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Forsterite dissolution is a surface-controlled reaction which is kinetically hindered at atmosphericconditions and favored at acidic pH and in the presence of organic compounds [2,3,4,5]. To enhance itseveral options can be applied, e.g., an increase of the temperature, an increase of the surface area, and atuning of the chemical composition of the aqueous system by the addition of chemical compounds whichcatalyze the dissolution reaction.
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