Lipid vesicles penetrate into intact skin owing to the transdermal osmotic gradients and hydration force.

Gradients across the outer skin layers may result in fields enforcing a lipid flow into or through the intact skin surface provided that lipids are applied in the form of special vesicles. The osmotic gradient, for example, which is created by the difference in the total water concentrations between the skin surface and the skin interior, provides one possible source of such driving force. It is sufficiently strong to push at least 0.5 mg of lipids per hour and cm2 through the skin permeability barrier in the region of stratum corneum. The lipid concentration gradient, on the contrary, does not contribute much to the lipid penetration into dermis. Occlusion, therefore, is detrimental for the vesicle penetration into intact skin.