The morphology of iron electrodeposit is shown to relate closely to the pH
of the electrolyte solution. Macroscopically, depending on the strength of
the interbranch convection, which is associated with the concentration of H
3O+ in the electrolyte, the deposit morphology varies from treelike pattern
to meshlike pattern and dense-branching morphology. Microscopically the de
posit is ramified and dense-branching at lower concentration of H3O+, while
it becomes relatively smooth and stringy at higher H3O+ concentration. The
symmetry of the convective vortices on the two sides of the growing tip is
observed to decide the growth behavior of the tip. We suggest that H3O+ in
fluences the pattern formation and pattern selection in the electrodepositi
on of iron from FeSO4 solution by either initiating interbranch convection
or changing the effective interfacial energy of the deposit and the electro
lyte.