Electrochemistry MAE-295 Dr. Marc Madou, UCI, Winter 2012 Class VII Pourbaix Diagrams Table of content Marcel Pourbaix Pourbaix Diagrams Marcel Pourbaix Marcel Pourbaix provided the brilliant means to utilize thermodynamics more effectively in corrosion science and electrochemistry in general. This development resulted in four important books that interpret his work: Thermodynamics of Dilute Aqueous Solutions, Atlas of Electrochemical Equilibria in Aqueous Solutions (solid-aqueous equilibria); Lectures on Electrochemical Corrosion (a teaching text); and, in his last years, Atlas of Chemical and Electrochemical Equilibria in the Presence of a Gaseous Phase (solid-gaseous equilibria). His outstanding work in thermodynamics provided one of the main underpinnings of electrochemistry, especially in corrosion science. Marcel Pourbaix b. 1904, Myshega, Russia d. September 28, 1998, Uccle (Brussels), Belgium Marcel Pourbaix Marcel Pourbaix (1904-1998) Marcel Pourbaix was born in Russia, where his father, a Belgian engineer, was working at the time. The significance of Marcel Pourbaix’s great achievement was pointed out by Ulick R. Evans, widely recognized as the “father of corrosion science,” in his foreword to Pourbaix’s Thermodynamics of Dilute Aqueous Solutions: “During the last decade (the 1940s) Dr. Marcel Pourbaix of Brussels has developed a graphical method, based on generalized thermodynamical equations, for the solution of many different kinds of scientific problems, involving numerous types of heterogeneous or homogeneous reactions and equilibria... Some of these problems have long been treated from the aspect of thermodynamics... The application of thermodynamics to typical corrosion reactions is a much newer development.” For Mr. Zhang Zhongcheng As a memory of his stay at Cebelcor in 1984/1985. With all best wishes from Marcel Pourbaix April 26, 1985 Prof Pourbaix, his wife, and Zhang Zhongcheng, in 1985 Prof Pourbaix with his colleagues at Cebelcor in 1984 The E-pH diagram of copper-water system Pourbaix Diagrams Through the use of thermodynamic theory (the Nernst equation), so-called Pourbaix diagrams can be constructed. These diagrams show the thermodynamic stability of species as a function of potential and pH. Although many basic assumptions must be considered in their derivation, such diagrams can provide valuable information in the study of corrosion phenomena. The diagram on the right represents a simplified version of the Pourbaix diagram for the ironwater system at ambient temperature. For the diagram shown, only anhydrous oxide species were considered and not all of the possible thermodynamic species are shown. How do we construct this diagram for water? Pourbaix Diagrams Use Nernst Equation: Oxidation Faster Reduction Slower Potential Oxidation Slower Reduction E = E0 - RT concentration of products ln nF concentration of reac tan ts Faster pH Rates equal Pourbaix Diagrams Besides the use of the Nernst equation the following relations are used to construct the PourBaix diagrams 0 i ln K eq (= Q*) = RT lnK E = nF eq = RT EnF RT RT iln a i nF i 0 i or also log K = i i i i 1,363 = ln a i i (a i are products and a 'i are reactants). To derive the Nernst equation from this equation i i i nF 0 i 0 : i 0 i 0.059 logK 0.059 0.059 = ilog a i i ilog a i or also with E n n i n 23,060 n i And finally E E = E0 - 25 o = Eo i RT nE 23,060 i iln a i and log K = = ilog a i nF i 2.303 1.987 298.1 2.303 1.987 298.1 i i nE ilog a i 0.059 i To derive the Nernst equation in log terms E 25o : 0.059 ilog a i this is the same expression as n i RT concentration of products ln nF concentration of reac tan ts For electrochemical reactions n 0 and for chemical reactions n = 0. 1 Coulomb - Volt = 1 Joule = 0.239 calorie 1 Faraday - Volt = 96 500 Joule = 23.060 calories i 0 i 0.059 log K = i o n n 23,060 : Pourbaix Diagrams Aqueous solutions cannot be at a lower potential than that required to reduce water : 2H + + 2e - = H 2 (E 0 0) p RT H2 E = E0 l og + ]2 nF [ H RT reduced species (also E = E 0 l og nF (oxidized species) (H + ) m RT RT E = E0 l og p H 2 + log [ H +] nF F ( pH = - log [H + ] and rH 2 l og p H 2 ) 2H2O = O2 + 4H+ + 4eEquilibrium potential falls as 2.0 pH increases 1.6 1.2 or RT pH = E = E 0 - 0.059 pH F at 1 atm hydrogen (hydrogen bubbles form) ! Aqueous solutions cannot be at a higher potential than that required to oxidize water : E = E0 + 0.4 H2O is stable 0.0 2H+ + 2e- = H2 Equilibrium potential falls as pH increases -0.4 -0.8 + 4e 2H 2O (E 1.229) [H + ]4 p RT O2 + l og 2 4F [ H 2 O ] - Potential 0.8 E = E0 - O 2 + 4H O2 is stable 0 taking water activity as unity E = 1.229 + 0.0148 l og p O 2 - 0.059 pH H2 is stable -1.2 -1.6 0 7 14 Pourbaix Diagrams For the general reaction : We will consider