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青藏高原高寒草甸土壤有机碳对氮添加和降水改变的响应

高延锋 宋成刚 王雯 张法伟 独威 祝景彬

中国农业气象2026,Vol.47Issue(8):1215-1223,9.
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中国农业气象2026,Vol.47Issue(8):1215-1223,9.DOI:10.3969/j.issn.1000-6362.2026.08.004

青藏高原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 Altered Precipitation in an Alpine Meadow on the Qinghai-Tibet Plateau

高延锋 1宋成刚 2王雯 2张法伟 3独威 4祝景彬5

作者信息

  • 1. 洛阳市园林绿化中心,洛阳 471027
  • 2. 青海省工程咨询中心有限责任公司,西宁 810001
  • 3. 中国科学院西北高原生物研究所高原生物适应与进化重点实验室,西宁 810008
  • 4. 生态环境部环境发展中心,北京 100029
  • 5. 枣庄学院旅游与资源环境学院,枣庄 277160
  • 折叠

摘要

Abstract

Enhancing soil organic carbon(SOC)sequestration capacity is a crucial nature-based solution for mitigating climate change.To elucidate the mechanisms underlying depth-resolved SOC responses to elevated atmospheric nitrogen(N)deposition and altered precipitation regimes,this study utilized a full-factorial experiment combining N addition(10g·m-2·y-1)and precipitation manipulation(±50%ambient precipitation)initiated in 2017 in a northeastern Qinghai-Tibet plateau alpine meadow.The dynamics of 0-40cm SOC,soil nutrients and plant biomass from 2022 to 2024 were quantified to reveal SOC responses to changes in nitrogen deposition and precipitation regimes.The results showed that aboveground biomass(AGB)increased significantly by approximately 30%under the N addition treatment compared to the control(CK,no N addition or precipitation change).Belowground biomass(BGB)showed depth-dependent variations and was more sensitive to precipitation change,where 30-40cm BGB was reduced by 35%under the decreased precipitation treatment.N addition decreased surface soil(0-10cm)pH by 7%but increased SOC and soil total nitrogen(STN)by 7%-9%in the same layer.Conversely,subsoil(30-40cm)SOC and STN declined by 2%-4%.N addition and precipitation change indirectly regulated 10-40cm STN and SOC through the soil pH pathway,rather than via changes in vegetation biomass.Specifically,precipitation change showed positive effects on 10-40cm SOC with a β of 0.08.These findings demonstrate a response of SOC with a"surface accumulation and subsurface depletion"pattern,which alters the vertical distribution of SOC and indicates a decoupling from plant-derived carbon inputs.This study provides valuable insights for assessing and projecting the soil carbon sink function of alpine meadows under future climate change scenarios.

关键词

高寒草甸/植被生物量/土壤有机碳/土壤全氮/土壤pH

Key words

Alpine meadow/Vegetation biomass/Soil organic carbon/Soil total nitrogen/Soil pH

引用本文复制引用

高延锋,宋成刚,王雯,张法伟,独威,祝景彬..青藏高原高寒草甸土壤有机碳对氮添加和降水改变的响应[J].中国农业气象,2026,47(8):1215-1223,9.

基金项目

青海省重点研发与转化计划科技国际合作专项项目(2024-HZ-801) (2024-HZ-801)

青海省寒区恢复生态学重点实验室开放课题(2023-KF-03) (2023-KF-03)

国家自然科学基金面上项目(32471752) (32471752)

河南省自然科学基金面上项目(242300420170) (242300420170)

青海省2021、2022昆仑英才-拔尖人才项目 ()

中国农业气象

1000-6362

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