Xianghe Zhanga,
Chenxi Zhang*b,
Xiaomin Suna,
Jiaoxue Yanga and
Chen Zhu*c
aEnvironment Research Institute, Shandong University, Jinan 250100, P. R. China
bDepartment of Biological and Environment, Binzhou University, Binzhou 256600, P. R. China. E-mail: sdzhangcx@163.com
cShandong Province Environmental Monitoring Center, Jinan 250013, P. R. China
First published on 18th June 2019
Benzoic acid (BA) is one of the most common organic acids in the Earth’s atmosphere and an important component of atmospheric aerosol particles. The reaction mechanism of OH, NO3 and SO4− radicals with BA in atmospheric water droplets and that of OH radicals with BA in the atmosphere were studied in this paper. The results show that in atmospheric water droplets the potential barriers of the elementary addition reactions of BA with OH radicals are lower than those of elementary abstraction reactions, and the potential barriers of OH-initiated reactions are less than for NO3 and SO4− reactions. The initiation reactions of OH radicals and BA are exothermic, but the abstraction reactions of NO3 and SO4− are endothermic processes. Among the products, 6-hydroxybenzoic acid (6-HBA) and 4,6-dihydroxybenzoic acid (4,6-DHBA) are the most stable, while 3-hydroxybenzoic acid (3-HBA) and 3,5-dihydroxybenzoic acid (3,5-DHBA) are much less stable and, thus, much less abundant compared to 6-HBA and 4,6-DHBA. The initiation and subsequent degradation of BA with OH radicals in the gas phase were calculated. The products of addition and abstraction reactions of BA with OH radicals can be further oxidized and degraded by O2/NO. According to the results of kinetic calculations, the total reaction rate constant of OH radicals with BA at 298.15 K in atmospheric water droplets is 2.35 × 10−11 cm3 per molecule per s. The relationship between reaction rate constants, temperature and altitude were also investigated and discussed in the present study.
The steam of BA may irritate the skin, eye and upper respiratory tract, and it has a toxic effect upon long term exposure to the human body. Studies have shown that the stabilizing efficiency of some organic acids appears to be close to or higher than NH3, which can contribute to the aerosol nucleation process by binding to H2SO4.9,10 BA can work as a catalyst to enhance the nucleation of H2SO4, which has been verified by experimental and theoretical research.11,12 Thus, the study of the chemical behavior of BA can help to analyze similar atmospheric processes.
Electrosorptive removal of BA was used in experimental research. With the development of the photo-Fenton oxidation and catalyst process, photocatalytic degradation of BA has been widely used. Aerobic and anaerobic microorganisms, like Burkholderia xenovorans and Thauera aromatica, were used to degrade BA through different methods.13,14 Moreover, the use of the OH radical is an effective method to remove organic contaminants. BA existing in atmospheric water droplets is mainly derived from the photodegradation process of various organic compounds in the atmosphere or by volatilisation with water vapor into the atmosphere. In the atmosphere, a variety of free radicals can be used for the removal of organic compounds.15,16 OH radical, an important atmospheric oxidant,17 plays a significant role in the conversion and removal of air pollutants.18,19 Besides, in a water droplet, the concentration of O2 is smaller than in the atmosphere, therefore, we only consider the participation of O2 in the gas phase.
Several studies have reported on the degradation of BA by OH radicals.20,21 As a strong oxidant, OH radicals are useful, common and fast when compared with other radicals.22 These research results are generally carried out through experiments to study the reaction process between OH radicals and BA.23 Determination of the products and intermediates is used to speculate upon the reaction process. A kinetic model is built to simulate the system behavior. The changing variables in the reaction are controlled to account for their effects on the degradation rate of the reaction, such as the difference between the photoelectrocatalytic degradation and photocatalytic degradation of BA, the pH or wavelength, the concentration of BA and the properties of the catalyst. As a result, a first order reaction kinetic equation is established to obtain the reaction rate constant.21,24 Studies have used heat-activated persulfate to produce SO4− radicals, and through their oxidative properties, BA undergoes decarboxylation and hydroxylation reactions to achieve degradation.25 In previous studies there were also degradation reactions using SO4− radicals and BA derivatives such as benzoate, and their reaction products were detected.26 At night, NO3 radicals can be used as an important oxidant to degrade atmospheric organic pollutants.27 Therefore, we can study the reaction of NO3 in the degradation of BA.
