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降水减少、降水事件减少和氮添加对半干旱草原生态系统碳通量的影响不同。

Reduction in precipitation amount, precipitation events, and nitrogen addition change ecosystem carbon fluxes differently in a semi-arid grassland.

机构信息

Key Laboratory of Grassland Ecology, School of Ecology and Environment, Inner Mongolia University, Hohhot 010021, China.

Key Laboratory of Grassland Ecology, School of Ecology and Environment, Inner Mongolia University, Hohhot 010021, China.

出版信息

Sci Total Environ. 2024 Jun 1;927:172276. doi: 10.1016/j.scitotenv.2024.172276. Epub 2024 Apr 6.

Abstract

The increases in extent and frequency of extreme drought events and increased nitrogen (N) deposition due to global change are expected to have profound impacts on carbon cycling in semi-arid grasslands. However, how ecosystem CO exchange processes respond to different drought scenarios individually and interactively with N addition remains uncertain. In this study, we experimentally explored the effects of different drought scenarios (early season extreme drought, 50 % reduction in precipitation amount, and 50 % reduction in precipitation events) and N addition on net ecosystem CO exchange (NEE), ecosystem respiration (ER), and gross ecosystem productivity (GEP) over three growing seasons (2019-2021) in a semi-arid grassland in northern China. The growing-season ecosystem carbon fluxes in response to drought and N addition were influenced by inter-annual precipitation changes, with 2019 as a normal precipitation year, and 2020 and 2021 as wet years. Early season extreme drought stimulated NEE by reducing ER. 50 % reduction in precipitation amount decreased ER and GEP consistently in three years, but only significantly suppressed NEE in 2019. 50 % reduction in precipitation events stimulated NEE. Nitrogen addition stimulated NEE, ER, and GEP, but only significantly in wet years. The structural equation models showed that changes in carbon fluxes were regulated by soil moisture, soil temperature, microbial biomass nitrogen (MBN), and the key plant functional traits. Decreased community-weighted means of specific leaf area (CWM) was closely related to the reduced ER and GEP under early season extreme drought and 50 % reduction in precipitation amount. While increased community-weighted means of plant height (CWM) largely accounted for the stimulated ER and GEP under 50 % reduction in precipitation events. Our study stresses the distinct effects of different drought scenarios and N enrichment on carbon fluxes, and highlights the importance of soil traits and the key plant traits in determining carbon exchange in this water-limited ecosystem.

摘要

由于全球变化,极端干旱事件的范围和频率增加以及氮(N)沉积增加,预计对半干旱草原的碳循环将产生深远影响。然而,生态系统 CO 交换过程如何单独应对不同的干旱情景以及与 N 添加的相互作用仍不确定。在这项研究中,我们通过实验探讨了不同干旱情景(早期极端干旱、降水量减少 50%和降水事件减少 50%)和 N 添加对中国北方半干旱草原三个生长季(2019-2021 年)净生态系统 CO 交换(NEE)、生态系统呼吸(ER)和总生态系统生产力(GEP)的影响。干旱和 N 添加对生长季生态系统碳通量的影响受到年际降水变化的影响,2019 年为正常降水年,2020 年和 2021 年为湿润年。早期极端干旱通过减少 ER 来刺激 NEE。三年中,降水量减少 50% 持续降低 ER 和 GEP,但仅在 2019 年显著抑制 NEE。降水量减少 50%刺激 NEE。N 添加刺激 NEE、ER 和 GEP,但仅在湿润年显著。结构方程模型表明,碳通量的变化受土壤水分、土壤温度、微生物生物量氮(MBN)和关键植物功能特征的调节。在早期极端干旱和降水量减少 50%的情况下,群落加权平均比叶面积(CWM)的降低与 ER 和 GEP 的降低密切相关。而在降水量减少 50%的情况下,群落加权平均株高(CWM)的增加在很大程度上解释了 ER 和 GEP 的刺激。本研究强调了不同干旱情景和 N 富集对碳通量的不同影响,并强调了土壤特征和关键植物特征在决定这个水分限制的生态系统碳交换中的重要性。

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