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FINAL REPORT Background Vast majority of literature work concludes that the strong Mg 2+ hydration is the ultimate blockage to low-T anhydrous Mg-CO 3 crystallization and the incorporation of Mg 2+ in carbonate (i.e. the dolomite problem). A direct manifestation of the strong Mg-H 2 O association can be found in the products of low-T Mg-CO 3 precipitation which yields exclusively hydrated phases (barringtonite MgCO 3 ·2H 2 O, nesquehonite MgCO 3 ·3H 2 O, lansfordite MgCO 3 ·5H 2 O;doi:10.2172/1089154 fatcat:wdexj25l6rdvbogdqfyfazwicu