ION EXCHANGE EQUILIBRIUM FOR SOME UNI-UNIVALENT AND UNI-DIVALENT REACTION SYSTEMS USING STRONGLY BASIC ANION EXCHANGE RESIN DUOLITE A-102 D

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, 107114. ISSN 10113924 Printed in Ethiopia 2008 Chemical Society of Ethiopia ION EXCHANGE EQUILIBRIUM FOR SOME UNIUNIVALENT AND UNIDIVALENT REACTION SYSTEMS USING STRONGLY BASIC ANION EXCHANGE RESIN DUOLITE A102 D R.S. Lokhande, P.U. Singare * and A.R. Kolte Department of Chemistry, University of Mumbai, Vidyanagri, Santacruz, Mumbai400 098, India (Received December 8, 2006; revised July 22, 2007) ABSTRACT. The study on thermodynamics of ion exchange equilibrium for uniunivalent Cl /I, Cl /Br, and unidivalent Cl /SO 4, Cl /C 2O 4 reaction systems was carried out using ion exchange resin Duolite A102 D. The equilibrium constant K was calculated by taking into account the activity coefficient of ions both in solution as well as in the resin phase. The K values calculated for uniunivalent and unidivalent anion exchange reaction systems was observed to increase with rise in temperature, indicating the endothermic exchange reactions having enthalpy values of 13.7, 38.0, 23.9, 22.9 kj/mol, respectively. KEY WORDS: Duolite A102 D ion exchange resin, Equilibrium constant, Endothermic ion exchange reaction, Enthalpy, Thermodynamic study INTRODUCTION For proper selection of ion exchange resin in a particular technical application, it is essential to have adequate knowledge regarding their physical and chemical properties, which forms the complementary part of resin characterization study. Extensive work was done by previous researchers to study the properties of the ion exchange resins [13], to generate thermodynamic data [47] related to various uniunivalent and heterovalent ion exchange systems. Recently theories explaining ion exchange equilibrium [8] between the resin phase and solution was developed. A number of researchers carried out equilibrium studies [931], extending over a wide range of composition of solution and resin phase. Attempts were also made to study the temperature effect on cation exchange systems for computing the thermodynamic equilibrium constants [923]. However very little work was carried out to study the equilibrium of anion exchange systems [12, 2429]. Therefore in the present investigation attempts were made to study the temperature effect on uniunivalent and unidivalent anion exchange reaction equilibrium, the result of which will be of considerable use in qualitatively assessing an ion exchange resin for its utility in a stipulated exchange process. EXPERIMENTAL The ion exchange resin Duolite A102 D as supplied by the manufacturer (Auchtel Products Ltd., Mumbai, India) was a strongly basic quaternary ammonium N(CH 3 ) + anion exchanger in chloride form containing 8 % styrene divinyl benzene of 2050 mesh size. For present investigation, the resin grains of 3040 mesh size were used. The soluble impurities of the resin were removed by repeated Soxhlet extraction using water and occasionally with distilled methanol to remove nonpolymerized organic impurities. In order to ensure complete conversion of resins in chloride form, the resins were conditioned with 10 % potassium chloride solution in a conditioning column. The resins were washed with distilled deionised water until the washings *Corresponding author. Email: pravinsingare@vsnl.net

108 R.S. Lokhande et al. were free from chloride ions. The resins in chloride form were air dried over P 2 O 5 and used for further studies. (a) Study of uniunivalent ion exchange equilibrium Ion exchange resins (0.500 g) in chloride form were equilibrated with iodide ion solution of different concentrations at a constant temperature of 30.0 0 C for 4 h. From the results of kinetics study reported earlier [32, 33]; it was observed that this duration was adequate to attain the ion exchange equilibrium. After 4 h, the iodide ion solutions in equilibrium with ion exchange resins in chloride form were analyzed for their chloride and iodide ion concentrations by potentiometric titration with standard 0.1 M silver nitrate solution. From the results the equilibrium constant K for the reaction RCl + I (aq) RI + Cl (aq) (1) was determined at 30.0 0 C. The equilibrium constants K for the above Cl /I system was determined for different temperatures in the range of 30.0 0 C to 45.0 0 C. Similar