Tailing pedogenesis and ecological reconstruction
We investigate mineral weathering, secondary mineral formation, organic carbon stabilization, and structural development during the transformation of mine tailings into soil-like substrates.
Mine tailings commonly have narrow particle-size distribution, limited aggregate structure, low organic matter and nutrient contents, abnormal pH or salinity, and potential metal mobility. These constraints limit plant establishment and ecological function recovery. This direction studies mineral weathering, element release, and secondary mineral formation during tailing pedogenesis driven by organic inputs, plant roots, and microbial activity.
We focus on the coupling between Fe, Si, and Al mineral transformation and organic matter stabilization, and examine how rhizosphere processes, microbial succession, and organo-mineral complexation regulate aggregate development, carbon and nitrogen accumulation, and contaminant retention. These results provide mechanistic support for optimizing tailing pedogenesis technologies and evaluating long-term ecological stability.