soil compaction

soil CO2 efflux

soil bulk density

small macropores

ridge tillage

soil CO 2 efflux

Physicochemical parameters

Limited information is available for how soil compaction affects carbon dioxide (CO₂) efflux under different tillage systems. To improve understanding of the effects of compaction and tillage on soil CO₂ efflux, an incubation study consisting of no tillage (NT), moldboard plow (MP), and ridge tillage (RT) was conducted to explore the relationships between CO₂ efflux and bulk density, as well as pore size distribution under different levels of bulk densities, and the thresholds of bulk density and the volume of pore size above which CO₂ efflux were affected in northeast China. Results showed that there was a significantly negative correlation (r = -0.990, p<0.05; r = -0.986, p<0.05; and r = -0.992, p<0.01, respectively, for NT, MP, and RT) between CO₂ efflux and bulk density, whereas the correlation was significantly positive (r ranges from 0.75 to 0.85, p<0.05 for each tillage practice under bulk densities of 1.0-1.6 g/cm³) for the volume of small macropores (30-100 μm). The critical value of bulk density for impeding CO₂ efflux was more produced in 1.6 g/cm³ and the volume of small macropores affected CO₂ efflux variation greatly. Ridge tillage is a better tillage practice for impeding soil CO₂ efflux than no tillage, as evidenced by the lesser volume of small macropores.