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Article

Natural Monocrystalline Pyrite as Sensor for Potentiometric Redox Titrations. Part I. Titrations with Permanganate

by
M. M. Antonijevic
1,*,
R. P. Mihajlovic
2 and
B. V. Vukanovic
1
1
Technical Faculty Bor, University of Belgrade, P.O.Box 50, 19210 Bor, Yugoslavia
2
Faculty of Science, University of Kragujevac, 34000 Kragujevac, Yugoslavia
*
Author to whom correspondence should be addressed.
Sensors 2002, 2(4), 153-163; https://doi.org/10.3390/s20400153
Submission received: 9 April 2002 / Accepted: 23 April 2002 / Published: 30 April 2002

Abstract

:
Results obtained in potentiometric titrations of Fe(II), Mn(II), Fe(CN)64−, C2O42− and As(III) with standard potassium permanganate solution, are presented. The titration end point (TEP) was detected with a universal electrode whose sensor is natural crystalline pyrite. The titrations of As(III) were carried out in HCl (1.2 M) and H2SO4 solutions (0.1-4.5 M), whereas oxalate was determined in H2SO4 (0.1-4.5 M). Iron(II) and hexacyanoferrate(II) were titrated in H2SO4 and also in H3PO4 solutions (0.1-4.5 M). The titrations of Mn(II) were performed in H2P2O72− media at pH 4.0, 5.0, 6.0 and 7.0. The results obtained by using the pyrite electrode were compared with those obtained by the application of a Pt-electrode, and good agreement, reproducibility and accuracy were obtained. The potentials in the course of the titration and at the end-point (TEP) are rapidly established. The potential changes at the TEP ranged from 90 to 330 mV/0.1 mL, depending on the titrated system. The highest changes were observed in titrations of Fe(II) in H3PO4 (240-330 mV/0.1 mL). Reversed titrations were also performed and accurate and reproducible results were obtained.

Introduction

Mn(II) can be determined in several ways: iodometrically 1, by differential stripping voltammetry 2, polarographically 3, fluorometrically 4, amperometrically 5, by indirect titration with EDTA 6, sprectrophotometrically 7,8, by the potentiometric titration with Mn(VII) in pyrophosphate media 9 as well as by potentiometric titration with polyamine ligands in acetonitrile 10.
Fe(II) can be determined by volumetric titration with cerium(IV) using ferroin as indicator 11, by liquid chromatography 12, photometrically 13,14, polarographically 15, ferrocenometrically 16, by using XeF2 as a standard titrating solution 17 as well as potentiometrically 10,18,19,20,21,22.
Hexacyanoferrate(II) can be determined by infrared spectroscopy 23, or amperometrically 24,25, coulometrically 26,27 as well as potentiometrically 28,29,30,31,32.
Arsenic(III) can be determined potentiometrically and by visual titration with bromoamine 28, by potentiometric stripping analysis 33, AFS method 34, cerimetrically 11,35, by potentiometric titration with XeF2 and also bipotentiometrically with Mn(III) and Mn(IV).
Oxalate can be determined chromatorgraphically 36, spectrophotometrically 37, gasometrically 38 as well as by potentiometric precipitation titrations.
From this short survey of methods for the determination of reducing substances it is seen that the potentiometric methods are of great importance for these determinations.Therefore, it is desirable to reveal and develop new sensors for the TEP detection. In the hitherto published papers the following indicator electrodes were used: Cu-wire, graphite electrode, Pt-electrode, Ag-electrode coated with Ag2S and Ag3Fe(CN)6 and picrate ion-selective electrode. All theafore-mentioned determinations were carried out either in aqueous or nonaqueous media, and are based on redox reactions, complex formation reactions or formation of precipitates.
In addition, Au, stainless steel, various inert electrodes can be also used as indicator electrodes in redox titrations, and one among the latter ones is the pyrite electrode which was found to be very effective in acid-base titrations in aqueous 40 and non-aqueous 41 solutions, as well as for complexometric titrations 42,43 and redox titrations 44,32.
In this paper results obtained in investigating pyrite as sensor of the indicator electrode in redox titrations with standard Mn(VII) solution, are presented.

Experimental

Chemicals and solutions

All solutions used in this paper were prepared from p.a. chemicals and distilled water.
The concentrations of standard solutions were determined titrimetrically by using visual or potentiometric TEP detection.
H2P2O72− solutions with pH values 4.0, 5.0, 6.0 and 7.0 respectively, were prepared by adding H2SO4 or NaOH to 0.02 M pyrophosphate solution, the pH being adjusted pH-metrically.

