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我国岩溶地区碳汇研究进展与展望

蒋忠诚 章程 罗为群 肖琼 吴泽燕

蒋忠诚,章程,罗为群,等. 我国岩溶地区碳汇研究进展与展望[J]. 中国岩溶,2022,41(3):345-355 doi: 10.11932/karst20220302
引用本文: 蒋忠诚,章程,罗为群,等. 我国岩溶地区碳汇研究进展与展望[J]. 中国岩溶,2022,41(3):345-355 doi: 10.11932/karst20220302
JIANG Zhongcheng, ZHANG Cheng, LUO Weiqun, XIAO Qiong, WU Zeyan. Research progress and prospect of carbon sink in karst region of China[J]. CARSOLOGICA SINICA, 2022, 41(3): 345-355. doi: 10.11932/karst20220302
Citation: JIANG Zhongcheng, ZHANG Cheng, LUO Weiqun, XIAO Qiong, WU Zeyan. Research progress and prospect of carbon sink in karst region of China[J]. CARSOLOGICA SINICA, 2022, 41(3): 345-355. doi: 10.11932/karst20220302

我国岩溶地区碳汇研究进展与展望

doi: 10.11932/karst20220302
基金项目: 国家重点研发计划(2019YFC0507504);国际地球科学计划(批准号:IGCP661);国家自然科学基金联合基金项目(批准号:U21A2016)
详细信息
    作者简介:

    蒋忠诚(1962-),男,博士,研究员,研究方向:岩溶生态学。E-mail:jzhongcheng@mail.cgs.gov.cn

  • 中图分类号: P642.25

Research progress and prospect of carbon sink in karst region of China

  • 摘要: 20世纪90年代,我国率先开展了岩溶作用与碳循环研究。文章在系统总结相关研究进展的基础上,阐明岩溶碳汇的原理,提出基于地球系统科学理念的岩溶流域6种碳循环过程模式,揭示了岩溶碳汇的稳定性并回答有关学者对岩溶碳汇的质疑,从四大圈层的碳循环角度提出发掘岩溶地区碳汇潜力的新理念。在综述岩溶地区碳汇人工干预研究进展的基础上,分析了石漠化综合治理、岩溶土壤改良、水生生物固碳、加速岩溶过程等人工干预措施的碳汇潜力及研究应用方面的不足。提出了下一步岩溶流域碳汇调查研究监测和技术创新发展方向,以及固碳增汇试验示范工作思路。

     

  • 图  1  岩溶流域碳循环过程模式

    Figure  1.  Carbon cycle process model of karst basin

    表  1  流域尺度岩溶系统碳循环过程及其碳源汇效应

    Table  1.   Carbon cycle process and carbon source sink effect of karst system at watershed scale

    序号碳循环过程碳源项碳汇项碳源汇效应
    1岩溶空间CO2循环洞穴碳排放洞穴空气碳封存汇大于源
    2岩溶水系统碳循环水体碳排放重碳酸根、颗粒有机碳、生物碳泵汇大于源
    3岩溶土壤系统碳循环土壤呼吸、土壤有机碳分解土壤有机碳、土壤空气CO2、碳酸钙结核无机碳汇大于源
    4岩溶植物系统碳循环植物呼吸、植物有机碳分解植物有机碳、根系有机碳汇大于源
    5岩溶沉积物碳循环沉积过程碳排放沉积物有机碳源大于汇
    6岩溶区人类活动碳循环产业碳排放、人类活动碳排放碳排放岩溶吸收、碳地质封存源大于汇
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  • 收稿日期:  2022-02-20
  • 刊出日期:  2022-06-30

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