Supporting Information Environmental Science & Technology Copper redox transformation and complexation by reduced and oxidized soil humic acid: 2. Potentiometric titrations and dialysis cell experiments Felix Maurer,1 Iso Christl,1* Beate Fulda,1 Andreas Voegelin,2 and Ruben Kretzschmar1 1 Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, CHN, CH-8092 Zurich, Switzerland. 2 Eawag, Swiss Federal Institute of Aquatic Science and Technology, CH-8600 Dübendorf, Switzerland. * Corresponding author, e-mail address: [email protected] Number of pages: 11 Number of figures: 6 Number of tables: 3 Contents S1: Cu(I) sensitivity of the copper ion selective electrode (Fig. S1) .............................. S2 S2: Total Cu(I) determination by complexation with bathocuproine (Fig. S2 & S3, and Tab. S1).................................................................................................................. S3 S3: Calculation of inorganic copper speciation (Tab. S2 & S3)..................................... S6 S4: Cu(I) formation during titration experiments plotted as fraction of total added copper (Fig. S4).................................................................................................................. S8 S5: Conditional stability constants for Cu-HA binding (Fig. S5) .................................... S9 S6: Speciation for solid phase samples (Fig. S6) ....................................................... S10 S1 60 40 20 Cu-ISE potential (mV) 80 100 S1: Cu(I) sensitivity of the copper ion selective electrode 0 Cu(II) only (1, 3, 10, 30, 100 μM) In presence of 30 μM Cu(I) 10.0 9.5 9.0 8.5 2+ −log{Cu } 8.0 7.5 7.0 Figure S1. Measured Cu-ISE electrode potential as a function of Cu2+ activity in solution for calibration experiments in the presence and absence of Cu+. Titration experiments were performed in 200 µM histamine (Fluka) for stabilization of both Cu+ and Cu2+, 0.1 M NaCl, and 20 mM phosphate buffer to adjust the pH value to 7.0. For Cu+ and Cu2+ additions, a 2 mM Cu(I) stock solution prepared in 0.1 M HCl and 1 M NaCl and a 2 mM Cu(II) stock solution prepared from CuCl2 were used, respectively. Best linear fit for the Cu(II) data is shown by the solid line with slope of 27.6 per logarithmic increase in calculated Cu2+ activities. The arrow illustrates the increase in Cu-ISE electrode potential due to the Cu+ spike to the solution containing 1 µM of Cu2+. S2 S2: Total Cu(I) determination by complexation with bathocuproine Experimental. The absorbance of the Cu(I)-bathocuproine complex and its interactions with untreated humic acid (HA) solutions were tested by measuring the UV–vis absorbance spectra of mixtures of HA (concentrations: 0, 46, 93, and 186 mg L–1), bathocuproine (Alfa Aesar, concentrations: 0 and 10 mM), Cu(I) (from 1 mM Cu+ stock solution prepared from CuCl (Merck, p.a.) in 0.1 M HCl (Sigma-Aldrich, p.a.) and 1 M NaCl (VWR, p.a.), concentrations: 0, 15, 30, and 100 µM) in 100 mM phosphate buffer at pH 7 (prepared from NaH2PO4·H2O and Na2HPO4·2 H2O, both Merck, p.a.). The amount of acid added by the addition of Cu(I) stock solution was balanced by the same volume of 0.1 M NaOH (Sigma-Aldrich, p.a.) to avoid effects on pH. Each combination of humic acid concentration, bathocuproine, and Cu(I) concentration was prepared in duplicate, leading to a total number of 64 samples. Data analysis. The dataset was analyzed by fitting the following model with interactions to the data by linear regression: y = β0 + β1·x1 + β2·x2 + β3·x3 + β12·x1·x2 + β13·x1·x3 + β23·x2·x3 + β123·x1·x2·x3 + ε (E1) where y is the absorbance of the mixture at 484 nm, and x1, x2, and x3 are the concentrations of HA, Cu(I), and bathocuproine in the sample, respectively. ε represents the residual error. Results. Figure S2 shows that the UV–vis absorbance of the HA and the Cu(I)-bathocuproine complex are additive, that is, the sum of the UV–vis