Radium-226 carbonate was synthesized from radium−barium sulfate ( 226 Ra 0.76 Ba 0.24 SO 4 ) at room temperature and characterized by X-ray powder diffraction (XRPD) and extended X-ray absorption fine structure (EXAFS) techniques. XRPD revealed that fractional crystallization occurred and that two phases were formed�the major Ra-rich phase, Ra(Ba)CO 3 , and a minor Ba-rich phase, Ba(Ra)CO 3 , crystallizing in the orthorhombic space group Pnma (no. 62) that is isostructural with witherite (BaCO 3 ) but with slightly larger unit cell dimensions. Direct-space ab initio modeling shows that the carbonate oxygens in the major Ra(Ba)CO 3 phase are highly disordered. The solubility of the synthesized major Ra(Ba)CO 3 phase was studied from under-and oversaturation at 25.1 °C as a function of ionic strength using NaCl as the supporting electrolyte. It was found that the decimal logarithm of the solubility product of Ra(Ba)CO 3 at zero ionic strength (log 10 K sp 0 ) is −7.5(1) (2σ) (s = 0.05 g•L −1 ). This is significantly higher than the log 10 K sp 0 of witherite of −8.56 (s = 0.01 g•L −1 ), supporting the disordered nature of the major Ra(Ba)CO 3 phase. The limited co-precipitation of Ra 2+ within witherite, the significantly higher solubility of pure RaCO 3 compared to witherite, and thermodynamic modeling show that the results obtained in this work for the major Ra(Ba)CO 3 phase are also applicable to pure RaCO 3 . The refinement of the EXAFS data reveals that radium is coordinated by nine oxygens in a broad bond distance distribution with a mean Ra−O bond distance of 2.885(3) Å (1σ). The Ra−O bond distance gives an ionic radius of Ra 2+ in a 9-fold coordination of 1.545(6) Å (1σ).