On the tracks of Nitrogen deposition effects on temperate forests at their southern European range – an observational study from Italy. (12th April 2014)

• Record Type: Journal Article
• Authors: Ferretti, Marco; Marchetto, Aldo; Arisci, Silvia; Bussotti, Filippo; Calderisi, Marco; Carnicelli, Stefano; Cecchini, Guia; Fabbio, Gianfranco; Bertini, Giada; Matteucci, Giorgio; de Cinti, Bruno; Salvati, Luca; Pompei, Enrico
• Is Part Of: Global change biology. Volume 20:Number 11(2014:Nov.)
• Page Start: 3423
• Page End: 3438
• Publication Date: 2014-04-12
• Subjects: Climatic changes -- Environmental aspects -- Periodicals; Troposphere -- Environmental aspects -- Periodicals; Biodiversity conservation -- Periodicals; Eutrophication -- Periodicals; 551.5
• DOI: 10.1111/gcb.12552
• Languages: English
• ISSNs: 1354-1013

Abstract

<abstract abstract-type="main" id="gcb12552-abs-0001"> <title>Abstract</title> <p>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‐NO<sub>3</sub>+N‐NH<sub>4</sub>) ranged between 4 and 29 kg ha<sup>−1</sup> yr<sup>−1</sup>, 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<sub>, </sub> levelling out for bulk deposition >4–6 kg ha<sup>−1</sup> yr<sup>−1</sup>. Partial Least Square (PLS) regression revealed that ‐ although stand and meteorological variables explained the largest portion of variance in relative basal area increment (BAI<sub>rel</sub> 2000–2009) ‐ N‐related predictors (topsoil BCE, C : N, pH; foliar N‐ratios; N deposition) nearly always improved the BAI<sub>rel</sub> 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<sub>rel</sub> 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<sup>−1</sup> yr<sup>−1</sup> (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.</p> </abstract>