Tippu S. Sheriff*,
Suhayel Miah†
and
Kit L. Kuok‡
Inorganic Chemistry Research Laboratories, Queen Mary University of London, London E1 4NS, UK. E-mail: t.s.sheriff@qmul.ac.uk; Tel: +44 (0)207 882 8466
First published on 29th July 2014
A rapid and selective visual colour method is described for detection of hydrogen peroxide (H2O2) and peroxide based explosive (PBE) vapours by the combination of three azo dyes – Calmagite, Orange G and Orange II. The bleaching of these dyes by H2O2 is catalysed by MnII. At pH 8.0 (EPPS, N-2-hydroxyethyl-piperazine-N′-3-propanesulfonic acid) Calmagite is quickly degraded but under these conditions Orange G and Orange II are not perceptibly bleached, especially in the presence of ethylenediaminetetraacetic acid (H4edta). However, fast bleaching of Orange G and Orange II was observed at pH 9.0 (Na2CO3, sodium carbonate) due to the in situ formation of the carbonate radical (CO3−˙). Hence by a combination of Calmagite at pH 8.0, and Orange G and Orange II at pH 9.0, selectivity to H2O2 vapours against Cl2, NO2 and O3 can be demonstrated. Initial studies were carried out on filter papers but reaction times were slow. With Calmagite rapid colour changes, within 15 minutes, were found when the dye was deposited on to polyvinyl alcohol (PVA) polymer which had been coated onto a borosilicate glass plate. However, with Orange G and Orange II the colour changes on the PVA/plates were slow and this may be due to the limited availability of CO2, as the activating species, in generating CO3−˙.
The explosive nature of PBEs is associated with the weakness of peroxide bonds (ΔHbond (O–O) = 147 kJ mol−1) giving spin-allowed reactions under ambient conditions hence, unlike reactions of O2, activation energies are low, and the heat generated in producing large volumes of thermodynamically stable gaseous products (CO2, H2O, acetone etc.).1,2 The explosive power of TATP has been described as an “entropic burst” but the negative enthalpy of this reaction cannot also be ignored which together generate large amounts of free energy that leads to rapid acceleration in reaction rates resulting in an explosive power comparable to that of TNT.3
It is reported that PBEs were first used in 19804 but have gained notoriety in their more recent uses including the Casablanca explosions in 2003,5 the London public transportation attacks in 20056 and the transatlantic flight bombing attempt in 2006.5 These events draw attention to the need for reliable and selective detection methods for PBEs. The ready availability of the simple chemicals required to manufacture PBEs and the relative ease of their syntheses allow for the clandestine manufacture of such explosives using “kitchen sink” methodologies. For example, H2O2 is used in hair and teeth bleaching, cleaning products and disinfectants, sulfuric acid is used as a household drain cleaner and acetone as nail varnish remover. Indeed there are concerns that TATP can be assembled from these innocuous precursor chemicals at the target site.
As well as their ease of manufacture, PBEs are very difficult to detect because they lack a nitro (NO2) group which by contrast makes nitro-based explosives (NBEs) easy to detect by mass spectrometry, and they also lack absorbance in the UV. Several detection methods for PBEs and H2O2 have been described in a review by Burks and Hage.4 These include colorimetric, spectroscopic (IR, Raman, luminescence, fluorescence) and electrochemical methods. However, these techniques are more suited to laboratories and the authors emphasised the need for portable or handheld devices such as test strips for the field detection of PBEs and their precursors. PBEs are volatile and generate a high vapour pressure7 under ambient conditions and therefore detection methods can be developed to detect H2O2 in the vapour, with the use of trained sniffer dogs being reported.8 Simple portable devices that are selective and sensitive to H2O2 vapour would be ideal for the rapid detection of PBEs at public places like airports and train stations.
Progress in the development of rapid colorimetric methods for the detection of H2O2 vapours have been made by Mills9 and Suslick.10 Mills used a single green/blue azo dye Lissamine Green (LG) dissolved in polyvinyl alcohol (PVA) which was rapidly bleached in the presence of H2O2 vapours. However, chlorine (Cl2), nitrogen dioxide (NO2) and ozone (O3) also produced bleaching of LG indicating non-selectivity to H2O2. By using a combination of sixteen dyes in an array, Suslick was able to show selectivity to H2O2 vapours with detection limits below 2 ppb. However, a flatbed scanner is needed to analyse the array and the need for so many dye formulations is also undesirable.
