Rosenberg, Yoav O.Sadeh, YonatanMetz, VolkerPina Martínez, Carlos ManuelGanor, Jiwchar2023-06-192023-06-1920140016-703710.1016/j.gca.2013.09.041https://hdl.handle.net/20.500.14352/34083Co-precipitation of Ra and Ba in barite (i.e., the formation of a RaxBa1-xSO4 solid solution) has long been established as an important process that has the potential to control Ra concentration. This process is commonly described by a distribution model. Ample studies have shown that the key parameter of this model, the partition coefficient, varies in the range of 1–2 as a function of temperature, salinity and precipitation kinetics of the RaxBa1-xSO4 solid solution. This roughly twofold change in the partition coefficient may lead to large differences in the concentration of dissolved Ra. The present study systematically investigated the co-precipitation kinetics of the RaxBa1-xSO4 solid solution from aqueous solutions up to 5.9 mol kg-1 H2O NaCl, circum-neutral pH and at ambient temperature. Laboratory batch experiments designed to follow the nucleation of the RaxBa1-xSO4 solid solution and the co-precipitation kinetics of Ba and Ra from aqueous solutions which were initially supersaturated with respect to barite (degree of supersaturation, ßbarite = 20 ± 2). The following empirical law describes the dependence of the activity-based partition coefficient, K¨D,barite, on the degree of supersaturation, ßbarite: = 20 ± 2). K¨D,barite =(199 ± 0,05) - (0,58 ± 0,06)log(ßbarite). This empirical law is in good agreement with other literature data. The outcomes of the empirical law are compared to the prediction of a model for the nucleation of two-dimensional islands.engAtribución-NoComercial-SinDerivadas 3.0 Españahttps://creativecommons.org/licenses/by-nc-nd/3.0/es/journal articlehttps://www.sciencedirect.com/science/article/pii/S0016703713005504open access548NucleationNaClCristalografía (Geología)