首页|林火干扰后多年冻土区土壤有机碳及其组分变化特征

林火干扰后多年冻土区土壤有机碳及其组分变化特征

扫码查看
北半球多年冻土区土壤有机碳(SOC)是全球碳库的重要组成部分,在全球碳平衡过程中具有重要作用。随着全球气候变化,中高纬度多年冻土区森林火灾频发,诱发多年冻土快速退化,导致SOC大量损失,对气候变暖形成正反馈效应。研究不同火烧强度后多年冻土区SOC及其组分的含量变化特征,对于火后SOC库的管理具有重要意义。本文选取大兴安岭阿龙山镇多年冻土区2009年火烧迹地为研究对象,通过相邻样地比较法,对不同火烧强度0~1 m深度的SOC含量、密度及其组分含量的变化规律进行分析。结果表明:(1)在未过火样地,随着土壤深度的增加,SOC含量及密度、游离态颗粒有机碳(fPOC)、闭蓄态颗粒有机碳(oPOC)和颗粒态有机碳(POC)含量下降,与0~10cm土层相比,90~100 cm处含量分别下降了 84。75%、2。78%、99。82%、91。86%和98。97%;矿物结合态有机碳(MAOC)含量变化趋势相反,与0~10 cm土层相比,90~100 cm处含量增加了 830。93%。(2)与未过火样地相比,在0~1 m深度,轻度火烧样地SOC含量和密度分别降低了 9。78%和9。30%;fPOC、oPOC、POC和MAOC含量分别增加了5。03%、39。95%、11。19%和 15。98%。重度火烧样地 SOC含量、SOC 密度、fPOC、POC 和MAOC含量分别降低了 65。11%、68。48%、72。53%、54。29%和81。81%;oPOC含量增加了 30。84%。(3)火烧强度、土层深度以及二者的交互作用对SOC含量、密度及其组分含量的影响均表现为极显著。综上所述,林火对SOC及其组分产生了显著影响,导致SOC及其组分大量损失,改变了 SOC库的分布格局,降低了土壤碳库的质量及其稳定性。本文结果可为大兴安岭多年冻土区火后土壤碳动态研究提供基础数据支撑。
Variation characteristics of soil organic carbon and its fractions in the permafrost region after forest fire disturbance
Soil organic carbon(SOC)in permafrost regions of the Northern Hemisphere is an important part of the global carbon pool and plays an important role in the global carbon balance process.With global climate change,forest fires occur frequently in mid-high latitudes permafrost regions,which induces rapid degradation of permafrost,leading to a large loss of SOC,and forming a positive feedback effect on climate warming.Therefore,it is of great significance to study the changes of SOC and carbon fraction in permafrost regions with varied fire severities for the management of SOC pool.In this paper,the burned area in 2009 in the permafrost area of Alongshan Town,Da Xing'anling Mountains was selected as the research object in 2023.The SOC con-tent,density and fraction were analyzed at depths of 0~1 m at different fire severity sites by the adjacent sample plot comparison method.The results showed that:(1)In the unburned plots,with increasing soil depth,SOC content and density,free particulate organic carbon(fPOC),occluded particulate organic carbon(oPOC)and particulate organic carbon(POC)contents decreased.Compared with 0~10 cm,the SOC content,SOC densi-ty,fPOC,oPOC and POC contents at depth of 90~100 cm decreased by 84.75%,2.78%,99.82%,91.86%and 98.97%,respectively;the content of mineral-associated organic carbon(MAOC)increased by 830.93%.(2)Compared with the unburned plots,the SOC content and density at the lightly burned plots decreased by 9.78%and 9.30%at the depth of 0~1 m,respectively.The contents of fPOC,oPOC,POC and MAOC in-creased by 5.03%,39.95%,11.19%and 15.98%,respectively.The SOC content,SOC density,fPOC,POC and MAOC contents at the severely burned plots decreased by 65.11%,68.48%,72.53%,54.29%and 81.81%,respectively.The content of oPOC increased by 30.84%.(3)The effects of fire severity,soil depth and their interaction on SOC content,density and its fractions contents were extremely significant.In conclu-sion,forest fire has a significant impact on SOC and its fractions,resulting in a large loss of SOC and its frac-tions,changing the distribution pattern of SOC pool,and reducing the quality and stability of soil carbon pool.The results of this study can provide basic data support for the post-fire soil carbon dynamics in the permafrost region of the Da Xing'anling Mountains.

permafrostDa Xing'anling Mountainsforest fire disturbancefire severitysoil organic carboncarbon fraction

陈魁、李晓英、蔡慧颖、韩易伦、刘静

展开 >

东北林业大学林学院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

中国科学院西北生态环境资源研究院冰冻圈科学与冻土工程重点实验室,甘肃兰州 730000

多年冻土 大兴安岭 林火干扰 火强度 土壤有机碳 碳组分

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(6)