Prof. YANG Lei | Publications & Academic Profile | SinoGreenTech

Research Publications & English Decoded Briefs

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SCIENCE CHINA Materials•2026•DOI: 10.1007/s40843-026-4244-0

Boosting the Operational Stability of Near-Infrared Perovskite LEDs Utilizing a Zinc Ion-Chelated Hybrid Electron-Transport Layer: The Critical Role of Interfacial Reactions

Near-infrared perovskite light-emitting diodes (NIR-PeLEDs) suffer from poor operational stability, largely due to interfacial reactions at the electron-transport layer (ETL)/perovskite interface. Here, we introduce a zinc ion (Zn2+)-chelated hybrid ETL derived from a Zn2+-chelated polyethylenimine ethoxylated (PEIE) complex, which partially retains the surface properties of ZnO but exhibits significantly reduced oxygen defects and surface-adsorbed hydroxyl groups. This well-modulated surface promotes perovskite crystallization and mitigates interface-induced deprotonation of organic cations during device operation. Consequently, NIR-PeLEDs employing this hybrid ETL achieve a peak external quantum efficiency (EQE) of 20.1%, a high radiance of 652 W sr-1 m-2, and an exceptional T50 lifetime of 270.7 hours at a high current density of 100 mA cm-2, which is over five times that of devices based on conventional ZnO nanocrystal (NC) ETLs. Our results present an effective ETL strategy for operationally stable NIR-PeLEDs and thoroughly reveal the critical role of regulating interfacial reactions in stabilizing buried interfacial contacts. These findings provide valuable insights for advancing perovskite optoelectronic devices that suffer from interface-induced performance degradation.

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Environmental Chemistry•2026•DOI: 10.7524/j.issn.0254-6108.2025010701

Long-term Effects of Biochar Application on Physicochemical Properties and Microplastic Accumulation in Aeolian Sandy Soils

This study investigated the long-term effects of biochar application on physicochemical properties and microplastic accumulation in aeolian sandy soils, based on a field experiment established in 2014. After seven years of mulched cultivation, soil samples were collected from 0–30 cm and 30–60 cm depths. Biochar application significantly increased soil porosity and available nitrogen, phosphorus, and potassium contents, while reducing bulk density. At a biochar rate of 126.00 t·hm−2, soil water content was significantly reduced. Microplastic abundance averaged 3459.57 pieces·kg−1 in the 0–30 cm layer, with the highest abundance at 126.00 t·hm−2; in the 30–60 cm layer, average abundance was 3163.50 pieces·kg−1, with the highest at 63.00 t·hm−2. Microplastics were predominantly transparent, film-shaped, and 0–0.5 mm in size. The results indicate that biochar application significantly increased microplastic abundance in aeolian sandy soils, providing insights into microplastic adsorption and enrichment in agricultural ecosystems. Further research is needed to elucidate underlying mechanisms.

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Environmental Chemistry•2026•DOI: 10.7524/j.issn.0254-6108.2026022502

Impact of Land Use Types on Topsoil Carbon and Nitrogen and Their Spatial Distribution Characteristics in the Karst Area of the Yunnan-Guizhou Plateau: A Case Study of the Sancha River Basin

This study investigates the effects of different land use types on topsoil carbon (C) and nitrogen (N) contents and their spatial distribution in the lower reaches of the Sancha River Basin, a karst region of the Yunnan-Guizhou Plateau. Grid sampling collected 0–20 cm topsoil from forestland (n=23), cultivated land (n=25), and grassland (n=32). Total C and N were measured. Results showed that topsoil C content followed grassland (40.36±22.92 g·kg−1) > forestland (37.05±12.83 g·kg−1) > cultivated land (34.06±14.57 g·kg−1), while N content followed forestland (2.89±0.76 g·kg−1) > grassland (2.67±1.19 g·kg−1) > cultivated land (2.50±0.65 g·kg−1). One-way ANOVA revealed no significant differences among land use types (P>0.05). Soil C and N were significantly positively correlated across all land uses (r>0.5, P<0.001). Coefficient of variation (CV) indicated grassland had the highest C variability (0.57), while forestland showed the most stable C and N (CV=0.35 and 0.26, respectively). Cultivated land had CVs of 0.43 for C and 0.26 for N. Spatially, forestland exhibited concentrated high C values with significant N heterogeneity; grassland had higher C in southern and eastern areas but scattered distribution, with generally low and variable N; cultivated land showed uniform but lowest C and N. Land use types significantly drive topsoil C and N dynamics through vegetation input, soil disturbance, and management practices, underscoring the importance of rational land use planning for enhancing carbon sink functions and sustainable development in karst watersheds.

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