Alpine meadow restorations by non-dominant species increased soil nitrogen transformation rates but decreased their sensitivity to warming

• Published in: Journal of soils and sediments 2017-09, Vol.17 (9), p.2329-2337
• Main Authors: Jiang, Liangbo, Zhang, Ling, Deng, Bangliang, Liu, Xishuai, Yi, Huiqin, Xiang, Hai, Li, Zhi, Zhang, Wenyuan, Guo, Xiaomin, Niu, Dekui
• Format: Article
• Language: English
• Subjects: 2015 International Symposium on Forest Soils; Degradation; Deposition; Dominant species; Earth and Environmental Science; Environment; Environmental Physics; Global warming; Grasses; Grasslands; Meadows; Mineralization; Nitrification; Nitrogen; pH effects; Pools; Restoration; Sensitivity; Soil; Soil Science & Conservation; Soils; Species; Temperature effects; Vegetation
• ISSN: 1439-0108; 1614-7480
• DOI: 10.1007/s11368-016-1488-0

Purpose Alpine meadow soils are large carbon (C) and nitrogen (N) pools correlated significantly with global C and N cycling. Soil N transformations, including nitrification and N mineralization, are key processes controlling N availability. Alpine meadow degradations are common worldwide, and vegetation restorations have been widely implemented. However, grass species used for restorations may alter soil N transformations or their response to warming and N deposition due to divergent plant traits and their different effects on soil characteristic. To understand the effects of meadow restorations by non-historically dominant species on N transformations, we measured N transformation rates in restored soils and control soils under the context of warming and N deposition. Materials and methods We collected soils from plots restored by dominant ( Miscanthus floridulus ) and non-dominant species (including Carex chinensis and Fimbristylis dichotoma ) and non-restored plots in alpine meadows of Wugong Mountain, China. We measured nitrification and N mineralization rates when soils were incubated at different temperature (15 or 25 °C) and N additions (control vs. 4 g m −2 ) to examine their responses to restoration species, warming, and N. Results and discussion Vegetation restored soils differed substantially from non-restored bare soils. Total N, total organic C, pH, and dissolved organic C contributed the most to the separation. Restoration altered soil N transformations substantially, even though the effects varied among restoration species. Specifically, non-historically dominant species accelerated N transformations, while the originally dominant species decreased N transformations. In addition, sensitivity of nitrification to warming in restored soils was decreased by restorations. Soils restored by originally dominant species were higher in sensitivity of N transformations to warming than those restored by the other two species. Warming increased nitrification rates by 45.5 and 17.4 % in bare soils and restored soils, respectively. Meanwhile, N mineralization rates were increased by 52.8 and 21.9 %, respectively. Conclusions Vegetation restoration of the degraded meadows impacted N transformations and their sensitivity to warming. The effects varied with identity of the restoration species, suggesting that grass species should be considered in future restorations of degraded meadows in terms of their divergent effects on N transformations and sensitivity