studies were carried out for Cl /Br system in the same temperature range, to study the equilibrium constant for the reaction RCl + Br (aq) RBr + Cl (aq) (2) (b) Study of unidivalent ion exchange equilibrium Ion exchange resins (0.500 g) in chloride form were equilibrated with sulfate ion solution of known initial concentration at a constant temperature of 30.0 0 C for 4 h, which was sufficient time to attain the ion exchange equilibrium. After 4 h the concentration of chloride ions exchanged in to the solution was estimated by potentiometric titration against standard 0.1 M silver nitrate solution using a semimicro burette having an accuracy of 0.02 ml. Since it is known that one mole of sulfate ions replaces two moles of chloride ions and from the knowledge of chloride ions in the solution at equilibrium, the amount of sulfate ions exchanged on the resin was calculated. After knowing the initial concentration of sulfate ions in the solution and the amount of sulfate ions exchanged on the resin, the equilibrium concentration of sulfate ions in the solution was calculated. Further from the known resin capacity and the amount of sulfate ions replacing the chloride ions on the resin, the amount of chloride ions remaining on the resin was calculated. Having thus known the equilibrium concentrations of chloride and sulfate ions in the solution and in the resin phase, the apparent equilibrium constant K app. for the reaction 2RCl + SO 4 2 (aq) R 2 SO 4 + 2Cl (aq) (3) was calculated. The same experiment was repeated for different initial concentrations of sulfate ions in the temperature range of 30.0 0 C to 45.0 0 C to calculate the apparent equilibrium constant K app for the above Cl 2 /SO 4 exchange. Similar experiment was performed for Cl /C 2 O 2 4 system by equilibrating ion exchange resins in chloride form with oxalate ion solution of different concentrations, and apparent equilibrium constants K app. for the reaction 2RCl + C 2 O 4 2 (aq) R 2 C 2 O 4 + 2Cl (aq) (4) was calculated in the same temperature range.

Ion exchange equilibrium for some uniunivalent and unidivalent reaction systems 109 The iodide, bromide, sulfate and oxalate ion solutions used in the entire experimental work were prepared by dissolving their corresponding potassium salts (Analytical grade) in distilled deionised water. RESULTS AND DISCUSSION The equilibrium constants for the reactions (1 and 2) can be given by the expression C RX.C Cl K = (5) (A C RX ).C X where A is the ion exchange capacity of the resin, x represents I or Br ions. For different concentrations of x ions in solution at a given temperature, K values were calculated from which average value of K for that set of experiment was calculated (Tables 1, 2). Similar values of K were calculated for both Cl /I and Cl /Br systems for different temperatures (Tables 3, 4). Table 1. Equilibrium constant for the ion exchange reaction: RCl + I aq RI + Cl aq in Duolite A102 D (Amount of the ion exchange resin in chloride form = 0.500 g, ion exchange capacity = 1.2 meq./0.5 g, volume of iodide ion solution = 50.0 ml, temperature = 30.0 0 C). System Initial conc. of iodide ion (M) Final conc. of iodide ions (M) C I Change in iodide ion conc. Conc. of Cl ions exchanged (M) C Cl Amount of iodide ions exchanged on the resin meq./0.5 g C RI Equilibrium constant K 1 0.02 0.0030 0.0170 0.0169 0.850 13.7 2 0.03 0.0094 0.0206 0.0206 1.030 13.3 3 0.04 0.0180 0.0220 0.0219 1.100 13.4 4 0.05 0.0274 0.0226 0.0225 1.130 13.3 5 0.06 0.0371 0.0229 0.0231 1.145 13.0 6 0.08 0.0567 0.0233 0.0235 1.165 13.8 Average equilibrium constant (K) = 13.4. Table 2. Equilibrium constant for the ion exchange reaction: RCl + Br (aq) RBr + Cl (aq) in Duolite A102 D (Amount of the ion exchange resin in chloride form = 0.500 g, ion exchange capacity = 1.2 meq./0.5 g, volume of bromide ion solution= 50.0 ml, temperature = 30.0 0 C). System Initial conc. of Br ion solution (M) Final conc. of Br ion solution (M) C Br Change in bromide ion conc. (M) Conc. of chloride ion exchanged (M) C Cl Amount of Br ions exchanged on the resin meq./0.500g C RBr Equilibrium constant K 1 0.02 0.0060 0.0140 0.0139 0.700 3.2 2 0.03 0.0130 0.0170 0.0171 0.850 3.2 3 0.04 0.0211 0.0189 0.0184 0.945 3.2 4 0.05 0.0301 0.0199 0.0200 0.995 3.2 5 0.06 0.0393 0.0207 0.0206 1.035 3.3 6 0.08 0.0585 0.0215 0.0217 1.075 3.2 Average equilibrium constant (K) = 3.2.

