Response of soil enzymatic activity to pore structure under inversion tillage with organic materials incorporation in a Haplic Chernozem.

Soil pore structure affects microbial survival environmental conditions and thus enzyme activity. The mechanisms underlying returning organic materials on soil pore structure and enzymatic activity, however, remain unclear. We therefore conducted a field experiment in the fall of 2018 in northeastern China with a chernozem soil and four treatments: CT, conventional tillage; SCT, returning maize straw incorporation with conventional tillage; SIT, returning maize straw incorporation with inversion tillage; SMIT, returning maize straw and organic manure with inversion tillage.

Soil aggregates stability and storage of soil organic carbon respond to cropping systems on Black Soils of Northeast China.

Monoculture and improper management may reduce soil fertility and deteriorate soil structure in Black soils (Mollisols) of Northeast China. The experiment was carried out from 2015 to 2016 in Black Soils comprising five cropping systems: continuous corn (CC), soybean-corn rotation (SC), corn-soybean rotation (CS), fallow-corn (FC), and fallow-soybean (FS). Our results showed that CS and FS treatments significantly increased mean weight diameter (MWD) and fractal dimension (D) in mechanical stability aggregates (MSAs), and increased MWD and geometric mean diameter (GMD) in water-stable aggregates (WSAs) compared with CC treatment.