Spatio-Temporal Distribution and Environmental Behavior of Dissolved Rare Earth Elements (REE) in the Zhujiang River, Southwest China.

Rare earth elements (REE) geochemistry can reveal the environmental information of solutes in river systems because REE is sensitive to hydro-geochemical changes in the earth's surface environment. This work collected the river water samples from Zhujiang River (the largest river in South China) to investigate the concentration, fractionation, and environmental implication of dissolved REE. The total dissolved REE (∑REE) concentrations are similar in different seasons. In mid-lower reaches, the REE concentrations tend to increase corresponding to low pH, and the normalized ratios of lanthanum (La) to ytterbium (Yb) are higher, suggesting weak fractionation between light REE and heavy REE. Compared to the previous study in 2000, the higher samarium (Sm) and europium (Eu) concentrations are most likely influenced by stronger water/particle interaction. These findings provide preliminary information for REE cycle in the surface environment.