Article
Mechanistic Insight into the Reactivity of Chlorine-derived Radicals in the Aqueous-phase UV/chlorine Advanced Oxidation Process: Quantum Mechanical Calculations Daisuke Minakata, Divya Kamath, and Shaye Maetzold Environ. Sci. Technol., Just Accepted Manuscript • Publication Date (Web): 25 May 2017 Downloaded from http://pubs.acs.org on May 28, 2017
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Mechanistic Insight into the Reactivity of Chlorine-derived Radicals in the Aqueous-
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phase UV/chlorine Advanced Oxidation Process: Quantum Mechanical Calculations
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Prepared for Environmental Science and Technology
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Daisuke Minakata*1, Divya Kamath1, Shaye Maetzold1
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1
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Michigan Technological University
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1400 Townsend Drive, Houghton, Michigan 49931
Department of Civil and Environmental Engineering
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*Corresponding author. Phone: +1-906-487-1830; fax: +1-906-487-2943; Email address:
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[email protected] 16 17
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Abstract
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The combined ultraviolet (UV) and free chlorine (UV/chlorine) advanced oxidation
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process that produces highly reactive hydroxyl radicals (HO•) and chlorine radicals (Cl•)
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is an attractive alternative to UV alone or chlorination for disinfection because of the
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destruction of a wide variety of organic compounds. However, concerns about the
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potential formation of chlorinated transformation products require an understanding of
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the radical-induced elementary reaction mechanisms and their reaction rate constants.
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While many studies have revealed the reactivity of oxygenated radicals, the reaction
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mechanisms of chlorine-derived radicals have not been elucidated due to the data scarcity
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and discrepancies among experimental observations. We found a linear free energy
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relationship between the quantum mechanical (QM) calculations of the free energies of
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reaction and the literature-reported experimentally measured reaction rate constants, kexp,
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for 22 chlorine-derived inorganic radical reactions in the UV/chlorine process. This
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relationship highlights the discrepancy among literature-reported rate constants and aids
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in the determination of the rate constant using QM calculations. We also found linear
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correlations between the theoretically calculated free energies of activation and kexp for
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31 reactions of Cl• with organic compounds. The correlation suggests that H-abstraction
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and Cl-adduct formation are the major reaction mechanisms. This is the first
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comprehensive study on chlorine-derived radical reactions, and it provides mechanistic
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insight into the reaction mechanisms for the development of an elementary reaction-
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based kinetic model.
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Introduction
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Ultraviolet combined with free chlorine (UV/chlorine) that produces highly reactive
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hydroxyl radicals (HO•) and chlorine radicals (Cl•) at ambient temperature and
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atmospheric pressure is one of the attractive aqueous-phase advanced oxidation processes
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(AOPs).1-3 UV/chlorine can serve as an alternative AOP to UV with hydrogen peroxide
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because of the utilization of the existing chlorination process or as an alternative to the
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UV process alone for the disinfection of pathogens and the destruction of dissolved
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organic compounds by both HO• and Cl•.4 Previous studies indicated the different degree
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of contribution of initial reaction of Cl• with a target compound to the overall
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degradation.5-7 In addition, chlorine residue after the UV/chlorine AOP can be used as a
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secondary disinfectant, rendering this process suitable for the application of drinking
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water treatment as well as wastewater reclamation for direct potable reuse.
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In the aqueous-phase UV/chlorine AOP, photolysis of hypochlorous
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acid/hypochlorite ions (HOCl/OCl-) generates HO• and Cl• radicals,8,9 which react with
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target organic compound(s) as well as with HOCl/OCl-. These highly reactive HO• (2.73
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V vs. SHE)10 and Cl• (2.43 V) radicals transform organic compounds into various
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degradation byproducts via complicated radical-involved reactions. In addition, chloride
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ions (Cl-) generated by the reaction of Cl• with HOCl/OCl- further react with Cl• to
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produce dichlorine radicals (Cl2•-, 2.13 V) that may react with organic compound(s). The
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reactions of HO• and Cl• with HOCl/OCl- produce oxychlorine radicals (ClO•, 1.39 V)
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whose reactivity with organic compounds is not well understood.5,7,11 Consequently, the
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involvement of various chlorine species raises serious concerns about the potential
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formation of toxic degradation byproducts, such as chlorinated byproducts.12,13 Given
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that there are many organic compounds in commercial use and production,14 the
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development of a kinetic model that can predict the fate of degraded organic compounds
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is needed for the preliminary design and screening of a number of these compounds.
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This type of predictive kinetic model requires three components: (1) the identification of
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reaction pathways; (2) the prediction of reaction rate constants, and (3) the numerical
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solution of ordinary differential equations (ODEs) for each species. Once the ODEs are
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numerically solved, the time-consequent concentration profiles of each species can be
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predicted.
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Although HO•-induced initial degradation pathways of organic compounds have
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been studied over the past several decades15,16 and predicting the degradation byproducts
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for small molecular weight aliphatic compounds and alkenes has become feasible,17 the
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reaction mechanisms in the UV/chlorine AOP are not well understood. For example,
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literature-reported experimentally obtained reaction rate constants (kexp) for the reaction
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of HO• with HOCl vary from 104 to 109 M-1s-1.3,18,19 This rate constant significantly
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affects the calculations of the concentration profile of subsequent byproducts because
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HOCl is dominantly present near a neutral pH (i.e., the pKa of HOCl is 7.5).20 Among
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approximately 30 kexp studies on Cl•,21 for saturated aliphatic compounds, some claim that
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a single electron transfer (SET) is the major Cl• reaction, but others find that
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hydrogen(H)-atom abstraction from a carbon-hydrogen (C-H) bond is the major
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reaction.22-25 These inconsistencies cause difficulties in defining the reaction products
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(e.g., carbon-centered radical vs. alkoxyl radical) of each elementary reaction (e.g.,
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carbon-centered radical from H-abstraction vs. radical cation or Cl-adduct from SET).
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Furthermore, while HO• predominantly attacks the α–position of organic compounds,26 it
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is unclear whether chlorine-derived radicals selectively react with specific sites of organic
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compounds. This reactivity can affect the branching ratio of reaction pathways and the
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estimation of the byproducts.
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Ab initio quantum mechanical (QM) calculations are robust techniques to identify
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elementary reaction pathways, and they can be used to predict aqueous-phase reaction
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rate constants. Successful applications of these calculations include an identification of
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elementary reaction steps and determining rate constants for HO• reactions with
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phthalate27 and ibuprofen28, as well as those for the formation of N-nitrosodimethylamine
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during ozonation.29 These studies, in general, calculated the aqueous-phase enthalpies
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and free energies of reaction to identify the thermodynamically preferable reaction
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pathways (e.g., ozone30) and free energies of activation for reaction rate constants (e.g.,
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HO• 31-33). While the use of ab initio QM methods can be applied for H-abstraction by
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Cl•, the lack of applicable theory and experimental evidence limits the QM application to
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SET reactions. The Marcus theory34 was used to calculate the aqueous-phase free
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energies of reaction for SET reactions, but significantly higher values were reported
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compared with those for H-abstraction and HO• addition due to the uncertainty of the
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reorganization of water molecules.35
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In this study, we use ab initio QM calculations to identify the dominant reaction
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mechanisms for chlorine-derived radicals to ultimately develop an elementary reaction-
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based UV/chlorine kinetic model. Our hypothesis is that for chlorine-derived radical
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reactions, the theoretically calculated aqueous-phase free energies of reaction (i.e.,
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react ) are linearly correlated with kexp based on a linear free energy relationship ∆Gaq,calc
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(LFER),35 and the theoretically calculated aqueous-phase free energies of activation (i.e.,
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act ) are linearly correlated with kexp based on Eyring’s transition state theory ∆Gaq,calc
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(TST)36 under the same reaction mechanism. Once these correlations are developed, we
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can predict the reaction rate constants for reactions that have not been investigated
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experimentally; these results will be used to solve ODEs for predicting the formation of
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byproducts.
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Materials and Methods
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All of the ab initio molecular orbital and density functional theory (DFT)-based QM
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calculations were performed with the Gaussian 09 revision D.02 program37 using the
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Michigan Tech high performance cluster “Superior”. The electronic structures of the
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molecules and radicals in the ground and transition states were optimized at the level of
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B3LYP/6-31G(2df,p) implemented in Gaussian-4 theory (G4)38 in both the gaseous and
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aqueous phases. The aqueous-phase calculations were performed using an implicit
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polarizable continuum model [universal solvation model (SMD)].39 Previously, we
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verified the combination of G4 with the SMD model by successful application to other
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aqueous-phase radical-involved reactions.40 The Supporting Information provides the
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detailed calculations of the transition state search, the aqueous-phase free energies of
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activation and reaction, and the associated computational methods.
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Results and Discussion
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Reactivity of Chlorine-derived Radicals with Inorganic Radicals
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Table 1 summarizes each elementary reaction in the UV/chlorine AOP, the literature-
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react values at 25 °C and the chemical reaction reported kexp as well as our calculated ∆Gaq,calc
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rate constant (kchem) obtained from the relationship with the diffusion reaction rate
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constant (kD) from kexp (equation 1).
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kexp =
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react We find a LFER between lnkchem and ∆Gaq,calc (Figure 1). With the decrease in the
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react values below -20 kcal/mol, the kchem values became constant at approximately ∆Gaq,calc
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(1.0-2.0) × 1010 M-1s-1 because of the limitation of the diffusion contribution and the
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exothermic reactions caused by the highly hydrolyzed reaction products in the aqueous-
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phase. Our calculated kD values using Smoluchowski’s equation41 (see Supporting
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information) are approximately 1.1 × 1010 M-1s-1 and the upper kexp value is
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approximately 8.0 × 109 M-1s-1; therefore, the kchem value can be estimated as 2.9 × 1010
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M-1s-1, which is close to the observed kchem values in Figure 1. In general, the G4 method
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provides 0.83 kcal/mol of average absolute deviation from the experimentally obtained
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gaseous-phase energy values.38 The SMD model at the various levels of DFT methods
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with a 6-31G* basis set provides mean unsigned errors of 0.6-1.0 kcal/mol in solvation
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free energies for neutral compounds and 4 kcal/mol on average for ions.39 Based on the
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react estimated computational error, ±5.0 kcal/mol of ∆Gaq,calc , corresponding to ±2.8 of
k D kchem kD +kchem
(1)
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lnkchem, it is found that 64% of kexp is within this error from the LFER. Indeed, many
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radical-involved reactions such as addition, SET, and H-abstraction do not follow the
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thermodynamic law, and kinetics may overrun thermodynamics.30 However, our findings
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react indicate that ∆Gaq,calc can be used to predict the rate constants. The LFER can also be
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used to evaluate the series of kexp values systematically and provide critical feedback for
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future experimental studies. In the following section, we discuss each chlorine-derived
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inorganic radical reaction.
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(Table 1 goes here)
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(Figure 1 goes here)
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Reactions with Hypochlorous Acid/Hypochlorite Ions
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While Cl• reacts with both HOCl and OCl- rapidly (i.e., 3.0 × 109 M-1s-1 in reaction 1 and
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8.2 × 109 M-1s-1 in reaction 3)42, there is disagreement among the kexp values for the
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reaction of HO• with HOCl (8.5 × 104 M-1s-1 3, 1.1-1.4 × 108 M-1s-1 19, and 2.0 × 109 M-1s-
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1 18
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H bond of HOCl by Cl• and HO• as 14.7 kcal/mol and 11.8 kcal/mol, respectively. The
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act addition of 1~3 explicit water molecules did not significantly change the ∆Gaq,calc values.
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act The calculated ∆Gaq,calc value is apparently too large for the observed kexp of 108 ~ 109 M-
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1 -1
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act allows the estimation of the kexp value of 8.5 × 104 M-1s-1 to correspond with the ∆Gaq,calc
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act value. Second, the ∆Gaq,calc values for Cl-abstraction by Cl• and HO• are 3.2 kcal/mol
act in reaction 2). First, we calculated ∆Gaq,calc for the H-abstraction reaction from an O-
act s for Cl• because 109 M-1s-1 of kexp corresponds to ~2 kcal/mol of ∆Gaq,calc . This result
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and 8.4 kcal/mol, respectively. However, while the gaseous-phase Cl-abstraction with a
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product of Cl2 was reported53, the experimentally observed product, ClO•, in the aqueous-
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phase is different from Cl2, thus eliminating the possibility of Cl-abstraction. Third, we
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act obtained ∆Gaq,calc values of 4.6 kcal/mol and 7.2 kcal/mol for the formation of the Cl- or
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HO-adduct, respectively, between each radical and the oxygen atom of HOCl. However,
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react our theoretically calculated ∆Gaq,calc values are positive and the adduct formation
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react reactions are not thermodynamically favorable. Finally, the ∆Gaq,calc value for a SET
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between HOCl and Cl• was calculated for the products of ClO• and HCl, and this energy
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is found to be negative (i.e., -5.2 kcal/mol). Consequently, Cl• reacts with HOCl via a
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act , as shown in Figure SET. In this case, the kexp value adheres to the LFER with ∆Gaq,calc
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1. In contrast, HO• does not react with an oxygen or chlorine atom of HOCl via SET.15
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The investigations above lead to the conclusion that H-abstraction from the O-H bond of
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HOCl by HO• is more reasonable, as this mechanism is consistent with the observed
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product (i.e., ClO•). Furthermore, our estimation of kexp for HO• is supported by Curtin-
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Hammett principle54,55 describing that dominant species (i.e., HOCl) in equilibrium with
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OCl- at pH below pKa has lower reactivity with an identical reactant (i.e., HO•)
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compared to that for minor species (OCl-).
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react For the reaction with OCl-, the ∆Gaq,calc values for SET are -23.1 kcal/mol for the
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reaction with Cl• producing •OCl and Cl- and -5.2 kcal/mol for the HO• reaction
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producing •OCl and HO-; therefore, SET for these reactions is thermodynamically
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favorable. This reaction mechanism is verified by the LFER and is consistent with the
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experimental observation.42,43 9
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Reactions with Chlorine-Derived Radicals
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react Cl• reacts with Cl- to produce Cl2•- reversibly. The ∆Gaq,calc for reaction 5 is -13.1
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kcal/mol and adheres to the LFER. Since Cl2•- is a stable radical, the reverse reaction 7 is
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substantially slow (kexp ~105 M-1s-1). Cl2•- is an intermediate species as Cl2•- that
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subsequently reacts with other radicals and undergoes uni-molecular decay. Cl• also
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react reacts with Cl2•- very rapidly to produce molecular chlorine, Cl2, via SET with a ∆Gaq,calc
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value of -37.5 kcal/mol (reaction 8). Molecular chlorine Cl2 is also produced from the
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disproportionation reaction of Cl2•- (reaction 9). A subsequent Cl-Cl bond rupture at
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different sites forms the different products, such as Cl2 or Cl3-. Cl3- produces Cl2 and Cl-
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react via a slightly exothermic reaction with a value of -0.22 kcal/mol for ∆Gaq,calc (reaction
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11). Molecular chlorine also reacts with Cl- to produce stable Cl3- (reaction 6). Because
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the reactions 6 and 11 do not undergo radical-involved single electron transfer, we did
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not include these in the correlation analysis for LFER. Because of the nature of Cl2•-, the
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react reaction of Cl2•- with HO• produces stable HOCl (reaction 10) with a negative ∆Gaq,calc
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value (i.e., -34.5 kcal/mol), which is substantially different from the reaction of Cl• with
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HO•. Finally, we investigated the reactivity of ClO•. In our preliminary non-steady-state
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kinetic simulation of the UV/chlorine system that followed the changes in pH, a
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significant amount of •ClO was produced (10-4 ~10-5 mol/L under typical low-pressure
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UV lamps with 4~5 mgCl2/L in DI water at an approximately neutral pH initially).
