森林土壤温室气体通量对森林管理和全球大气变化的响应

doi:10.3969/j.issn.1000-2006.201603051

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南京林业大学学报（自然科学版） ›› 2017, Vol. 41 ›› Issue (04): 173-180.doi: 10.3969/j.issn.1000-2006.201603051

森林土壤温室气体通量对森林管理和全球大气变化的响应

高菲,高雷,崔晓阳^*

东北林业大学林学院,黑龙江哈尔滨 150040

出版日期:2017-08-18 发布日期:2017-08-18
基金资助:
收稿日期:2016-03-24 修回日期:2017-04-12
基金项目:国家重点研发计划(2016YFA0600803); 国家自然科学基金重点项目(41330530); 中央高校基本科研业务费专项资金项目(2572016AA06)
第一作者:高菲(gaofei880922@126.com)。*通信作者:崔晓阳(c_xiaoyang@126.com),教授。
引文格式:高菲,高雷,崔晓阳. 森林土壤温室气体通量对森林管理和全球大气变化的响应 Symbol`@@ [J]. 南京林业大学学报(自然科学版),2017,41(4):173-180.

Response of forest soil greenhouse gases fluxes to forest management and global atmospheric change

GAO Fei, GAO Lei, CUI Xiaoyang^*

College of Forestry, Northeast Forestry University, Harbin 150040, China

Online:2017-08-18 Published:2017-08-18

摘要/Abstract

摘要： 森林土壤是温室气体重要的源和汇。探讨不同森林管理和全球大气变化下土壤温室气体通量特征,为有效减少温室气体排放及森林可持续管理等提供参考。笔者从森林土壤温室气体(forest soil green house gases)、森林管理(forest mangement)和全球大气变化(global atmospheric change)3个关键研究点,查阅近年来相关研究成果,归纳森林管理和全球大气变化下土壤温室气体通量的一般性模式。CO₂、CH₄和N₂O是3种重要温室气体,其通量间存在协同、消长和随机型耦合关系。森林管理如火烧、采伐和造林等显著影响土壤温室气体通量。一般情况下,火烧导致土壤N₂O通量降低,CH₄吸收量增加,CO₂通量因火烧类型、火烧强度、生态系统类型不同出现增加、减低和无影响3种结果; 采伐通常导致土壤CO₂、CH₄和N₂O排放增加; 造林可使土壤CO₂排放减少,对N₂O和CH₄通量的影响随生态系统类型、造林树种等而改变。全球大气变化如CO₂浓度升高、氮沉降和气温升高影响森林土壤温室气体通量。通常,CO₂浓度升高导致土壤CO₂和N₂O排放量增加,CH₄吸收量降低; 氮沉降促进土壤N₂O排放、抑制CH₄吸收。气温升高导致土壤CO₂和N₂O排放增加。森林管理和全球大气变化对土壤温室气体通量的综合影响是非叠加的,有效的森林管理可能改变土壤温室气体通量对全球大气变化的响应。

Abstract: Forest soils are important sources and sinks of greenhouse gases(GHG). The objectives of this study were to explore the characteristics of forest soil GHG fluxes under different forest management practices and global atmospheric change, and to provide a reference for the reduction of GHG release and sustainable forest management. Publications were searched by using China Knowledge Resource Integrated Database, Wanfang Database, Science Direct, and Springer Link, using three keywords “forest soil greenhouse gases”, “forest management”, and “atmospheric change”. Papers reporting on forest soil GHGs were analyzed, and the general pattern of forest soil GHG fluxes under different forest management practices and global atospheric change scenarios was analyzed. CO₂, CH₄ and N₂O are three important GHGs, and the coupling between them are complex including synergism, antagonism and random interactions. Forest soil GHG fluxes were affected by forest management practices, such as forest fire occurrence and suppression, cutting and afforestation. Forest fire occurrence generally decreased soil N₂O flux, and increased soil CH₄ absorption. Forest fires could enhance, reduce or show no effects on soil CO₂ flux, depending on fire type, fire intensity and ecosystem type. Forest cutting usually increased soil CO₂, N₂O and CH₄ emission. Afforestation might reduce soil CO₂ emissions, where asits effects on N₂O and CH₄ varied with ecosystem type, planted tree species, etc. Generally, atmospheric change impacts that may affect forest soil GHG fluxes are elevated atmospheric CO₂, nitrogen deposition, and rising temperatures. Elevated atmospheric CO₂ increased soil CO₂ and N₂O emission, and decreased soil CH₄absorption. Nitrogen deposition stimulated soil N₂O emissions, and suppressed soil CH₄ absorption. Rising temperatures increased soil CO₂ and N₂O emissions. The combined effects of forest management practices and atmospheric change on forest soil GHG fluxes may be non-additive, and effective forest management may alter the response of soil GHG fluxes to atmospheric change.

中图分类号:

S714

高菲,高雷,崔晓阳. 森林土壤温室气体通量对森林管理和全球大气变化的响应[J]. 南京林业大学学报（自然科学版）, 2017, 41(04): 173-180.

GAO Fei, GAO Lei, CUI Xiaoyang. Response of forest soil greenhouse gases fluxes to forest management and global atmospheric change[J].Journal of Nanjing Forestry University (Natural Science Edition), 2017, 41(04): 173-180.DOI: 10.3969/j.issn.1000-2006.201603051.

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森林土壤温室气体通量对森林管理和全球大气变化的响应

Response of forest soil greenhouse gases fluxes to forest management and global atmospheric change

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