Using quantum chemistry methods, the specific processes and mechanism of the reaction can be explored and the rate constant of the reaction can be calculated. In this paper, the mechanism of the production of hydroxybenzoic acids and the initiated reactions of BA with NO3 and SO4− radicals in atmospheric water droplets, as well as the reaction of BA with OH radicals in the atmosphere, were studied by MPWB1K density functional theory. Then, the rate constants of the elementary reactions were calculated using transition state theory, which can provide useful data for further study.
k(T) = Aexp(−Ea/RT), | (1) |
The reactions pathways of BA and OH radicals are shown in Fig. 1 and 2, and the atom labels of carbon sites are also indicated. In addition, transition states (TS), intermediates (IM), the reaction potential barriers (ΔEb) and reaction energy (ΔEr) are labeled for convenience. Meanwhile a & b show the two pathways; the unit of energy is kcal mol−1.
Fig. 1 Reaction pathways for the abstraction and addition reaction of BA with OH radicals in atmospheric water droplets. |
Fig. 2 Reaction pathways for the addition and abstraction reaction of BA with OH radicals in atmospheric water droplets. |
In other carbon sites of the benzene ring, the reaction processes are similar. The OH radical is close to the hydrogen atom in the benzene ring and forms the transition state TS; meanwhile, the hydrogen atom vibrates between the OH radical and the original carbon atom. After the hydrogen atom is abstracted, the formation of intermediate IM and the loss of a molecule of H2O has a potential barrier of 7.35–8.56 kcal mol−1 and releases 2.86–3.95 kcal mol−1 of heat. Then, another OH radical is close to the carbon atom which has lost the hydrogen atom and through the transition state TS, monohydroxybenzoic acid (MHBA) is formed. These processes have potential barriers of 2.63–3.56 kcal mol−1 and release reaction heats from 112.91 to 118.62 kcal mol−1. As shown in Fig. 1, the potential barriers in the process of intermediate generation at the ortho-position reaction, 6-hydroxybenzoic acid (6-HBA), and the meta-position, 3-hydroxybenzoic acid (3-HBA), are smaller, while those of the para-position reaction, 4-hydroxybenzoic acid (4-HBA), is relatively larger.
The meaning of each symbol in the following Figures is similar to those of Fig. 1, as well as the atom labels of carbon sites. After optimization of the products and energy comparison, the products with the lowest energy in two pathways were consistent. There are 10 kinds of dihydroxy addition reaction products, and these are shown in Fig. 3. For these reactions, the two pathways to form the product DHBA are described in the ESI.†
The potential barriers of elementary addition reactions are smaller than the elementary abstraction reactions, and the released heat of the addition-initiated reactions is also less than that of the abstraction-initiated reactions. Besides, in the abstraction-initiated reactions, the potential barrier to finally get 4,6-DHBA is the smallest, 7.30 kcal mol−1; while that to finally produce 3,4-DHBA is the biggest, 9.08 kcal mol−1. In the addition initiated reactions, the potential barrier to finally get 3,4-DHBA is the smallest, 0.06 kcal mol−1; while that to finally produce 4,5-DHBA is the biggest, 4.68 kcal mol−1.
Fig. 4 Reaction pathways for the abstraction reaction of BA with NO3 radicals in atmospheric water droplets. |
Taking the reaction at the C2 site as an example, the O atom with a single electron on the NO3 radicals is close to the H atom, the C–H bond is broken and then the H–O bond is formed. The reaction is endothermic and requires 4.41 kcal mol−1 of energy, and this reaction needs a slightly higher barrier of 13.43 kcal mol−1. The reactions at the C3, C4, C5 and C6 sites are similar to the C2 sites; the reaction potential barriers are 12.05 to 13.64 kcal mol−1. All the reactions are endothermic and the reaction energies are 3.87 to 4.97 kcal mol−1. In these reaction pathways, the reaction potential barriers in the meta-position are lowest and the reactions in the ortho-position are the highest.
