“…It was estimated that the production of reactive N increased from 15 Tg N in 1860 to 156 Tg N in 1995, with a further increase up to 187 Tg N in 2005 (Galloway et al, 2008). On the one hand, atmospheric N deposition has a positive effect on maintaining plant productivity of terrestrial ecosystems through enhancing the N availability (Fleischer et al, 2013;Reay et al, 2008;Thomas et al, 2010;Ti et al, 2012); on the other hand, excessive N deposition has negative impacts on ecosystem health and services, such as N saturation (Aber et al, 1989;Kopacek et al, 2013), soil acidification (Bowman et al, 2008;Maljanen et al, 2013;Vitousek et al, 1997), and loss of biodiversity (Bobbink et al, 2010;Stevens et al, 2004).…”