The bleaching of the azo dyes Calmagite, Orange G and Orange II using in situ generated H2O2 has been described.11 These results show that at pH 8.0, the o,o-dihydroxy dye Calmagite is rapidly bleached but the monohydroxy azo dyes Orange II and Orange G (Fig. 2) are not bleached, or their reactions are very slow.
When using added H2O2, Orange G and Orange II are rapidly bleached at pH 9.0 in the presence of added sodium carbonate (Na2CO3). It has been suggested that this is due to the in situ generated peroxycarbonate ion (HCO4−), a more potent oxidising agent,12–14 formed (eqn (1)) from the reaction of H2O2 with bicarbonate (HCO3−).
| H2O2 + HCO3− → HCO4− + H2O | (1) |
However, Fridovich15 argues that it is CO2 and not HCO3− that is the enhancing species and that it is the carbonate radical (CO3−˙) not HCO4− that is responsible for the oxidative degradation of the dye. This work provides some evidence to support the involvement of CO2/CO3−˙. In any case, it should be possible to selectively detect H2O2 vapours from a suitable combination of the bleaching of Calmagite at pH 8.0 (EPPS), and Orange G and Orange II at pH 9.0 (Na2CO3), with a lack of bleaching of Orange G and Orange II at pH 8.0 (EPPS), especially in the presence of the complexing agent ethylenediaminetetraacetic acid (H4edta). In the case of Cl2, NO2 and O3, no discrimination would be expected thus providing selectivity to H2O2 and PBE vapours. These colour tests can be used in combination with the use of aqueous, acidified, titanium(IV) which is known to form a bright yellow-orange coloured complex,16, [Ti(O2)(OH)(H2O)3]+ with solutions containing H2O2 (eqn (2)) due to a ligand-to-metal charge transfer (LMCT).17
| [Ti(OH)3(H2O)3]+ + H2O2 → [Ti(O2)(OH)(H2O)3]+ + 2H2O | (2) |
000–186
000, 99+% hydrolysed]. Square (22 mm) borosilicate glass plates were used to provide a transparent substrate for the inks. De-ionised water (ELGA Purelab) was used in all experiments. Filter papers were purchased from Whatman (No. 1). Hydrogen peroxide solutions were prepared from the dilution of 30% (w/w) aqueous H2O2 stock solutions. Aqueous titanium(IV) in sulfuric acid (10%) was prepared according to reported methods.18 Nitrogen dioxide was generated by the dropwise addition of concentrated HNO3 onto copper turnings while chlorine gases was generated by the dropwise addition of concentrated HCl on to MnO2; ozone was generated via an O2 cylinder using a Wallace & Tiernan Type BA.023 laboratory ozonator with the voltage set at 200 V and with O2 gas at a flow rate of 150 L h−1. All three gases were separately fed into desiccators containing filter papers or ink coated plates.
The methodology adopted of coating PVA first on to glass plates and then the dye inks onto PVA was adopted because when solid Calmagite was added to the PVA solution (using the method by Mills9), the ink would solidify immediately which made application of the ink to the glass plates very difficult. As soon as both layers were applied they mixed naturally. Dissolving the dye in aqueous solution first and then mixing it with the PVA also worked. All three methods were tried and gave comparable results. Keeping the dye solution and PVA separate meant a much longer shelf life for the ink components.
This would form the basis for the selective detection of H2O2 vapours as the rationale is that only in the presence of H2O2 can HCO4− or CO3−˙ be generated in situ and this is required for the oxidative degradation of O G and O II. It should also be noted that the rate of bleaching of O G and O II in the presence of sodium carbonate (Na2CO3) is pH dependent, with the rate of bleaching at pH 8.0 being very slow.
After exposure to H2O2 vapours from solutions containing 0.50 M or 5.0 M H2O2 for 24 h in shallow petri dishes (Fig. 5) under ambient conditions, the Calmagite disks were almost completely bleached (purple to pale pink), the O G pH 9.0 disks were completely bleached (yellow-orange to colourless) and the O II pH 9.0 disks were partially bleached (dark orange to light orange), with the 5.0 M H2O2 vapour disk exhibiting more bleaching than the one exposed to 0.50 M H2O2. In contrast, the O G and O II disks at pH 8.0 showed no bleaching.