110 R.S. Lokhande et al. Table 3. Effect of temperature on equilibrium constant for uniunivalent ion exchange reaction: RCl + I (aq) RI + Cl (aq) in Duolite A102 D (Amount of ion exchange resin in chloride form = 0.500 g, volume of I ion solution = 50 ml). Temperature O C 30.0 35.0 40.0 45.0 Equilibrium constant (K) 13.4 14.5 15.6 17.1 Slope of graph log K vs. temperature (Kelvin) 1/T x 10 3 = 718.01, enthalpy change of the ion exchange reaction = 13.7 kj/mol. Table 4. Effect of temperature on equilibrium constant for uniunivalent ion exchange reaction: RCl + Br (aq) RBr + Cl (aq) in Duolite A102 D (Amount of ion exchange resin in chloride form = 0.500 g, volume of Br ion solution = 50 ml). Temperature O C 30.0 35.0 40.0 45.0 Equilibrium constant (K) 3.2 4.0 5.1 6.3 Slope of graph log K vs. temperature (Kelvin) 1/T x 10 3 = 1988.15, Enthalpy change of the ion exchange reaction = 38.0 kj/mol. The equilibrium constants for the unidivalent ion exchange reactions (3, 4) would be given by the expression (α R2y ) (α X ) 2 aq K = (6) (α RX ) 2 (α y ) aq where α is the activities of various species, x = Cl ion and y = SO 4 or C 2 O 4 ions. In the above expression, the activities of x and y in the aqueous solution are obtained from their respective concentrations and activity coefficients derived from Debye Huckel limiting law. As regards the activities of the two ions in the resin are concerned, the situation is different. Ordinarily the activity should be obtained as a product of concentration and the activity coefficient. In lieu of the concentration of the ions in the resin, their respective amounts in milliequivalents can be used, as shown by the satisfactory results obtained for the equilibrium constant of uniunivalent exchange reactions. On this basis, the equilibrium constant would be given by the expression (C R2y.γ R2y ) (C x.γ x ) 2 K = (7) (C Rx.γ Rx ) 2 (C y.γ y ) where γ is the activity coefficient of ions in the solution at equilibrium. In this expression, the concentrations of ions in the resin phase in terms of their amounts in milliequivalents are known while their individual activity coefficients i.e. γ R2y and γ Rx are not known. Indeed, it appears that there is no way for evaluating them individually. In case of uniunivalent exchange reactions, they could be ignored because they where likely to be of the same magnitude (being for univalent ions) and in the expression for equilibrium their ratio is nearly one. In the present case for unidivalent exchange however, the activity coefficients can not be ignored because in the expression for the equilibrium constant they appear as γ R2y /(γ Rx ) 2. Since γ R2y and γ Rx are likely to vary with the concentration of the ions y and x in the resin, the above mentioned quantity is also likely to vary with the concentrations of the ions in the resin. This is confirmed from the fact that the equilibrium constant as calculated from the expression (C R2Y ) (C X ) 2 (γ X ) 2 K app = (8) (C RX ) 2 (C Y ) (γ Y ) varies with the concentration of the ions in the resin (Tables 5, 6).

