Literature DB >> 31183400

Mechanisms and competition of halide substitution and hydrolysis in reactions of N2O5 with seawater.

Laura M McCaslin1, Mark A Johnson2, R Benny Gerber1,3.   

Abstract

SN2-type halide substitution and hydrolysis are two of the most ubiquitous reactions in chemistry. The interplay between these processes is fundamental in atmospheric chemistry through reactions of N2O5 and seawater. N2O5 plays a major role in regulating levels of O3, OH, NO x , and CH4. While the reactions of N2O5 and seawater are of central importance, little is known about their mechanisms. Of interest is the activation of Cl in seawater by the formation of gaseous ClNO2, which occurs despite the fact that hydrolysis (to HNO3) is energetically more favorable. We determine key features of the reaction landscape that account for this behavior in a theoretical study of the cluster N2O5/Cl-/H2O. This was carried out using ab initio molecular dynamics to determine reaction pathways, structures, and time scales. While hydrolysis of N2O5 occurs in the absence of Cl-, results here reveal that a low-lying pathway featuring halide substitution intermediates enhances hydrolysis.

Entities:  

Year:  2019        PMID: 31183400      PMCID: PMC6551187          DOI: 10.1126/sciadv.aav6503

Source DB:  PubMed          Journal:  Sci Adv        ISSN: 2375-2548            Impact factor:   14.136


INTRODUCTION

Hydrolysis and SN2-type halide substitution reactions are two ubiquitous families of reactions that are important throughout many disciplines of chemistry. One area in which the interplay of these key processes has major implications in heterogeneous atmospheric chemistry is the reactions of N2O5 with seawater and halide-containing sea spray aerosols. The reactive uptake of N2O5 on sea spray aerosols is widely believed to be the most influential set of reactions in heterogeneous atmospheric chemistry (–). Model studies indicate that changes in the probability of the reactive uptake of N2O5 on aerosols change atmospheric levels of NO, O3, and OH by up to 25, 12, and 15%, respectively (). N2O5 is formed from NO2 and NO3 during the night, as NO3 is photolyzed by sunlight. HNO3, the hydrolysis product of N2O5 reactions with seawater, serves as a major sink for NO species in the atmosphere, which has been validated by a variety of modeling and field studies (, , –). NO species are widely known to affect levels of O3, OH, and CH4, thus motivating the need to study their formation and depletion pathways (). Studies have also shown formation of ClNO2 from N2O5 interacting with chloride-containing liquids, aerosols, and small water clusters (, –) in a wide range of chloride concentrations. These ClNO2 compounds can photolyze to form NO2 and chlorine radicals, which is a major source of activated Cl in the atmosphere (, ). The competition between formation of ClNO2 from halide substitution reactions and HNO3 from hydrolysis reactions of N2O5 and seawater thus has major consequences for the fate of NO species, CH4, and O3, which are known to greatly affect Earth’s radiative forcing and thus global climate (). Recently, experiments on both liquid surfaces and aerosols have been performed to unravel the competition between numerous reaction pathways when N2O5 interacts with seawater and sea spray aerosols (–). Limits on the total reactive uptake of N2O5 on both pure and salty water have been determined to be between 0.01 and 0.03. However, due to the complexity of chemical environments of sea spray aerosols, studies of the relative yields of ClNO2 and HNO3 are still under way (, , ). While some theoretical studies have explored hydrolysis and halide substitution of N2O5 interacting with small water clusters, mechanisms of the competition between these reactions have yet to be established (, –). Faced with the need to understand these complex reactions and their mutual influence on each other, it is necessary to design model systems that help to develop intuition from first-principles studies. In this work, we seek to reveal intrinsic features of the reaction between N2O5 and aqueous Cl− that control the competition between hydrolysis and halide substitution reactions. We specifically address how water competes with Cl− for reaction with N2O5 in a theoretical study of the ternary ionic cluster with composition N2O5/Cl−/H2O. Scrutiny of this microscopic regime is also warranted by the results of a recent mass spectrometric experimental study of N2O5 interactions with small halide-water clusters [X−(H2O)]. (). Intermediates were isolated and characterized with infrared spectroscopy to reveal formation of XNO2/NO3− species with composition X−(N2O5). In the present work, we address the features in the reaction dynamics that control the competition between halide substitution and hydrolysis in a sufficiently small system that it can be studied using very accurate ab initio methods. In studying the reaction pathways and time scales of these processes, insights will be gained into the microscopic details of unresolved questions in heterogeneous atmospheric chemistry. Our method integrates the calculations of transition states (TSs), intrinsic reaction coordinates (IRCs), and ab initio molecular dynamics (AIMD). An additional strength of this small model is its ability to evaluate how mechanistic details for the reactions of N2O5 with aqueous chloride will evolve in larger systems. We take the perspective that even in bulk environments, the chemistry of halide substitution and hydrolysis of N2O5 is likely a local phenomenon. Thus, even as the addition of water molecules to the system will inevitably change the rates of the processes because of a decrease in accessibility of the TS, the configurations and relative energies of the TS will be preserved and continue to provide a microscopic paradigm for the overall kinetics.

