Non-transition metal oxides, including major minerals of the early Solar System, are known to evaporate decomposing into multiple gas molecules, while maintaining their stoichiometric compositions (dissociative congruent evaporation). Here, we derived the absolute rate of this type of evaporation using the transition state theory. In our modified transition state theory, the activation energy closely corresponds to the average energy of the molecules at the transition state, reflecting the degree of decomposition at the potential energy barrier along the reaction coordinate of evaporation. By comparing the theoretical and experimental evaporation rates for the reaction MgO (s) → Mg (g) + O (g), we found that there is an activation barrier close to the product side (i.e., “late” barrier) where the decomposition is almost achieved. The present theory is advantageous to the Hertz–Knudsen equation, which is essentially formulated as the evaporation rate in equilibrium based on the detailed balance, in that it describes dissociative congruent evaporation as a non-equilibrium process and thus provides the link between the experiments and the reaction dynamics.
I. INTRODUCTION
Evaporation is a ubiquitous phenomenon in nature and plays important roles in various natural systems. For example, the depletion of volatile elements is a common chemical feature of meteorites and rocky celestial bodies in the Solar System,1 suggesting that evaporation contributed to the volatile loss from Solar System materials.
Thermodynamics predicts that some compounds evaporate, accompanied by decomposition into multiple gas molecules while maintaining their stoichiometric compositions. The previous studies have experimentally confirmed the preservation of stoichiometry during the Langmuir evaporation of these compounds and have investigated the kinetics of this type of evaporation (hereafter denoted as “dissociative congruent evaporation”) for substances such as non-transition metal oxides (including major minerals of the early Solar System)2–9 and III–V compounds.10–13 The activation energies for dissociative congruent evaporation reported in these studies are generally smaller than the enthalpy of sublimation or vaporization per composition formula, which is distinct from evaporation without decomposition.14–18
Evaporation of crystalline MgO is one of the simplest cases of dissociative congruent evaporation that has been experimentally investigated so far. Ref. 3 conducted thermal desorption experiments of crystalline thin films of MgO and detected mass signals of atomic Mg and O, indicating that MgO evaporates by the reaction MgO (s) → Mg (g) + O (g). The kinetics of MgO evaporation was also investigated by Ref. 2, where the evaporation rates were quantified by measuring the weight losses in the polycrystalline MgO samples after heating at 1880–2180 K in vacuum. The reported data yield the activation energy for the evaporation of MgO of 542 ± 9 kJ mol−1. This value is smaller than the enthalpy of the reaction MgO (s) → Mg (g) + O (g) (ΔH0 = 982 kJ mol−1 at 2000 K19) as is typical for dissociative congruent evaporation.
The heterogeneous chemical dynamics of dissociative congruent evaporation, particularly on crystalline surfaces, has attracted interest in order to understand its kinetics from a microscopic point of view. For example, Ref. 8 discussed the evaporation mechanisms of crystalline Mg2SiO4 (forsterite) based on the morphologies of three crystallographic surfaces after evaporation. Combining these observations with experimental kinetic data, they concluded that the evaporation is governed by lateral motion of steps or direct detachment from the crystal surface depending on the temperature and surface orientation. In Ref. 12, evaporation of GaAs from the surfaces of three crystallographic orientations was investigated by observing gas-phase species. As a result, they found that GaAs evaporates congruently below ∼900 K as Ga (g) and As2 (g) and proposed that the evaporation of GaAs is controlled by the desorption of a hypothetical surface phase of Ga produced by the decomposition of the crystal lattice. However, it is still difficult to develop a unified understanding of the dynamics of dissociative congruent evaporations from these limited specific experiments. Consequently, there is currently no dynamics-based general theory capable of describing experimental kinetic data, including absolute rates and activation energies.
However, as explained above the Hertz–Knudsen equation is essentially derived as the evaporation rate when the whole system is in equilibrium. This is apparent from the fact that the molecular species commonly considered in the Hertz–Knudsen equation are those equilibrated with the condensed phase,6,9,13,22 which can be different from the actual products of evaporation in non-equilibrium (e.g., the products of evaporation of MgO in the vacuum experiments are Mg (g) and O (g),3 while the dominant gas species in equilibrium with MgO (s) are Mg (g) and O2 (g)19). Thus, when the Hertz–Knudsen equation is applied to non-equilibrium conditions, both the ideal evaporation rate and γ lose clear physical meanings. Consequently, the comparison between the ideal rate and the experimental non-equilibrium evaporation rates, as well as the evaluation of γ, does not provide further insights into the kinetics nor dynamics of dissociative congruent evaporation. It is also possible to calculate the evaporation rates for metastable species using the Hertz–Knudsen equation,2,4 but such calculations are not even supported by the detailed balance, and their ability to describe non-equilibrium conditions is uncertain.