Ion exchange equilibrium for some uniunivalent and unidivalent reaction systems 111 Table 5. Equilibrium constants for the unidivalent ion exchange reaction: 2RCl + SO 4 (aq) R 2SO 4 + 2Cl (aq) in Duolite A102 D (Amount of the ion exchange resin in chloride form = 0.500 g, volume of the sulfate ion solution = 100 ml, temperature = 30.0 0 C). Initial conc. of SO 4 ions in solution (M) Equilibrium conc. in solution (M) C Cl C SO4 Amount of the ions on the resin meq./0.500 g C RCl C R2SO4 Apparent equilibrium constant K app K std (γ R2SO4) = K app (γ RCl) 2 0.007 0.0074 0.0024 0.46 0.370 30.1 1.14 0.008 0.0077 0.0031 0.43 0.385 29.3 1.18 0.009 0.0080 0.0041 0.40 0.400 27.9 1.26 0.010 0.0082 0.0051 0.38 0.410 26.1 1.31 0.015 0.0088 0.0112 0.32 0.440 18.3 1.83 0.020 0.0090 0.0156 0.30 0.450 14.9 2.38 0.030 0.0093 0.0264 0.27 0.462 10.3 3.49 0.050 0.0098 0.0457 0.22 0.490 8.7 3.93 Equilibrium constant in standard state (K std) = 32.7. Table 6. Equilibrium constants for the unidivalent ion exchange reaction: 2RCl + C 2O 4 (aq) R 2C 2O 4 +2Cl (aq) in Duolite A102 D (Amount of the ion exchange resin in chloride form = 0.500 g, volume of the oxalate ion solution = 100 ml, temperature = 30.0 0 C). Initial conc. of C 2O 4 ions in solution (M) Equilibrium conc. in solution (M) C Cl C C2O4 Amount of the ions on the resin meq./0.500 g C RCl C R2C2O4 Apparent equilibrium constant K app K std (γ R2C2O4) = K app (γ RCl) 2 0.007 0.0074 0.0026 0.46 0.370 27.6 1.11 0.008 0.0077 0.0034 0.43 0.385 26.5 1.15 0.009 0.0079 0.0042 0.41 0.395 25.0 1.23 0.010 0.0081 0.0051 0.39 0.405 23.9 1.29 0.015 0.0087 0.0109 0.33 0.435 17.2 1.80 0.020 0.0090 0.0172 0.30 0.450 13.2 2.33 0.030 0.0092 0.0266 0.28 0.460 9.3 3.45 0.050 0.0098 0.0466 0.22 0.490 8.5 3.90 Equilibrium constant in standard state (K std) = 31.4. In absence of any method to determine the activity coefficients of the ions in the resin individually the best that can be done is to attempt to determine the quantity γ R2y /(γ Rx ) 2 and to determine the true equilibrium constant. In ionic equilibrium it is conventional to regard zero concentration as the standard state when the mean activity coefficient becomes unity. In the present situation however, such standard state can not be chosen for the ions in the resin because the ion exchange resin will always contains its capacity full of ions which can not be decreased. No doubt the ions in the resin might all be univalent or all be divalent or partly univalent and partly divalent. In any case the resin contain ions to its full capacity. However, when the resin is entirely in the chloride form (univalent), its ionic strength will be much different from that when the resin is entirely in sulfate or oxalate (divalent) form. Therefore it is expected that the quantity γ R2y /(γ Rx ) 2 will vary according to what extent the resin is in the univalent and divalent ionic form. In view of the above, it is found best to choose the ion exchange resin completely in univalent ionic form as the standard state and refer the resin at any other composition of the

112 R.S. Lokhande et al. uni/divalent ions to this standard state. Therefore the apparent equilibrium constants calculated by the Eq. 8 have been plotted versus the equilibrium concentrations of the divalent ions in the solution (Figures 1, 2). Lower the equilibrium concentration of the divalent ion lower would be its concentration in the resin and in the limiting case of zero equilibrium concentration of the divalent ion in the solution, the resin would be in its standard state. Therefore on extrapolating the above curve to zero equilibrium concentration of divalent ion in the solution, one obtains the equilibrium constant in the standard state, K std. Having thus obtained the equilibrium constant in the standard state one can obtain the activity coefficient ratio of ions γ R2y /(γ Rx ) 2 at any finite equilibrium concentration of divalent ion in the solution as the ratio of K std /K app The results of such calculations are presented in the Tables 5, 6. 