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Limited information is available for the reactivity of •ClO with other species.5,7,11 The
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disproportionation reaction of ClO• was reported as (2.5~7.5) × 109 M-1s-1 (reaction
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22).42,43 We identified a thermodynamically stable pathway via an adduct of Cl-O…O-Cl
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react with -8.1 kcal/mol of ∆Gaq,calc , which adheres to the LFER. We propose that O2 and Cl•
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are the primary reaction products and postulate that this Cl• is rapidly hydrolyzed to
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produce •Cl(H2O), as shown experimentally.42 The majority of chlorine-derived radical
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reactions (reactions 5~11 and reaction 22) in the UV/chlorine AOP undergoes either
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radical combination or SET, and these reactions are found to adhere to the LFER in
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Figure 1.
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Formation of •OHCl- and •Cl(H2O)
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The formation of •OHCl- from the reaction of HO• with Cl- (reaction 12) has been studied
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experimentally46,55 and theoretically56-58 due to the intriguing nature of the reactions.
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While the majority of chlorine-derived reactions with other inorganic radials adheres to
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the LFER, the reactions involving •OHCl- do not apparently adhere to this relationship.
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Our attempt here is to identify the thermodynamic properties for reactions 12 by
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examining various solvated states of the •OHCl- species and to determine whether these
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reactions adhere to the LFER.
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The reaction of HO• with Cl- to produce a covalently bonded adduct, Cl- -•OH ,
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react was found to be endothermic with a ∆Gaq,calc value of 2.99 kcal/mol, which is
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inconsistent with the LFER. We added explicit water molecule(s) to hydrolyze Cl• and
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react found that while the ∆Gaq,calc value with one water molecule remained positive (i.e., 3.7
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react kcal/mol), the ∆Gaq,calc values became negative with two (i.e., -1.87 kcal/mol) and three
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explicit water molecules (i.e., -2.4 kcal/mol). The adduct with 2 or 3 explicit water
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molecules has a charge of -0.95 on Cl and 7% of the spin density distribution on Cl with
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the hemi-bonded structure, which is consistent with the ESR observation.46 With this
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react value, reaction 12 adheres to the LFER. Our observations with explicit water ∆Gaq,calc
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molecules are consistent with previous theoretical studies56-58 and highlight the
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importance of including explicit water molecules in calculating the thermodynamic
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properties of Cl- -•OH . For reaction 19, we observed the formation of a covalently
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bonded adduct •Cl(H2O) in the absence or presence of explicit water molecules.
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react values were positive Regardless of the addition of explicit water molecules, the ∆Gaq,calc
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but still adhered to the LFER because of the observed smaller kexp (i.e., ~105 M-1s-1). We
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propose that reaction 19 undergoes hydration where water molecules form new covalent
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bonds to •Cl.
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Reactivity of Chlorine-derived Radicals with Organic Compounds
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Chlorine Radicals
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act react We calculated the ∆Gaq,calc and ∆Gaq,calc values for each elementary reaction with 31
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organic compounds, including 9 alcohols, 5 aldehydes and ketones, 6 carboxylic acids
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and carboxylates, 6 esters and ethers, 2 haloalkanes, 2 alkenes and 1 aromatic compound
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(Table S1 of the Supporting Information).
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Overall, we find linear correlations for H-abstraction from a C-H bond and Cl-
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act act adduct formation between lnkexp and ∆Gaq,calc , respectively (i.e., lnkexp = -0.50 ∆Gaq,calc
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act +20.53 for H-abstraction from 23 organic compounds and lnkexp = -0.95 ∆Gaq,calc + 23.43
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for Cl-adduct formation from 14 alcohols and carboxylic compounds) (Figures 2 and 3).
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The linear correlation results from Eyring’s TST based on quantum and statistical 12
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mechanics using partition functions to quantize energy states of reactants and activated
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intermediates.36 Note that the conventional TST requires an accuracy of ±0.4 kcal/mol of
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act to predict kexp within a difference of a factor of two from the experimental ∆Gaq,calc
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observations, which is analogous to the experimental accuracy of kinetic measurements.
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act Accordingly, the direct calculation of k based on ∆Gaq,calc values is not feasible because
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the estimated computational error resulting from the corresponding QM method exceeds
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the required accuracy. Based on the estimated computational error, ±5.0 kcal/mol of
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act , corresponding to ±2.4 of lnkchem, it was found that 96% of kexp is within this ∆Gaq,calc
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error from the linear correlation for H-abstraction. For Cl-adduct formation, based on the
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act ±5.0 kcal/mol of ∆Gaq,calc , corresponding to ±4.8 of lnkchem , it was found that 100% of
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kexp is within the error from the linear correlation. Therefore, the linear correlations
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developed here are valid within the estimated computational error and can be used to
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predict k for compounds that have not been examined experimentally. Note that we did
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react not observe the LFER based on our calculated ∆Gaq,calc for the reactions with organic
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compounds, most likely because kinetics overrun thermodynamics for these reactions. In
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the following section, we discuss each Cl• reaction with organic compounds.
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(Figures 2 and 3 go here)
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Alcohols
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A total of 9 compounds containing alcohol functional groups were investigated in this
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study. Ninety nine percent of formaldehyde61, 55% of acetaldehyde62, and 0.1% of
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acetone are hydrolyzed to form geminal diols in the aqueous-phase; therefore, hydrated
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act forms of these compounds were included in the alcohol group. The calculated ∆Gaq,calc
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values for H-abstraction from a C-H bond ranged from -4.5 kcal/mol to 5.3 kcal/mol.
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act The experiment-based ∆Gaq,exp values calculated from the Arrhenius kinetic parameters
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are 3.6±1.0 ~ 5.3±1.2 kcal/mol. Notably, both the theoretical calculation and the
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act experimental values had the highest ∆Gaq,exp for methanol. The estimated k based on the
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linear correlation for methanol was 6.0 × 107 M-1s-1, which was more than one order of
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magnitude smaller than the value of kexp. The kexp value for H-abstraction from C-H bond
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at β-position of ethanol also indicated the similar trend. Therefore, we did not include
281
these data points in the correlation. Except for methanol, we observe a linear correlation
282
act between kexp and ∆Gaq,calc obtained from the H-abstraction of all tested alcohols (Figure
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2). Regardless of the addition of 1~3 explicit water molecule(s), no significant changes
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act were observed in the ∆Gaq,calc values for methanol. This finding is probably because
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methanol does not undergo H-abstraction by Cl• but by another reaction mechanism. For
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H-abstraction from the oxygen-hydrogen (O-H) bond of alcohol functional groups, the
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act values ranged from 5.4 kcal/mol to 12.0 kcal/mol, indicating the insignificance ∆Gaq,calc
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react of this reaction. The calculated ∆Gaq,calc values for SET are positive and range from 23.6
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kcal/mol to 27.1 kcal/mol for all the tested alcohols. Consequently, our theoretical
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calculations indicate that SET by Cl• is not thermodynamically favorable.
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Next, we investigated the formation of a Cl-adduct by the reaction of Cl• with the oxygen of alcohol functional groups. This reaction was studied because ab initio QM
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act calculations do not allow the calculation of ∆Gaq,calc for a specific site via SET, although
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act Gilbert (1988) proposed SET for these sites.22 The ∆Gaq,calc values range from 2.3
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kcal/mol to 3.8 kcal/mol, indicating that the formation of the Cl-adduct competes with H-
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atom abstraction reactions; accordingly, another linear correlation is found (Figure 3).
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The investigation here reveals that Cl• forms an adduct with the OH of alcohols and
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subsequently SET is thought to occurs. Note that the data point for methanol is
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consistent with a linear correlation, and Cl-adduct formation is the dominant mechanism
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for methanol.
