Journal of Integrative Agriculture ›› 2025, Vol. 24 ›› Issue (3): 815-826.DOI: 10.1016/j.jia.2024.07.033

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高寒草甸植物磷库和土壤有效磷对短期氮添加的非线性响应

  

  • 收稿日期:2024-03-04 接受日期:2024-06-19 出版日期:2025-03-20 发布日期:2025-02-28

Non-linear responses of the plant phosphorus pool and soil available phosphorus to short-term nitrogen addition in an alpine meadow

Bing Han1, Yicheng He1, Jun Zhou2, Yufei Wang1, Lina Shi1, Zhenrong Lin1, Lu Yu1, Wantong Zhang1, Yiyi Geng1, Xinqing Shao1, 3#   

  1. 1 Department of Grassland Resources and Ecology, College of Grassland Science and Technology, China Agricultural University, Beijing 100193, China
    2 Key Laboratory of Mountain Surface Processes and Ecological Regulation, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610299, China
    3 Qinghai Provincial Key Laboratory of Adaptive Management on Alpine Grassland, Xining 810016, China
  • Received:2024-03-04 Accepted:2024-06-19 Online:2025-03-20 Published:2025-02-28
  • About author:Bing Han, Mobile: +86-18369839879, E-mail: hbing_edu@163.com; #Correspondence Xinqing Shao, Tel: +86-10-62733835, E-mail: shaoxinqing@163.com
  • Supported by:
    This research was funded by the National Natural Science Foundation of China (31971746 and 32171685).

摘要:

氮富集会促进土壤磷循环,同时也增加了植物对磷的需求。然而,高寒草甸生态系统中植物磷库、土壤有效磷对氮添加的响应模式及调控机制还不清楚。基于此,以青藏高原高寒草甸为研究对象,设置4个氮添加水平(0, 5, 10和15 g N m-2 yr-1),通过测定植物、土壤和微生物中的磷,探究短期氮添加的影响机制。结果表明:(1)氮添加显著增加植物地上生物量,植物磷库对氮添加水平表现为非线性响应;(2)土壤有效磷随着氮添加梯度的增加呈先上升后下降的趋势,氮添加显著降低了稳定无机磷;(3)调控土壤有效磷的关键因子在不同氮添加水平下发生改变。在低氮添加水平下(0和5 g N m-2 yr-1),土壤pH下降促进了稳定无机磷的溶解,增加了土壤有效磷。相反,在高氮添加水平下(10和15 g N m-2 yr-1),微生物生物量磷增加,加剧了植物和微生物对磷的竞争,导致土壤有效磷下降。研究结果强调了植物磷库和土壤有效磷对氮添加的非线性响应,未来需要关注氮添加速率对磷的不同影响,从而更准确的预测氮富集下生态系统磷循环。

Abstract:

Nitrogen (N) enrichment is expected to induce a greater phosphorus (P) limitation, despite the acceleration of soil P cycling.  However, the changing patterns in plant P and soil available P after N enrichment, and their regulatory mechanisms, remain poorly understood in alpine meadows.  Here, we conducted a field experiment with four N addition rates (0, 5, 10, and 15 g N m–2 yr–1) in an alpine meadow, and investigated the P in plants, microorganisms, and soil to determine their patterns of change after short-term N addition.  Our results showed that N addition significantly increased plant biomass, and the plant P pool showed a non-linear response to the N addition gradient.  Soil available P initially increased and then declined with increasing N addition, whereas the occluded inorganic P decreased markedly.  The critical factors for soil available P varied with different N addition rates.  At lower N addition levels (0 and 5 g N m–2 yr–1), soil acidification facilitated the mobilization of occluded inorganic P to increase soil available P.  Conversely, at higher N addition levels (10 and 15 g N m–2 yr–1), the elevated soil microbial biomass P intensified the competition with plants for soil P, leading to a decline in soil available P.  This study highlights the non-linear responses of the plant P pool and soil available P concentration to N addition rates.  These responses suggest the need for developing ecosystem models to assess different effects of increasing N rates, which would enable more accurate predictions of the plant P supply and soil P cycling under N enrichment.


Key words: nitrogen addition rates , Qinghai-Tibetan Plateau ,  unimodal response ,  microbial biomass phosphorus ,  soil phosphorus fractions