Uranium dissolution from rock samples containing uranophane or carnotite was tested in acid mineral salts solutions in the presence and absence of Fe-and Soxidizing bacteria (Thiobacillus ferrooxidans) and with FeSO 4 or S 0 as the substrate.The addition of FeSO 4 enhanced the solubilization of uranium from uranophane. S 0 -amendment was also effective, because uranium solubilization was enhanced at low pH resulting from the bacterial oxidation of S 0 . Uranium was readily dissolved from carnotite.However, the carnotite-containing rock sample was predominantly composed of calcite that excessively consumed acid, increasing the pH and thereby reducing the concentration of uranium dissolved in leach solution. § Present address: