Jack E. Fulker and
Wendy A. Brown*
Department of Chemistry, University of Sussex, Falmer, Brighton, BN1 9QJ, UK. E-mail: w.a.brown@sussex.ac.uk
First published on 5th November 2024
Complex organic molecules (COMs) have been detected in a wide range of astrophysical environments, including the interstellar medium, comets and proto-planetary disks. The icy mantles that form on dust grains in these environments are thought to be the chemical nurseries that allow the formation of many of the COMs that have been identified. As such, the adsorption, thermal processing and desorption of COMs from dust grain surfaces are important in understanding the astrochemical networks as a whole. To study these processes, surface science techniques (temperature programmed desorption (TPD) and reflection absorption infrared spectroscopy (RAIRS)) have been used to investigate ices of the simple esters, methyl acetate and methyl propanoate, adsorbed on a graphitic dust grain analogue surface (highly oriented pyrolytic graphite, HOPG) at 28 K. From the TPD experiments, kinetic parameters have been determined for the desorption of the esters from graphite. The data show a clear coverage dependence for the desorption energies and pre-exponential factors in the sub-monolayer regime. For methyl acetate, the desorption energies and pre-exponential factors range from 57.1 ± 0.4 to 47.2 ± 0.3 kJ mol−1 and 3.1 × 1019±0.2 to 1.6 × 1019±0.1 s−1 respectively. For methyl propanoate the same parameters range from 57.0 ± 0.1 to 51.0 ± 0.1 kJ mol−1 and 7.7 × 1019±0.1 to 4.4 × 1019±0.1 s−1. As expected, neither ester shows coverage dependent values for multilayer ices. The determined desorption energies and pre-exponential values for the multilayer ices are 43.5 ± 0.9 kJ mol−1 and 4.2 × 1032±0.4 molecules cm−2 s−1 for methyl acetate and 45.7 ± 0.9 kJ mol− 1 and 8.7 × 1029±0.4 molecules cm−2 s−1 for methyl propanoate. Experimental RAIRS data were also recorded, showing that the ices undergo an irreversible phase change from an amorphous to a crystalline structure when thermally processed. This study provides fundamental data for use in astrochemical models as well as the basis for a future investigation of methyl acetate and methyl propanoate adsorbed in mixed ice environments with water ice.
Experimental research therefore plays an important role in astrochemistry, with spectroscopic studies providing valuable reference data to both validate current observations and also give approximate target regions for the search for new species.3 Additionally, kinetic data retrieved from temperature programmed desorption (TPD) experiments (both quantitative parameters and qualitative behaviour) can be used in theoretical models to better describe the adsorption and desorption processes that occur in these interstellar environments, for example, in astrochemical simulations of gas–grain chemistry in the interstellar medium or the snowline chemistry of protoplanetary disks.6–8
One particularly under-researched phenomenon in this area is the effect of coverage-dependent kinetic desorption parameters. Thin film molecular ices are generally categorised as either sub-monolayer/monolayer or multilayer ices, each obeying certain desorption characteristics according to observed standards in the literature.9 This in itself is coverage dependent behaviour, however, previous TPD studies have shown that within the sub-monolayer regime, the kinetic parameters vary considerably due to intermolecular interactions.10–12 These effects are often omitted from theoretical models, with many groups opting to treat these sub-monolayer ices with averaged kinetic parameters. This research aims to extend the work of Ligterink et al.13 in applying their Transition-State-Theory (TST) methods to two test species (methyl acetate and methyl propanoate) to show how the calculated kinetic parameters vary for these highly coverage dependent data sets. This is with a view to using these coverage dependent kinetic parameters in astrochemical simulations of gas–grain exchange. Such models currently account for binding energy distributions derived from different binding sites on the surface, but do not yet explicitly consider the other interactions, such as intermolecular repulsions described here.14–16
Methyl acetate (Fig. 1) is a COM that has been detected in the Orion nebula and on comet 67P/Churyumov–Gerasimenko, making it an appropriate and relevant species for this study.17 COMs containing the ester functional group are of particular interest to astrochemists and astrobiologists, as they are believed to act as building blocks for prebiotic species such as amino acids, and could therefore play an early role in the origins of life.18–20 Such acetyl amino acids have also been identified in primitive meteorites along with their precursors, including methyl acetate and several other esters.21,22 Possible routes of formation and destruction of methyl acetate in the interstellar medium also include propionic acid formation, a likely precursor for the formation of another simple ester–methyl propanoate (Fig. 1).23 Although methyl propanoate has not yet been observed in astrophysical environments, with the current state of observational astrochemistry constantly discovering new COMs of similar sizes and with the same functional groups, methyl propanoate has been theorised as a likely candidate for interstellar detection in the future.24 As such, experimental studies into these likely candidates are important for validating and supporting both observational and theoretical studies.
In addition to astrochemical studies, the interactions of simple esters and graphitic substrates are also important in atmospheric chemistry. Methyl acetate and methyl propanoate are established pollutants that exist in the Earth's atmosphere as a consequence of industrial processes across the planet.25,26 Several studies have shown that these species play a role in atmospheric ozone formation and that their lifetimes in the atmosphere are dictated by oxidation mechanisms with initiators such as chlorine, hydroxyl, and nitro radicals.25–28 Despite the conditions of the interstellar medium and the Earth's atmosphere being very different, the same principles of gas phase reactions dictate how these species can interact, and so particulates of polycyclic aromatic hydrocarbons (PAHs) can play the same role as carbonaceous dust grains to provide surfaces for reactive species to accrete onto.29 As such, the adsorption and desorption behaviour of COMs on graphitic substrates is also important to atmospheric chemistry, particularly for the simulation of pollutant lifetimes.
Interstellar dust grains are primarily composed of rough and porous carbonaceous or siliceous material and are therefore difficult to simulate reproducibly in a laboratory environment.30 Several different surface analogues have been used by experimentalists to date, with highly ordered metallic surfaces including gold,31,32 silver,33,34 copper,35,36 nickel,37 and platinum38 being generally preferred to give reproducible data that compare well with theoretical models. Highly oriented pyrolytic graphite (HOPG), the surface used in this work, is another commonly used surface,39–43 as it provides a uniform carbonaceous surface that gives reproducible results as well as being a semi-metal that obeys the metal-surface selection rule, thus allowing for reflection absorption infrared spectroscopy (RAIRS) to be performed.44–46 In addition to adsorption/desorption studies, HOPG has been widely used to investigate the formation of small molecules and COMs, providing the basis for many theoretical studies into both gas and solid phase reaction networks of astrochemical environments.47–50 When comparing highly ordered vs. rough, porous graphitic surfaces, there is likely to be some variation in the kinetic desorption parameters. However, the methods described here show that these parameters are highly coverage dependent even on the HOPG surface, thus highlighting the need for these kinetic parameters to be given as a range of values as opposed to the discreet values usually reported.
Previous surface science investigations of methyl acetate and methyl propanoate provide reference data for comparison to the work described here. Zahidi et al. investigated methyl acetate (as well as methyl formate and ethyl formate) chemisorbed on a Ni(111) surface.37 This study used RAIRS and TPD to investigate the annealing of the esters between 140 K and 350 K.37 Methyl acetate began thermal decomposition at ∼180 K to produce adsorbed methoxy, acetyl, and carbonyl species. The methoxy species was unstable and immediately dissociated, while the acetyl species was stable up to 300 K. While chemisorbed methyl acetate is not directly comparable to the physisorbed ices investigated here, the thicker, condensed phase, ices studied by Zahidi et al.37 are relevant to the multilayer ices described here. A study by Sivaraman et al. investigated the electron irradiation of methyl acetate ices on a ZnSe surface.51 Similar decomposition products to those reported in the work of Zahidi et al.37 were identified, with the addition of more stable methoxy species. Another infrared investigation focused on methyl acetate condensed on a gold substrate.52 It was found that ices grown at 12 K formed an amorphous structure and upon thermal processing to between 110 K and 120 K, the ice underwent an irreversible phase change to a crystalline structure. This hypothesis was supported by the observation of shifts and splitting in the fundamental, overtone, and combination bands of the infrared spectra. Several infrared studies of methyl propanoate adsorbed on non-graphitic substrates (KBr,24 ZnSe,53 and Cs I23) have been undertaken and show spectra that can be compared to the work described here. These studies also reported a phase change for methyl propanoate at 120 K, similar to that observed for methyl acetate.
With the adsorption/desorption processes of COMs from carbonaceous particulates and dust grains being important to the fields of both astrochemistry and atmospheric chemistry, methyl acetate and methyl propanoate ice adsorption and thermal processing on an HOPG surface have been studied using surface science techniques. TPD experiments have been performed to investigate the desorption and crystallisation of the esters on HOPG, and RAIRS experiments have been undertaken to follow how the surface structure of the molecular ices changes when thermally processed. These studies aim to provide reference data to aid in future astrochemical detection efforts and coverage dependent kinetic parameters for use in theoretical models of gas–grain exchange processes.
