Origin and distribution of rare earth elements (REEs) in the soils of Meizhou City, southern China with high abundance of regolith-hosted REEs. (December 2022)

• Record Type: Journal Article
• Authors: Lin, Zhuoling; Wei, Gaoling; Zhang, Jinlan; Liang, Xiaoliang; Huang, Guangqing
• Is Part Of: Applied geochemistry. Volume 147(2022)
• Publication Date: 2022-12
• Subjects: Rare earth elements -- Regolith-hosted REEs -- Enrichment -- Fractionation -- Land types; Environmental geochemistry -- Periodicals; Water chemistry -- Periodicals; Geochemistry -- Social aspects -- Periodicals; Geochemistry -- Periodicals; 551.9
• DOI: 10.1016/j.apgeochem.2022.105514
• Languages: English
• ISSNs: 0883-2927

Abstract

Abstract: Currently, regolith-hosted rare earth element (REE) deposits in South China are the major source of global REEs, particularly heavy REEs (HREEs). This type of REE resource contains abundant movable, bioavailable, and ion-exchangeable REEs and may act as an environmental hazard; however, little is known regarding REEs in soils from areas with abundant deposits. Here, we investigated the REEs in the soil, surface water and crops, collected from Meizhou City, Guangdong Province, South China, as a representative region with abundant regolith-hosted REEs. Mean REE concentration (ΣREE) in the soil (318 μg g −1 ) exceeded the local soil background (169 μg g −1 ). The LREE/HREE ratio ranged from 2.04 to 69.4 in soil samples, suggesting the enrichment of light REEs (LREEs) compared with HREEs. Most soil samples exhibited positive Ce anomalies and negative Eu anomalies. The highest ΣREE (1162 μg g −1 ) was detected in forest land, followed by garden land (793 μg g −1 ) and paddy field (519 μg g −1 ). According to the correlation analysis, pH as well as soil organic matter (SOM), Fe, and Mn content contributed to REE enrichment, while SOM and Mn content affected REE fractionation. REE enrichment in soil may be related to natural sources (e.g., parent materials) and anthropogenic activities (e.g., fertilizer application and coal combustion). The REE contamination of surface water was not serious. However, ΣREE in crops (7.08 μg g −1 ·dw) indicated that these elements migrate from soils to plants, producing potential adverse effects on crops and humans. These findings shed new light on the geochemical behavior of REEs in the environments with abundant regolith-hosted REEs and can serve as a reference to prevent and control REE contamination. Highlights: High REE levels were detected in soils from areas with abundant ion-adsorbed REEs. REEs migrate from soils and are accumulated in crops. REE enrichment is related to pH and soil organic matter, Fe, and Mn content. REE fractionation is positively correlated to soil organic matter and Mn content.