Publications by authors named "Jianfei Yuan"

The acid mine drainage (AMD) is characterized by its highly acidic nature and elevated concentrations of metal ions, thereby exerting significant impacts on both human health and the environment. This study employed a dispersed alkaline substrate (DAS) consisting of thermal activation magnesite and pine shavings for the treatment of AMD. The investigation focused on determining the optimal thermal activation conditions of magnesite, evaluating the effectiveness of the DAS in regulating acidity and removing metal ions from AMD, identifying critical factors influencing treatment efficiency, and conducting toxicity assessment on the effluent.

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The coexistence of phosphorus (P) and cadmium (Cd) in river sediments poses a significant challenge for remediating these contaminants in aquatic environments, given the ongoing debates regarding their interactions. This study aimed to elucidate the impact of water-soluble phosphorus (PO) on the fate and transformation of sediment-associated Cd under varying conditions. The findings revealed that the impact of PO on the release of sediment-associated Cd depends on the presence or absence of cations such as Ca and Mg, with Ca exerting a more pronounced effect than Mg.

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The coexistence of hexavalent chromium (Cr(VI)) and nitrate (NO) in groundwater and surface water presents a considerable challenge for the natural attenuation of these two contaminants because their interactions in nature remain contentious. This study investigated the interplay between Cr(VI) and NO in hyporheic zone (HZ) sediments by integrating Cr(VI) reduction kinetics, NO transformation, microbial community structure, and a three-rate model. The concurrent natural attenuation of Cr(VI) and NO in the sediments was significantly influenced by their initial concentrations and redox conditions.

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The geogenic As enrichment occurs extensively in the major river basin from the Tibetan Plateau, while the knowledge involved with the underlying mechanisms is far from completion. The present study utilized the geochemical behaviors of rare earth elements (REE) to study the hydrogeochemical evolution and As enrichment in the Singe Tsnagpo River basin, a typical As-rich river basin in the Tibetan Plateau. The river water was characterized by significant positive Eu anomalies and slight negative Ce anomalies, indicating the hydrogeochemical control of oxidative weathering of sourcing rocks and the contribution of felsic rocks.

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Article Synopsis
  • The study focuses on the detonation of shelled charges, analyzing the fracture and fragmentation of the shell as it explodes.
  • It employs a thermochemical code and the Jones-Wilkins-Lee equation of state (JWL EOS) to better understand the energy output of the explosive and the casing's response.
  • Findings include improved accuracy in predicting fragment displacement and velocity, alongside insights into the shear failure of the shell, which can inform the design of more effective warheads.
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Clarifying the sources and historical variation of metal(loid)s in agricultural river sediments is vital for watershed contamination control and environmental improvements. In this study, a systematical geochemical investigation of Pb isotopic characteristics and the spatial-temporal distribution of metal(loid)s abundances was conducted to delineate the origins of metal(loid)s (Cd, Zn, Cu, Pb, Cr, and As) in sediments from an agricultural river, Sichuan Province, Southwest China. The results showed significant enrichment of Cd and Zn in the whole watershed, with substantial anthropogenic contributions of 86.

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Evaluation of aquifer response to earthquakes is important to understanding the evolution of aquifer properties and contaminant transport. In Changan Landfill, a multi parameter monitoring system was installed to collect data every 12 h. Principal Component Analysis (PCA), energy density and wavelet analysis, and tidal analysis were used to reveal the response mechanisms to four earthquakes, sensitivity of various parameters to seismic stimuli, and permeability evolution, respectively.

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