Gábor
Lente
*a and
James H.
Espenson
b
aDepartment of Inorganic and Analytical Chemistry, University of Debrecen, Debrecen, Hungary. E-mail: lenteg@delfin.unideb.hu; Fax: +36-52-489-667; Tel: +36-52-512-900 Ext.: 2373
bAmes Laboratory and Department of Chemistry, Iowa State University, Ames, IA, USA. E-mail: espenson@ameslab.gov; Fax: +1-515-294-5233; Tel: +1-515-294-5370
First published on 25th November 2004
A systematic study of the stoichiometric and kinetic efficiencies of catalysts in the oxidation of 2,4,6-trichlorophenol by hydrogen peroxide was carried out. Six different iron-based activators were used: Fe3+(aq), Fe(TPPS)+, cis-[(cyclam)Fe]3+, trans-[(cyclam)Fe]3+, [Fe(TPA)]2+, and [Fe(6-Me2-TPA)2+ (ligand abbreviations: TPPS = meso-tetra(4-sulfonatophenyl) porphine, cyclam = 1,4,8,11-tetraazacyclotetradecane, TPA = tris(2-pyridylmethyl)amine, 6-Me2-TPA = bis[(6-methyl-2-pyridyl)methyl](2-pyridylmethyl)amine). The stoichiometric efficiencies of the catalyst were characterized by comparing the total organic carbon content, chloride ion concentration, and remaining oxidant concentration to the ideal stoichiometry where carbon dioxide, water and inorganic chloride are the only products. The kinetic efficiencies of the catalysts were compared using the rate of chloride ion formation and H2O2 consumption. It was shown that Fe(TPPS)+ is the best catalyst. Illumination by visible light significantly enhances the rate of oxidation.
2,4,6-Trichlorophenol (TCP) is one of the most significant pollutants among chlorinated phenols and is often used to test the efficiency of oxidation methods.1,3 These methods usually use H2O2 or KHSO5 as a stoichiometric oxidant. Aqueous H2O2 is generally regarded as an environmentally friendly, “green” reagent21–27 partly because it gives water as the sole by-product of oxidation. However, H2O2 does not oxidize TCP or other chlorinated phenols in the absence of catalysts.28 The activators are usually transition metal complexes, most often iron(II) or iron(III) complexes involving N-donor ligands.1–12
Collins and co-workers recently reported the use of an oxidatively robust iron(III) complex of a TAML (tetra amido macrocyclic ligand) for the oxidation of TCP.3 Meunier and co-workers used iron tetrasulfophthalocyanine1 and iron(III) porphine derivatives.5,6 These complexes have a common feature: all of them have 4 N donor atoms in a planar arrangement surrounding the iron center. Iron-based non-heme activators for H2O2 are also being developed and studied for the epoxidation of olefins.29–33 We postulated that these might also be successful in the oxidation of TCP. Que and co-workers used iron complexes of tripodal polypyridyl ligands and they found characteristic differences between the catalytic activity of high-spin and low-spin iron(II) complexes which otherwise were very similar.30–32 Iron(III) cyclam complexes have also been successfully used to activate H2O2 toward epoxidation of olefins.29 Two separable isomers of the iron(III) cyclam complex are known: the cis complex is high-spin, the trans complex is low-spin.34
In this work, we present a systematic study of the efficiencies of iron catalysts in the aqueous oxidation of TCP by H2O2. Six different complexes were used (HS: high-spin, LS: low-spin): Fe(TPPS)+ (LS), cis-[(cyclam)Fe]3+ (HS), trans-[(cyclam)Fe]3+ (LS), [Fe(TPA)]2+ (LS), [Fe(6-Me2-TPA)]2+ (HS), and Fe(H2O)63+ (HS) for comparison. The structural formulas of the ligands are shown in Chart 1. We report the development of several methods to characterize and compare the stoichiometric and kinetic efficiencies of the different catalysts.
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Chart 1 Ligands used in this study. |
C6H3Cl3O + 11H2O2 → 6CO2 + 11H2O + 3H+ + 3Cl− | (1) |
One method often used to characterize the final organic product distribution is GC-MS.3 This method usually requires considerable sample treatment, which, together with possible secondary reactions on the GC column, can potentially introduce considerable error.35 In addition, reliable quantification of GC-MS data requires time consuming calibration for each organic component measured. Used with caution, GC-MS can still be a highly valuable source of information on the organic products. Our GC-MS experiments did not prove any formation of highly toxic dioxins at any time, which is of particular concern in chlorophenol oxidations in general.3 This is probably the only really important piece of information from GC-MS studies for the purposes of this work, as the overall stoichiometric efficiency involves mostly inorganic substances (see eqn 1), which cannot be analyzed by this method. After describing our observations on the choice of oxidant and the possible use of buffers, this paper will summarize our efforts to develop methods to characterize the stoichiometric and kinetic efficiency of catalytic TCP oxidation with special emphasis on the environmentally relevant aspects of the process.