Fig. 5 Reaction pathways for the abstraction reaction of BA with SO4− radicals in atmospheric water droplets. |
The reaction at the C2 site has a reaction potential barrier of 16.44 kcal mol−1, and the reaction needs to absorb 6.99 kcal mol−1 of energy. The reactions at the remaining carbon sites are all similar and endothermic. The reaction potential barriers are 14.89–16.84 kcal mol−1. Comparing the energy changes of the reaction process, the reaction potential barriers of the para-position and meta-position reactions are lower, and in the ortho-position reactions they are relatively higher.
Fig. 6 is about the abstraction reactions and the subsequent reactions of BA and OH radicals in the atmosphere. The two reactions can generate the intermediates IM1g and IM5g with a single electron, and release 2.10 and 1.97 kcal mol−1, respectively. Meanwhile, the reaction potential barriers are slightly smaller than those in the liquid phase (7.34 and 7.82 kcal mol−1). Then, the intermediates can further react with O2 and NO, and this process will release energy. After these reactions, a molecule of NO2 is removed. The reactions need to cross 18.54 and 19.00 kcal mol−1 of energy, and release 13.30 and 12.91 kcal mol−1 of energy, respectively. These products respectively have an oxygen atom with a single electron and thus can combine with water in the atmosphere to generate MHBA and OH radical. This reaction is an endothermic reaction, and the reaction potential barriers are slightly higher (27.16 and 26.85 kcal mol−1, respectively).
As for the addition reaction of OH radicals with BA in the atmosphere, the reaction potential barrier to get IM1g′ is also lower than that in the liquid phase, only 1.53 kcal mol−1, and this reaction will release 17.54 kcal mol−1 of energy. After the addition reaction in the benzene ring, due to the substituent positioning effect, the density of the electron cloud changes and affects the conjugation effect, which makes the further ortho and para-position addition reactions of the OH group on the benzene ring easier. In addition, the reaction energy of different carbon sites are significantly different. The reaction heat and reaction potential barriers of C2, C3, C4 and C6 sites are given in Fig. 7.
In the corresponding subsequent meta-reactions, the reaction of IM1g′ with O2 is an exothermic reaction with no reaction potential barrier and releases 0.63 kcal mol−1. The addition reaction of NO and IM7g′ results in an intramolecular cyclization reaction, with the C2 and C4 bonds on the benzene ring, then obtains a five-membered ring; this reaction generates more heat than other sites (64.65 kcal mol−1). When a molecule of NO2 is removed, the C–C bond between C2 and C3 is broken, and the O–O bond is also disconnected. In product IM9g′, there is an aldehyde group at the C3 site, and the energy that must be crossed is slightly lower than other reactions (18.94 kcal mol−1), while the energy released is slightly higher, 22.16 kcal mol−1.
In the relative ortho-position reaction of OH radicals, the reaction products IM2g′, IM10g′ and IM13g′ are exothermic (releasing energies of 49.77, 48.99, and 51.66 kcal mol−1, respectively), and then the reactions of the peroxide group with NO and H2O take place. The following reaction processes involve the nitrogen atom in NO attacking the terminal oxygen atom and then removing one molecule of NO2. The NO addition reaction is an exothermic reaction. The energy generated by these three intermediate products is less than those of the O2 addition reaction, which are 18.75, 19.95 and 19.30 kcal mol−1, respectively. The NO2 removal reactions are slightly different. The corresponding ortho-position reactions are exothermic, with reaction potential barriers of 29.72 and 32.65 kcal mol−1, respectively. An epoxy group is formed on the benzene ring of the final reaction products. Meanwhile the reaction of the corresponding para-position reaction is endothermic, and the reaction potential barrier is slightly higher than that of the ortho-reactions, which is 38.27 kcal mol−1. The oxygen with a single electron in the product can react with H2O in the atmosphere and extract the hydrogen in the H2O to give the products IM5g′ and an OH. This reaction is endothermic (10.61 kcal mol−1). After that, it will extract two hydrogen atoms from the C5 and C2 sites on the benzene ring by OH radicals to give the final product DHBA. These two reactions both release a large amount of heat (49.17 and 93.54 kcal mol−1), but the reaction potential barriers are not high (1.52 and 0.92 kcal mol−1, respectively).