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act To investigate the selectivity of Cl• for H-abstraction, we compared the ∆Gaq,calc
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act values for longer chain alcohols. The ∆Gaq,calc values at the α- and β-positions of
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ethanol are -2.4 kcal/mol and 4.8 kcal/mol, respectively. This observation agrees with
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the experimentally obtained partial rate constants for ethanol (1.5 × 109 M-1s-1 at the α-
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position and 7.5 × 108 M-1s-1 at the β-position).22 A similar trend was observed for 1-
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propanol and 2-butanol (Table S2 of the Supporting Information). In general, Cl•
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reactions have an earlier transition state with a lower occurrence of bond breaking and a
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contribution from the resonance stabilization of H-abstraction at the α-position in the
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transition state.22 This fact explains why the calculated bond length of carbon-hydrogen
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is significantly shorter than that of the hydrogen-chlorine bond at the transition states.
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Because of this phenomenon, Gilbert proposed the non-selective reactivity of Cl•;22
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however, our calculations do not support this concept. Except for methanol, the
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act values at the α-positions for the other 8 alcohols are much smaller (i.e., -5.3 ~ ∆Gaq,calc
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2.0 kcal/mol). Our observation of the selective Cl• reactivity for H-abstraction can be
315
explained with the bond dissociation energies (BDE) of the C-H bonds in alcohols at
316
various positions25, although the BDE are measured in the gaseous-phase. For example,
317
the BDE of C-H at α- and β-positions in ethanol are 95.8 kcal/mol and 100.7 kcal/mol,
318
respectively.63 Similar trend can be seen for the BDE of 2-propanol (i.e., 91.7 kcal/mol
319
and 94.3 kcal/mol at α- and β-positions, respectively).
320
Aldehydes and Ketones
321
act The ∆Gaq,calc values for H-abstraction for a total of 5 aldehydes and ketones range from
322
0.17 kcal/mol to 7.1 kcal/mol, which are significantly larger values than those for
323
alcohols. These values are consistent with the kexp (i.e., 106~108 M-1s-1). In general, H-
324
abstraction involves a considerable charge separation between the negatively charged
325
chlorine atom and the positively charged hydrogen that is abstracted from a C-H bond in
326
act the transition state.22 As a result, a higher ∆Gaq is required for the reaction to occur.
327
Two reported kexp values for acetone have a large discrepancy (i.e., < 5.0 × 106 M-1s-1 23
328
and (7.8 ±0.7) × 107 M-1s-1 24). We investigated 0.1% of the hydrolyzed form of
329
act acetone,64 but we did not observe a significant difference in the ∆Gaq,calc values compared
330
with those for acetone. We find that a kexp of (7.8 ±0.7) × 107 M-1s-1 is consistent with the
331
linear correlation in Figure 2. It was found that the data point of chloroacetone
332
significantly decreased the linear correlation in Figure 2. It is not clear whether our
333
act or the kexp value caused the significant inconsistency with the correlation for ∆Gaq,calc
334
chloroacetone. Because of this, we did not include chloroacetone in the assessment of the
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act linear correlation in Figure 2. An investigation of the ∆Gaq,calc values for
336
propionaldehyde (i.e., an aldehyde with a longer hydrocarbon branch) indicates that the
337
reactivity at the α-position (6.9 kcal/mol) is slightly higher than that at the β-position (7.1
338
kcal/mol).
339
Carboxylic Acids and Carboxylates
340
A total of six carboxylic compounds including dissociated forms of formate and acetate
341
were evaluated in this study. The dissociated forms of formate and acetate show higher
342
reactivity with Cl• than that of non-dissociated forms by approximately one order of
343
magnitude. Two inconsistent kexp values were reported for formic acid [(1.3±0.1) × 108
344
M-1s-1 23 and (2.8 ±0.3) × 109 M-1s-1 25] and acetic acid [[(3.2±0.2) × 107 M-1s-1 23 and
345
act (1.0±0.2) × 108 M-1s-1 25]. Our ∆Gaq,calc values for H-abstraction from a C-H bond of
346
formate and formic acid are -10.1 kcal/mol and 15 kcal/mol, respectively, and these
347
act values deviate greatly from the linear correlation in Figure 2. The ∆Gaq,calc values for the
348
same reaction for acetate and acetic acid are 0.94 kcal/mol and 5.3 kcal/mol, respectively,
349
act and both values agree with the linear correlation in Figure 2. The ∆Gaq,calc value for
350
act acetic acid is close to the ∆Gaq,exp of 6.7±2.4 kcal/mol.25 Consequently, the dominant
351
reaction mechanism for carboxylic acids/carboxylates, except for formic acid/formate, is
352
H-abstraction from a C-H bond; the same trend was also observed for propionic acid and
353
isobutyric acid.
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To investigate the reaction mechanism for formate and formic acid, we calculated
355
act the ∆Gaq,calc for the Cl-adduct formation of formate and formic acid as 1.4 kcal/mol and 6
356
act kcal/mol, respectively, showing good agreement with the ∆Gaq,exp values (i.e., 3.8±0.48
357
kcal/mol for formate25 and 4.8±1.4 kcal/mol for formic acid25). Similarly, we obtained a
358
act value of 1.2 ~ 6.0 kcal/mol for the Cl-adduct formation for all other tested ∆Gaq,calc
359
carboxylic acids and carboxylates and found a linear correlation, as shown in Figure 3.
360
As was observed for the tested alcohols, Cl• reacts with carboxylic/carboxylate groups
361
via both H-abstraction and Cl-adduct formation. In particular, formate and formic acid
362
undergo Cl-adduct formation dominantly.
363
Esters and Ethers
364
Four of the kexp values for the tested esters show very low reactivity with Cl• (i.e., < 108
365
M-1s-1)24, and one kexp value for the tested diethyl ethers shows a much larger value of
366
(1.3±0.1) × 109 M-1s-1.25 This simple comparison implies that the overall reaction
367
mechanism with Cl• is H-abstraction from a C-H bond that is affected by the neighboring
368
act –COO- functional group. Our ∆Gaq,calc values range from -2.6 kcal/mol to 16.4
369
kcal/mol, and there is a linear correlation for these compounds under H-abstraction.
370
act Our ∆Gaq,calc values indicate that the H-abstraction from a C-H bond that is
371
bound to a –C(O)O functional group is preferable to H-abstraction from a C-H bond that
372
is bound to a –OC(O) functional group because of the stronger electron-withdrawing
373
effect from the –OC(O) functional group (e.g., a Taft constant of 2.00 for COOCH3 and
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2.45 for OCOCH3).65 We observed the same effect from the ether functional group (-O-)
375
in diethylether and methyl-tert-butyl ether.
376
Halogenated alkanes
377
act The ∆Gaq,calc value for dichloromethane for H-abstraction from a C-H bond is 4.9
378
kcal/mol, which is consistent with the correlation in Figure 2. We were unable to find the
379
aqueous-phase transition state for trichloromethane in the absence and presence of 1~3
380
act explicit water molecules. The gaseous phase ∆Ggas,calc values (i.e., 4.8 kcal for
381
dichloromethane and 4.7 kcal/mol for trichloromethane) suggest a smaller value of
382
act for trichloromethane than that of dichloromethane if the solvation effect is ∆Gaq,calc
383
linear.
