Response of Soil CO2 Emission to Addition of Biochar and Dissolved Organic Carbon along a Vegetation Restoration Gradient of Subtropical China

被引:1
作者
Zhu, Yulin [1 ]
Tang, Xinghao [2 ]
Huang, Yunpeng [2 ]
Jiang, Jing [1 ]
Fang, Xiong [3 ]
机构
[1] Fujian Agr & Forestry Univ, Coll Resources & Environm, Fuzhou 350002, Peoples R China
[2] Fujian Acad Forestry Sci, Fuzhou 350012, Peoples R China
[3] Jiangxi Agr Univ, Coll Land Resources & Environm, Nanchang 330045, Peoples R China
来源
FORESTS | 2024年 / 15卷 / 05期
基金
美国国家科学基金会;
关键词
biochar; vegetation restoration; dissolved organic matter addition; CO2; emission; soil enzyme; GREENHOUSE-GAS EMISSIONS; HETEROTROPHIC RESPIRATION; MICROBIAL PROPERTIES; COMMUNITY STRUCTURE; ENZYME-ACTIVITIES; AMENDMENT; MINERALIZATION; SEQUESTRATION; MATTER; ECOSYSTEMS;
D O I
10.3390/f15050753
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Biochar, as a soil amendment, has been widely confirmed to increase soil carbon sequestration. However, how biochar addition affects soil carbon changes during the vegetation restoration process is still unclear, which constrains our ability to explore biochar's application in the technology of soil carbon sequestration in forests. We conducted an incubation experiment on biochar and dissolved organic matter (DOM) addition to soil at three stages of revegetation (degraded land (DS), plantation forest (PS), and secondary natural forest (NS) in Changting County in Fujian province, China) to investigate the effects of vegetation restoration, biochar, DOM, and their interaction on soil CO2 emission and its relative mechanisms. We found that the accumulative release of CO2-C in the NS and PS soils was 7.6 and 6.8 times higher, respectively, in comparison to that from the DS soil. In the DS, biochar addition significantly increased the accumulative release of CO2-C, soil pH, NH4+-N content, qCO(2), phenol oxidase, and peroxidase activities. Peroxidase activities were positively correlated with the accumulative release of CO2-C, and oxidase was the most important direct factor influencing the accumulative release of CO2-C in the DS. However, the accumulative release of CO2-C, soil NH4+-N content, qCO(2), beta-glucosidase, and N-acetylglucosaminidase activities was significantly reduced after the application of biochar in the PS and NS. These two hydrolases were positively associated with the accumulative release of CO2-C, and hydrolase was the most vital direct factor influencing the accumulative release of CO2-C from the PS and NS soils. The positive effect of DOM addition on CO2 emission under biochar application declined with a vegetation restoration age increase. Our results indicated that biochar could alter microbial physiological processes, inhibit qCO(2) and hydrolase activities, and further decrease CO2 emission in relatively fertile soil from the PS and NS; but in the relatively barren soil from the DS, biochar might promote CO2 emission by stimulating microorganisms to enhance qCO(2) and oxidase activities.
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页数:15
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