Upward migration of either acidity or sodium is often cited as a concern when soil covers are placed over mine wastes. Regulatory concerns associated with upward migration are commonly used to justify capillary barriers or increased cover thickness. Upward migration of soluble salts is known to occur in soils with permanent or seasonal water tables near the soil surface and is a common problem in agricultural contexts. Short-term studies conducted at mine reclamation sites where changes in pH or salinity occurred at the contact between the soil cover and waste have been used to infer that upward migration would ultimately degrade cover quality. Thus, we investigated the potential for upward migration in soil covers overlying acid mill tailing and coal spoils 20 to 25 years after cover placement and revegetation. The soils were sampled and analyzed at discreet intervals above the soil-waste contact to assess upward migration. Changes in soil pH and/or extractable constituents were inconsistent among sites and varied from about 2 to 10 cm above the soil cover-waste contact. Field observations suggest that physical mixing of the cover and tailing during construction, rather than advection, accounted for acidification of the basal soil cover. Based on evidence from our investigations and an understanding of soil developmental processes in arid-regions, we conclude that upward migration of constituents from wastes is not a time-transgressive process that will result in cover degradation in arid and semi-arid regions where permanent or seasonal water tables occur well below the soil surface. Finally, we consider the changes in chemistry at the soil cover above the waste interface to be biologically insignificant.