384
Alkenes and Aromatic Compounds
385
Two kexp values were reported as 1.9 × 108 M-1s-1 66 and 4.88 × 1010 M-1s-1 67 for
386
trichloroethylene and one kexp value of 2.8 × 108 M-1s-1 for perchloroethylene68. The
387
act values are 2.5 kcal/mol for Cl• addition to an unsaturated carbon (C) of ∆Gaq,calc
388
HClC=CCl2 and -0.25 kcal/mol for addition to HClC=CCl2. For perchloroethylene, we
389
act obtain a ∆Gaq,calc value of -0.49 kcal/mol. In the reaction of HO• with alkenes, the
390
addition occurs on an unsaturated carbon that has fewer functional groups because of the
391
stability of the generated germinal chlorohydrin carbon-centered radical; this finding is
392
act supported by our calculated ∆Gaq,calc (5.9 kcal/mol for HClC=CCl2 and 10.5 kcal/mol for
393
HClC=CCl2). However, our calculations indicate less selectivity for Cl• addition to the
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act unsaturated carbons of alkenes. In addition, the calculated ∆Gaq,calc for Cl• addition is
395
much smaller than that for HO•. At this point, it is unclear what caused this result, as we
396
act have only two kexp values for alkenes. If the ∆Gaq,calc values are correct, then kexp should
397
be close to the diffusion limited rate constant, such as 4.88 × 1010 M-1s-1 67.
398
act The ∆Gaq,calc value for the addition of Cl• to an aromatic benzene ring is 8.9
399
react kcal/mol, yielding a chlorocyclohexadienyl radical as the product with a ∆Gaq,calc of -2.7
400
kcal/mol, which agrees with the experimental observation69. This Cl• addition to a
401
benzene ring is similar to that of HO• in which a hydroxycyclohexadienyl radical is
402
act formed as a product ( ∆Gaq,calc of 9.9 kcal/mol). While we were unable to locate the
403
transition state for H-abstraction from the benzene ring by Cl•, we obtained a value of
404
act 11.6 kcal/mol of ∆Gaq,calc for H-abstraction by HO•. Thus, we conclude that H-
405
abstraction from the benzene ring is a minor reaction and that addition to the benzene
406
ring is the major reaction mechanism. Although Martire et al. (2001)70 did not report the
407
kexp for an individual compound, their reported kexp, (1.8±0.3)×1010 M-1s-1, for
408
chlorobenzene, toluene, and benzoic acid and the reaction mechanisms are consistent
409
with our findings based on our QM calculations.
410
Reactivity of Cl2•- and ClO•
411
Because of the space limitation, a detailed discussion on the reactivity of Cl2•- and ClO•
412
with organic compounds is found in the Supporting Information.
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Environmental Implications
414
The systematic evaluations of kexp with the LFER and TST-based correlations based on
415
ab initio QM calculations highlight several key gaps in the understanding of the reactivity
416
of chlorine-derived radicals. Previous experimental studies have shown discrepancies
417
among the kexp values for some Cl• and HO• radicals with inorganic species, particularly
418
act for the reaction of HO• with HOCl. Our investigations based on the ∆Gaq,calc and
419
react values revealed that H-abstraction is the major reaction mechanism, which ∆Gaq,calc
420
supports the kexp of 8.5 × 104 M-1s-1. This kexp value is critical in developing an
421
elementary reaction-based kinetic model because HOCl is the more dominant species at
422
an approximately neutral or below neutral pH, which is the typical condition in the
423
UV/chlorine AOP. In addition, the lower scavenging effect of HO• by HOCl indicates
424
that more HO• is used to destroy target organics and microorganisms in the UV/chlorine
425
AOP. We are currently evaluating this dynamic effect by developing our elementary
426
reaction-based kinetic model. The established LFER can also be used to evaluate the kexp
427
values in the literature and can provide mechanistic insight into various elementary
428
reaction mechanisms.
429
The systematic evaluations of the reactions of Cl• with a wide variety of organic
430
act react and ∆Gaq,calc values revealed the dominant reaction compounds based on the ∆Gaq,calc
431
mechanisms. Although a product study is necessary to confirm the reaction byproducts,
432
the identification of the major reaction mechanisms such as H-abstraction and Cl-adduct
433
formation for alcohol and carboxylic functional groups will help formulate an elementary
434
reaction-based kinetic model. The established correlation can be used to predict the
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435
unknown reaction rate constants that have not been experimentally measured and to
436
screen a large number of potential organic contaminants for the applicability of the
437
UV/chlorine AOP. Finally, chlorine-derived radical species play critical roles in other
438
environmental processes, such as the formation of atmospheric water droplets, and
439
findings from this study can be used to advance the understanding of those environmental
440
processes.
441
Associated Content
442
Supporting information includes a table that summarizes the reactivity of Cl• with
443
organic compounds. The SI also includes detailed descriptions of the methods for the
444
theoretical calculations, the diffusion-limited reaction rate constants, the reactivity
445
of Cl• with aromatic compounds, and the reactivity of Cl2•- and ClO• with organic
446
compounds.
447
Acknowledgement
448
This work was partially supported by the National Science Foundation Award #:
449
CBET-1435926. Any opinions, findings, conclusions, or recommendations
450
expressed in this publication are those of the authors and do not necessarily reflect
451
the view of the supporting organization.
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Literature Cited
453
1.
Wang, D.; Bolton, J.R.; Hofmann, R. Medium pressure UV combined with
454
chlorine advanced oxidation for trichloroethylene destruction in a model water.
455
Wat. Res. 2012. 46 (15), 4677-4686.
456
2.
Watts, M.J.; Rosenfeldt, E.J.; Linden, K.G. Comparative OH radical oxidation
457
using UV-Cl2 and UV-H2O2 processes. J. Water Supply Res. Technol. AQUA.
458
2007, 56 (8), 469-477.
459
3.
Watts, M.J. and Linden, K.G. Chlorine photolysis and subsequent OH radical
460
production during UV treatment of chlorinated water. Wat. Res. 2007, 41, 2871-
461
2878.
462
4.
Rattanakul, S.; Oguma, K. Analysis of hydroxyl radicals and inactivation
463
mechanisms of bacteriophage MS2 in response to a simultaneous application of
464
UV and chlorine. Environ. Sci. Technol. 2017, 51(1), 455-462.
465
5.
Sun, P.; Lee, W-N.; Zhang, R.; Huang, C-H. Degradation of DEET and caffeine
466
under UV/chlorine and simulated sunlight/chlorine conditions. Environ. Sci.
467
Technol. 2016, 50, 13265-13273.
468
6.
Wang, W-L.; Wu, Q-Y.; Huang, N.; Wang, T.; Hu, H-Y. Synergistic effect
469
between UV and chlorine (UV/chlorine) on the degradation of carbamazepine:
470
Influence factors and radical species. Wat. Res. 2016, 98, 190-198.
471
7.
Wu, Z.; Fang, J.; Xiang, Y.; Shang, C.; Li, X.; Meng, F.; Yang, X. Roles of
472
reactive chlorine species in trimethoprim degradation in the UV/chlorine process:
473
Kinetics and transformation pathways. Wat. Res. 2016, 104, 272-282.
23
ACS Paragon Plus Environment
Environmental Science & Technology
474
8.
475 476
Photochem. Photobiol. A. 1991, 66, 133-140. 9.
477 478
Vogt, R.; Schindler, R.N. Product channels in the photolysis of HOCl. J.
Nowell, L.H.; Hoigne, J. Photolysis of aqueous chlorine at sunlight and ultraviolet wavelengths- II. Hydroxyl radical production. Wat. Res.1992, 26 (5), 599-605.
10.
Armstrong, D.A.; Huie, R.E.; Lymar, S.; Koppenol. W.H.; Merényi, G.; Neta. P.;
479
Stanbury, D.M.; Steenken, S.; Wardman, P. Standard electrode potentials
480
involving radicals in aqueous solution inorganic radicals. Biolnorg React Mech.
481
2013, 9 (1-4), 59-61.
482
11.
Alfassi, Z.B.; Huie, R.E.; Mosseri, S.; Neta, P. Kinetics of one-electron oxidation
483
by the ClO radical. International Journal of Radiation Applications and
484
Instrumentation. Part C. Radiation Physics and Chemistry, 1988, 32(1), 85-88.
485
12.
