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