环境科学
覆盖作物
土壤碳
农学
土壤呼吸
生物群落
耕作
异养
碳循环
碳纤维
呼吸
生物量(生态学)
分解者
碳汇
常规耕作
生态系统
肥料
种植
总有机碳
种植制度
土壤有机质
作物残渣
固碳
生物地球化学
土壤水分
生物地球化学循环
大气碳循环
初级生产
碳呼吸
营养物
作者
Wen-Yu Tseng,Bishal Subedi,Toshiyuki Hirata,Yo Toma
标识
DOI:10.1080/00380768.2026.2718070
摘要
Cover cropping combined with reduced tillage is increasingly being adopted to enhance carbon sequestration. A better understanding of the short-term response and carbon dynamics associated with cover cropping is essential for reducing uncertainties during its initial adoption. This study quantified net biome production under reduced-tillage cover cropping system and compared it with conventional tillage, tillage without fertilizer, and no-till without fertilizer in Hokkaido, Japan. Heterotrophic respiration, labile carbon fractions, and their linkages with residue inputs were also assessed during the fallow (in the presence of cover crop) and the subsequent soybean phase in the first-year adoption. Our results revealed that cumulative heterotrophic respiration was higher under reduced-tillage cover cropping than under treatments with bare fallow during the fallow phase, whereas no treatment differences were observed during the soybean phase. Although cover cropping increased water-extractable organic carbon at seeding time, neither microbial biomass carbon nor labile carbon fractions differed among treatments. Heterotrophic respiration was negatively associated with labile organic carbon in deeper soil layers during the fallow phase, whereas no linkage was detected among residue inputs, labile carbon fractions, and heterotrophic respiration during soybean phase. Nevertheless, reduced-tillage cover cropping resulted in moderate soil temperature sensitivity of heterotrophic respiration and basal respiration, falling between those of conventional tillage and reduced-tillage without cover cropping. Overall, the implementation of reduced-tillage cover cropping increased net biome production to 0.85 Mg C ha−1 in the first-year, shifting the system from a carbon source to a carbon sink by replacing the bare fallow phase with an additional period of carbon assimilation.
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