“…The mobility of REE in soils is a function of their ionic radii and speciation in solution, pH, Eh, water fluxes, and the nature of secondary intermediate minerals formed under different conditions [5,95]. Sorption on clay minerals [149][150][151][152], phosphates [17,104,153], Fe-/Mn-hydroxides [11,18,[154][155][156], Al hydroxides [156], and soil organic matter (SOM) [72,104,136,154,157,158] decrease the solubility and mobility of REE in soils. Conversely, the presence of inorganic and organic ligands such as sulfate, carbonates, fluorides [9,159], carboxylates [14,73,77,160,161], humic and fulvic acids [136,158,162] can counteract sorption and foster their presence in the soil solution.…”