In this study, we propose another theoretical approach capable of describing dissociative congruent evaporation as a non-equilibrium process. Considering that previous experimental studies often focused on obtaining macroscopic evaporation rates and activation energies, a statistical reaction rate theory is first desirable to interpret these experiments. Therefore, here, we derive the absolute rate of dissociative congruent evaporation based on the transition state theory as an extension of the theory for single-component evaporation without decomposition.23–25 In general, the transition state theory enables the calculation of absolute reaction rates under non-equilibrium conditions solely from the statistical properties of reactive systems without requiring detailed microscopic dynamics. Taking advantage of this, we can calculate absolute rates of specific evaporation reactions by assuming the properties of the transition state. This provides further insights into the reaction dynamics of dissociative congruent evaporation through comparison with experiments. In particular, the activation energy is shown to be sensitive to the number of molecules at the transition state, which depends on the extent that the decomposition has been completed at the transition state. To test the validity of the theory, we apply it to the evaporation of MgO solid and show that there is an activation barrier at a late stage of the reaction where the decomposition is almost achieved. In addition, we show the statistical mechanical reformulation of the Hertz–Knudsen equation, which can be directly compared to the present non-equilibrium evaporation rate based on the transition state theory. This enables us to discuss the physical meaning of the ideal evaporation rate of the Hertz–Knudsen equation as the rate of non-equilibrium dissociative congruent evaporation.
The paper is organized as follows: in Sec. II, we show the derivation of the absolute rate of dissociative congruent evaporation. In Sec. III, we apply the theory to evaporation of MgO solid and compare the theoretical evaporation rate to the experimental data, based on which implications for the reaction dynamics of evaporation of MgO are discussed. We also discuss the physical meaning of the Hertz–Knudsen equation by reformulating it using statistical mechanics, followed by the conclusion in Sec. IV.
II. THEORY
The transition state theory26–28 describes absolute reaction rates by a statistical approach based on the concept of a transition state, which is located at a saddle point of a potential energy surface between reactants and products. The reaction rate is given by the rate with which molecular systems pass over the transition state in the forward direction along the reaction coordinate.
A basic assumption of the transition state theory is that the reactants are distributed among their states in accordance with the Boltzmann distribution. In addition, it requires the following assumptions: (i) molecular systems that have crossed the transition state in the direction of products cannot turn back, and (ii) in the transition state, motion along the reaction coordinate can be separated from the other motions and treated in terms of a classical translation. It has been shown that under assumption (i), the concentrations of the molecules in the transition state that are becoming products can be calculated using the equilibrium theory even when the whole system is not in equilibrium,29,30 which we also use in the following derivation.
As the reaction coordinate at the transition state, we choose collective coordinates32–34 representing the translational motions of the l transition-state molecules that are perpendicular to the surface of the condensed phase. On the other hand, based on assumption (ii), the motion along the reaction coordinate should be, in principle, one-dimensional at the transition state. Here, we consider that the collective coordinates are mutually dependent on the transition state, constituting a single one-dimensional reaction coordinate. This requirement corresponds to the fact that evaporation into multiple molecules needs to proceed in a concerted way to maintain the stoichiometry of the reactant in dissociative congruent evaporation. In the following derivation, the reaction coordinate is first treated as if it is a set of coordinates with l independent degrees of freedom, which, however, does not provide a single solution due to the excessive degrees of freedom of the molecular system at the transition state. Then, we later introduce additional equations [Eq. (6)] to ensure the preservation of the macroscopic stoichiometry during evaporation. The requirement of congruency results in the reduction in the degrees of freedom at the transition state and enables us to reach the final result.
In general, the transition state theory defines the dividing surface as what separates reactants and products at the configuration of no return orthogonally to the reaction coordinate. The reaction rate is then calculated by counting the number of molecular systems passing through this dividing surface per unit time. For the present case, the dividing surface has (3n − l) dimensions orthogonal to the l collective reaction coordinates out of 3n total degrees of freedom of the molecular system. Since these collective coordinates are defined to be perpendicular to the surface of the condensed phase (i.e., geometrically parallel to each other), motions of the molecular system on the dividing surface are within a two-dimensional thin layer in a real space that separates the reactant condensed phase and the product gas phase parallel to their interface (Fig. 1). Here, we consider that among these (3n − l) degrees of freedom, each molecule has two translational degrees of freedom, which are geometrically two-dimensional translations parallel to the condensed phase surface. In that case, they are regarded as delocalized and thus follow Boltzmann statistics for indistinguishable particles.