Control experiments with pure water rather than aqueous H2O2 showed no bleaching of any of the disks indicating that bleaching was due to H2O2 vapours and not degradation of the dye through environmental exposure. These results are consistent with the aqueous solution studies and indicate pH selective bleaching of the O G and O II azo dyes which in combination with the bleaching of Calmagite and the formation of a yellow colour (Fig. 5, centre) of [Ti(O2)(OH)(H2O)3]+ peroxo complex with Ti(IV) provide a potentially useful way to distinguish H2O2 vapours from other chemical vapours.
Fig. 6 shows the effect of exposure of the filter papers to Cl2(g), NO2(g)and O3(g) for 24 h under ambient conditions.
It is immediately clear the bleaching results are very different to those with H2O2 vapours. With Cl2(g) all the azo dye disks are fully bleached, with the exception of O II at pH 8.0 and pH 9.0 which are ∼95% bleached and no reaction with Ti(IV) is discernible. In the case of NO2(g), all the azo dye disks are partially bleached with the exception of O II at pH 8.0 where there appears to be only partial bleaching and again there appears to be no reaction with Ti(IV). Lastly, with O3(g) there is only partial bleaching of the azo dyes (with the change of Calmagite being the most distinctive) and with the Ti(IV) disk there is a definite yellowing which could in isolation give a false positive for H2O2 vapours. This may be caused by the formation of a Ti(IV)–O3 complex which is also yellow or the catalysed reduction of O3 to H2O2, with the subsequent formation of the Ti(IV)-peroxo complex (eqn (2)). These somewhat surprising results with O3 were reproducible.
The sensitivity of Ti(IV) to aqueous H2O2 and H2O2 vapours is shown in Fig. 7 where concentrations as low as 0.010 M (∼3 ppm) can be detected and may be used to estimate the concentration of H2O2 vapour.
These experiments were repeated using Cl2(g), NO2(g) and O3(g) (Fig. 9).
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| Fig. 9 Images of films (a) before and after exposure to vapours from (b) Cl2(g), (c) NO2(g) and (d) O3(g). | ||
Again it is clear that results with these three gases are very different to those of H2O2. The most dramatic dye bleaching is observed with NO2(g), with no change in the Ti(IV) film. Most surprisingly, O3(g) shows virtually no bleaching of the azo dyes but there is a colourisation of the Ti(IV) plate suggesting that the yellowing of Ti(IV) is not selective to H2O2. In the case of Cl2(g) rapid bleaching of Calmagite and O G at pH 8.0 is observed, while the bleaching of the other azo dyes is much slower, with no change in colour of the Ti(IV) plate.
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| Fig. 10 The absorption spectrum of a Calmagite film at pH 8.0 before (blue) and after (red) exposure to vapours for 10 min from a 5.0 M (∼15%) aqueous solution of H2O2. | ||
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| Fig. 11 The absorption spectrum of a Orange G film at pH 8.0 during exposure to vapours at 10 min intervals from a 5.0 M (∼15%) aqueous solution of H2O2. | ||
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| Fig. 12 The absorption spectrum of an Orange G film at pH 9.0 during exposure to vapours at 10 min intervals from a 5.0 M (∼15%) aqueous solution of H2O2. | ||
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| Fig. 13 The absorption spectrum of an Orange II film at pH 8.0 during exposure to vapours at 10 min intervals from a 5.0 M (∼15%) aqueous solution of H2O2. | ||
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| Fig. 14 The absorption spectrum of an Orange II film at pH 9.0 during exposure to vapours at 10 min intervals from a 5.0 M (∼15%) aqueous solution of H2O2. | ||
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| Fig. 15 Normalised absorption spectrum of a Ti(IV) film before (blue) and after (red) exposure to vapours from a 5.0 M (∼15%) aqueous solution of H2O2. | ||
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| Fig. 16 A plot of ΔAbs490 against time for the Orange II film at pH 9.0 during exposure to vapours from a 5.0 M (∼15%) aqueous solution of H2O2. | ||
The most rapid (within 5 min) and distinctive bleaching is with the dark purple Calmagite dye and this in itself provides a rapid (but non-selective) indication of the presence of oxidising vapours.