We also tested KHSO5 as an oxidizing agent for TCP in a few experiments. KHSO5 can often be used as an inexpensive alternative to H2O2 in organic transformations, and its use was preferred even in TCP oxidation in a few earlier studies.5 Although reactions with KHSO5 were usually faster than those with H2O2 and the same catalyst, a major problem was revealed by monitoring the concentration of Cl− formed in the reaction. After its initial formation, a decrease was detected in Cl− concentration during the oxidation process. To identify the reaction responsible for the decrease, experiments were carried out using Cl−, KHSO5 and Fe(TPPS)+ as a catalyst (without the addition of TCP). A substantial decrease was detected in Cl− concentration (see Electronic Supplementary Information†), and the formation of chlorine was confirmed. Thus, KHSO5 oxidizes the Cl− formed in the primary reaction to Cl2 under catalytic conditions. This procedure is disadvantageous because it consumes additional oxidizing agent and produces a toxic gas. The use of KHSO5 also has the inherent disadvantage of forming considerable amounts of K2SO4 as a by-product. It is concluded that H2O2 is a more environmental friendly oxidizing agent for the oxidation of chlorinated phenols.
In our experiments, we have shown that the presence of citric acid, a common buffer compound,5,6 inhibits the Fe(TPPS)+-catalyzed oxidation of TCP (see ESI†). In agreement with the considerations presented at the beginning of this section, we did not use buffers in this study. In a few examples, the acidity of the solutions was monitored with a pH electrode. These measurements showed that the original pH of the TCP solutions (about 5.5) decreased during the oxidation to 3.2–2.8 depending on the exact initial concentrations. This showed that acid is produced in the reaction as shown in eqn. 1. However, this pH change did not cause any dramatic change in the activity of the catalysts used in this study.
2H NMR experiments were carried out using a saturated aqueous solution of TCP-d2 (∼2.2 mM), in which the only detectable signals were those of TCP-d2 and HDO, the latter from the natural isotope distribution of hydrogen in solvent water. After the addition of H2O2 and the catalyst, the intensity of the signal of TCP-d2 decreased, the intensity of the HDO signal increased gradually. Only the HDO signal was detectable after ca. 12 h. This shows that all the hydrogens present in the initial TCP were oxidized to water or became exchangeable (OH or CO2H) protons. No separate signal corresponding to a 2H-containing intermediate was detected in these experiments.
A few 2H NMR experiments were carried out with the standard CD3CN added directly to the solution rather than used as an external standard. In these experiments, clear evidence was found for the oxidation of CD3CN as well: the intensity of its signal decreased whereas the intensity of the HDO signal increased. This observation further emphasizes that oxidation of added organic substances including buffers or standards may be a serious concern during TCP oxidation.
Before performing the test runs, separate experiments, in which the concentration of a TCP stock solution was followed spectrophotometrically, were carried out to exclude any possible aqueous self- or light-induced decomposition of TCP. In these experiments, there was no measurable decrease in the TCP concentration over 2–3 months.
Samples were prepared by adding a solution of H2O2 to a solution of TCP, and the reaction was initiated by adding the catalyst. To make sure that all processes go to completion, the samples were stored at room temperature in the dark for 10 days before analysis in a sealed glass container that was opened three times during this period to allow gases to escape. After this time, the samples were analyzed for total organic carbon (TOC) content, Cl− concentration and H2O2 concentration. The catalyst Fe(TPPS)+ was used in two batches of experiments. In the first, the samples were stored in the dark similarly to other samples. In the second, the samples were illuminated with a 500 W halogen lamp for the first day and then stored in room light.
