Mf. Suarez et Rg. Compton, DISSOLUTION OF MAGNESIUM-OXIDE IN AQUEOUS ACID - AN ATOMIC-FORCE MICROSCOPY STUDY, JOURNAL OF PHYSICAL CHEMISTRY B, 102(37), 1998, pp. 7156-7162
The dissolution of the surfaces (100), (110), and (111) of MgO in aque
ous hydrochloric acid is studied by in-situ AFM experiments in a flow
cell with known hydrodynamics,which permits the modeling of the rate o
f proton transport to the solid surface. Comparison with directly meas
ured rates of dissolution determined via monitoring the absolute heigh
t of the surface in real time shows that the dissolution of all three
surfaces is a surface-controlled reaction. Examination of the surface
morphology shows that the (100) plane dissolves via the growth of etch
pits which are of circular or square shape depending on the acid conc
entration. In contrast, the (110) surface dissolves to form a corrugat
ed surface of parallel ridges whose surfaces are predominantly compose
d of (100) planes. The (111) surface dissolves via triangular etch pit
s of a fixed orientation where (100) planes are partly re-expressed du
ring the pit growth. These observation are in concordance with previou
s reports that the (100) plane is the most stable surface of MgO.