Because includes the translational partition functions for two degrees of freedom parallel to the surface of the condensed phase as explained above, it is proportional to the surface area S, meaning that J does not depend on S. When l = 1, Eq. (13) is the same as the previously proposed expression of the evaporation rate of a single-component molecular liquid,23 indicating that single-component evaporation is a specific case of the present theory for dissociative congruent evaporation.
Schematic of the energy profile of evaporation and the relation with the geometry of the reactive system. The horizontal axis for the potential energy curve represents the reaction coordinate that is perpendicular to the surface of the condensed phase. The dividing surface is located between the reactant condensed phase and the product gas phase, separating them perpendicularly to the reaction coordinate (i.e., in parallel to the surface of the condensed phase). The transition state defined with this dividing surface thus occurs in the middle of the reaction path of the decomposition from the condensed phase to the product molecules.
Schematic of the energy profile of evaporation and the relation with the geometry of the reactive system. The horizontal axis for the potential energy curve represents the reaction coordinate that is perpendicular to the surface of the condensed phase. The dividing surface is located between the reactant condensed phase and the product gas phase, separating them perpendicularly to the reaction coordinate (i.e., in parallel to the surface of the condensed phase). The transition state defined with this dividing surface thus occurs in the middle of the reaction path of the decomposition from the condensed phase to the product molecules.
III. RESULTS AND DISCUSSION
A. Application to evaporation of MgO solid
(a) Arrhenius plot of the experimental evaporation rates of MgO solid.2 The linear fitting of the data (shown by the solid line) yields Ea = 542 ± 9 kJ mol−1. (b) Arrhenius plot of the calculated evaporation rate of MgO solid for the extremely “late” barrier case (the blue dashed line) and the extremely “early” barrier case (the red dashed line), shown with the experimental evaporation rates.2
(a) Arrhenius plot of the experimental evaporation rates of MgO solid.2 The linear fitting of the data (shown by the solid line) yields Ea = 542 ± 9 kJ mol−1. (b) Arrhenius plot of the calculated evaporation rate of MgO solid for the extremely “late” barrier case (the blue dashed line) and the extremely “early” barrier case (the red dashed line), shown with the experimental evaporation rates.2
In reaction (17), MgO solid is completely dissociated into the same species as the products (atomic Mg and O) at the transition state. This situation is realized at least when the evaporation of MgO solid is a barrierless reaction, in which the transition state locates distant from the reactant along the reaction coordinate,37 and thus, is virtually identical to the products. On the other hand, in reaction (18), Mg and O atoms are not yet separated and exist as a MgO molecule at the transition state. This indicates that the potential energy barrier occurs at an early stage of the reaction. Thus, reactions (17) and (18) can be contrasted as extremely “late” and “early” barrier reactions, where the locations of the transition state are very close (or even identical for the former case) to the product and the reactant, respectively.34,38
To calculate the evaporation rate for these cases, we assume that the rotations and the surface-parallel translations of the transition-state molecules are completely free just as gas-phase molecules without any hindrance originating from interactions with the surface of the condensed phase (two-dimensional ideal gas39). This approximation is valid when the energy kBT (∼17 kJ mol−1 at 2000 K) exceeds the barrier height for the molecules to rotate or move parallel to the surface but otherwise overestimates the corresponding partition functions.40,41 For the energy barrier E0, we used the internal energy difference between MgO (s) and Mg (g) + O (g), 949 kJ mol−1 (=ΔH0 − 2RT at 2000 K).19 This is correct for the barrierless (i.e., the extremely “late” barrier) case but could be smaller than the actual E0 of the “early” barrier.
Partition functions per degree of freedom and parameters used for the calculations of the evaporation rates.