The TOC of the oxidized sample was considerably lower than that of the original sample in each case. This clearly indicates that carbon dioxide (or less likely carbon monoxide) was formed during the process. Results for the different catalysts are shown in Fig. 1, where the decrease of TOC is shown relative to the initial TCP sample. The higher the decrease, the more carbon dioxide is formed and the more efficient the oxidation is. The best catalyst is Fe(H2O)63+, with a TOC decrease of 58%; the others gave slightly lower decreases, 35–45%. The TOC decrease values given in Fig. 1 were calculated assuming that the TOC reduction occurs only because of TCP decomposition, and not because of the oxidation of the organic ligand present in the catalyst (which accounted for only a small fraction, less than 10% of the TOC of the original solution). The observational basis of this assumption was that we did not see significant loss of TOC in experiments where no TCP was used, i.e. the organic-containing iron-catalyst was reacted with hydrogen peroxide.
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Fig. 1 Decrease in total organic carbon content during the oxidation of 2,4,6-trichlorophenol with H2O2 using different catalysts. Initial concentrations: [TCP] = 1.63 mM, [H2O2] = 136 mM, [catalyst] = 30 mg L−1; reaction time: 10 days; room temperature. |
The chloride yield, defined as the amount of chloride ion in the final solution relative to the original total organic chlorine content, was also used to characterize the stoichiometric efficiencies. Fig. 2 shows that chloride yields are generally better than 90% and in two cases are quantitative (i.e., 100%) within experimental error. This shows that chlorine is removed from the organic compounds quite efficiently and little chlorinated organics or chlorinated aromatics remain in the solution after the oxidation. The only exception is Fe(6-Me2TPA)2+, where the chloride yield is only 75%. This value is significantly different from that determined for Fe(TPA)2+ (90%). The difference is not unexpected as these catalysts are known to have different reactivity patterns in epoxidation studies.31
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Fig. 2 Chloride ion yield during the oxidation of 2,4,6-trichlorophenol with H2O2 using different catalysts. Initial concentrations: [TCP] = 1.63 mM, [H2O2] = 136 mM, [catalyst] = 30 mg L−1; reaction time: 10 days; room temperature. |
The concentration of H2O2 remaining in the samples was also determined by iodometric titration.40Fig. 3 shows the amount of H2O2 consumed relative to the amount originally added. Under the standardized initial concentrations, the quantitative H2O2 consumption according to eqn. 1 is 13% and the determined values are usually close to or somewhat lower than this limit. The oxidant consumption was much higher in two cases: 25% for Fe3+(aq) and 64% for Fe(TPA)2+. Extra consumption of H2O2 is possible through its decomposition to water and dioxygen. It is concluded that a considerable amount of H2O2 is lost to catalytic decomposition when Fe3+(aq) or Fe(TPA)2+ is used as a catalyst. In the case of Fe(TPPS)+ and the two cyclam complexes, data for TOC, chloride ion, and oxidant consumption show that catalytic decomposition cannot be a major source of H2O2 loss.
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Fig. 3 Hydrogen peroxide consumpsion during the oxidation of 2,4,6-trichlorophenol with H2O2 using different catalysts. Initial concentrations: [TCP] = 1.63 mM, [H2O2] = 136 mM, [catalyst] = 30 mg L−1; reaction time: 10 days; room temperature. |
In summary, the H2O2 consumption is the only really significant difference between the catalysts in terms of overall stoichiometric efficiency. The catalyst systems based on tripodal polypyridyl ligands—Fe(TPA)2+ and Fe(6-Me2TPA)2+—are probably less efficient than the others because Fe(TPA)2+ consumes a significant quantity of H2O2 in reactions not involved in the catalytic oxidation, whereas Fe(6-Me2TPA)2+ leaves considerable chlorinated organics in the system. It should also be noted that the stoichiometric efficiency of Fe3+(aq) is comparable to other catalysts. Light does not have significant effects on the stoichiometric efficiency.
The rate of chloride ion formation was characterized in terms of the half-times (t1/2) necessary to reach a chloride ion concentration corresponding to half the total organic chlorine content of the original solution. It should be noted that this quantity is not completely analogous to half lives because the chloride ion formation did not follow an exponential (first-order) curve. Still, t1/2 values are suitable for the semi-quantitative comparison of different catalysts, as shown in Fig. 4. Three of the catalysts are similar, with t1/2ca. 16–18 h. Fe(6-Me2-TPA)2+ is slower than other systems, t1/2ca. 24 h, whereas Fe(H2O)63+ is somewhat faster, t1/2 = 12.6 h. Without doubt Fe(TPPS)+ is the fastest (t1/2 = 4.5 h), and illumination with visible light further lowers t1/2 to <1 h. These experiments were done using the different catalysts with the same mass concentrations. If molar concentrations are considered, the advantage of Fe(TPPS)+ is even larger because it has the highest molecular weight. It is also seen that light considerably enhances the rate of chloride ion formation and most likely the rate of overall oxidation.