When growing molecular ices on a cryogenically cooled surface at 28 K, the sticking probability is assumed to be equal to one, meaning that if a gas phase molecule collides with the surface then it will accrete and become part of the ice. This sticking probability is closely related to the surface temperature, and so an increased temperature (up to 120 K in this work) leads to a reduction in the sticking probability, with fewer gas-surface collisions leading to additions to the ice. This was accounted for by increasing the dosing exposures when dosing gases at a higher surface temperature than base temperature. TPD experiments were then used to check that comparable amounts of ice had been deposited at the higher temperature.
TPD experiments were conducted by resistive heating of the HOPG surface at a rate of 0.5 ± 0.01 K s−1. Thermal desorption of the esters was monitored using a quadrupole mass spectrometer (QMS, Hiden HAL 301/PIC). The parent ions as well as several fragment masses were followed for each ester, with m/z = 43 and 57 giving the strongest signals for the desorption of methyl acetate and methyl propanoate respectively.
RAIRS experiments were performed using a Fourier transform infrared (FTIR) spectrometer (Thermo Nicolet 6700) coupled to an external liquid nitrogen cooled mercury–cadmium–telluride (MCT) detector. All spectra were recorded as the coaddition of 256 scans at 4 cm−1 resolution, taking 2 minutes 40 seconds to collect each spectrum (approximately 0.63 seconds per scan). Annealing experiments involved heating the HOPG surface in increments of 10 K and holding the temperature for 3 minutes before cooling to base temperature to record the infrared spectrum.
Gaussian16 was used to calculate the rotational constants of the two esters to obtain the principal moments of inertia for use in TST analysis of TPD data (described later). These calculations were run at the CAM-B3LYP/aug-cc-pVDZ level of theory.58,59 These calculations treat the esters as monomers in the gas phase, rather than as adsorbates on a surface, but the values are used to predict how the species transition between the two phases, and are therefore a good representation of the desorption process.
Fig. 2 shows a series of infrared data recorded for methyl acetate. The red and blue traces show the experimental RAIR spectra of 400 Lm methyl acetate ices adsorbed on HOPG at 28 K and 120 K respectively.27 With the 120 K surface being hotter than the 28 K base temperature, the sticking probability of molecules landing on the surface was decreased, and so the exposures had to be adjusted so that the ice coverages were comparable.
Beginning with the methyl acetate ice grown at 28 K in Fig. 2 (red trace), the most intense peaks at 1753 cm−1 and 1269 cm−1 are assigned to the carbon–oxygen stretches of the carbonyl and ester functional groups respectively. Other peaks at 1450 cm−1 and 1371 cm−1 are the asymmetric and symmetric bends of the CH3 groups respectively, while the 1057 cm−1 peak is assigned to the stretching mode of the O–CH3 group. Although much lower in intensity than the other bands, the C–H stretching modes of the CH3 groups are also identified at 2958 cm−1 and 3001 cm−1. The assignments of the observed infrared bands are given in Table 1, along with a comparison to the literature.
Assignment | This work | Literature | ||||
---|---|---|---|---|---|---|
Dosed at 28 K | Dosed at 120 K | KBr surface60 | Au Surface52 | |||
Amorphous | Crystalline | Amorphous | Crystalline | |||
a Symbols: symmetric stretching (νs), asymmetric stretching (νas), symmetric bending (δs), asymmetric bending (δas), and rocking (ρ), shoulder (sh). | ||||||
νas (C)CH3 | 3020 (sh) | 3032 | — | — | 3022 | 3031 |
νas (O)CH3 | 3022 | — | — | — | 3022 | |
νas (O)CH3 | 3001 | 3001 | 2999 | 3001 | 2998 | 3001 |
νas (C)CH3 | 2987 (sh) | — | — | — | 2987 | |
νs (O)CH3 | 2958 | 2958 | 2958 | 2957 | 2957 | 2959 |
νs (C)CH3 | 2941 (sh) | 2941 (sh) | — | — | 2942 | 2941 |
ν CO | 1753 | 1740 | 1741 | 1723 | 1736 | 1726 |
δas (O)CH3 | 1495 (sh) | 1495 | — | — | 1491 | 1495 |
δas (O)CH3 | 1473 (sh) | 1471 | — | — | 1465 | 1469 |
δas (C)CH3 | 1450 | 1458 (sh) | — | — | — | 1457 |
δas (C)CH3 | 1450 | — | — | — | 1448 | |
δs (O)CH3 | 1440 | 1441 | 1448 | 1440 | 1439 | |