Apparatus and electrodes

The apparatus used and the preparation of electrodes are described in an earlier paper 40.

Procedure

Measurement of the stationary potential

The stationary potential of the Fe(CN)63−/Fe(CN)64− and Fe(III)/Fe(II) systems was measured at I = 0.1 M. The ionic strength was adjusted by the addition of NaNO3. The measurements were carried out for the following concentration (cOx/cRed) rations: 9:1, 7:3, 5:5. 3:7 and 1:9. The stationary potential was measured by noting the potential changes after each minute, in the course of 15 minutes. Potential values measured after 15 minutes were taken for the calculation of the slopes and correlation coefficients.

Potentiometric titrations

An appropriate volume of the reductant solution was placed in a 150 mL beaker and made up to 80 mL with an acid solution of known concentration (or pyrophosphate solution of known pH value, in the case of Mn(II) determination), the electrode couple SCE-FeS2 was then dipped into the solution, the magnetic stirrer was switched on and the potential change was measured after the addition of each increment of Mn(VII). The exact amount of consumed Mn(VII) solution was calculated by the mathematical method from the second derivative.

Results and Discussion

The electronic structure of crystalline pyrite indicates that this mineral is a low-spin complex with d2sp3 hybridization. All hybrid orbitals are occupied with electrons which makes pyrite a diamagnetic and non-reactive compound. Since pyrite is a semiconductor of n or p type, it is possible to use it, on account of its chemical inactivity, for themeasurements of the redox potentials.
The potential changes in potentiometric titrations in this case can be explained by polarization curves for pyrite and the components taking part in the redox reaction ( Fig.1.).
Figure 1. Anodic and cathodic polarization curves by means of which potential changes at the titration end-point are explained [Ox1, Ox2 (Ox’2), Ox3 and Ox4 are different oxidants].
Figure 1. Anodic and cathodic polarization curves by means of which potential changes at the titration end-point are explained [Ox1, Ox2 (Ox’2), Ox3 and Ox4 are different oxidants].
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It is known that in acid media pyrite dissolves slightly (becomes corroded), giving rise to soluble products 45:
F e S 2 + 8 H O 2 + 15 e = F e 3 + + 2 S O 4 2 + 16 H +
The rest potential of pyrite in open-circuit is 0.62 V vs. SCE, and at more positive potentials the dissolutions of pyrite occurs, which may be shown by the anodic polarization curve. The degree of pyrite oxidation is equivalent to the corrosion current and depends on several parameters (temperature, state of pyrite surface, oxidant concentration, oxidant nature, acidity of medium etc.). In potentiometric titrations, however, a polished mineral (small surface area), room temperature and low oxidant concentrations are used, so that all these conditions ensure an insignificant dissolution of pyrite. These data indicate that in the abscence of oxidizing agents, the value of the corrosion potential will be more negative (Fig.1.). Under these conditions the value of the corrosion current is also small. Such a state of the pyrite electrode occurs at the beginning of the potentiometric titrations. The efect of oxygen in the solution may be eliminated by bubbling nitrogen through the solution. Besides, the initial solutions may contain some ions which might cause the corrosion of pyrite at low potentials (EIcorr.). It may be assumed that the solutions a contains a reducing species (Red2) which on oxidationgives Ox2, when being titrated with the oxidant Ox3. Under these conditions the following reaction takes place in the solution:
Red2 + Ox3 = Red3 + Ox2
