引用本文: | 杨 慧, 宁 静, 马 洋, 周孟霞, 曹建华.西南岩溶区植被碳循环研究进展[J].广西植物,2022,42(6):903-913.[点击复制] |
YANG Hui, NING Jing, MA Yang, ZHOU Mengxia, CAO Jianhua.Research progress on carbon cycle of karst vegetation in Southwest China[J].Guihaia,2022,42(6):903-913.[点击复制] |
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西南岩溶区植被碳循环研究进展 |
杨 慧1, 宁 静1,2, 马 洋1, 周孟霞1, 曹建华1,3*
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1. 中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室, 广西 桂林 541004;2. 桂林理工大学
环境科学与工程学院, 广西 桂林 541006;3. 联合国教科文组织国际岩溶研究中心, 广西 桂林 541004
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摘要: |
由于岩溶关键带是地球关键带系统中重要的部分,岩溶区的植被是陆地生态系统重要的碳汇项,岩溶区植被的地上部分通过植物生长固碳的同时其地下部分的碳储量也非常可观,地下生物量生长和凋落物分解也会提高土壤有机碳和无机碳的含量,因此岩溶区植被碳循环已成为当前岩溶碳汇研究的热点之一。该文梳理了近四十年来岩溶植被固碳过程的研究文献,阐述了西南岩溶区植被特有的生理学特征,重点论述了以下4个方面的内容:(1)西南岩溶区植被生物量、生产力、碳储量评估;(2)西南岩溶区植被时空变化格局与碳源汇效应;(3)岩溶区植被碳利用特殊机制;(4)岩溶区植被碳循环模型预测与碳汇潜力。同时,提出了目前研究中存在的问题,并对今后的研究方向进行了展望,认为今后应在岩溶区植被碳循环的相关参数系统测定和机理过程研究,精细识别西南岩溶地区植被景观类型、量化固碳过程,以及对岩溶植被碳循环模型进行校正和修改等方面开展研究。该文可为深入理解岩溶区碳的时空演化规律、探索区域碳循环机理提供参考。 |
关键词: 岩溶区, 植被, 固碳, 生物量, 碳循环 |
DOI:10.11931/guihaia.gxzw202106060 |
分类号:Q948 |
文章编号:1000-3142(2022)06-0903-11 |
基金项目:国家重点研发计划项目(2021YFE0107100); 广西科技基地和人才专项(桂科AD20297090,桂科AD19245176); 桂林市科技计划项目(2020010403); 中国地质科学院岩溶地质研究所基本科研业务费项目(2020004)[Supported by National Key Research Development Program of China(2021YFE0107100); Natural Scientific Foundation of Guangxi Zhuang Autonomous Region of China(Guike AD20297090, Guike AD19245176); Guilin Science and Technology Project(2020010403); Special Fund for Basic Scientifc Research of Institute of Karst Geology, CAGS(2020004)]。 |
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Research progress on carbon cycle of karst vegetation in Southwest China |
YANG Hui1, NING Jing1,2, MA Yang1, ZHOU Mengxia1, CAO Jianhua1,3*
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1. Key Laboratory of Karst Dynamics, MNR/Guangxi, Institute of Karst Geology, CAGS, Guilin 541004, Guangxi, China;2. College
of Environmental Science and Engineering, Guilin University of Technology, Guilin 541006, Guangxi, China;3. International
Research Center on Karst Under the Auspices of UNESCO, Guilin 541004, Guangxi, China
1. Key Laboratory of Karst Dynamics, MNR/Guangxi, Institute of Karst Geology, CAGS, Guilin 541004, Guangxi, China; 2. College
of Environmental Science and Engineering, Guilin University of Technology, Guilin 541006, Guangxi, China; 3. International
Research Center on Karst Under the Auspices of UNESCO, Guilin 541004, Guangxi, China
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Abstract: |
Because the karst critical zone is an important part of the Earth Critical Zone system, the vegetation in karst area is an important carbon sink of terrestrial ecosystem, and the aboveground part of the vegetation in the karst area sequestrates carbon through plant growth, the carbon storage in the underground part is also very considerable, the growth of underground biomass and decomposition of litter also increase soil organic carbon and inorganic carbon content. Therefore, vegetation carbon cycle in karst area is one of the hotspots of karst carbon sink research. Based on the reviewing of research literature on carbon sequestration of karst vegetation in the past 40 years, this paper expounds the unique physiological characteristics of karst vegetation in Southwest China, and focuses on the following four aspects:(1)Evaluation of vegetation biomass, productivity and carbon storage in karst area of Southwest China;(2)Temporal and spatial variation patterns of vegetation and carbon source and sink effect in karst area of Southwest China;(3)Special mechanism of vegetation carbon utilization in karst area;(4)Prediction of vegetation carbon cycle model and carbon sink potential in karst area. The problems existing in the current research are put forward, and the future research direction is prospected. It is proposed that the future research should be carried out in the aspects of systematic determination of relevant parameters and mechanism process of vegetation carbon cycle in karst area, fine identification of vegetation landscape types in southwest karst area, quantification of carbon sequestration process, and correction and modification of karst vegetation carbon cycle model. This paper provides a reference for in-depth understanding the temporal and spatial evolution of carbon cycle in karst region and for exploring regional carbon cycle mechanism. |
Key words: karst area, vegetation, carbon sequestration, biomass, carbon cycle |
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