Aragonite was synthesized inorganically using a seeded-growth technique to characterize precipitation kinetics for the heterogeneous growth of solid from dilute solutions (ionic strength: 0.05-0.07 mol l -1 ). The concentration of all aqueous constituents, including Ca (*5-15 mmol l -1 ), Na (*10-35 mmol l -1 ), Cl (*30-35 mmol l -1 ), and carbon (as total alkalinity: *10 to 17 meq l -1 ), was held constant by the addition of titrants that contained excess solute concentrations to balance the growth of solid phase during the precipitation reaction, and a CO 2 /N 2 gas mixture (0.009-0.178) was bubbled through each solution to facilitate mass exchange between gaseous and aqueous carbon species. Forty-three experiments were conducted at 10°(n = 13), 25°(n = 21), and 40°C (n = 9), over a range of average saturation states with respect to aragonite from 8.3 to 28.5, 2.9 to 19.6 and 2.0 to 12.2, and average precipitation rates from 10 2.8 to 10 3.8 , 10 2.3 to 10 4.0 , and 10 2.5 to 10 4.1 micromol m -2 h -1 , respectively. Reaction orders averaged 1.7 ± 0.10 at 10°, 1.7 ± 0.07 at 25°and 1.5 ± 0.06 at 40°, and they were independent of temperature while rate constants averaged 10 1.3 ± 0.12, 10 1.9 ± 0.06, and 10 2.6 ± 0.04 micromol m -2 h -1 , respectively, increasing one-half order of magnitude for each 15°C rise in temperature. From these data, an Arrhenius activation energy of 71.2 kJ mol -1 is calculated for the heterogeneous precipitation of aragonite. This value is comparable to a sole independent measurement of 80.7 kJ mol -1 reported for the solid-solution recrystallization of monohydrocalcite to aragonite (Munemoto and Fukushi in J Mineral Petrol Sci 103: 345-349, 2008).