δs (C)CH3 | 1377 | 1383 | 1372 | 1381 | 1369 | 1365 |
ν C(O)–O | 1269 | 1267, 1250 (sh) | 1254 | 1251 | — | 1278 |
ρ (O)CH3 | — | 1186 | — | — | 1192 | 1186 |
ρ (O)CH3 | — | 1161 | — | — | 1158 | 1160 |
ν O–CH3 | 1057 | 1057 | 1050 | 1054 | 1044 | 1048 |
ρ (C)CH3 | — | 1032 | — | — | — | 1036 |
ρ (C)CH3 | 984 | 991 | 981 | 989 | 977 | 990 |
Skel. Def | 852 | 856 | 851 | 854 | 849 | 853 |
Moving to the blue trace in Fig. 2, recorded for 400 Lm methyl acetate grown on HOPG at 120 K, some key differences in the RAIR spectrum compared to the red trace show that this ice has formed as a crystalline ice, as opposed to the amorphous methyl acetate grown at 28 K. The CO carbonyl peak sharpens and shifts by 13 cm−1, from 1753 cm−1 to 1740 cm−1, and a similar effect is observed for the C–O ester stretch, which shifts by 2 cm−1 from 1269 cm−1 to 1267 cm−1 and splits to reveal a shoulder at 1250 cm−1. Similar observations have been previously seen for the crystallisation of methyl formate and ethyl formate,10,62 which both showed a sharpening of the CO and C–O peaks due to a uniform alignment of the dipole moments in the crystalline ices.10,62 In addition, several peaks between 3032–2987 (CH3 stretching) and 1458–1440 cm−1 (CH3 bending) take the place of the broad features seen in the amorphous ice.
The infrared spectra recorded for methyl acetate grown at 28 K and 120 K are in good agreement with the transmission IR spectra of methyl acetate on KBr (Yarnall et al.)60 and with the RAIR spectra on Au (Sivaraman et al.),52 suggesting that similar amorphous and crystalline ices are being grown in this work.
A 100 Lm methyl acetate ice was also annealed between 28 K and 130 K in increments of 10 K to follow the thermal processing of the amorphous ice. These spectra are shown in Fig. S1.† No changes were observed in the spectrum between 28 K and 110 K, but upon heating to 120 K, the same shifts and peak splittings that were discussed earlier for Fig. 2 were observed. This suggests that the crystallisation behaviour is the same for thermally processed ices grown at 28 K and those grown at 120 K.
To investigate the amorphous and crystalline structures of methyl propanoate, the same RAIRS experiments were carried out as previously described. Fig. 3 shows RAIR spectra recorded for the adsorption of 100 Lm of methyl propanoate on HOPG at 28 K (red trace) and 120 K (blue trace), with the assignments given in Table 2.
Assignment | This work | Literature | |||
---|---|---|---|---|---|
Dosed at 28 K | Dosed at 120 K | KBr substrate24 | ZnSe substrate23 | ||
Amorphous | Crystalline | ||||
a Symbols: symmetric stretching (νs), asymmetric stretching (νas), bending/scissoring (δ), wagging (ω), twisting (τ), and rocking (ρ). | |||||
νas (O)CH3 | 3030 | 3030 | — | — | 3028 |
Individual and combination bands of: νas (O)CH3, νas (C)CH3, νs (O)CH3, νs (C)CH3, νas CH2, and νs CH2 | 3001 (sh), 2983 | 2997, 2987, 2978 | 2981 | 2998, 2995, 2986, 2976 | 2982 |
2956 | 2958, 2945 (sh) | 2953 | 2958, 2955, 2943 | 2951 | |
2930 | 2928 | 2925 | 2929 | 2927 | |
2886 | 2883 | 2883 | 2883 | 2884 | |
2852 | 2855, 2848 | 2851 | 2855, 2847 | 2848 | |
ν CO | 1747 | 1741 | 1741 | 1735, 1731 | 1739 |
δ (C)CH3 | 1444 | 1471, 1460 | 1463 | 1470, 1467, 1460, 1455 | 1461 |
ω (O)CH3 or ρ (O)CH3 | 1446, 1435, 1417 | 1439 | 1445, 1435, 1421, 1417 | 1439, 1418 | |
ω [CH3CH2] or ω (C)CH3 | 1363 | 1362 | 1362 | 1358 | 1362 |
ρ [CH3CH2] or ν (O)C–O | 1213 | 1209 | 1208 | 1200 | 1207 |
ρ [OCH3] | 1184 (sh) | 1184 | 1181 | 1178 | 1181 |
ω CH3 or ρ (C)CH3 | 1092 | 1092 | 1090 | 1091 | 1090 |
ν O–CH3 + | 1022 | 1022 | 1021 | 1021 | 1021 |
ν H3C–CH2 + ν O–CH3 | 970 | 964 | 966 | 963 | 965 |
ν C–C(O) + ν C(O)–O | 854 | 856 | 854 | 854 | 854 |
ρ (C)CH3 + ρ CH2 | 810 | 808 | 808 | 810, 807 | 807 |
Methyl propanoate behaves similarly to methyl acetate, with the infrared spectra of the amorphous and crystalline forms being distinguished from each other by distinct band shifts and splitting of broad features. This is evident in Fig. 3, with the peak at 1747 cm−1 (assigned to the CO carbonyl stretching mode) sharpening and shifting by 6 cm−1 to 1741 cm−1. This is also true for the C–O ester stretching mode at 1213 cm−1, which shifts to 1209 cm−1.