where Ox2/Red2 and Ox3/Red3 denote corresponding redox pairs. After the first addition of the oxidizing agent Ox3 a corrosion potential EIIcorr. is established at the pyrite electrode, whereby pyrite is oxidized by the oxidizing form of the reducing species ( Ox2). On further addition of the oxidizing agent Ox3, the concentration of the Ox2 species increases (Ox’2) and that results in the shift of the corrosion potential to EIIIcorr. At the end-point, when in the solution the oxidant Ox3 is in excess, the corrosion potential is abruptly shifted towards the more positive region, since under these conditions the dissolution of pyrite is defined by the Ox3/Red3 system. This change of the corrosion potential from EIIIcorr. to EIVcorr. makes possible the applications of the pyrite electrode as the indicator electrode in potentiometric redox titrations. From Fig.1. it is also seen that higher potential changes of the pyrite electrode at the titration end-point are observed in case oxidizing agents with more positive equilibrium potentials (stronger oxidants ) are used. The reagents which display a great overvoltage in cathodic reduction at pyrite are not suitable as titrating agents, since the potential changes at the titration end-point in that case are small. Similar consideration hold for titrations of oxidizing agents with reducing agents, but then, the corrosion potential of pyrite is shifted towards the more negative region.
The measurements of the standard potential were carried out with solutions having different cOx/cRed rations of the Fe(III)/Fe(II) and Fe(CN)63−/Fe(CN)64− systems, and the results obtained are shown in Fig. 2.
The calculated correlation coefficients (ccorr) shown the linearity of the results obtained, whereas the hitherto performed investigations point out the effectiveness of the pyrite electrode as the indicator electrode for potentiometric titrations.
Figure 2. Plots of E against log (cOx/cRed): (1) Fe(CN)63−/Fe(CN)64−; (2) Fe(III)/Fe(II).
Figure 2. Plots of E against log (cOx/cRed): (1) Fe(CN)63−/Fe(CN)64−; (2) Fe(III)/Fe(II).
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The chemical process taking place in the potentiometric titration of the Mn(II) with permanganate in pyrophosphate media is given by the following equation:
4 M n 2 + + M n O 4 + 8 H + + 15 H 2 P 2 O 7 2 = 5 M n ( H 2 P 2 O 7 ) 3 3 + 4 H 2 O
The main factor of this process is the concentration of H2P2O72− on account of the stabilization of Mn(III) in the form of the pyrophosphate complex. The titrations were performed at pH values 4.0, 5.0, 6.0 and 7.0 (Fig. 3).
Figure 3. Potentiometric titrations of Mn(II) in pyrophosphate at various pH values (1. pH 4.00; 2. pH 5.00; 3. pH 6.00; 4. pH 7.00).
Figure 3. Potentiometric titrations of Mn(II) in pyrophosphate at various pH values (1. pH 4.00; 2. pH 5.00; 3. pH 6.00; 4. pH 7.00).
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From the graph in Fig. 3. it is seen that pH 6.0 is the optimum pH, and that the tirations at pH-values 4.0, 5.0 and 7.0 do not afford good results since the TEP is shifted. At pH 6.0 the concentration of H2P2O72− ion in the solution is maximal which enables the stabilization of Mn(III) form, a decrease of the standard Mn(III)/Mn(II) potential and shifts the reaction to the right.
Pastor et al 9. carried out the determination of Mn(II) under the same conditions but they applied Pt and graphite electrodes as indicator electrodes. Comparison of results obtained by the application of the pyrite, Pt and graphite electrodes, is given in Table 1.
Table 1. Comparison of the results obtained with the pyrite, Pt and carbon indicator electrode in pyrophosphate media.
Table 1. Comparison of the results obtained with the pyrite, Pt and carbon indicator electrode in pyrophosphate media.
Titrated ionTitrantpHElectrodePotential change at the TEPReference
Mn(II)Mn(VII)6.2Pt110 - 1309
Mn(II)Mn(VII)6.2Carbon165 - 1909
Mn(II)Mn(VII)6.0FeS2100 - 190Results presented in this paper
From Table 1 it is seen that the pyrite electrode is applicable to the titrations of Mn(II) in pyrophosphate media at pH 6.0 with the same effectiveness as the Pt and graphite electrodes. The total potential changes range from 200 to 260 mV, whereas the jumps at the TEP from 100 to 190 mV/0.1 mL, depending on Mn(II) concentration in the titrated solution.
An increase in sulphuric acid concentration has a small effect on the increase of the total potential changes in the course of iron(II) titration, but not on the potential changes at the TEP.
