The high corrosion resistance of copper is a key feature in the design of copper-lined canisters that will be utilized to protect people and the environment from dangers of spent nuclear fuel far into the future. Our present study sheds light on the effects that sulfide ions in otherwise relatively benign anoxic groundwater may have on the copper of the container material. Using soft X-ray spectroscopy, we have studied the chemistry of the transformation of single-phase copper oxide cover layers (cuprite, tenorite, paratacamite) as well as single-phase oxide powders (paratacamite and malachite) when exposed to aqueous sulfide solutions. While X-ray diffraction shows that the main bulk of the oxides are nearly unaffected, Cu L-edge absorption spectroscopy shows that a cover layer of about 100 nm thickness on the metal substrate is transformed from Cu(II)-to Cu(I)-species. By contrast, paratacamite and malachite powders exposed to the same kind of aqueous sulfide solutions show much less transformation to Cu(I)-species. We conclude that the main mechanism for reduction of Cu(II) on copper is the comproportionation reaction between divalent copper ions from the covering oxide and the underlying metallic copper atoms to form monovalent copper ions. By contrast, the absence of metallic copper inhibits this mechanism in the powders. Sweden and Finland have selected copper as the outer material for containers for disposal of spent nuclear fuel from nuclear reactors. Copper is also being considered in Canada as a possible container material. This choice is based on thermodynamic stability of this metal in the anoxic saline groundwaters that are anticipated to prevail in the waste repositories of these countries. The only potentially available oxidant at the depth of the repository will be aqueous sulfide; the sulfide source being dissolution of minerals or microbial activity. The sulfide levels are expected to be relatively low. At the Swedish repository site at Forsmark the measured sulfide concentrations have been measured to be generally below 1.3 · 10 −5 M.
1Even though the undisturbed deep groundwaters are oxygen-free, oxygen will of course be present at the repository level during the initial construction phase. After sealing the repository, this oxygen will be consumed by reactions with minerals, by microbial activity and by corroding the copper containers. At the time when dissolved sulfide will reach the containers, they will be covered by corrosion products from the initial construction phase. These corrosion products may include cuprite (Cu 2 O), tenorite (CuO), and, due to the high chloride content in the deep groundwaters at the Swedish and Finnish repository sites in the fennoscandian shield, paratacamite (a polymorph of copper hydroxychloride with the chemical formula Cu 2 Cl(OH) 3 ). In the presence of increased carbonate concentrations, malachite (a copper carbonate hydroxide with the chemical formula Cu 2 CO 3 (OH) 2 ) may also form.X-ray spectroscopy 2-4 and X-ray photoelectron spectroscopy [5][6][7][...