Yang, X.; Sun, J.; Fu, W.; Shang, C.; Li, Y.; Chen, Y.; Gan, W.; Fang, J. PPCP
486
degradation by UV/chlorine treatment and its impact on DBP formation potential
487
in real waters. Wat. Res. 2016, 98, 309-318.
488
13.
Wang, D.; Bolton, J.R.; Andrews, S.A.; Hofmann, R. Formation of disinfection
489
by-products in the ultraviolet/chlorine advanced oxidation process. Sci. of the
490
Total Environ. 2015, 518-519, 49-57.
491
14.
CAS Website; https://www.cas.org/ accessed in January, 2017.
492
15.
Buxton, G. V.; Greenstock, C. L.; Helman, W. P.; Ross, A. B. Critical review of
493
rate constants for reactions of hydrated electrons, hydrogen atoms and hydroxyl
494
radicals (•OH/•O−) in aqueous solution. J. Phys. Chem. Ref. Data 1988, 17,
495
513−886.
24
ACS Paragon Plus Environment
Page 24 of 38
Page 25 of 38
496
Environmental Science & Technology
16.
Minakata, D.; Li, K.; Westerhoff, P.; Crittenden, J. Development of a group
497
contribution method to predict aqueous phase hydroxyl radical (HO•) reaction
498
rate constants. Environ. Sci. Technol. 2009, 43, 6220−6227.
499
17.
Guo X.; Minakata, D.; Niu, J.; Crittenden, J. Computer-based first-principles
500
kinetic modeling of degradation pathways and byproduct fates in aqueous-phase
501
advanced oxidation processes. Environ. Sci. Technol. 2014, 48, 5718-5725.
502
18.
503 504
Connick, R.E. The interaction of hydrogen peroxide and hypochlrous acid in acidic solutions containing chloride ion. JACS. 1947, 69 (6), 1509-1514.
19.
Zuo, Z.; Katsumura, Y.; Ueda, K.; Ishigure, K. Reactions between some inorganic
505
radicals and oxychlorides studies by pulse radiolysis and laser photolysis. J.
506
Chem. Soc. Faraday Trans. 1997, 93 (10), 1885-1891.
507
20.
508 509
1966, 70, 3798-3805. 21.
510 511
Morris, J.C. The acid ionization constant of HOCl from 5 to 35˚. J. Phys. Chem..
Herrmann, H. Kinetics of aqueous phase reactions relevant for atmospheric chemistry. Chem. Rev. 2003, 103, 4691-4716.
22.
Gilbert, B.C.; Stell, J.K.; Peet, W.J.; Radford, K. J. Generation and reactions of
512
the chlorine atom in aqueous solution. J. Chem. Soc., Faraday Trans. 1. 1988, 84
513
(10), 3319-3330.
514
23.
515 516
Buxton, G.V.; Bydder, M.; Salmon, G.A.; Williams, J.E. The reactivity of chlorine atoms in aqueous solution. PCCP. 2000, 2, 237-245.
24.
Buxton, G.V.; Wang, J.; Salmon, G.A. Rate constants for the reactions of NO3•,
517
SO4•-, and Cl• radicals with formate and acetate esters in aqueous solution. PCCP.
518
2001, 3, 2618-2621.
25
ACS Paragon Plus Environment
Environmental Science & Technology
519
25.
Wicktor, F.; Donati, A.; Herrmann, H.; Zellner, R. Laser based spectroscopic and
520
kinetic investigations of reactions of the Cl atom with oxygenated hydrocarbons
521
in aqueous solution. PCCP. 2003, 5, 2562-2572.
522
26.
Asmus, K.-D.; Möckel, H.; Henglein, A. Pulse radiolytic study of the site of OH•
523
radical attack on aliphatic alcohols in aqueous solution. J. Phy. Chem. 1973, 77
524
(10), 1218-1221.
525
27.
An, T.; Guo, Y.; Li, G.; Kamat, P.V.; Peller, J.; Joyce, M.V. Kinetics and
526
mechanisms of •OH mediated degradation of dimethyl phthalate in aqueous
527
solution: Experimental and theoretical studies. Environ. Sci. Technol. 2014, 48,
528
641-648.
529
28.
Xiao, R.; Noerpel, M.; Luk, H.L.; Wei, Z.; Spinney, R. Thermodynamic and
530
kinetic study of ibuprofen with hydroxyl radical: A density functional theory
531
approach. Int. J. Quantum. Chem. 2014, 114, 74-83.
532
29.
Trogolo, D.; Mihra, B,K.; Heeb, M.; von Gunten, U.; Arey, J.S. Molecular
533
mechanism of NDMA formation from N,N-dimethylsulfamide during ozonation:
534
Quantum chemical insights into a bromide-caatalyzed pathway. Environ. Sci.
535
Technol. 2015, 49, 4163-4175.
536
30.
Naumov, S.; von Sonntag, C. standard gibbs free energies of reactions of ozone
537
with free radicals in aqueous solution: Quantum-chemical calculations. Environ.
538
Sci. Technol. 2011, 45, 9595-9204.
539 540
31.
Minakata, D.; Song, W.; Mezyk, S.P.; Cooper, W.J. Experimental and theoretical studies on aqueous-phase reactivity of hydroxyl radicals with multiple
26
ACS Paragon Plus Environment
Page 26 of 38
Page 27 of 38
Environmental Science & Technology
541
carboxylated and hydroxylated benzene compounds. PCCP., 2015, 17, 11796-
542
11812.
543
32.
Minakata, D.; Song, W.; Crittenden, J. Reactivity of aqueous phase hydroxyl
544
radical with halogenated carboxylate anions: Experimental and theoretical
545
studies. Environ. Sci. Technol. 2011, 45, 6057-6065.
546
33.
Minakata, D.; Crittenden, J. Linear Free Energy Relationships between the
547
Aqueous Phase Hydroxyl Radical (HO•) Reaction Rate Constants and the Free
548
Energy of Activation. Environ. Sci. & Technol. 2011, 45, 3479-3486.
549
34.
550 551
transfer. I. J. Chem. Phys. 1956, 24 (5), 966-978. 35.
552 553
Brezonik, P.L. Chemical Kinetics and Process Dynamics in Aqueous Systems; Lewis Publishers: Boca Raton, FL, 2002.
36.
554 555
Marcus, R.A. On the theory of oxidation-reduction reactions involving electron
Eyring, H.; Gershinowitz, H.; Sun, C.E. The absolute rate of homogeneous atomic reactions. J. Chem. Phys. 1935, 3, 786-796.
37.
Frisch, M. J.; Trucks, G. W.; Schlegel, H. B.; Scuseria, G. E.; Robb, M. A.;
556
Cheeseman, J. R.; Scalmani, G.; Barone, V.; Mennucci, B.; Petersson, G. A.;
557
Nakatsuji, H.; Caricato, M.; Li, X.; Hratchian, H. P.; Izmaylov, A. F.; Bloino, J.;
558
Zheng, G.; Sonnenberg, J. L.; Hada, M.; Ehara, M.; Toyota, K.; Fukuda, R.;
559
Hasegawa, J.; Ishida, M.; Nakajima, T.; Honda, Y.; Kitao, O.; Nakai, H.; Vreven,
560
T.; Montgomery, Jr., J. A.; Peralta, J. E.; Ogliaro, F.; Bearpark, M.; Heyd, J. J.;
561
Brothers, E.; Kudin, K. N.; Staroverov, V. N.; Kobayashi, R.; Normand, J.;
562
Raghavachari, K.; Rendell, A.; Burant, J. C.; Iyengar, S. S.; Tomasi, J.; Cossi, M.;
563
Rega, N.; Millam, N. J.; Klene, M.; Knox, J. E.; Cross, J. B.; Bakken, V.; Adamo,
27
ACS Paragon Plus Environment
Environmental Science & Technology
564
C.; Jaramillo, J.; Gomperts, R.; Stratmann, R. E.; Yazyev, O.; Austin, A. J.;
565
Cammi, R.; Pomelli, C.; Ochterski, J. W.; Martin, R. L.; Morokuma, K.;
566
Zakrzewski, V. G.; Voth, G. A.; Salvador, P.; Dannenberg, J. J.; Dapprich, S.;
567
Daniels, A. D.; Farkas, Ö.; Foresman, J. B.; Ortiz, J. V.; Cioslowski, J.; Fox, D. J.
