Technosol Micromorphology Reveals the Early Pedogenesis of Abandoned Rare Earth Element Mining Sites Undergoing Reclamation in South China
2025
Watteau, Françoise | Morel, Jean Louis | Liu, Chang | Tang, Yetao | Huot, Hermine | Laboratoire Sols et Environnement (LSE) ; Université de Lorraine (UL)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) | Sun Yat-sen University [Guangzhou] (SYSU) | Institut d'écologie et des sciences de l'environnement de Paris (iEES Paris) ; Institut de Recherche pour le Développement (IRD)-Sorbonne Université (SU)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) | International Joint Lab-ECOLAND | Fundamental Research Funds for Colleges and Universities 171gpy90 | Young Teacher Training Program of Sun Yat-sen University 21850410450 | National Natural Science Foundation of China (NSFC) 20192ACB70016 | National Key Research & Development Program of China 41771343 | National Natural Science Foundation of China (NSFC) 2022A0505090002 | Guangdong Province Science and Technology Program
International audience
Mostrar más [+] Menos [-]Inglés. The process of anthropogenic pedogenesis has necessarily become an important aspect of the study of today's soils. The sustainable reclamation or remediation of soils degraded by industrial or mining activities is currently of great interest worldwide. In this field, the study of thin soil sections can provide relevant answers, particularly to questions concerning the evolution of these soils under the impact of reclamation practices. Here, we describe an experiment to reclaim former rare earth element mining sites in China using organic soil amendments and plantations of a local fiber plant, Boehmeria nivea. Two years after the start of the experiment, a study of soil structure, considered as an indicator of soil biofunctioning, was carried out on the different plots, supplemented by monitoring of physico-chemical properties. Morphological (light microscopy) and analytical (SEM-EDX, µ-XRF) characterization of thin sections allowed us to pinpoint some pedological processes as aggregation with particular reference to the contribution of biological factors and mineral species, highlighting the impact of the practices implemented. Using a soil micromorphology approach enabled us to track the rapid evolution of the early stages of pedogenesis of these Technosols and to provide insight into the potential for reclamation of these mined sites in the future.
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