“…Given the limitations of SEI extension A, as well as the restricted geometries available using modified Derjaguin methods, prior methodologies have not been able to characterize DLVO interactions for particles within valleys of rough surfaces. As a result, studies typically consider interactions on only particles positioned well above a rough surface ,,− or, in the case of adhesion, assume the particle is positioned directly above an asperity of the rough surface. ,− ,, Such assumptions are justified when the particle is much larger than the wavelengths of surface roughness and cannot fit in the valleys. However, smaller particles can fit within valleys of rough surfaces, where they have been shown to preferentially deposit. ,, …”