absorbance of the complex of Cu(I) with bathocuproine alone and the absorbance of the HA alone equals the absorbance of the mixture of HA, Cu(I), and bathocuproine. Table S1 lists the estimated parameters and test results for the linear fit to equation (E1). Graphical analysis of residuals showed that model assumptions (constant, zero variance and normal distribution of residuals) are fulfilled sufficiently (Figure S3). The only parameters that significantly influenced the measured UV–vis absorbance (i.e., p-value < 0.01) were the cuvette absorbance (intercept β0), the HA concentration (β1), and the interaction of Cu(I) and bathocuproine concentrations (β23). Molar absorbance of HA was found to be 0.0031 per (mg L–1) at 484 nm, which is the same as determined by Maurer et al.1 (0.00308 per (mg L–1)). The interaction of Cu(I) and bathocuproine concentrations (β23) corresponds to the molar absorbance coefficient of the Cu(I)- bathocuproine complex (11156 ±10 M–1 cm–1) that can be used for quantification of Cu(I) (compare with 12700 M–1 cm–1 found by Moffett et al.2). The presence of Cu(I) or bathocuproine had no significant influence on the absorbance of HA (p > 0.01 for the corresponding interaction parameters β12 and β13). Further, also the HA concentration was found to have no significant influence on the absorbance of the Cu(I)bathocuproine complex (p > 0.01 for the corresponding three-fold interaction parameter β123). Therefore, the method measured always total Cu(I) present in the sample including Cu(I) bound to HA. From the standard error of the residuals (0.0095), a detection limit (±3 standard errors) of 0.029 in absorbance units or about 3 µM Cu(I) can be deduced. The residual standard error was found to depend strongly on the number of solutions that were added to a cuvette before measurement of the absorbance (number of pipette actions), however. For this reason, the residual standard error for the main experiments (see main article) could be lowered considerably by using only two solutions (sample and reagent solution) for preparation of the sample. S3 0.7 0.4 0.3 0.0 0.1 0.2 Absorbance 0.5 0.6 buffer HA BC CuI BC.CuI BC.CuI.HA sum 400 450 500 550 600 650 700 Wavelength (nm) Figure S2. UV–vis absorbance spectra for 15 µM Cu(I), 93 mg L–1 HA, and 10 mM bathocuproine (BC) illustrating the additivity of the absorbance of HA and the Cu(I)bathocuproine complex. The dashed line shows the calculated sum of the spectra recorded from the HA and Cu(I)-bathocuproine (BC.CuI) solutions only. S4 Table S1. Parameter estimates, estimated standard error, and p-value of t-tests testing for significance of the parameter for the linear model given in equation (E1). 1.0 3 2 1 -2 -1 0 1 2 Fitted values Theoretical Quantiles Scale-Location Residuals vs Leverage 0.5 3 1 0 1 2 0.5 1.0 Fitted values 1.5 0.5 Cook's distance -4 0.5 48 12 -2 35 1.0 1.5 Standardized residuals 93 34 34 93 1.5 0.0 Standardized residuals 0.5 35 -1 0 -0.01 93 -3 35 0.01 34 Normal Q-Q Standardized residuals Residuals vs Fitted -0.03 Residuals 0.03 Parameter Estimate Std. Error p –2 –3 <10–16 β0 7.44·10 3.59·10 <10–16 β1 3.11·10–3 3.37·10–5 0.899 –8.64·10–6 6.80·10–5 β2 –3 –3 0.257 β3 5.81·10 5.07·10 0.588 β12 3.48·10–7 6.39·10–7 –7 –5 0.994 β13 3.88·10 4.77·10 –2 –2 <10–16 β23 1.12·10 9.62·10 –7 –7 0.649 4.14·10 9.04·10 β123 0.00951 (56 degrees of freedom) ε R2 0.9995 0.0 0.1 0.2 93 0.3 1 0.4 Leverage Figure S3. Graphical residual analysis for the linear model fit of equation (E1) shown in Table S1. S5 S3: Calculation of inorganic copper speciation Inorganic copper speciation was determined using a fixed ratio of complexed to free species concentrations calculated using laws of conservation of mass and mass action. For Cu+, the relationship between total ([Cu+]tot) and free ([Cu+]) Cu+ was formulated as: [Cu+]tot = [Cu+] + [CuCl] + [CuCl2–] + [CuCl32–] = {Cu+}/γ1 + {CuCl} + {CuCl2–}/γ1 + {CuCl32–}/γ2 = {Cu+} · (1/γ1 + KCuCl · {Cl–} + KCuCl2 · {Cl–}2/γ1 + KCuCl3 · {Cl–}3/γ2) = [Cu+] · γ1 · (1/γ1 + KCuCl · {Cl–} + KCuCl2 · {Cl–}2/γ1 + KCuCl3 · {Cl–}3/γ2) = αI* · [Cu+], using [] and {} to denote concentrations and activities, respectively, and γ1 and γ2 to denote activity coefficients for species with charge 1 or 2, respectively. Ki refer to stability constants listed in Table S3. For a NaCl concentration of 0.1 M, the ratio of total ([Cu+]tot) and free ([Cu+]) Cu+ concentration (αI*) becomes αI* = γ1 · (1/γ1 + KCuCl · {Cl–} + KCuCl2 · {Cl–}2/γ1 + KCuCl3 · {Cl–}3/γ2) = 0.78 · (1/0.78 + 103.1 · 0.078 + 105.68 · 0.0782/0.78 + 105.02 · 0.0783/0.36) = 3064 For Cu2+, a similar calculation leads to: [Cu2+]tot = [Cu2+] + [CuOH+] + [Cu(OH)2] = {Cu2+}/γ2 + {CuOH+}/γ1 + {Cu(OH)2} = {Cu2+} · (1/γ2 + KCu(OH)+ · {OH–}/γ1 + KCu(OH)2 · {OH–}2) = γ2 · [Cu2+] · (1/γ2 + KCu(OH)+ · {OH–}/γ1 + KCu(OH)2 · {OH–}2) = αII* · [Cu2+] For a NaCl concentration of 0.1 M, the ratio of total ([Cu2+]tot) and free ([Cu2+]) Cu2+ concentration (αII*) becomes αII* = γ2 · (1/γ2 + KCu(OH)+ · {OH–}/γ1 + KCu(OH)2 · {OH–}2) = 0.36 · (1/0.36 + 10(6.5–7)/0.78 + 10(11.8–14)) = 1.32 Table S2 lists values for αI* and αII* calculated for concentrations of NaCl used here and in the first part of this study3. Table S2. Total dissolved to free ratios for Cu2+ (αII*) and Cu+ (αI*) used for calculation of inorganic speciation in solutions with selected NaCl concentrations. – {Cl } (M) γ1 γ2 αI * αII* 0.1 0.078 0.78 0.36 3064 1.32 NaCl concentration (M) 0.073 0.023 0.058 0.020 0.80 0.86 0.40 0.56 1716 212.8 1.16 1.21 S6 Table S3. Stability constants used for calculation of inorganic copper speciation. no. 1 2 3 4 5 6 7 8 9 10 reactions Cu+ + Cl– = CuCl (aq) Cu+ + 2 Cl– = CuCl2– Cu+ + 3 Cl– = CuCl32– Cu2+ + OH– = Cu(OH)+ Cu2+ + 2 OH– = Cu(OH)2 Cu2+ + e– = Cu+ Cu(0) = Cu2+ + 2 e– CuCl(s) = Cu+ + Cl– Cu2O(s) = 2 Cu+ + H2O – 2 H+ CuO(s) = Cu2+ + H2O – 2 H+ Eh0 (V) 0.153 0.34 log K at 25 °C, I=0 M 3.10 5.68 5.02 6.5 11.8 2.59 –11.49 –6.73 –2.17 7.66 reference Martell et al.4 Wang et al.5 Wang et al.5 Martell et al.4 Morel and Hering6 Moffett and Zika7 Lindsay8 Martell et al.4 Lindsay8 Lindsay8 S7 S4: Cu(I) formation during titration experiments plotted as fraction of total added copper 1.4 1.3 1.2 reduced HA (N2) reoxidized HA (N2) reoxidized HA (O2/N2) Total Cu(I) to total Cu ratio 1.1 1.0 0.9 0.8 0.7 0.6 0.5 0.4 0.3 0.2 0.1 0.0 1 3 6 23 1 3 6 23 1 3 6 23 1 3 6 23 +0 + 24 + 48 + 72 Reaction time (h) Figure S4. Ratios of measured total Cu(I) to total added copper in the titrations solutions 1, 3, 6, and 23 h after Cu2+ addition for each of the four copper spikes (indicated by dotted vertical lines). The nominal copper loadings resulting from copper spikes were 9.5 mmol kg–1, 46 mmol kg–1, 180 mmol kg–1, and 600 mmol kg–1 during the first, second, third, and fourth day, respectively. The same data are shown in Figure 1A (main article) as absolute concentrations of total Cu(I). Symbol types correspond to HA treatments and experimental conditions during titration. Error bars represent a 95% confidence interval (±2 standard errors). S8 100 12 S5: Conditional stability constants for Cu-HA binding 10 1 0.01 Cu(I)-Cl species + 5 10 20 50 100 200 −1 Cu(I) tot (mmol kg ) 500 Cu 1 100 2 2 5 (d) 10 20 50 100 200 −1 Cu(I) tot (mmol kg ) 500 Cu(II)-HA 7 0.01 0.1 Fraction of total Cu(II) (%) 10 9 8 c 1 10 11 (c) −1 (L kg ) [HA-Cu(II)] [HAtot][Cu(II)] Cu(I)-HA 0.001 7 6 12 1 log K = (b) 0.1 Fraction of total Cu(I) (%) 10 9 8 [HA-Cu(I)] c log K = [HAtot][Cu(I)] −1 (L kg ) 11 (a) 2+ 6 0.001 Cu 1 2 5 10 20 50 100 200 −1 Cu(II) tot (mmol kg ) 500 1 2 5 10 20 50 100 200 −1 Cu(II) tot (mmol kg ) 500 Figure S5. Conditional stability constants for binding of (a) Cu+ and (c) Cu2+ to humic acid as calculated from dialysis cell experiment data for Cu+ (Figure 2b) and titration experiment data corresponding to 23 h