35 Apparent equilibrium constant (Kapp) 30 25 20 15 10 5 0 0 0.01 0.02 0.03 0.04 0.05 Equilibrium concentration of sulfate ions in solution (M) Figure 1. Variation of apparent equilibrium constant (K app ) with equilibrium concentration of sulfate ions solution for unidivalent ion exchange reaction: 2RCl + SO 4 (aq) R 2 SO 4 + 2Cl (aq) using Duolite A102 D resins Amount of the ion exchange resin in chloride form= 0.500 g, volume of the sulfate ion solution = 100 ml, temperature = 30.0 0 C It is significant that when the log K app is plotted against 1/T, different slopes and hence different values of enthalpy of ion exchange reaction are obtained. However, a satisfactory linear graph with definite slope was obtained when log K std was plotted against 1/T giving a definite value of enthalpy of ion exchange reactions. This is an ample justification for the choice of standard state for equilibrium constant. Bonner and Pruett [16] studied the temperature effect on uniunivalent exchanges involving some divalent ions. In all divalent exchanges, the equilibrium constant decreases with rise in temperature resulting in exothermic reactions. However in the present investigation, for both the uniunivalent and unidivalent exchange reactions the value of equilibrium constant increases with rise in temperature giving positive enthalpy value (Tables 3, 4, 7, 8), indicating the endothermic ion exchange reactions. The low enthalpy and higher K values for Cl /I exchange as compared to that for Cl /Br exchange, indicate that the resins in chloride form are having more affinity for larger ionic size iodide ions

Ion exchange equilibrium for some uniunivalent and unidivalent reaction systems 113 in solution as compared to that for bromide ions also in the solution. Similarly, the K values for unibivalent exchange reactions are higher than that for uniunivalent exchange reactions, indicating that the affinity of resins in chloride form for the ions in solution increases with increase in ionic charge of the exchangeable ions in the solution. 35 Apparent equilibrium constant (Kapp) 30 25 20 15 10 5 0 0 0.01 0.02 0.03 0.04 0.05 Equilibrium concentration of oxalate ions in solution (M) Figure 2. Variation of apparent equilibrium constant (K app ) with equilibrium concentration of oxalate ions solution for unidivalent ion exchange reaction: 2RCl + C 2 O 4 2 (aq.) R 2 C 2 O 4 + 2Cl (aq) using Duolite A102 D resins Amount of the ion exchange resin in chloride form = 0.500 g, volume of the oxalate ion solution = 100 ml, temperature = 30.0 0 C. Table 7. Effect of temperature on equilibrium constant in standard state (K std.) for uni divalent ion exchange reaction 2RCl + SO 4 (aq) R 2SO 4 + 2Cl (aq) in Duolite A102 D (Amount of ion exchange resin in chloride form = 0.500 g, volume of SO 4 ion solution = 100 ml). Temperature O C 30.0 35.0 40.0 45.0 K std. 32.7 44.7 51.9 60.0 Slope of graph log K std vs. temperature (Kelvin) 1/T x10 3 = 1249.0. Enthalpy change of the ion exchange reaction = 23.9 kj/mol. Table 8. Effect of temperature on equilibrium constant in standard state (K std) for unidivalent ion exchange reaction in Duolite A102 D 2RCl + C 2O 4 (aq) R 2C 2O 4 +2Cl (aq.) (Amount of ion exchange resin in chloride form = 0.500 g, volume of oxalate ion solution = 100 ml). Temperature O C 30.0 35.0 40.0 45.0 K std. 31.4 42.4 48.9 56.2 Slope of graph log K std vs. temperature (Kelvin) 1/T x 10 3 = 1198.1. Enthalpy change of the ion exchange reaction = 22.9 kj/mol.

