The mineral dissolution rate law gives the rate of dissolution per unit of mineral surface, in molm−2s−1, as a sum over acid, neutral and basic mechanisms,
r=j∑kje−REj(T1−298.151)aHX+nj(1−Ωpj)qj,
with rate constants kj at 25∘C, activation energies Ej, reaction orders nj (negative for the basic mechanism) and two exponents pj, qj, commonly taken as 1.