equilibration for Cu2+ (Figure 2a). Speciation of (b) Cu(I) and (d) Cu(II) as a function of copper loading in solutions containing 1 g L–1 HA and 0.1 M NaCl. The species are plotted as fractions of total copper. S9 S6: Speciation for solid phase samples (a) 0.5 Cu Calculated Eh (V) 0.4 2+ CuO(s) 0.3 0.2 Cu2O(s) - CuCl2 0.1 0.0 Cu(0) -0.1 -0.2 -11 -10 (b) -9 -8 -7 -6 -5 -4 log total inorganic copper (M) -3 Calculated Eh (V) 0.3 0.2 Cu(II)-HA 0.1 0.0 Cu(I)-HA Cu(0) -0.1 -11 -10 -9 -8 -7 -6 -5 log total copper (M) untrox redox untranox redanox L1 L2 -4 -3 untrox redox untranox redanox H1 H2 Figure S6. Calculated redox potentials as a function of (a) calculated total inorganic copper and (b) total added copper in HA solutions used for preparation of solid phase samples described in the first part of this study.3 Fractions of redox species based on LCF of Cu K-edge XANES spectra were used as input data (see Table S2 in Supporting Information of Fulda et al.3). Redox potentials were calculated using the Nernst equation and free Cu+ and Cu2+ activities derived from isotherms corresponding to Cu+ binding (Figure 2b) and Cu2+ binding after 23 h equilibration (Figure 2a) without correction for ionic strength deviations. Areas divided by lines depict in plot (a) the most abundant inorganic copper redox species or oversaturation of a solid phase as predicted by thermodynamics for the given experimental conditions (L: 0.023 M NaCl (dashed lines) or H: 0.078 M NaCl (solid lines), 25 °C). For plot (b), the speciation calculation additionally included HA copper species. Adjacent lines reflect the range of HA concentrations used in the titration experiments. Symbol type corresponds to redox treatment (untrox: untreated HA under oxic conditions; redox: reduced HA under oxic conditions; untranox: untreated HA under anoxic conditions; redanox: reduced HA under anoxic conditions) and type (1: added as Cu(I); 2: added as Cu(II)) and amount (L: 7.5 mmol kg–1; H: 150 mmol kg–1) of copper added (see first part of this study3). Error bars represent a 95% confidence interval for the derived redox potentials and were calculated using Monte Carlo estimation procedures with 1000 calculations per point and assuming standard errors for the Cu+ isotherm parameters as shown in Figure 2b (main article), and an absolute standard error of 5% for species fractions estimated by XANES LCF. S10 References (1) (2) (3) (4) (5) (6) (7) (8) Maurer, F.; Christl, I. and Kretzschmar, R. Reduction and reoxidation of humic acid: Influence on spectroscopic properties and proton binding. Environ. Sci. Technol. 2010, 44 (15), 5787–5792. Moffett, J. W.; Zika, R. G. and Petasne, R. G. Evaluation of bathocuproine for the spectrophotometric determination of copper(I) in copper redox studies with applications in studies of natural-waters. Anal. Chim. Acta 1985, 175, 171–179. Fulda, B.; Voegelin, A.; Maurer, F.; Christl, I. and Kretzschmar, R. Copper redox transformation and complexation by reduced and reoxidized soil humic acid: 1. X-ray absorption spectroscopy study. Environ. Sci. Technol. 2013, (this issue). Martell, A. E.; Smith, R. M. and Motekaitis, R. J. NIST Database 46: Critically Selected Stability Constants of Metal Complexes, Version 8. National Institute of Standards and Technology: Gaithersburg, MD, 2004. Wang, M.; Zhang, Y. and Muhammed, M. Critical evaluation of thermodynamics of complex formation of metal ions in aqueous solutions III. The system Cu(I,II)–Cl––e at 298.15 K. Hydrometallurgy 1997, 45 (1–2), 53–72. Morel, F. M. M. and Hering, J. Principles and Applications of Aquatic Chemistry. Wiley: New York, 1993. Moffett, J. W. and Zika, R. G. Reaction-kinetics of hydrogen-peroxide with copper and iron in seawater. Environ. Sci. Technol. 1987, 21 (8), 804–810. Lindsay, W. L. Chemical Equilibria in Soils. John Wiley & Sons: New York, 1979. S11
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