Publications by authors named "Shuai-Long Wen"

Dissolved organic matter (DOM) is a heterogeneous pool of compounds and exhibits diverse adsorption characteristics with or without phosphorous (P) competition. The impacts of these factors on the burial and mobilization of organic carbon and P in aquatic ecosystems remain uncertain. In this study, an algae-derived DOM (ADOM) and a commercially available humic acid (HA) with distinct compositions were assessed for their adsorption behaviors onto iron (oxy)hydroxides (FeOx), both in the absence and presence of phosphate.

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  • Algal-dissolved organic matter (ADOM) is a crucial part of dissolved organic carbon in nutrient-rich waters, influenced by microbial and sunlight-induced processes.
  • In a study lasting 18 days, three treatment methods were tested: light exposure (L), microbial activity (M), and a combination of both (L&M), with varying effectiveness on the breakdown of organic compounds.
  • Results indicated that microbial processes were better at removing dissolved organic carbon, while sunlight was more effective in altering specific fluorescent components, and the combination of both processes affected the decay rate of organic matter differently.
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  • - The stability of organic matter-iron-phosphate (OM-Fe-P) associations is crucial for understanding how organic carbon (OC) and phosphorus (P) move and are stored in the environment.
  • - The study explored how the abiotic reduction of these associations using Na-dithionite affects the release of iron (Fe), P, and organic matter (OM), finding that adsorbed OM and P are released quickly, while coprecipitated forms release them more slowly.
  • - Results showed that the type of organic matter used (algae-derived vs. terrestrial humic acid) and the method of association formation significantly influenced release rates, with coprecipitated associations being more stable and having a different distribution of
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  • Color dissolved organic matter (CDOM) in lakes is influenced by both external (allochthonous) inputs and internal (autochthonous) production, significantly affecting its composition and cycling.
  • A study was conducted in Lake Fuxian, China, to analyze CDOM during the wet season and compare its characteristics with other lakes, revealing that riverine CDOM had higher levels of humic-like substances while Lake Fuxian's CDOM was mainly protein-like.
  • The findings showed that although CDOM composition varied across various lakes, the quantity increased significantly in deeper lakes with well-vegetated catchments, suggesting that allochthonous inputs impact CDOM but can be moderated by in-lake processing dynamics.
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  • Shallow lakes can be dominated by either macrophytes or algae, which leads to distinct types of organic matter (OM) in their sediments that affect carbon storage and processing.
  • A study compared sediments from Taihu Lake's macrophyte-dominated (East Taihu Lake) and algae-dominated zones (Meiliang Bay), using various spectroscopic techniques to analyze the water-soluble organic matter (WSOM).
  • Results indicated that the WSOM from the macrophyte zone had larger molecular sizes and higher humification levels compared to the algae zone, while there was a greater presence of protein-like substances in the algae-dominated sediments.
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The generation of organic matter (OM) occurs synchronously with phytoplankton growth. Characterization of the generated particulate and dissolved OM during algal blooms in eutrophic lakes is crucial for better understanding the carbon cycle but remains limited. We speculate that sediments play a critical role in the biogeochemical transformation of OM derived from algal blooms in shallow lakes.

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Humic acid (HA) and phosphate interactions play a vital role in the biogeochemical cycle of carbon and nutrients and thus the trophic state of a lake. The adsorption behavior of HAs to sediments in the absence and presence of phosphate was investigated in this study. Three types of HAs were used, AHA from algae-dominated lake sediments, MHA from macrophyte-dominated lake sediments, and a reference HA (RHA) with terrestrial sources.

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The effect of external pollution inputs on phosphorus recovery, transport, and transformation in newborn surface layers from sediment dredging remains unclear. Clarifying this issue is important for the control and management of external pollution loads at the watershed scale, particularly after the implementation of sediment dredging activities. In this study, sediments in Meiliang Bay of Lake Taihu were investigated.

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It is of great importance to study the environmental significance of phosphorus fractions in overlying water and sediments of typical phytoplankton-and macrophyte-dominated zones. It will help to clarify the process of phosphorus migration and transformation in the sediment-water interface, and has practical significance for understanding the eutrophication process and its treatment in different regions of Taihu Lake. The investigation was conducted within typical phytoplankton-and macrophyte-dominated zones of Taihu Lake over four seasons to analyze the spatial and temporal differences between phosphorus fractions in water and sediments, and reveal their environmental significance.

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  • The study focused on the generation and emissions of nitric oxide (NO) in different ecological areas of Taihu Lake during summer, highlighting spatial variations across grass-type and algal-type zones.
  • Results indicated that areas with emergent macrophytes had significantly higher NO fluxes and dissolved concentrations compared to algae and submerged macrophyte areas, likely due to plant dominance and inorganic nitrogen levels.
  • Laboratory experiments revealed that factors like nitrate, organic carbon, and temperature play crucial roles in influencing NO production, with high NH-N levels potentially inhibiting it.
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Yuqiao Reservoir is an important source of drinking water in Tianjin. In recent years, the eutrophication status is becoming more and more serious, but its internal loading and distribution characteristics of nitrogen and phosphorus is not clear. The profiles of nitrogen and phosphorus at the sediment-water interface were analyzed using the Peeper (pore water equilibrium) technique and the spatial distribution was investigated.

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