Publications by authors named "Gege Yin"

Dissolved organic matter (DOM), the most reactive fraction of forest soil organic matter, is increasingly impacted by wildfires worldwide. However, few studies have quantified the temporal changes in soil DOM quantity and quality after fire. Here, soil samples were collected after the Qipan Mountain Fire (3-36 months) from pairs of burned and unburned sites.

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Constructed wetlands (CWs) are frequently used for effective biological treatment of nitrogen-rich wastewater with external carbon source addition; however, these approaches often neglect the interaction between plant litter and biochar in biochar-amended CW environments. To address this, we conducted a comprehensive study to assess the impacts of single or combined addition of common reed litter and reed biochar (pyrolyzed at 300 and 500 °C) on nitrogen removal, greenhouse gas emission, dissolved organic matter (DOM) dynamics, and microbial activity. The results showed that combined addition of reed litter and biochar to CWs significantly improved nitrate and total nitrogen removal compared with biochar addition alone.

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Article Synopsis
  • Membrane fouling and high concentrate production limit the effectiveness of membrane distillation (MD) for treating landfill leachate, but integrating activated carbon and biochar adsorption can help resolve these issues.
  • The study found that reversible and irreversible foulants in leachate differ significantly, with biochar outperforming activated carbon in removing foulant precursors.
  • The biochar-assisted MD system achieved improved results with 40% membrane flux recovery, higher filtration rates, and reduced concentrate production, leading to a potentially longer membrane lifespan.
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Heating temperature (HT) during forest fires is a critical factor in regulating the quantity and quality of pyrogenic dissolved organic matter (DOM). However, the temperature thresholds at which maximum amounts of DOM are produced (TT) and at which the DOC gain turns into net DOC loss (TT) remain unidentified on a component-specific basis. Here, based on solid-state C nuclear magnetic resonance, absorbance and fluorescence spectroscopies, and Fourier transform ion cyclotron resonance mass spectrometry, we analyzed variations in DOM composition in detritus and soil with HT (150-500 °C) and identified temperature thresholds for components on structural, fluorophoric, and molecular formula levels.

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