114 R.S. Lokhande et al. In the present study, a semimicro burette having an accuracy of 0.02 ml was used in the titrations against silver nitrate solution. The titration readings were accurate to ± 0.02 ml. Considering the magnitude of the titre values, the average equilibrium constants reported in the experiment are accurate to ± 3 %. REFERENCES 1. Andreev, N.N; Kuznetsov, Yu.I. Russ. J. Phys. Chem. 1990, 64, 1537. 2. Bhargava, A.; Janardanan, C. Indian J. Chem. 1997, 36A, 624. 3. Muraviev, D.; Gonzalo, A.; Valiente, M. Anal. Chem. 1995, 67, 3028. 4. Boyd, G.E.; Vaslow, F.; Lindenbaum, S. J. Phys. Chem. 1967, 71, 2214. 5. Duncan, J.F. Aus. J. Chem. Soc. 1955, 8, 1. 6. Boyd, G.E.; Vaslow, F.; Lindenbaum, S. J. Phys. Chem. 1964, 68, 590. 7. Schwarz, A.; Boyd, G.E. J. Phys. Chem. 1965, 69, 4268. 8. Gamayunov, N.I. Russ. J. Phys. Chem. 1990, 64, 1787. 9. Boyd, G.E.; Myers, G.E. J. Phys. Chem. 1956, 60, 521. 10. Bonner, O.D. J. Phys. Chem. 1955, 59, 719. 11. Bonner, O.D. J. Phys. Chem. 1954, 58, 318. 12. Lindenbaum, S.; Jumper, C.F.; Boyd, G.E. J. Phys. Chem. 1959, 63, 1924. 13. Kraus, K.A.; Raridon, R.J. J. Phys. Chem. 1959, 63, 1901. 14. Bonner, O.D.; Payne, W.H. J. Phys. Chem. 1954, 58, 183. 15. Argersinger, W.J.; Davidson, A.W. J. Phys. Chem. 1952, 56, 92. 16. Bonner, O.D.; Pruett, R.R. J. Phys. Chem. 1959, 63, 1420. 17. Bonner, O.D.; Livingston, F.L. J. Phys. Chem. 1956, 60, 530. 18. Bonner, O.D.; Smith, L.L. J. Phys. Chem. 1957, 61, 326. 19. Bonner, O.D.; Jumper, C.F.; Rogers, O.C. J. Phys. Chem. 1958, 62, 250. 20. Bonner, O.D.; Smith, L.L. J. Phys. Chem. 1957, 61, 1614. 21. Kielland, J. J. Soc. Chem. Ind. 1935, 54, 232T. 22. Vanselow, A.P. J. Am. Chem. Soc. 1932, 54, 1307. 23. Gaines (Jr.) G.L.; Thomas, H.C. J. Chem. Phys. 1953, 21, 714. 24. Kraus, K.A.; Raridon, R.J.; Holcomb, D.L.; Chromatogr. J. 1960, 3, 178. 25. Lokhande, R.S.; Singare, P.U. Asian J. Chem. 1998, 10, 898. 26. Lokhande, R.S.; Singare, P.U. Chem. Environ. Res. 1998, 7, 283. 27. Lokhande, R.S.; Singare, P.U. Orient. J. Chem. 1998, 14, 247. 28. Lokhande, R.S.; Singare, P.U. Indian J. Chem. 1999, 38A, 87. 29. Lokhande, R.S.; Singare, P.U. Asian J. Chem. 2001, 13, 43. 30. Bonner, O.D.; Dickel, G.; Brummer, H. Z. Physik. Chem. 1960, 25, 81. 31. Starodinet, G.L.; Soldatov, V.S.; Krylova, A.A. Russ. J. Phys. Chem. 1967, 41, 194. 32. Lokhande, R.S.; Singare, P.U. Asian J. Chem. 2003, 15, 33. 33. Lokhande, R.S.; Singare, P.U. Asian J. Chem. 1998, 10, 890.