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重庆岩溶碳汇时空变化特征及其驱动因素

LU Hui WANG Chen LI Cheng SI Hongtao MA Lei WANG Fengwen

生态学报2025,Vol.45Issue(24):12347-12357,11.
生态学报2025,Vol.45Issue(24):12347-12357,11.DOI:10.20103/j.stxb.202503030456

重庆岩溶碳汇时空变化特征及其驱动因素

Spatial-temporal characteristics of karst carbon sink in Chongqing and its driving factors

LU Hui 1WANG Chen 2LI Cheng 2SI Hongtao 3MA Lei 2WANG Fengwen1

作者信息

  • 1. College of Environment and Ecology,Chongqing University,Chongqing 400044,China
  • 2. Chongqing Institute of Geology and Mineral Resources,Chongqing 401120,China
  • 3. College of Environment and Ecology,Chongqing University,Chongqing 400044,China||Chongqing Institute of Geology and Mineral Resources,Chongqing 401120,China
  • 折叠

摘要

Abstract

Although karst regions account for 39%of the total area of Chongqing,there is still considerable uncertainty in the estimation of karst carbon sink flux(CSF).Additionally,the contributions of climate change and ecological restoration to the CSF in this region remain uncertain.Based on this,the spatial and temporal patterns of karst carbon sinks in Chongqing from 2003 to 2022 were estimated by the GEM-CO2 model using lithological geological data and meteorological data.We also explored the impact mechanisms of climate change and ecological restoration on CSF.From 2003 to 2022,the karst carbon sink in Chongqing exhibited a fluctuating downward trend,with a decline rate of 0.064 tC km-2 a-1.The carbon sequestration flux was 9.17 tC km-2 a-1,and the total amount was 24.09×104 tC/a.The CSF in the northern karst regions of Chongqing was higher than in the south,showing an increasing gradient from south to north.The contributions of precipitation,temperature,evapotranspiration,soil moisture,and normalized vegetation index to CSF were 38.20%,30.88%,14.19%,8.37%,and 8.36%,respectively.Compared with temperature and evapotranspiration,the decrease in precipitation was the primary driver of the declining CSF flux over the past 20 years.The results of this study reveal the spatial-temporal characteristics of karst carbon sequestration and its driving factors in Chongqing,providing data support for the realization of carbon neutrality in Chongqing.Additionally,it offers valuable experience for other provinces and even countries in diagnosing carbon neutrality capacity and analyzing gaps.

关键词

岩溶作用/碳汇通量/GEM-CO2模型/时空演变/重庆

Key words

karst processes/carbon sink flux/GEM-CO2 model/spatiotemporal evolution/Chongqing

引用本文复制引用

LU Hui,WANG Chen,LI Cheng,SI Hongtao,MA Lei,WANG Fengwen..重庆岩溶碳汇时空变化特征及其驱动因素[J].生态学报,2025,45(24):12347-12357,11.

基金项目

重庆市技术创新与应用发展专项重点项目(CSTB2022TIAD-KPX0202) (CSTB2022TIAD-KPX0202)

自然资源部重庆典型矿区生态修复野外科学观测研究站开放课题(CQORS-2023-1) (CQORS-2023-1)

生态学报

OA北大核心

1000-0933

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