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首页|期刊导航|生态学报|祁连山南麓高寒草甸土壤有机碳对氮添加和降水改变的响应

祁连山南麓高寒草甸土壤有机碳对氮添加和降水改变的响应

祝景彬 张法伟 李红琴 宋成刚 魏海霞 张治国 王春雨 李英年 贺慧丹

生态学报2026,Vol.46Issue(1):49-61,13.
生态学报2026,Vol.46Issue(1):49-61,13.DOI:10.20103/j.stxb.202503300727

祁连山南麓高寒草甸土壤有机碳对氮添加和降水改变的响应

Responses of soil organic carbon to nitrogen addition and precipitation change in alpine meadow at the southern foot of Qilian Mountains

祝景彬 1张法伟 2李红琴 3宋成刚 4魏海霞 5张治国 5王春雨 6李英年 2贺慧丹1

作者信息

  • 1. 枣庄学院旅游与资源环境学院,枣庄 277160||中国科学院西北高原生物研究所,西宁 810001
  • 2. 中国科学院西北高原生物研究所,西宁 810001
  • 3. 洛阳师范学院生命科学学院,洛阳 471934
  • 4. 青海省工程咨询中心,西宁 810001
  • 5. 枣庄学院旅游与资源环境学院,枣庄 277160
  • 6. 齐鲁师范学院地理与旅游学院,济南 250000
  • 折叠

摘要

Abstract

Alpine meadows,as one of the dominant vegetation types on the Qinghai-Tibet Plateau,are significantly influenced by atmospheric nitrogen(N)deposition and altered precipitation patterns under global climate change,which profoundly affect carbon balance in these ecosystems.However,the interactive effects of these two factors on soil organic carbon(SOC)dynamics remain highly uncertain.This study,conducted from 2019 to 2021 in an alpine meadow in the northeastern Qinghai-Tibet Plateau,investigated the responses of plant biomass and surface soil(0-10cm)SOC content to N addition(coated urea at 10 g N m-2a-1)and precipitation manipulation(50%increase and 50%decrease),with three replicates per treatment.Results indicated that N addition alone significantly increased peak aboveground biomass(AGB)by 19.1%(83.8g/m2)and the AGB/BGB ratio by 23.3%(0.057).Notably,both AGB and SOC content exhibited significant interannual variations.To mitigate annual variability,relative changes(ΔAGB,ΔBGB,and ΔSOC)between treatments and the control were analyzed,revealing that these relative changes were also insensitive to experimental manipulations.Both Random Forest and Structural Equation Model analyses demonstrated that SOC and ΔSOC contents were primarily regulated by temperature fluctuations rather than plant carbon inputs(AGB,BGB,or their relative changes).This study demonstrated the positive effect of climate change on SOC accumulation in alpine meadows,likely attributable to the dominant role of sustained temperature increases over recent decades,rather than atmospheric N deposition or precipitation regime shifts.The pronounced interannual effects,rather than treatment-specific responses,highlight the urgent need for long-term,multifactorial experiments to unravel the complex responses and mechanisms underlying soil carbon sequestration in alpine meadows under climate change.

关键词

高寒草甸/氮添加/降水改变/植被生产力/土壤有机碳

Key words

alpine meadow/nitrogen addition/precipitation change/vegetation productivity/soil organic carbon

引用本文复制引用

祝景彬,张法伟,李红琴,宋成刚,魏海霞,张治国,王春雨,李英年,贺慧丹..祁连山南麓高寒草甸土壤有机碳对氮添加和降水改变的响应[J].生态学报,2026,46(1):49-61,13.

基金项目

山东省自然科学基金(ZR2021QC222,ZR2023QC254) (ZR2021QC222,ZR2023QC254)

国家自然科学基金面上项目(32471752) (32471752)

山东省高等学校青创科技计划创新团队项目(2022KJ278) (2022KJ278)

生态学报

1000-0933

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