General formula . | Partition function . | Parameter . | Value (T = 2000 K) . |
---|---|---|---|
Translation (per unit length) | |||
, L: length of the system and m: molecular mass | m = 24.3 amu | 1.26 × 1011 m−1 | |
m = 16.0 amu | 1.02 × 1011 m−1 | ||
m = 32.3 amu | 1.46 × 1011 m−1 | ||
Rotation | |||
, I: moment of inertial | |||
I = 29.3 amu Å2 a | 49.2 | ||
Vibration | |||
, ν: vibrational frequency | ν = 785 cm−1 a | 2.32 | |
ν = 443 cm−1 b | 3.66 | ||
Electron | |||
, gi: degeneracy of the ith state and Ei: energy of the ith state | |||
1S0: g = 1 | 1 | ||
3P2: g = 5 (ground state) | 8.53 | ||
3P1: g = 3, E = 158.3 cm−1 c | |||
3P0: g = 1, E = 227.0 cm−1 c | |||
1Σ+: g = 1 | 1 |
General formula . | Partition function . | Parameter . | Value (T = 2000 K) . |
---|---|---|---|
Translation (per unit length) | |||
, L: length of the system and m: molecular mass | m = 24.3 amu | 1.26 × 1011 m−1 | |
m = 16.0 amu | 1.02 × 1011 m−1 | ||
m = 32.3 amu | 1.46 × 1011 m−1 | ||
Rotation | |||
, I: moment of inertial | |||
I = 29.3 amu Å2 a | 49.2 | ||
Vibration | |||
, ν: vibrational frequency | ν = 785 cm−1 a | 2.32 | |
ν = 443 cm−1 b | 3.66 | ||
Electron | |||
, gi: degeneracy of the ith state and Ei: energy of the ith state | |||
1S0: g = 1 | 1 | ||
3P2: g = 5 (ground state) | 8.53 | ||
3P1: g = 3, E = 158.3 cm−1 c | |||
3P0: g = 1, E = 227.0 cm−1 c | |||
1Σ+: g = 1 | 1 |
Comparing these results to the experimental data, the experimental activation energy [Ea = 542 ± 9 kJ mol−1, Fig. 2(a)] is slightly larger than that of the extremely “late” barrier case and much smaller than that of the extremely “early” barrier case. Because the pre-exponential terms do not largely differ between Jlate and Jearly, the absolute rates also show the same tendency: the experimental rate is smaller than the rate of the extremely “late” barrier case only by 1–2 orders of magnitude, while it is larger by ∼9 orders of magnitude than the rate of the extremely “early” barrier case. This implies that the evaporation of MgO solid is likely to be the “late” barrier reaction rather than the “early” barrier reaction, which is consistent with the expectation from its endothermicity.42 On the other hand, it should not be completely barrierless (extremely “late” barrier), considering the larger experimental activation energy than the theoretical value calculated by assuming the extremely “late” barrier case. Therefore, we infer that there is a potential energy barrier at the location slightly before the products along the reaction coordinate, and the MgO solid is almost, but not completely, converted into the product atomic gas at the energy barrier (Fig. 3).
Schematic of the potential energy of the evaporation of MgO solid along the reaction coordinate. The blue and red dotted curves show the energy profiles of the extremely “late” barrier (barrierless) and extremely “early” barrier cases, respectively. The experimental data of evaporation of MgO solid suggest that there is an energy barrier closer to the product as shown by the black line. The barrier height E0 is equal to (for barrierless case) or larger than (for earlier barrier case) the potential energy difference between the reactant and the product, which is designated as ΔE.
Schematic of the potential energy of the evaporation of MgO solid along the reaction coordinate. The blue and red dotted curves show the energy profiles of the extremely “late” barrier (barrierless) and extremely “early” barrier cases, respectively. The experimental data of evaporation of MgO solid suggest that there is an energy barrier closer to the product as shown by the black line. The barrier height E0 is equal to (for barrierless case) or larger than (for earlier barrier case) the potential energy difference between the reactant and the product, which is designated as ΔE.
Note that the above-mentioned discussion is not largely affected by the simplicity of the approximation that we have made here about the properties of the transition state. Since both the possible larger internal energy E0 and the hindered rotations and translations of the MgO molecules at the “early” barrier result in the decrease in Jearly, the discrepancy between the extremely “early” barrier case and the experiments could be even larger. On the other hand, the difference in the activation energy between the extremely “late” barrier case and the experiments is not likely to be ascribed only to the free translation approximation because the temperature dependence of the partition functions is not significant even when the hindered translators are considered.40 This means that based on the present theory, even the simplest model can provide the implication about the reaction dynamics of evaporation of MgO.
B. Comparison with the Hertz–Knudsen equation
One should notice that the statistical mechanical expression of the ideal rate of the Hertz–Knudsen equation [Eq. (28)] has a similar form to Eq. (13) derived from the transition state theory. They become equal when the transition state is identical to the equilibrated products in terms of the internal energy and the molecular structures and can be regarded as two-dimensional ideal gas with free rotations and surface-parallel translations35 (i.e., , l = leq, and ). This means that in non-equilibrium conditions, the ideal rate of the Hertz–Knudsen equation can be interpreted as the rate of evaporation with the “ideal transition state” having the above-mentioned properties.