Cu in an aqueous aA + bB + cH 2O + mH + + ne = 0 we can write that logK - mpH = solution as the next exercise: five different reactions are involved. nE (A) a log 0.059 (B) b proton number m and electron number = n 0.059 0.059 (A) a (A) a mpH + log with n = 0 logK - mpH = log b n n (B) (B) b a 1 (A) or pH = logK + log m (B) b or E E 0 1. Cu 2+ 2H 2O CuO 2 H - + 3H + 0 i log K = pH = i i = 1, 363 15, 912 - 2 56, 560 + 60, 960 26.6 1, 363 Cu 2+ 1 (Cu 2+ ) 1 (26.6 log ) logK + log m (CuO 2 H - ) 3 CuO 2 H - Cu 2+ Every time the ratio CuO 2 H - increases by a factor of 10, the pH decreases with At equal concentrations pH = 1 (26.6) 8.9 3 2. CuO 2 H - H + CuO 22 i log K = i 1, 363 0 i CuO H CuO - 13.2 and pH = -(logK + log 2 22 The pH changes with one unit per decade change in of ratio of reaction partners. At equal concentrations: pH = 13.2 7 1 of a pH unit. 3 Pourbaix Diagrams 3. Cu 2+ Cu + + e = 0 Cu 2+ 0.059 E = E0 log . The potential increases with 0.059 V everytime the ratio of 1 Cu + Cu Cu 2+ + increases with a factor of 10. E is independent of the pH. 4. CuO 2 H - + 3H + e Cu + + 2H 2O or also CuO 2 H - - Cu + - 2H 2O + 3H + e = 0 CuO 2 H 0.059 0.059 E = E0 mpH + log . E will decrease with 0.177 V everytime the pH increases with 1 unit. n n Cu + At equal concentrations : E = E 0 0.059 mpH = 1.74 - 0.177pH. At constant pH E increases with 0.059 V everytime n with a factor of 10. 5. CuO 2 2- - Cu + CuO 2 20.059 0.059 - 2H 2O + 4H e = 0. E = E 0 4pH + log 1 1 Cu + + E decreases 0.236 V for every pH unit increase and at equal concentration : E = E 0 0.236 pH CuO increases with a factor of 10 (at constant pH), E increases with 0.059V. Cu 2- Every time 2 + The bolder lines in the Pourbaix diagram represent pH and E values for equal concentrations. The interesections determine four domains where Cu 2+ + , CuO 2 H - , CuO 22 and Cu are dominant. The finer lines are for different ratios of reactants/products [0.1 - 1 - 9; 91 - 99 - 99.9]. CuO H increases Cu - 2 + Pourbaix Diagrams Pourbaix Diagrams The diagram shown here shows how the potentials for reduction and oxidation of water vary with pH for natural waters. These are the inner two lines that slope downward from low pH to high pH. Note that the pH scale only runs from 2-10 (we are talking here about natural waters). For both oxidation and reduction of water, an additional line is shown that lies 0.6V above (for oxidation of water) or below (for reduction) the theoretical E. This pair of lines represents the potentials including an approximation for the overvoltage. Lastly, there is a pair of vertical lines at pH=4 and 9. These are reflective of the fact that most natural waters have a pH somewhere between these limits. . 2008 MAE 217-Professor Marc J. Madou Pourbaix Diagrams A Pourbaix diagram is an attempt to overlay the redox and acid-base chemistry of an element onto the water stability diagram. The data that are required are redox potentials and equilibrium constants (e.g. solubility products). On the right is the Pourbaix diagram for iron. Below that is the same diagram showing only those species stable between the water limits. 2008 MAE 217-Professor Marc J. Madou Pourbaix Diagrams Equilibrium Reactions of iron in Water 1. 2 e- + 2H+ = H2 14. FeOH+ + H2O = Fe(OH)2(sln) + H+ 2. 4 e- + O2 + 4H+ = 2H2O 15. Fe(OH)2(sln) + H2O = Fe(OH)3- + H+ 3. 2 e- + Fe(OH)2 + 2H+ = Fe + 2H2O 16. Fe3+ + H2O = FeOH2+ + H+ 4. 2 e- + Fe2+ = Fe 5. 2 e- + Fe(OH)3- + 3H+ = Fe + 3H2O 17. FeOH2+ + H2O = Fe(OH)2+ + H+ 6. e- + Fe(OH)3 + H+ = Fe(OH)2 + H2O 18. Fe(OH)2+ + H2O = Fe(OH)3(sln) + H+ 7. e- + Fe(OH)3 + 3H+ = Fe2+ + 3H2O 19. FeOH2+ + H+ = Fe2+ + H2O 8. Fe(OH)3- + H+ = Fe(OH)2 + H2O 20. e- + Fe(OH)2+ + 2H+ = Fe2+ + 2H2O 9. e- + Fe(OH)3 = Fe(OH)310. Fe3+ + 3H2O = Fe(OH)3 + 3H+ 21. 11. Fe2+ + 2H2O = Fe(OH)2 + 2H+ 22. e- + Fe(OH)3(sln) + 2H+ = FeOH+ + 2H2O 12. e- + Fe3+ = Fe2+ 23. e- + Fe(OH)3(sln) + 3H+ = Fe2+ + 3H2O 13. Fe2+ + H2O = FeOH+ + H+ MAE 217-Professor Marc J. Madou e- + Fe(OH)3(sln) + H+ = Fe(OH)2(sln) + H2O 2008 Pourbaix Diagrams Some limitations of Pourbaix diagrams include: No information on corrosion kinetics is provided by these thermodynamically derived diagrams. The diagrams are derived for specific temperature and pressure conditions. The diagrams are derived for selected concentrations of ionic species (10-6 M for the above diagram). Most diagrams consider pure substances only - for example the above diagram applies to pure water and pure iron only. Additional computations must be made if other species are involved. In areas where a Pourbaix diagram shows oxides to be thermodynamically stable, these oxides are not necessarily of a protective (passivating) nature. 2008 MAE 217-Professor Marc J. Madou Pourbaix Diagrams MAE 217-Professor Marc J. Madou 2008