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Fig. 4 The time (t1/2) needed to reach 50% Cl− yield during the oxidation of 2,4,6-trichlorophenol with H2O2 using different catalysts. [TCP] = 1.61 mM; [H2O2] = 95 mM; [catalyst] = 50 mg L−1; μ = 0.1 M (NaNO3); T = 25.0 °C. |
It was also possible to follow the time course of H2O2 concentration by taking samples from a reaction mixture and determining the concentration of H2O2. The results from an experiment series with Fe3+(aq) as a catalyst are shown in Fig. 5. Experiment a was carried out under usual TCP oxidation conditions. In experiment b, no TCP was added, and the rate of H2O2 consumption was clearly faster, an interesting fact that will be interpreted later. Experiment c was carried out without the addition of the catalyst. No H2O2 consumption was detected in this experiment showing once again that TCP is not oxidized by H2O2 without catalysts.
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Fig. 5 Concentration of H2O2 as a function of time during the oxidation of 2,4,6-trichlorophenol with H2O2 catalyzed by Fe3+(aq). [TCP] = 1.01 mM (a, c), 0 (b); [Fe3+(aq)] = 160 µM (a, b), 0 (c); T = 25.0 °C. |
This series of experiments was repeated with every catalyst. The ratios of the initial rates measured in the presence (vTCP) and absence (vblank) of TCP were used as a semi-quantitative indicator. Fig. 6 shows these ratios for every catalyst. Ratios span a large range from 54 for Fe(TPPS)+, through 5–10 for the cyclam complexes, to 0.16–0.21 for Fe3+(aq), Fe(TPA)2+ and Fe(6-Me2-TPA)2+. The last three catalysts had the same value within experimental error.
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Fig. 6 Initial rate ratios of H2O2 consumption in the presence (vTCP, [TCP] = 1.0 mM) and absence (vblank) of TCP. T = 25.0 °C. Note the logarithmic scale on the y axis. |
Fe(TPA)2+ induced a sudden burst of H2O2 decomposition with intense formation of bubbles. This initial burst was over in a few minutes and then a relatively slow decrease in H2O2 concentration was detected (see ESI†). No similar results were obtained with Fe(6-Me2-TPA)2+, which again shows that these two catalysts are dissimilar. The slowly decreasing region was used for evaluation with Fe(TPA)2+, because chloride ion kinetic measurements show without doubt that oxidation of the substrate occurs in this stage. The initial burst of H2O2 decomposition can likely be attributed to the catalyst in its original form accelerating the decomposition of H2O2 efficiently, but then being transformed to another form during the first few minutes.
It is well known that the decomposition of hydrogen peroxide is sensitive to experimental conditions and the possible presence of impurities. The consistency of the results and the general reliability of the procedures used was also checked in two ways. First, the stock concentration of the stock solutions of hydrogen peroxide, which were prepared from commercially available 30% hydrogen peroxide, was followed using iodometric titration. In a ca. 1 M stock solution, a gradual decrease in hydrogen peroxide concentration was observed. The overall decrease was 3.5% relative to the original concentration in 125 days, implying that decomposition because of the impurities present in the water used is probably not significant on the time scale of the initial rate studies (typically a few hours). Second, a test directly connected to the conditions of the initial rate measurements was also performed. Samples with hydrogen peroxide were prepared without a catalyst and in one case with phosphate-buffered Fe(TPPS)+, where the porphyrin forms a catalytically inactive dimer. No measurable loss of hydrogen peroxide was detected in either case for 5–6 hours.
A second possible mechanism is a catalytic cycle involving the catalyst, H2O2 and TCP. The substrate is oxidized in a direct reaction with an active high oxidation state iron complex. In this case, the catalytic cycle cannot operate without substrate and the rate of H2O2 consumption is clearly expected to be larger in the presence of substrate than in its absence. Fe(TPPS)+ and the cyclam complexes seem to follow this pattern. They are inefficient catalysts of H2O2 decomposition as shown by the high ratios in Fig. 6. The actual catalytic cycle and the species participating in it may be different for the different catalysts and further studies are needed to identify them.
Footnote |
† Electronic supplementary information (ESI) available: additional experimental observations. See http://www.rsc.org/suppdata/gc/b4/b411269e/ |
This journal is © The Royal Society of Chemistry 2005 |