首页|火干扰和黑炭输入对油松林生长季土壤甲烷通量的影响

火干扰和黑炭输入对油松林生长季土壤甲烷通量的影响

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[目的]火干扰作为森林生态系统中一个重要的扰动因子,对森林土壤性质及结构都会产生剧烈作用,而森林土壤又是大气CH4 最重要的汇,因此火干扰对森林土壤CH4 通量的影响是不可忽视的。同时在林火发生后由于植被的不完全燃烧也会产生大量黑炭。黑炭是一种具有多孔结构的芳香化合物,进入土壤后可以影响土壤孔隙度、pH等理化性质从而改变土壤结构,因此常被用作土壤改良剂减少农田土壤CH4 的排放,但对于火后黑炭输入是否可以影响森林土壤CH4 通量及其影响因素尚不明确。[方法]以沈阳棋盘山地区油松林作为研究对象,探究火干扰和黑炭输入后土壤CH4 的动态变化及其影响因素。[结果]1)火干扰会增加油松林生长季土壤CH4 通量,其中重度火烧样地土壤CH4 通量显著高于对照样地及轻度火烧样地。2)黑炭输入会降低油松林生长季土壤CH4 通量,且随着黑炭输入量的增加,土壤CH4 通量降低的幅度也会增加。3)火干扰强度对土壤CH4通量具有直接的极显著正向作用,解释了 46。9%(P<0。001);黑炭输入对土壤CH4 通量具有直接的显著负向作用,解释了8。8%(P<0。05);MBC和MBN对土壤具有直接的极显著正向作用,分别解释了29。0%、49。3%(P<0。001)。[结论]火干扰会显著增加土壤CH4 通量,黑炭输入可以在一定程度上减缓火干扰对土壤CH4通量的影响,并且火干扰和黑炭输入主要通过改变微生物生物量影响土壤CH4 通量。研究为如何降低火后温室气体排放,从而改善火烧迹地的生态环境以及火后林下管理提供了理论依据。
Effect of fire disturbance and black carbon input on soil methane flux during growing season of Pinus tabulaeformis forest
[Objective]As an important disturbance factor in forest ecosystems,fire disturbance can have drastic effects on both the nature and structure of forest soils,which are the most important sink for atmospheric CH4,so the effects of fire disturbance on CH4 fluxes from forest soils cannot be ignored.At the same time,a large amount of black carbon is produced after fire due to incomplete combustion of vegetation.Black carbon is an aromatic compound with a porous structure,which can affect soil porosity,pH and other physicochemical properties after entering the soil and thus change the soil structure,so it is often used as a soil conditioner to reduce CH4 emissions from agricultural soils,but,there is a lack of clarity as to whether post-fire black carbon inputs can affect forest soil CH4 fluxes and the factors influencing them.[Method]In this study,we investigated the dynamic changes of soil CH4 fluxes and influence factor after fire disturbance and post-fire black carbon inputs using Pinus tabulaeformis forest in Shenyang's Checkboard Mesa as the research object.[Result]1)The fire disturbance increased soil CH4 fluxes during the growing season in P.tabulaeformis forests,with soil CH4 fluxes in the heavily burned sample plots being significantly higher than those in the control sample plots and the lightly burned sample plots.2)Black carbon input decreased soil CH4 fluxes during the growing season in P.tabulaeformis forests,and the magnitude of the decreased in soil CH4 fluxes increase with the increase in the amount of black carbon input.3)The fire intensity had a direct and highly significant positive effect on soil CH4 fluxes,with a direct and highly significant positive effect on soil CH4 fluxes,which explaining 46.9%(P<0.001);Black carbon input had a direct significant negative effect on soil CH4 flux,explaining 8.8%(P<0.05);And MBC and MBN hada direct highly significant positive effect on soil,explaining 29.0%and 49.3%,respectively(P<0.001).[Conclusion]Fire disturbance significantly increase soil CH4 fluxes,black carbon input can mitigate the effect of fire disturbance on soil CH4 fluxes to a certain extent,and that fire disturbance and black carbon input affect soil CH4 fluxes mainly by changing microbial biomass.The study provides a theoretical basis for how to reduce post-fire greenhouse gas emissions and thus improve the ecological environment of fire sites as well as post-fire understory.

CH4fire disturbanceblack carbonmicrobial biomass

胡同欣、王玉崧、窦旭、孙奥博、于澄、韩宇、孙龙

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东北林业大学林学院,黑龙江 哈尔滨 150040

东北林业大学森林生态系统可持续经营教育部重点实验室,黑龙江 哈尔滨 150040

甲烷 火干扰 黑炭 微生物生物量

国家自然科学基金项目中国科协青年托举工程项目黑龙江省自然基金优秀青年-联合引导项目

32001324YESS20210370LH2021C012

2024

中南林业科技大学学报
中南林业科技大学

中南林业科技大学学报

CSTPCD北大核心
影响因子:1.442
ISSN:1673-923X
年,卷(期):2024.44(7)