植物生态学报

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极端降水对不同草原土壤总硝化及总氮矿化及其敏感性的影响

韩菲1,王袼2,武帅楷1,林茂1,董宽虎1,王常慧2,苏原1   

  1. 1. 山西农业大学
    2. 山西农业大学草业学院
  • 收稿日期:2023-12-29 修回日期:2024-05-18 出版日期:2024-05-23 发布日期:2024-05-23

Effects of Extreme Precipitation on Gross Nitrification Rate Gross Nitrogen Mineralization and Sensitivity of Different Types of Grassland

Fei HAN1,Wang Ge2,shuaikai Wu1,Mao LIN3,Kuan-Hu DONG4,Chang-Hui Wang5,Yuan Su1   

  1. 1. 山西农业大学
    2. College of grassland science, Shanxi Agricultural University
    3. Shanxi Agricultural University
    4. Shanxi Agriculture University
    5.
  • Received:2023-12-29 Revised:2024-05-18 Online:2024-05-23

摘要: 全球气候变化背景下极端降水事件频发将会影响半干旱草原土壤氮(N)的转化过程, 但土壤氮转化关键过程如何响应降水变化及其总氮矿化速率对不同降水水平的敏感性尚不清楚。该研究依托中国北方草原全球变化联网试验平台的草甸草原, 典型草原和荒漠草原3种草原类型, 采用15N库稀释法, 测定了土壤总氮矿化速率(GNM)、土壤总硝化速率(GN), 以及相关的生物(微生物生物量碳含量、氮含量、地下生物量(BGB))、非生物(土壤温度(ST)、土壤含水量(SWC))和土壤底物(土壤铵态氮(NH4+-N)、硝态氮(NO3—N)、可溶性有机碳、氮含量)指标。结果表明: 不同类型草原GNM存在显著差异, 从高到低依次是草甸草原((3.284 ± 0.613) mg·kg–1·d–1)、典型草原((1.370 ± 0.167) mg·kg–1·d–1)和荒漠草原((0.724 ± 0.216) mg·kg–1·d–1)。增减50%的降水对3种草原土壤GNM和GN没有产生显著影响。典型草原和荒漠草原土壤GNM和GN对减少降水的敏感性显著高于降水增加的敏感性, 而草甸草原土壤GNM和GN的敏感性在增减降水间无显著差异。结构方程模型(SEM)分析揭示了土壤水分是影响土壤GNM的主要因子。以上结果表明短期的极端降水对中国北方3种重要草原土壤GNM和GN没有产生显著影响, 但改变了其对降水变化的敏感性。未来极端降水事件增加如何影响陆地生态系统土壤N的转化过程尚需进行长时间尺度, 大空间格局的系统研究

关键词: 北方草原, 总氮矿化, 极端降水, 敏感性, 土壤水分

Abstract: Aims: Under the background of global climate change, frequent extreme precipitation events will affect the soil nitrogen transformation process in the semi-arid steppe. However, how the key processes of soil nitrogen transformation respond to precipitation change and the sensitivity of total nitrogen mineralization rate to different precipitation levels remains unclear. Methods: In this study, the gross nitrogen mineralization rate (GNM), and gross nitrification rate (GN) of soil were measured by the 15N pool dilution method based on meadow steppe, typical steppe, and desert steppe of the Global Change Network test platform of northern China Steppe. And related biological (microbial biomass carbon, microbial biomass nitrogen, background biomass (BGB)), and abiotic (soil temperature (ST), soil water content (SWC)) soil substrate (soil ammonium nitrogen (NH4+-N), nitrate nitrogen (NO3--N, soluble organic carbon, soluble organic nitrogen) indexes. Important findings:The results showed that there were significant differences in GNM among different steppe types. The highest GNM was in meadow steppe (3.284 ± 0.613mg·kg-1·d-1), followed with typical steppe (1.370 ± 0.167 mg·kg-1·d-1) and desert steppe (0.724 ± 0.216 mg·kg-1·d-1). However, A 50% decrease in rainfall had no significant effect on GNM and GN of the three grasslands. The sensitivity of GNM and GN to precipitation reduction in typical steppe and desert steppe soil were significantly higher than that of precipitation increase, while the sensitivity of GNM and GN in meadow steppe soil was not significantly different between precipitation increase and decrease. Structural equation model (SEM) analysis revealed that soil moisture was the main factor affecting soil GNM. These results indicate that short-term extreme precipitation has no significant effect on GNM and GN of three important grasslands in northern China, but changes their sensitivity to precipitation change. How the increase of extreme precipitation events will affect the soil nitrogen conversion process in terrestrial ecosystems in the future needs to be systematically studied on long-term scales and large spatial patterns.

Key words: Northern grassland, gross nitrogen mineralization, Extreme precipitation, Sensitivity, Soil moisture