Enrichment mechanisms of Mo in soil in the karst region Guangxi, China.

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⁻¹ (with a mean of 0.22 mg·kg⁻¹). In comparison, the soil Mo derived from carbonate rocks can reach up to 6.00 mg·kg⁻¹ (with a mean of 2.75 mg·kg⁻¹), 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. [Display omitted] • Soil Mo is correlated with the distribution of carbonate rocks in karst area. • Soil Mo higher in karst regions (mean 2.32 mg kg⁻¹) than in non-karst regions. • Bedrocks volume reduction and mineral composition affect soil Mo enrichment. • Adsorption of Mo by Fe-Mn nodules contributes to the enrichment. [ABSTRACT FROM AUTHOR]