The kinetic data for the elementary reactions of BA and OH radicals are shown in Table 1. The rate constants for the abstraction reactions of the ortho-position, meta-position and para-position shown in Fig. 1 are 4.44 × 10−15, 1.23 × 10−13, 3.63 × 10−15, 4.80 × 10−14 and 1.77 × 10−13 cm3 per molecule per s, respectively. The rate constants for the addition reactions of the ortho-position, meta-position and para-position shown in Fig. 2 are 1.15 × 10−12, 1.3 × 10−11, 6.65 × 10−13, 3.53 × 10−12 and 4.79 × 10−12 cm3 per molecule per s, respectively. The total rate constant is 2.35 × 10−11 cm3 per molecule per s at 298.15 K, which corresponds well with the value of 4.22 × 10−11 cm3 per molecule per s.34
Reactions | k298.15 K | Arrhenius formulas | R2 |
---|---|---|---|
R + OH → IM1a + H2O | 4.44 × 10−15 | 3.31 × 10−10exp(−3330.7/T) | 0.9991 |
R + OH → IM2a + H2O | 1.23 × 10−13 | 1.10 × 10−9exp(−2697/T) | 0.9970 |
R + OH → IM3a + H2O | 3.63 × 10−15 | 2.36 × 10−10exp(−3298.2/T) | 0.9992 |
R + OH → IM4a + H2O | 4.8 × 10−14 | 1.71 × 10−9exp(−3114.2/T) | 0.9993 |
R + OH → IM5a + H2O | 1.77 × 10−13 | 9.54 × 10−9exp(−3233.7/T) | 0.9993 |
R + OH → IM1b | 1.15 × 10−12 | 3.24 × 10−10exp(−1672/T) | 0.9996 |
R + OH → IM2b | 1.3 × 10−11 | 2.89 × 10−10exp(−914.34/T) | 0.9995 |
R + OH → IM3b | 6.65 × 10−13 | 2.73 × 10−10exp(−1783.3/T) | 0.9998 |
R + OH → IM4b | 3.53 × 10−12 | 1.74 × 10−9exp(−1837.6/T) | 0.9996 |
R + OH → IM5b | 4.79 × 10−12 | 2.45 × 10−9exp(−1849.1/T) | 0.9996 |
Total | 2.35 × 10−11 |
The atmospheric lifetimes of the reactants can be calculated and analyzed according to the rate constants of the elementary reactions. For the average OH radical concentration of 9.7 × 105 molecule cm3, the atmospheric lifetimes (τ) can be calculated by τ = 1/(kOH[OH]), from which the lifetime of BA in the atmosphere is determined to be 0.51 days.38
In the troposphere, the temperature decreases as the altitude increases, as well as the reaction rate constant. At the bottom of the stratosphere, the temperature varies little with the altitude, and the rate constant also increases slowly. At the upper side of the stratosphere, the temperature increases with altitude, as does the rate constant.
(1) Among the products of MHBA and DHBA, 6-HBA and 4,6-DHBA have the lowest energy. By comparing reaction potential barriers and reaction heat, it was found that the reaction of OH radicals with BA is easier than that of NO3 and SO4− radicals. In the gas phase, the intermediate which initiates the reaction can be further reacted with O2/NO, and hydroxybenzoic acid can be obtained.
(2) The total reaction rate constant of OH radicals and BA is 2.35 × 10−11 cm3 per molecule per s, and the elementary reaction rate constants of the hydrogen atom abstraction reactions are smaller than those of addition reactions. The lifetime of BA in the atmosphere is determined to be 0.51 days.
(3) The reaction rate constants increase with the increasing temperature. At the bottom of the troposphere and the top of the stratosphere, the temperature is relatively higher, and the reaction constants of the BA with OH radicals are also higher.
Footnote |
† Electronic supplementary information (ESI) available: Mechanism and kinetic study on the reaction of benzoic acid with OH, NO3 and SO4− radicals in the atmosphere. See DOI: 10.1039/c9ra02457c |
This journal is © The Royal Society of Chemistry 2019 |