RESULTS AND DISCUSSION

Figure 1 represents the reaction pathway for N2O5 interacting with H2O and Cl−. Solid lines connecting the various structures indicate an IRC, the steepest gradient pathway from a TS to nearest local minimum (). Here, two TSs and thus two IRCs are indicated. First, the left IRC corresponds to the pathway from Cl−/H2O interacting with intact N2O5 through an extremely small barrier (0.6 kcal/mol) into the formation of substitution products: ClNO2, NO3−, and H2O. This small barrier to substitution and small distance in configuration space between the reactant and TS1 structures implies a very fast process. Within the substitution product region (i.e., configurations of ClNO2/NO3−/H2O), there is a rich array of configurations accessible to the system at ambient temperatures due to the electrostatically bound nature of the ternary cluster. Besides the local minima associated with IRCs, an additional minimum is indicated: a planar conformation of ClNO2/NO3−/H2O. The planar ClNO2/NO3− substructure has the same orientation as the reaction intermediate recently detected by Kelleher et al. (). As Kelleher et al. found, this structure with a relative energy of 15.6 kcal/mol has the lowest energy of the substitution products. The third substitution structure shown in Fig. 1 (differing in orientation and number of hydrogen bonds) has a relative energy of 21.1 kcal/mol and connects to the second IRC shown in Fig. 1, linking substitution and hydrolysis reactions (i.e., configurations of HNO3/NO3−/HCl or 2HNO3/Cl−). The TS with relative energy of 35.5 kcal/mol connecting the substitution and hydrolysis product regions (TS2) exhibits the interesting structural feature that the charge-separated NO2+ and NO3− moieties accommodate Cl− and H2O on opposite sides of the NO2+ constituent such that both nucleophiles are positioned to attack the nitrogen atom. This configuration illustrates the mutual influence of the halide substitution and hydrolysis reactions of N2O5, indicating that the conditions for one reaction necessarily affect the other. On the right side of the second IRC, a structure corresponding to a hydrolysis reaction sits at 0.0 kcal/mol, the lowest-lying structure found. This HCl/NO3−/HNO3 structure is 15.6 kcal/mol and 30.4 kcal/mol more stable than the lowest-lying substitution and intact N2O5 configurations, respectively. Both O─H bonds of the water have broken, and the protons have formed new bonds to make HCl and HNO3. Last, another low-lying minimum structure of 2HNO3/Cl− is shown to the far right at 0.4 kcal/mol.
Fig. 1

Low-lying reaction pathway of N2O5 interacting with H2O + Cl−.

Structures were optimized at the ωB97X-D/aug-cc-pVDZ level of theory with CCSD(T)/aug-cc-pVDZ single-point energy corrections. All relative energies are shown with harmonic zero-point energy corrections.

Low-lying reaction pathway of N2O5 interacting with H2O + Cl−.

