In this study, the dissolution of stibnite, Sb2S3, which is an antimon
y ore, in HCl solutions was investigated, taking into consideration th
e effect of particle size, acid concentration, stirring speed, solid-t
o-liquid ratio, and temperature. It was observed that the dissolution
rate increased with increasing temperature and with decreasing particl
e size and solid-to-liquid ratio, while no pronounced effect of stirri
ng speed was observed. Using the experimental data, we attempted to es
tablish a kinetic model for the dissolution of the ore in HCl solution
s. Employing graphical and statistical methods, the following kinetic
model including the effect of the above choosen parameters was establi
shed to represent the dissolution process -In(1 - X) = 9.79 x 10(-10).
(D)(-0.908)(C)(10.600)(S/L)(-0.321)e(-6244/T) t, where X is the conve
rsion fraction of the mineral, D is the particle size, C the acid conc
entration in weight percent, and S/L is the solid-to-liquid ratio in g
rams per milliliter. The activation energy for this dissolution proces
s was calculated as 52 kJ mol(-1).