“…Less disturbed activity was conducive to the formation of soil aggregates (Li et al, ; Wang, Li, Pan, & Wang, ), which in turn enhanced the protection of soil organic matter against decomposition and thereby reduced soil OC and N losses (Christensen, ; Jenkinson, ). This phenomenon is consistent with other studies conducted in semiarid rangelands, farmlands, and the conversion of land use from cropland to woodland via shrubland (Dou, Xu, Shu, Zhang, & Cheng, ; Mishra, Ussiri, & Lal, ; Nosetto et al, ). Increased accumulations of soil OC and N after plant restoration were mainly attributable to increases in organic matter inputs to soils (Ding et al, ; Li et al, ; Yang et al, ).…”