568
Gaussian 09, Revision D.1; Gaussian, Inc., Wallingford CT, 2009.
569
38.
570 571
Curtiss, L. A.; Redfern, P. C.; Raghavachari, K. Gaussian-4 theory. J. Chem. Phys. 2007, 126, 084108.
39.
Marenich, A. V.; Cramer, C. J.; Truhlar, D. G. Universal solvation model based
572
on solute electron density and on a continuum model of the solvent defined by the
573
bulk dielectric constant and atomic surface tensions. J. Phys. Chem. B 2009, 113,
574
6378−6396.
575
40.
Minakata, D.; Mezyk, S.P.; Jones, J.W.; Daws, B.R.; Crittenden, J.C.
576
Development of linear free energy relationships for aqueous phase radical-
577
involved chemical reactions. Environ. Sci. Technol. 2014, 48, 13925-13932.
578
41.
579 580
von Smoluchowski, M. Versuch eine mathematicschen Theorie der Koagulationskinetik kolloidaler Losungern. Z. Phys. Chem. 1917, 92, 129−168.
42.
Kläning, U.K.; Wolff, T. Laser flash photolysis of HClO, ClO-, HBrO, and BrO-
581
in aqueous solution. Reactions of Cl- and Br-atoms. Ber. Bunsenges. Phys. Chem.
582
1985, 89, 243-245.
583
43.
Buxton, G.V.; Subhani, M.S. Radiation chemistry and photochemistry of
584
oxychlorine ions. Part 1.-radiolysis of aqueous solutions of hypochlorite and
585
chlorite ions. J. Chem. Soc., Faraday Trans. 1, 1972, 68, 947-957.
28
ACS Paragon Plus Environment
Page 28 of 38
Page 29 of 38
586
Environmental Science & Technology
44.
Yu, X-Y.; Barker, J.R. Hydrogen peroxide photolysis in acidic aqueous solutions
587
containing chloride ions. II. Quantum yield of HO•(Aq) radicals. J. Phys. Chem.
588
A. 2003, 107, 1325-1332.
589
45.
590 591
Ershov, B. G.: Kinetics, mechanism and intermediates of some radiation-induced reactions in aqueous solutions. Russian Chem. Rev. 2004, 73, 101–113.
46.
Jayson, G. Some simple, highly reactive, inorganic chlorine derivatives in
592
aqueous solution. Their formation using pulses of radiation and their role in the
593
mechanism of the Fricke dosimeter. J. Chem. Soc., Faraday Transactions I. 1973,
594
69, 1597-1607.
595
47.
Yu, X-Y.; Bao, Z-C.; Barker, J.R. Free radical reactions involving Cl•, Cl2•-, and
596
SO4•- in the 248 nm photolysis of aqueous solutions containing S2O82- and Cl-.
597
J. Phys. Chem. A. 2004, 108, 295-308.
598
48.
599 600
anion radical. Radiat. Phys. Chem. 1980, 15, 159-161. 49.
601 602
Navaratnam, S.; Parsons, B.J.; Swallow, A.J. Some reactions of the dichloride
Woods, R.J.; Lesigne, B.; Gilles, L.; Ferradini, C.; Pucheault, J. Pulse radiolysis of aqueous lithium chloride solutions. Phys. Chem. 1975, 79 (24), 2700.
50.
Ross, A. B., Bielski, B. H. J., Buxton, G. V., Cabelli, D. E., Helman, W. P., Huie,
603
R. E., Grodkowski, J., Neta, P., Mulazzani, Q. G., and Wilkinson, F.: NIST
604
Standard Reference Database 40: NDRL/NIST Solution Kinetics Database V. 3.0,
605
Gaithersburg, MD, 1998.
606
51.
Grigor'ev, A. E., Makarov, I. E., and Pikaev, A. K.: Formation of Cl2- in bulk
607
solution during the radiolysis of concentrated aqueous solutions of chlorides.,
608
High Ener. Chem., 1987, 21, 99-102.
29
ACS Paragon Plus Environment
Environmental Science & Technology
609
52.
subsequent decay of Cl2- in aqueous solution. J. Phys. Chem. 1990, 94, 2435.
610 611
McElroy, W. J. A laser photolysis study of the reaction of SO4- with Cl- and the
53.
Kukui, A.; Roggenbuck, J.; Schindler, R.N. Mechanisms and rate constants for
612
the reactions of Cl atoms with HOCl, CH3OCl and tert-C4H9OCl. Ber.
613
Bunsenges. Phys. Chem. 1997, 101, 281-286.
614
54.
Curtin, D.Y. Stereochemical control of organic reactions. Differences in behavior
615
of diastereoisomers. I. Ethane derivatives. The cis effect. Rec. Chem. Prog. 1954,
616
15, 111-128.
617
55.
618 619
Pollak, P.I.; Curtin, D.Y. Stereospecificity in the rearrangement of amino alcohols. JACS, 1950, 72, 961-965.
56.
Anastasio, C.; Matthew, B.M. A chemical probe technique for the determination
620
of reactive halogen species in aqueous solution: Part 2- chloride solutions and
621
mixed bromide/chloride solutions. Atm. Chem. Phys. 2006, 6, 2439-2451.
622
57.
623 624
Faraday Trans. 1. 1995, 91, 330358.
625 626
Adams, J.; Barlow, S.; Buxton, G.V.; Malone, T.M.; Salmon, G. A. J. Chem. Soc.,
Yamaguchi, M. Hemibonding of hydroxyl radical and halide anion in aqueous solution. J. Phys. Chem. A. 2011, 115, 14620-14628.
59.
Sevilla, M.D.; Summerfield, S.; Eliezer, I.; Rak, J.; Symons, M.C.R. Interaction
627
of the chlorine atom with water: ESR and ab initio MO evidence for three-
628
electron (σ2σ*1) bonding. J. Phys. Chem. A. 1997, 101, 2910-2915.
629 630
60.
Valiev, M.; D’Auria, R.; Tobias, D.J.; Garrett, B.C. Interactions of Cl- and OH radical in aqueous solution. J. Phys. Chem. A. Lett. 2009, 113, 8823-8825.
30
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Page 30 of 38
Page 31 of 38
631
Environmental Science & Technology
61.
632 633
edition. 2015, Cengage Learning. 62.
634 635
Kurz, J.L. The hydration of acetaldehyde. I. Equilibrium thermodynamic parameters. JACS. 1967, 59 (14), 3524-3528.
63.
636 637
McMurry, J. Nucleophilic addition of H2O: Hydration in Organic Chemistry 9th
Lide, D.R.; Frederikse, H.P.R. in CRC Handbook of Chemistry and Physics, CRC Press, Boca Raton, FL, 2013-2014.
64.
Greenzaid, P.; Rappoport, Z.; Samuel, D. Limitations of ultra-violet spectroscopy
638
for the study of the reversible hydration of carbonyl compounds. J. Chem. Soc.
639
1967, 63, 2131-2139.
640
65.
641 642
Karelson, M. Molecular Descriptors in QSAR/QSPR; John Wiley & Sons, Inc.: New York, 2000.
66.
Li, K.; Stefan, M.I.; Crittenden, J.C. Trichloroethene degradation by UV/H2O2
643
advanced oxidation process: Product study and kinetic modeling. Environ. Sci.
644
Technol. 2007, 41, 1696-1703.
645
67.
646 647
study and kinetic modeling. 2004, 38, 6685-6693. 68.