The difference between Eq. (28) and the actual rate can arise both from the pre-exponential and exponential terms. If rotations and/or translations of the transition-state molecules are hindered, Eq. (28) overestimates the pre-exponential term, as previously pointed out for evaporation without decomposition.23–25 At higher temperatures where those hindered motions approach the free rotor and translator limits,40,41 the effect of the exponential term becomes more important. When the average energy of the transition state per molecule E0/l is larger (smaller) than that of the equilibrated products, J is expected to be smaller (larger) than the ideal rate of the Hertz–Knudsen equation with γ exponentially dependent on the temperature. However, as discussed earlier, experimental evaporation rates often agree with the ideal rate to some extent with small temperature dependence of γ, suggesting that E0/l and are not largely different. Such agreement is expected when the stabilization from the transition state to the equilibrated products associated with the decrease in one molecule (i.e., ) is comparable to the activation energy ∼E0/l. For the case of MgO and presumably for other oxides, this situation is likely to be achieved reflecting the similarity between the activation energy (542 ± 9 kJ mol−1 for MgO) and the internal energy change in the reaction 2O (g) → O2 (g), 494 kJ mol−1,19 in which the number of molecules decreases by 1 (Fig. 4). Further verification of this condition for the agreement between experiments and the Hertz–Knudsen equation requires speciation of the transition state for a wide range of substances that evaporate by dissociative congruent evaporation.
Internal energy difference (in kJ mol−1) among 2MgO (s), the experimental products 2Mg (g) + 2O (g), and the equilibrium species 2Mg (g) + O2 (g) at 2000 K. As discussed in Sec. III A, the experimental activation energy 542 ± 9 kJ mol−1 is close to the average energy of the experimental products, 1897/4 = 474 kJ mol−1. Due to the similarity between these values and the energy difference between 2O (g) and O2 (g), 494 kJ mol−1, the average energy of the equilibrium species is also similar (1403/3 = 468 kJ mol−1).
Internal energy difference (in kJ mol−1) among 2MgO (s), the experimental products 2Mg (g) + 2O (g), and the equilibrium species 2Mg (g) + O2 (g) at 2000 K. As discussed in Sec. III A, the experimental activation energy 542 ± 9 kJ mol−1 is close to the average energy of the experimental products, 1897/4 = 474 kJ mol−1. Due to the similarity between these values and the energy difference between 2O (g) and O2 (g), 494 kJ mol−1, the average energy of the equilibrium species is also similar (1403/3 = 468 kJ mol−1).
IV. CONCLUSION
In this study, we formulated the absolute rate of dissociative congruent evaporation based on the transition state theory and applied it to the evaporation of MgO solid. In the derived expression of the rate of dissociative congruent evaporation, the activation energy closely corresponds to the average energy of the molecules at the transition state, reflecting the degree of decomposition at the potential energy barrier. Consequently, by comparing the theoretical and the experimental evaporation rates, we were able to discuss the location of the activation barrier along the reaction coordinate of the evaporation of MgO. As a result, it was suggested that the barrier occurs at a late stage of the reaction, where the decomposition into product atoms (Mg and O) is almost achieved.
Although the present theory is expected to be generally applicable to dissociative congruent evaporation, the evaporation products are not always experimentally confirmed, as in the case of MgO solid. A wider application of this theory will be possible through experimental speciation of evaporation products from a wider variety of compounds. It is also expected that the properties of the transition state of dissociative congruent evaporation inferred from the present theory will be compared to precise quantum mechanical computations. Another application of this theory will be the evaluation of kinetic isotope effects in evaporation, which is currently in progress.
As our understanding of the heterogeneous reaction dynamics of dissociative congruent evaporation is still limited, the statistical rate theory is an essential approach to interpret the experimental kinetic data of evaporation under non-equilibrium conditions. On the other hand, it is also desirable for the molecular-level evaporation dynamics to be uncovered through future experimental studies and to be theoretically connected to the macroscopic evaporation kinetics.
ACKNOWLEDGMENTS
This work was supported by JSPS Kakenhi (Grant No. 20H05846). The authors thank Professor Naoki Watanabe for the helpful discussions and the two anonymous reviewers for the constructive comments.
AUTHOR DECLARATIONS
Conflict of Interest
The authors have no conflicts to disclose.
Author Contributions
Shiori Inada: Conceptualization (equal); Data curation (lead); Formal analysis (lead); Methodology (lead); Validation (equal); Visualization (lead); Writing – original draft (lead); Writing – review & editing (equal). Tetsuya Hama: Conceptualization (equal); Validation (equal); Writing – review & editing (equal). Shogo Tachibana: Conceptualization (equal); Funding acquisition (lead); Project administration (lead); Supervision (lead); Validation (equal); Writing – review & editing (equal).
DATA AVAILABILITY
The data that support the findings of this study are available from the corresponding author upon reasonable request.