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

Abstract 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 an...

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Autores principales: Jiaoneng Yu, Xu-Ri, Songbo Qu, Fengzi Li, Da Wei, Almaz Borjigidai
Formato: Artículo
Lenguaje:English
Publicado: Nature Portfolio 2023-01-01
Colección:Scientific Reports
Acceso en línea:https://doi.org/10.1038/s41598-023-27392-y
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author Jiaoneng Yu
Xu-Ri
Songbo Qu
Fengzi Li
Da Wei
Almaz Borjigidai
author_facet Jiaoneng Yu
Xu-Ri
Songbo Qu
Fengzi Li
Da Wei
Almaz Borjigidai
author_sort Jiaoneng Yu
collection DOAJ
description Abstract 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 (Ncr). The maximum N retention capacity (MNRC) of plants at Ncr 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 Ncr. 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 Ncr.
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spelling doaj.art-62d97a1042c4458c8ce42c1a9b6937f62023-01-22T12:09:36ZengNature PortfolioScientific Reports2045-23222023-01-0113111310.1038/s41598-023-27392-yPlant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen additionJiaoneng Yu0Xu-Ri1Songbo Qu2Fengzi Li3Da Wei4Almaz Borjigidai5Key Laboratory of Ethnomedicine, Ministry of Education, Minzu University of ChinaState Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of SciencesKey Laboratory of Ethnomedicine, Ministry of Education, Minzu University of ChinaState Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of SciencesState Key Laboratory of Tibetan Plateau Earth System, Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of SciencesKey Laboratory of Ethnomedicine, Ministry of Education, Minzu University of ChinaAbstract 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 (Ncr). The maximum N retention capacity (MNRC) of plants at Ncr 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 Ncr. 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 Ncr.https://doi.org/10.1038/s41598-023-27392-y
spellingShingle Jiaoneng Yu
Xu-Ri
Songbo Qu
Fengzi Li
Da Wei
Almaz Borjigidai
Plant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen addition
Scientific Reports
title Plant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen addition
title_full Plant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen addition
title_fullStr Plant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen addition
title_full_unstemmed Plant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen addition
title_short Plant nitrogen retention in alpine grasslands of the Tibetan Plateau under multi-level nitrogen addition
title_sort plant nitrogen retention in alpine grasslands of the tibetan plateau under multi level nitrogen addition
url https://doi.org/10.1038/s41598-023-27392-y
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