648 649
Li, K.; Stefan, M.I.; Crittenden, J.C. UV photolysis of trichloroethylene: Product
Martens, R.; von Sonntag, C. Photolysis (λ=254 nm) of tetrachloroethene in aqueous solutions. J. Photochem. Photobiol. A: Chemistry. 1995, 85, 1-9.
69.
Alegre, M.L.; Geronés, M.; Rosso, J.A.; Bertolotti, S.G.; Braun, A.M.; Mártire,
650
D.O.; Gonzalez, M.C. Kinetic study of the reactions of chlorine atoms and Cl2•-
651
radical anions in aqueous solutions 1. Reaction with benzene. J. Phys. Chem. A.
652
2000, 104, 3117-3125.
31
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Environmental Science & Technology
653
70.
Mártire, D.O.; Rosso, J.A.; Bertolotti, S.; Roux, G.C.L.; Braun, A.M.; Gonzalez,
654
M.C. Kinetic study of the reactions of chlorine atoms and Cl2•- radical anions in
655
aqueous solutions. II. Toluene, benzoic acid, and chlorobenzene. J. Phys. Chem.
656
A. 2001, 105, 5385-5392.
657
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Figure Captions
659
react Figure 1: Linear free energy relationship between lnkchem and ∆Gaq,calc for chlorine-
660 661 662 663 664 665 666
derived inorganic radical reactions. ◊ : reactions with HOCl/OCl-, : Cl• and Cl2•involving reactions, : •OHCl- involving reactions, and : OCl• reaction. The vertical bar results from the range of the reported kexp values in the literature. Note that data points 6 and 11 are not included in the LFER analysis due to the different reaction mechanism.
667
act Figure 2: Linear correlation between lnkexp and ∆Gaq,calc for H-abstraction by Cl• from a
668 669 670 671 672 673 674 675 676 677 678
C-H bond. The vertical bar results from the range of the reported kexp values in the literature. 2: ethanol (α-position); 3: 1-propanol; 4: 2-propanol; 5: 2-butanol; 6: tertbutanol (C-H bond); 6’ tert-butanol (O-H bond): 7: hydrated formaldehyde; 8: acetaldehyde; 9: hydrated acetaldehyde; 10: propionaldehyde; 11: acetone; 14: 2butanone; 17: acetate; 18: acetic acid; 19: propionic acid; 20: isobutyric acid; 21: methylformate; 22: ethylformate; 23: methylacetate; 24: ethylaceate; 25: diethyl ether; 26: methyl-tert-butyl ether, and 28: dichloromethane. Note that compounds are not included from 1: methanol; 12: hydrated acetone; 13: chloroacetone; 15: formate, and 16: formic acid due to either different mechanism or uncertainty.
679
act Figure 3: Linear correlation between lnkexp and ∆Gaq,calc for Cl-adduct formation of
680 681 682 683 684 685 686 687 688 689 690 691 692
alcohol and carboxylic compounds. The vertical bar results from the range of the reported kexp values in the literature. 1: methanol; 2: ethanol; 3: 1-propanol; 4: 2-propanol; 5: 2butanol; 6: tert-butanol; 7: hydrated formaldehyde; 9: hydrated acetaldehyde; 15: formate; 16: formic acid; 17: acetate; 18: acetic acid; 19: propion acid, and 20: isobutyric acid.
693
react literature and our calculated ∆Gaq,calc , kchem, and kD values.
Table Captions Table 1: Twenty-two elementary reactions in the UV/chlorine AOP with kexp values in the
694 695
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30 25
9
8
12 5
21
20
4 17
14
3
10
1 16 22
lnkchem
15
15
13 y = -0.53x + 17.25 R² = 0.78
10
19 7
11 6 18
20
5 0 -40 696 697
-20 0 ∆Greactaq,calc, kcal/mol
Figure 1
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25 4
3 26
17 20
5
6 8 18
25
20
2
7 14
lnkexp
6
19
24
11
9
22 21
13
15
28
10 23
y = -0.50x + 20.53 R² = 0.70
10
5
0 -10 698 699
-5
0
5 ∆Gactaq,calc, kcal/mol
Figure 2
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15
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17
4
5
1
20
15
2 19 6
20 3
7 9
lnkexp
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16 18
15
y = -0.95x + 23.43 R² = 0.70
10
5
0 0 700 701
2
4 6 ∆Gactaq,calc, kcal/mol
Figure 3
702
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Table 1
No.
Elementary reaction
kexp, M-1s-1
References
HOCl + Cl• → •OCl + HCl HOCl + Cl• → Cl2 + HO-
1
3×109
42
HOCl + Cl• → HOCl(Cl•) HOCl + HO• → •OCl + H2O 4
-5.9
3.2
-132.6
4.6
4.6
11.8
-20.8
8.4 7.2
kD , M-1s-1
4.2×109
1.1×1010
0
8.5×104 2.4×109
8.5×104 1.2×1010
3.3×1010 3.4×1010
1.1×1010 1.2×1010
HOCl + HO• → HO• + HOCl 8.46×10 - 2.0×10
3 4
HOCl + HO• → HOCl(HO•) OCl- + Cl• → •OCl + Cl8.2×109 OCl- + HO• → •OCl + HO8.8×109
42 43
5.7 -23.1 -5.2
5
Cl- + Cl• → Cl2•-
6.5-8.5 × 109
42,44
-13.1
1.6×1010
1.1×1010
6
Cl- + Cl2 → Cl3-
2.0 × 104
45
0.22
2.0 × 104
1.0×1010
7
Cl2•- → Cl• + Cl-
5.2 × 104 - 1.4 × 105 44,46
13.1
5.2 × 104 1.4 × 105
1.2×1010
8
(2.1 ± 0.05) × 109
47
-37.5
2.6 × 109
1.1×1010
(0.9-9.0) × 109
46,48,49
-24.4 (-24.2) 1.0 × 109
1.0×1010
10
Cl• + Cl2•- → Cl2 + ClCl2•- + Cl2•- → Cl2 + 2Cl- (or Cl3- + Cl-) Cl2•- + HO• → HOCl + Cl-
1 × 109
50
-34.5
1.1 × 109
1.2×1010
11
Cl3- → Cl2 + Cl-
1.1 × 105
45
-0.22
1.1 × 105
1.2×1010
12
HO• + Cl- → •OHCl-
(4.3 ± 0.4) × 109
50
2.99 (-2.4)* 6.8 × 109
1.2×1010
13
Cl• + H2O → •OHCl- + H+
(1.6 ± 0.2) × 105
46
1.6 × 105
1.2×1010
14
Cl• + OH- → •OHCl-
1.8 × 1010
42
-14.9
1.8 × 1010
1.1×1010
15
Cl2•- + OH- → •OHCl- + Cl-
4.5 × 107
51
-1.8
4.5 × 107
1.0×1010
16
•OHCl- → HO• + Cl-
(6.1 ± 0.8) × 109
46
-2.99
17
•OHCl- + H+ → Cl• + H2O
(2.6 ± 0.6) × 1010
46
18
•OHCl- + Cl- → Cl2•- + OH-
1.0 × 105
51
1.84
1.0 × 105
1.0×1010
19
Cl• + H2O → •Cl(H2O)
2.5 × 105
52
3.8
2.5 × 105
1.3×1010
20
Cl2•- + H2O → •Cl(H2O) + Cl- 1.3 × 103
52
16.9
1.3 × 103
1.2×1010
21
•Cl(H2O) + Cl- → Cl2•- + H2O 5 × 109
52
-16.9
9.9 × 109
1.0×1010
22
•OCl + •OCl + H2O → HClO + HClO2
42,43
-8.1
3.3 27.0 × 109
1.1×1010
2.5 - 7.5 × 109
3,18,19
14.7
kchem, M-1s-1
2
9
704
9
∆Gactaq,calc ∆Greactaq,calc kcal/mol kcal/mol
*value with 2 explicit water molecules
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UV HOCl/OCl- HO Cl Cl2- ClO H-abstrac1on? Cl-adduct? Electron-transfer?
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