However, an increase in H3PO4 concentration effects considerably both the potential changes in the course of the titration and the potential changes at the TEP. These observations are expected since Fe(III) which is formed in the course of the titration, in phosphoric acid solution forms the complex Fe(HPO4)+ whose formation constant is 2.3*109(46). The formation of such a stable complex causes a decrease of the potential of the Fe(III)/Fe(II) system and in this manner the potential differences with respect to the Mn(VII)/Mn(II) is increased. All that results in an increase of total potential changes in the course of the titration andalso of potential changes at the TEP (Table 2).
Table 2. Results obtained in potentiometric titrations of reducing substances with standard potassium permanganat solution (electrode couple FeS2-SCE).
Table 2. Results obtained in potentiometric titrations of reducing substances with standard potassium permanganat solution (electrode couple FeS2-SCE).
Taken (mol)cacid (mol.dm3)TitrantTotal change of E (mV)Change of E at the TEP (mV/0.1ml)Found
Fe(II)1Mn(VII)
0.00270.1280 - 36090 - 12099.4±0.1
0.00274.5340 - 35090 - 12099.7±0.2
0.00100.5290 - 300140 - 150100.6±0.4
0.00190.5305 - 310100 - 130100.1±0.3
0.00290.5745 - 750450 - 500100.0±0.0*
Mn(VII)Fe(II)
0.00071.5260 - 27050 - 6099.9±0.2
0.00074.5260 - 30040 - 7099.2±0.2
0.00041.5280 - 29075 - 8099.2±0.1
0.00061.5270 - 29050 - 60100.0±0.6
Fe(II)2Mn(VIII)
0.00290.1390 - 400180 - 240100.5±0.1
0.00291.5440 - 470260 - 330100.5±0.1
0.00210.5430 - 440260 - 270100.0±0.0
0.00370.5440 - 445240 - 25099.9±0.1
Fe(II)
0.00070.1340 - 350130 - 16099.5±0.2
0.00071.5430 - 440130 - 19099.8±0.3
0.00040.5410 - 420190 - 20099.2±0.1
0.00070.5400 - 405170 - 19099.8±0.1
Fe(CN)64−Mn(VII)1
0.00310.1470 - 480180 - 19099.9±0.0
0.00311.5370 - 38060 - 6599.9±0.1
0.00180.5380 - 390100 - 120100.4±0.1
0.00380.5400 - 41090 - 100100.3±0.1
0.00310.5730 - 770430 - 460100.0±0.0*
Mn(VII)Fe(CN)64−
0.00040.1320 - 330140 - 150100.3±0.1
0.00041.5205 - 21030 - 3599.9±0.3
0.00040.5260 - 27075 - 8099.9±0.3
0.00050.5280 - 28560 - 8099.6±0.2
Fe(CN)64−Mn(VII)2
0.00310.5440 - 450150 - 18099.7±0.1
0.00314.5330 - 35020 - 4099.7±0.2
0.00120.5420 - 430170 - 180101.1±0.1
0.00380.5440 - 470130 - 150100.1±0.1
0.00310.5710 - 780440 - 510100.0±0.0*
As(III)3Mn(VII)
0.00131.2230 - 290150 - 200100.7±0.1
0.00201.2240 - 270150 - 20099.9±0.1
As(III)1Mn(VII)
0.00200.1280 - 330160 - 230100.3±0.2
0.00201.5260 - 380200 - 310100.2±0.1
0.00090.5230 - 250150 - 16098.9±0.1
0.00200.5300 - 340180 - 270100.1±0.1
0.00130.5690 - 740350 - 620100.0±0.0*
C2O42−Mn(VII)1
0.00140.1180 - 25090 - 140101.8±0.2
0.00144.5230 - 28040 - 50101.9±0.8
0.00140.5220 - 280110 - 160101.0±0.2
0.00200.5230 - 320120 - 200100.4±0.1
0.00140.5550 - 560360 - 420100.0±0.0*
1- Titrations in H2SO4; 2- Titrations in H3PO4; 3- Titrations in HCl; *-Titrations by the use of a Pt-el.
The increase in H2SO4 and H3PO4 concentrations has a more significant influence of potential changes in titrations of hexacyanoferrate(II). At lower H2SO4 concentrations the process of hexacyanoferrate(II) oxidation takes place more readily since a small amount of H+ is available for the formation of H4Fe(CN)6.
With increasing H+ concentration the reaction of H4Fe(CN)6 formation is favoured, and in conditions of satisfactory high H+ concentration (4.5 M H2SO4) the process of hexacyanoferrate(II) oxidation is very slow. At lowe H2SO4 concentrations (0.1, 0.5 and 1.5 M) the process of hexacyanoferrate(II) oxidation proceeds with a more considerable decrease in potential shanges with the increasing acidity. However, since H3PO4 is a weaker acid than H2SO4, a H3PO4 solution of the same concentration as that of H2SO4 will contain less H+ ions, and therefore, with increasing H3PO4 concentration the formation of H4Fe(CN)6 will have less priority. On account of these reasons the titration of hexacyanoferrate(II) in 4.5 M H3PO4 is possible (Table 2).
With standard solutions of Mn(III) in 1.0 M H2SO4 and Mn(IV) in 2.0 M H2SO4 the bipotentiometric titrations (Pt-electrodes) of hexacyanoferrate(II) were performed with a total potential change of 400-750 mV. The results obtained with Mn(III) were 99.2+0.2% and those with Mn(IV) 100.2+0.3%. Hexacyanoferrate(II) can be determined also by potentiometric precipitation reactions with AgNO3, the indicator electrode being based on a mixture of Ag2S and Ag4Fe(CN)6, whereby the obtained jumps amounted to about 150 mV/0.1 mL 30, or a picrate ion-selective electrode can be used.
