Abstract
The dissolved organic carbon (DOC) depth profiles and the morphology of in-vitro coagulated dissolved organic matter (DOM) were investigated in a steady-state mostly anoxic aquatic system (Lac Pavin monimolimnion). High-resolution cryo-scanning electron microscopy (Cryo-HRSEM) was used to reveal the ultrastructure of the coagulated matter. The study focused on differences in DOC concentrations and coagulation morphotypes between microfiltered and nanofiltered waters. Two types of molecular weight (MW) DOC profiles were identified: although all MW DOC concentrations increased across the chemocline, high MW DOC (> 1 kDa) continued to increase significantly below, while low MW DOC (< 1 kDa) had a quasi-constant value downward the monimolimnion. Cryo-HRSEM images showed organic material composed on the one hand of various distinct shapes such as sheets, nanobelts, tubes, rings, platelets and globules entangled with each other, and on the other hand of fragments of netted threads, trapping Fe-phosphate grains. MW DOC depth profiles and the coagulation morphotype distribution suggest that the distinct organic shapes (sheets, tubes, rings, etc.) correspond to lower MW DOM equally distributed through the monimolimnion, while netted material should be attributed to higher MW DOM scavenged during its upward turbulent diffusion through the monimolimnion. It is concluded that recycling by sedimentation in the monimolimnion does not involve the total DOC but specifically the higher MW DOC imaged by meshed threads coagulated and aggregated in flocculation networks. Ultrastructural 3D morphological observation through Cryo-HRSEM is proposed as a tool to characterize DOM.
Highlights
• Dissolved organic carbon molecular weights are fractionated through the water column.
• 3D Cryo-HRSEM images distinguish different coagulate morphotypes.
• Flocculation limits high molecular weight dissolved organic carbon diffusion.
• Differential nanostructural gelation controls diffusion, flocculation, and sedimentation.
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Acknowledgements
All members of the teams involved in the Metanox and Methanolac projects, and in particular Didier Jézéquel, are thanked for their commitment to the organization of the sampling campaigns and their help during the field work. The municipal authority of Besse-et-Saint-Anastaise is thanked for the provision of facilities on the banks of the lake and Clermont-Auvergne University (formerly Blaise Pascal University) for accommodation at the biological station of Besse-en-Chandesse. François and Hélène Joubert, former hoteliers-restaurateurs of the Lac Pavin Hôtel Restaurant, are kindly thanked for their warm and unfailing welcome. Annie Richard (Centre de Microscopie Electronique of the University of Orléans) helped in Cryo-HRSEM observations and analyses. Elizabeth Rowley-Jolivet helped improve the English. The reviewers are acknowledged for their critical and highly constructive comments.
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Funding was provided through Agence National de la Recherche (ANR) and EC2CO Institut National des Sciences de l'Univers (INSU) under the grants Metanox and Methanolac.
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The planning of the study, sampling and fractionations in the field and geochemical analysis were performed by Patrick Albéric. Supervising cryo-HRSEM observations and analysis were performed by Christian Défarge with Patrick Albéric and the help of the technician of the Centre de Microscopie Electronique of the University of Orléans. The manuscript was drafted by Patrick Albéric, with contributions from Christian Défarge.
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Albéric, P., Défarge, C. Forms of Spontaneous Coagulation and Recycling of Dissolved Organic Carbon in a Monimolimnetic Water Body. Environ. Process. 11, 25 (2024). https://doi.org/10.1007/s40710-024-00699-2
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DOI: https://doi.org/10.1007/s40710-024-00699-2