Mechanistic Insight into the Reactivity of Chlorine-Derived Radicals in

May 25, 2017 - Department of Civil and Environmental Engineering, Michigan Technological University, 1400 Townsend Drive, Houghton, Michigan 49931, ...
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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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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]

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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

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these data points in the correlation. Except for methanol, we observe a linear correlation

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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

313

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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703

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- HOŸ ClŸ Cl2Ÿ- ClOŸ H-abstrac1on? Cl-adduct? Electron-transfer?



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