The titrations of As(III) were carried out in HCl (1.2 M) and H2SO4 (0.1 - 4.5 M). Because the reaction of As(III) with Mn(VII) is slow, it had to be catalyzed. In titrations of As(III) in HCl, only the concentration of As(III) was changed. The changes in As(III) concentration had no significant effect either on the potential changes or on the accuracy of the results. An increasein H2SO4 concentration in titrations of As(III) had a more significant effect on potential changes. With increasing acidity the oxidizing ability of Mn(VII) is increased, and be cause of that the difference in potential is increased which causes an increase in potential changes (Table 2).
The titrations of oxalate were carried out in H2SO4 (0.1-4.5 M). It is known that the presence of higher amounts of H2SO4 inhibits the reaction of oxalate with Mn(VII) making it slow, which has a considerable effect on the decrease of potential change at the TEP (with increasing acidity the potential change is decreased for about 90 mV/0.1 mL) (Table 2).
In reversed titrations the behaviour of the pyrite electrode was similar to that in direct titrations. The total potential changes and the potential changes at the TEP were smaller with respect to those in direct titrations. The highest changes at the TEP were observed in titrations of Mn(VII) with iron(II) in 1.5 M H3PO4 (130 - 190 mV/0.1 mL), whereas the smallest ones in titrations of Mn(VII) with iron in H2SO4 (50 - 60 mV/0.1 mL).
The accuracy and the reproducibility in direct and reverse titrations were satisfactory (Table 2).
In all direct and reverse titrations, in the presence of MnO4 ion in excess, potential oscillations were observed (±5mV). These oscillations are most probably due to unequal rates of MnO4 reduction on the pyrite surface. A change in the reduction rate (cathodic current density) causes a change in the position of the corrosion potential, which gives rise to its oscillations.
In the course of the titration and also at the TEP the potential was rapidly established (<1 ) except in titrations of oxalate where on account of a slow reaction a somewhat longer time-interval was required, as well as in the determination of As(III) where the reaction had to be catalyzed.
Data in Tables show that the behaviour of pyrite in all the investigated systems is in accordance with the expected one: higher jumps were obtained with those systems where the difference between the standard potential values was greater. Also higher jumps at the TEP were registered in cases where the medium can influence the reaction equilibrium (titration of Fe(II) in H3PO4 or Mn(II) in pyrophosphate medium at the pH 6.0). In addition, taking into account the accuracy and the reproducibility as well as therate of potential establishment at the FeS2 electrode in the course of the titration and at the TEP, it may be concluded that pyrite as sensor of the indicator electrode is suitable for the TEP detection in redox potentiometric titrations where standard Mn(VII) solution is used as the titrant.

Acknowledgments

The authors wish to thank the Scientific Fund of the Republic of Serbia for financial support ( Project No: 1622, 2002)

References

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Antonijevic, M.M.; Mihajlovic, R.P.; Vukanovic, B.V. Natural Monocrystalline Pyrite as Sensor for Potentiometric Redox Titrations. Part I. Titrations with Permanganate. Sensors 2002, 2, 153-163. https://doi.org/10.3390/s20400153

AMA Style

Antonijevic MM, Mihajlovic RP, Vukanovic BV. Natural Monocrystalline Pyrite as Sensor for Potentiometric Redox Titrations. Part I. Titrations with Permanganate. Sensors. 2002; 2(4):153-163. https://doi.org/10.3390/s20400153

Chicago/Turabian Style

Antonijevic, M. M., R. P. Mihajlovic, and B. V. Vukanovic. 2002. "Natural Monocrystalline Pyrite as Sensor for Potentiometric Redox Titrations. Part I. Titrations with Permanganate" Sensors 2, no. 4: 153-163. https://doi.org/10.3390/s20400153

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