生物炭
胡敏
土壤碳
环境科学
温带气候
生物量(生态学)
总有机碳
化学
土壤水分
土壤有机质
固碳
土壤科学
环境化学
农学
碳纤维
二氧化碳
热解
生态学
数学
生物
有机化学
算法
复合数
作者
Jhon Kenedy Moura Chagas,Cícero Célio de Figueiredo,Maria Lucrécia Gerosa Ramos
标识
DOI:10.1016/j.jenvman.2021.114403
摘要
Biochar is a carbon-rich material that increases soil C sequestration and mitigates climate change. However, due to the variability of experimental conditions, types of biochar and soil, the influence of biochar on the accumulation of different soil carbon fractions remains unclear. Therefore, a meta-analysis was performed that included 586 paired comparisons obtained from 169 studies conducted in various countries around the globe. The data set average showed significant relative increases of 64.3, 84.3, 20.1, 22.9 and 42.1% for total C, organic C, microbial biomass C, labile C and fulvic acid, respectively. The dissolved organic C, humic acid and humin fractions showed no significant variations. The relative increase in TC was favored by increasing biochar rates applied to fine-textured soils with low C content in temperate climate regions seen through short-term experiments conducted under controlled conditions. This behavior was different for each soil C fraction. Therefore, variations between experimental conditions, types of biochar and soil show that it is necessary to consider multiple factors when choosing the conditions of biochar use to maximize C sequestration in the soil and/or the increase of labile C fractions in the soil.
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