Plant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen addition

• Published in: Scientific reports 2023-01, Vol.13 (1), p.877-877, Article 877
• Main Authors: Yu, Jiaoneng, Xu-Ri, Qu, Songbo, Li, Fengzi, Wei, Da, Borjigidai, Almaz
• Format: Article
• Language: English
• Subjects: 704/158/2165; 704/158/2453; 704/158/853; 704/47/4112; Alpine environments; Biomass; Ecosystem; Fertilization; Grassland; Grasslands; Humanities and Social Sciences; multidisciplinary; Nitrogen; Nitrogen - metabolism; Plants - metabolism; Prairies; Retention; Retention capacity; Science; Science (multidisciplinary); Soil; Steppes; Tibet
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/s41598-023-27392-y

Nitrogen (N) deposition might alleviate degradation of alpine grassland caused by N limitation on the Tibetan Plateau (TP). To determine such limitation and quantify the N-induced N retention in plant, a six-year fertilization experiment with six levels of N addition rates (0, 1, 2, 4, 8 and 16 g N m −2  yr −1 ) was conducted in the Namco alpine steppe and additional 89 experiments with multi-level N addition were also synthesized worldwide among which 27 sites were on the TP. In general, N addition promoted N retention in plants, and this increasing trend diminished at the critical N rate (N cr ). The maximum N retention capacity (MNRC) of plants at N cr was strongly correlated with initial aboveground net primary productivity with a slope of 0.02, and the MNRC of grasslands globally ranged from 0.35 to 42.59 g N m −2  yr −1 , approximately account for 39% of N cr . Tibetan alpine grassland had a low average MNRC (2.24 g N m −2  yr −1 ) with distinct regional characteristic, which was much lower in the western TP (0.80 g N m −2  yr −1 ) than the eastern TP (4.10 g N m −2  yr −1 ). Our results inferred 0.33–1.21 Tg N yr −1 (0.22–0.79 g N m −2  yr −1 ) can be retained and 5.65–20.11 Tg C yr −1 (3.67–13.06 g C m −2  yr −1 ) can be gained by Tibetan alpine grasslands under current N deposition level. With the aggravation of N deposition, the alpine steppe ecosystem might continuously absorb N and C until N deposition reaches N cr .