Lin Kun, Yang Zhongfang, Yu Tao, Ji Wenbing, Liu Xu, Li Bo, Wu Zhiliang, Li Xuezhen, Ma Xudong, Wang Lei, Tang Qifeng
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; Key Laboratory of Ecogeochemistry, Ministry of Natural Resources, Beijing 100037, China.
Ecotoxicol Environ Saf. 2023 Apr 15;255:114808. doi: 10.1016/j.ecoenv.2023.114808. Epub 2023 Mar 21.
Soils developed in karst regions have naturally high background values of molybdenum (Mo) due to geological factors. However, the enrichment mechanism of Mo in these soils are not fully understood, making it challenging to assess their ecological risk and utilize Mo-rich land resources. To shed light on this issue, this study collected and analyzed data from the 1:50,000 geochemical survey in Guangxi, including 536,503 sets of soil data and 3043 sets of rock data, as well as 40 sets of carbonate rock-soil from typical karst regions. The results showed that soil Mo enrichment is highly correlated with the distribution of carbonate rocks in karst regions. The carbonate rocks in these regions contain Mo ranging from 0.03 to 1.06 mg·kg (with a mean of 0.22 mg·kg). In comparison, the soil Mo derived from carbonate rocks can reach up to 6.00 mg·kg (with a mean of 2.75 mg·kg), representing an average enrichment of soil Mo that is 24 times higher compared to the carbonate parent rock. The enrichment of soil Mo in karst regions is primarily controlled by secondary enrichment during the weathering process of carbonate. During the insoluble residue accumulation process, the dissolution of carbonate leads to a dramatic reduction in bedrock volume, and the adsorption of clay minerals and Fe minerals in insoluble residues plays an essential role in Mo enrichment during these stages. During the soil-forming stage of the insoluble residue, most Mo leaches into the water body due to the mineral transformation of insoluble residue. Consequently, as Fe-Mn nodules in soils become more enriched with increasing weathering intensity, some Mo is absorbed and passivated by iron and manganese oxides (hydroxides). Accordingly, the contribution of Fe-Mn nodules and the degree of leaching were closely related to the enrichment of soil Mo in karst regions. This study provides insights into the enrichment mechanisms of Mo in soils developed in karst regions, which will help to evaluate their ecological risk in these environments.
由于地质因素,喀斯特地区发育的土壤钼(Mo)背景值天然较高。然而,这些土壤中钼的富集机制尚未完全明确,这使得评估其生态风险和利用富钼土地资源具有挑战性。为阐明这一问题,本研究收集并分析了广西1:50000地球化学调查的数据,包括536503组土壤数据、3043组岩石数据,以及来自典型喀斯特地区的40组碳酸盐岩-土壤数据。结果表明,土壤钼富集与喀斯特地区碳酸盐岩分布高度相关。这些地区的碳酸盐岩含钼量在0.03至1.06毫克·千克之间(平均为0.22毫克·千克)。相比之下,源自碳酸盐岩的土壤钼含量可达6.00毫克·千克(平均为2.75毫克·千克),表明土壤钼平均富集程度比碳酸盐母岩高24倍。喀斯特地区土壤钼的富集主要受碳酸盐风化过程中的次生富集控制。在不溶残渣积累过程中,碳酸盐溶解导致基岩体积大幅减小,不溶残渣中黏土矿物和铁矿物的吸附在这些阶段的钼富集中起关键作用。在不溶残渣成土阶段,由于不溶残渣的矿物转化,大部分钼淋溶到水体中。因此,随着土壤中铁锰结核随着风化强度增加而更加富集,一些钼被铁和锰的氧化物(氢氧化物)吸收并钝化。相应地,铁锰结核的贡献和淋溶程度与喀斯特地区土壤钼的富集密切相关。本研究为喀斯特地区发育土壤中钼的富集机制提供了见解,这将有助于评估这些环境中的生态风险。