沉降对土壤和树木营养的影响的证据是一致的:随着氮沉降的增加,表土可交换碱性阳离子(BCE)和pH值降低,而叶面养分氮比(尤其是N:P和N:K)增加。大量裸露场和穿透数据之间的比较表明,对于大于4-6kgha(-1)yr(-1)的大量沉积物,可能吸收N-,N-水平的冠层。偏最小二乘(PLS)回归表明-尽管林分和气象变量解释了相对基础面积增加量的最大方差(BAI(rel)2000-2009)-与氮有关的预测因子(表土BCE,C:N,pH;叶面N比率; N沉积几乎总是从解释的方差(从78.2到93.5%)和误差(从2.98到1.50%)方面改善了BAI(rel)模型。即使考虑到林分,管理和与大气有关的变量(气象学和对流层臭氧),氮沉降也是最强的预测因子。每增加一千克体重,BAI(rel)的最大年度响应估计为0.074-0.085%。这对应于每增加一千克牛顿,地上木质生物量中固存的碳的年度最大相对增加量为0.13-0.14%,即中位数为每千克牛顿ha(-1)yr(-1)159 kgC(范围: 50-504 kgC / kgN,具体取决于站点)。在检测到可能的信号(也许是最近的N饱和)的位点也发生了正向生长反应。这可能暗示了有害的氮素效应存在时间滞后,但是在持续的高氮素输入下,所报告的正增长响应在长期内可能无法持续。

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