Structures were optimized at the ωB97X-D/aug-cc-pVDZ level of theory with CCSD(T)/aug-cc-pVDZ single-point energy corrections. All relative energies are shown with harmonic zero-point energy corrections. Thermodynamically, the trends in the potential energy surface are clear: Hydrolysis products are by far the most stable species, although substitution products are more stable than intact N2O5/Cl−/H2O by 9.3 to 14.8 kcal/mol. The stability of the hydrolysis products fits the current model of HNO3 as a sink for NO species (, , ). We note that ClNO2 production is found to exceed that of HNO3 in most media, although the relative yields of these species need further investigation (, , ). Analogous studies of the hydrolysis reaction of N2O5 with two water molecules (where a second H2O replaces Cl− in our system) determine the barrier to reaction from the associated N2O5/2H2O cluster to be ~20 kcal/mol (). Here, the difference between the low-lying isomer of N2O5 at 30.4 kcal/mol (Fig. 1) and the TS to hydrolysis (TS2) at 41.3 kcal/mol (Fig. 1) is a mere 5.1 kcal/mol. Despite this ~15 kcal/mol lowering of the barrier to N2O5 hydrolysis in the presence of Cl−, the addition of a third body adds entropic complexity. The presence of Cl−, as opposed to another water molecule, near NO2+ stabilizes the hydrolysis process by removing a proton from the water, lowering the barrier to hydrolysis. While the hydrolysis process is thermodynamically favored, the substitution process occurs much more quickly because of its low barrier. The heights of the barriers are correlated with the configurational distance between reactants and products. Because the TS of the halide substitution process (TS1) is very close in configuration to the intact N2O5/Cl−/H2O minimum, the barrier is quite small (0.6 kcal/mol). Despite the close proximity of the attacking water to NO2+ in TS2, the system must undergo a much greater change in geometry between the adjacent ClNO2/H2O/NO3− minimum and charge-separated TS structure, resulting in a much higher barrier (14.4 kcal/mol). Because of the rich array of pathways through the substitution product region, a simple calculation of rates using, for example, transition state theory, is not sufficient for determining the time scales of these reactions. For such a system, exploration via AIMD is likely to yield greater insight into the conformationally complex pathways connecting the two IRCs shown in Fig. 1 due to the propensity for these systems to explore portions of the potential energy landscape away from the IRC. It is not computationally feasible to run trajectories from initial reagents to the final products since the total simulation time required is prohibitively long. AIMD simulations were therefore performed such that the initial geometry was one of the two TS structures shown in Fig. 1. Thus, an understanding of the time scales involved in this process is formed from “stitching” together the process from multiple post-TS calculations. Initial velocities were sampled from a Boltzmann distribution at 300 K and run for a maximum of 10 ps. These initial conditions allow large regions of the potential energy surface to be efficiently sampled and thus provide new insights into reaction probabilities, time scales, and dissociation products. Figure 2 illustrates a computed sequence of events, hence a reaction mechanism, for the halide substitution and hydrolysis reactions of N2O5 interacting with Cl− and H2O. As expected from the small barrier and proximity of the TS and minimum, halide substitution is a fast process, with an average time of 188 fs between minima, as shown in Fig. 2 (A to C). While there is not a substantial geometrical difference between intact N2O5/Cl−/H2O and the TS structure (shown in Fig. 2, A and B), the O─N bond in N2O5 adjacent to the Cl− is stretched to 1.80 Å at TS1 and relaxed to 1.62 Å at the minimum. The relaxation of this bond takes an average of 94 fs. Subsequent formation of the Cl─N bond in Fig. 2C also requires, on average, 94 fs. The mean time scales between local structures on the IRC is of the same order of magnitude as the Cl─N vibrational period of ClNO2, which is ~90 fs (). Thus, the reactive events are neither ballistic nor slow with respect to intramolecular vibrations.
Fig. 2

Snapshots (A-I) of calculations of the reaction of N2O5 with Cl− and H2O.