| MnII + H3CAL ⇌ [MnII(CAL)]− + 3H+ | (3) |
| [MnII(CAL)]− + 1½H2O2 → [MnIII(CAL)(O2H)]− + H2O | (4) |
| [MnIII(CAL)(O2H)]− → oxidised CAL → CO2 + H2O + N2 | (5) |
This is similar to the mechanism proposed for the oxidative degradation of Calmagite using in situ generated H2O2, where EPR solution studies suggested the presence of MnIII but no MnIV
O species.11 Under these conditions (pH 8.0 and in the absence of sodium carbonate), O G and O II are bleached only very slowly, presumably because they only weakly coordinate to MnII. At pH 9.0 (Na2CO3), rapid bleaching of O G and O II was observed in solution and on filter papers but the reactions were more sluggish with the inks coated on to PVA coated borosilicate glass plates. The oxidative degradation of O II by peracetic acid catalysed by the oxo-bridged [Mn2III/IV(μ-O)2(bpy)4](ClO4)3 complex and its mononuclear analogue [MnII(bpy)2Cl2] have been studied by van Eldik et al. who proposed that the reaction proceeds via the in situ formation of HCO4−/HOOCO2− which on coordination to MnII results in the formation of MnIV
O (Scheme 2).14 In this proposed mechanism there is a requirement for at least weak binding of O II to the manganese centre to effect its oxidative degradation. Yin has proposed a different mechanism for the HCO3− activated H2O2 oxidative degradation of methylene blue using supported CoII that involves the carbonate radical (CO3−˙) and possibly singlet dioxygen (1O2).20 The involvement of the CO3−˙ is also supported by Fridovich in which the terminal step would involve a one-electron oxidation of the organic substrate (SH) leading to its oxidative decomposition (eqn (6)).15
| CO3−˙ + SH → HCO3− + S˙(→ CO2 + H2O + N2) | (6) |
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| Scheme 2 Mechanism proposed by van Eldik et al. for the MnII catalysed oxidative degradation of Orange II (SH) by H2O2 in the presence of carbonate buffer at pH 8–9. | ||
While the formation of CO3−˙ can be thought to be easily generated from the one-electron oxidation of HCO3− coordinated to MnIII or MnIV species, Fridovich intriguingly suggests that the presence of CO2 may enhance the MnII catalysed peroxidation of a substrates by the following mechanism (eqn (7)–(10)).
| MnII + H2O2 ⇌ [MnIV(O)]2+ + H2O | (7) |
![]() | (8) |
| MnIV + CO2 ⇌ MnIII + CO2+ | (9) |
| CO2+ + HO− ⇌ CO3−˙ + H+ | (10) |
It can be argued that the presence of CO2 displaces the equilibrium of reaction (7) to the right by consuming [MnIV(O)]2+ and this enhances the rates of consumption of both MnII and H2O2 and regenerates MnIII. While it may seem strange that CO2 is more readily oxidised than HCO3−, Fridovich argues that as well as an uncharged linear molecule, an alternative resonance form that can exist for CO2 is one with one oxygen atom positive and the other negative (Scheme 3).21
In this case the loss of an electron from the negative oxygen atom yields CO2+ and this may explain why CO2 is more readily oxidised than HCO3−. This result would explain the sluggish bleaching of O G and especially O II inks deposited on an impermeable PVA/borosilicate plate, which is somewhat off-set by the favourable polar environment created by the PVA, while on porous filter paper the reactions are slow but not inhibited.
More work is needed to produce a commercially viable system, especially in making the colour change with O G and especially O II at pH 9.0 clearer and more rapid, while also attempting to completely inhibit the reactions at pH 8.0. From both a theoretical and practical point of view, it would also be useful to investigate the role of CO2 in the reactions of O G and especially O II at pH 9.0. The use of O II being a much darker shade of orange could potentially be a more useful dye to use than O G in any detection system. One attractive feature of this method is the inexpensive materials that are used and the ease of making the substrate solutions and inks. Indeed, work in these laboratories has shown that EPPS buffer, a somewhat expensive biological buffer, can be replaced by phosphate buffer for the pH 8.0 dye solutions, thus reducing the cost even further.
Footnotes |
| † Graduated in chemistry from Queen Mary, University of London in 2013 with a 1st class honours. |
| ‡ Graduated in chemistry with forensic science from Queen Mary, University of London in 2012 with a 1st class honours. |
| This journal is © The Royal Society of Chemistry 2014 |