As previously discussed, the ternary cluster ClNO2/H2O/NO3− has a rich array of accessible configurations. Although direct observation of the hydrolysis from the initial ClNO2/H2O/NO3− cluster is not observed in the calculations, 74% of trajectories that undergo substitution remain as an intact ClNO2/H2O/NO3− cluster, while the other 26% exhibit dissociation into ClNO2 and H2O/NO3− products. The time scales of these dissociation processes are shown between Fig. 2 (C and D) (0.0 to 7.5 ps) and Fig. 2 (D and E) (0.0 to 6.1 ps), reflecting the time spent as an intact cluster entering from TS1 and TS2, respectively. Because most of the ClNO2/H2O/NO3− clusters remain intact, the arrow between Figs. 2C and 2E, essentially the time spent between the two computed IRCs in Fig. 1, is set at a lower limit of 9.5 ps. The halide substitution cluster can, in theory, recross TS1 to form intact N2O5/Cl−/H2O, although this was not observed. Lastly, time scales of the hydrolysis reaction are determined from trajectories initialized at TS2. All trajectories exhibiting hydrolysis form the ternary cluster HCl/NO3−/HNO3, although the HCl proton moves freely between NO3− and Cl−. HCl is efficiently ejected from this assembly to leave the NO3−/HNO3 binary complex behind, with 67% of trajectories that undergo hydrolysis resulting in separation of HCl from the cluster. The time scales for this process range from 0.0 to 6.7 ps, where 0.0 ps indicates that HCl moves away from the cluster immediately after the reaction.

CONCLUSIONS

This theoretical study has identified mechanisms and time scales for the competing halide substitution and hydrolysis reactions of N2O5/H2O/Cl−, thus providing the first microscopic understanding of the key features underlying the reaction kinetics and pathways available for reactive uptake of N2O5 in the presence of aqueous Cl−. Although the presence of Cl− lowers the barrier to hydrolysis relative to the three-body N2O5/(H2O)2 reaction by ~15 kcal/mol, the third body adds significant entropic complexity. The predominance of halide substitution over hydrolysis is enabled by the proximity of the halide to N2O5 in the ternary cluster. In systems with larger water content, halide substitution is therefore expected to become less probable relative to hydrolysis. Qualitative insights into the behavior of these processes in more complicated systems such as larger clusters and macroscopic aerosols should nonetheless benefit from analysis of the local structures of the reagent molecules.

MATERIALS AND METHODS

Analysis

In analysis of bond formation and breaking in the molecular dynamics trajectories, various bond lengths were used as cutoffs. For formation of the Cl─N bond, a cutoff of 1.93 Å was used, which corresponds to the longest Cl─N bond length seen in the computed minima. The O─N bond distance cutoff in the hydrolysis reaction was set at 1.34 Å, the longer length observed in the hydrolysis products.

Theoretical calculations

All stationary geometries on the potential energy surface were optimized with the long-range corrected hybrid density functional ωB97X-D and basis set aug-cc-pVDZ (–). The diffuse functions included in the aug-cc-pVDZ basis set were needed to describe the diffuse nature of the negatively charged system. Zero-point energy corrections were made to the stationary point energies, computed using the harmonic approximation. IRCs were computed as described by Fukui (). To improve calculations of the relative energies of the structures in Fig. 1, single-point energy calculations were performed on top of the ωB97X-D–optimized geometries using coupled cluster theory with single, double, and perturbative triple excitations [CCSD(T)] paired with the aug-cc-pVDZ basis set (–). AIMD calculations were performed at the ωB97X-D/aug-cc-pVDZ level of theory, as used for geometry optimizations and harmonic calculations. All calculations were initialized from each of the two TS structures shown in Fig. 1 (25 trajectories initialized from each geometry). Each trajectory was run with a time step of 0.2 fs for 10 ps or until the cluster dissociated. The relatively small time step was chosen to accurately describe hydrogen motion. All initial velocities were sampled from a Boltzmann distribution at 300 K. Fock extrapolation was performed with polynomial order 6 over 12 points (, ). All calculations reported here were performed using Q-Chem () except for the CCSD(T)/aug-cc-pVDZ single-point energy calculations, which were performed in cfour ().
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