Similarly to methyl acetate, several broad features in the amorphous methyl propanoate spectrum at 2983 cm−1, 2956 cm−1 (CH3 and CH2 stretching), and 1444 cm−1 (CH3 and CH2 bending, wagging and/or rocking) split to give individual bands in the crystalline spectrum. While the infrared bands of methyl acetate were straightforward to assign, methyl propanoate proved more difficult, even with reference to the literature studies of Hudson et al.24 and Sivaraman et al.23 This is due to the extra CH2 group of methyl propanoate, which gives the molecule more flexibility around the skeletal structure, leading to most of the vibrational modes being combination bands of several stretching and bending motions. With this in mind, the assignments provided in Table 2 are only approximate descriptions. Despite this, the band positions of the experimental RAIRS in this work are in good agreement with spectra for amorphous and crystalline methyl propanoate grown on KBr by Hudson et al.24 and with the amorphous ice grown by Sivaraman et al.23 Annealing experiments were also performed for a 100 Lm methyl propanoate ice grown at 28 K, with similar results showing the amorphous to crystalline phase change at 120 K (Fig. S2†).
Fig. 4B shows that exposures of 50 Lm and higher lead to the formation of a high temperature shoulder at around 134 K, that increases in intensity as the coverage increases. This shoulder most likely arises due to the desorption of crystalline methyl acetate, the formation of which was seen previously in the RAIRS data. This was further investigated by growing a 150 Lm methyl acetate ice at 120 K (accounting for the change in sticking probability) to compare the differences in the desorption profiles. This is shown in Fig. 4C, with the same desorption features being present for both ices, but with the high temperature shoulder having much larger intensity. This confirms the assignment of the high temperature shoulder, seen in Fig. 4B, to the desorption of crystalline methyl acetate. RAIRS data (shown earlier) clearly showed the formation of crystalline methyl acetate following dosing at 120 K.
The structure of methyl propanoate differs from methyl acetate only by an extra CH2 group on the ester chain, as shown in Fig. 1. As such, the desorption and phase change behaviour of the two esters are expected to be similar. TPD data for pure methyl propanoate adsorbed on HOPG are shown in Fig. 5. As for methyl acetate, the low desorption temperatures suggest physisorption of the molecule on the HOPG surface. Fig. 5A and B show the desorption of increasing exposures of methyl propanoate, with very similar trends to those seen for methyl acetate (decreasing peak temperatures from repulsive interactions and a shared leading edge at higher coverages). However, an important distinction between the two esters is the slightly higher temperatures at which methyl propanoate desorbs from the HOPG surface, desorbing between 2 and 10 K higher than corresponding exposures of methyl acetate. This higher desorption temperature arises because methyl propanoate is the larger of the two species.
The desorption of the 50 Lm ice (Fig. 5B) shows two distinct desorption features at 134 K and 137 K, which are assigned to the desorption of amorphous and crystalline methyl propanoate, in line with the conclusions from the RAIRS data and with the observations seen for methyl acetate. As for methyl acetate, methyl propanoate ices were also grown at a higher temperature (120 K) to investigate the formation and desorption of crystalline methyl propanoate (Fig. 5C). Unlike the spectra recorded for methyl acetate, both the base temperature (red trace) and high temperature (blue trace) experiments in Fig. 5C show very similar desorption profiles. This is a consequence of the higher desorption temperature of multilayer methyl propanoate, where the desorption of amorphous methyl propanoate occurs at a very similar temperature to the phase change. Hence, the majority of the methyl propanoate ice crystallises before desorption and therefore only the desorption of crystalline ice is seen in the TPD spectra.
The analysis begins with identifying the point at which the ice growth changes from monolayer growth to multilayer growth, as the kinetic parameters of these two regimes are calculated using different methods (PW and TST). These two different analysis methods are required due to the coverage dependency of the energy of desorption and pre-exponential factor for the lowest exposure ices, described in detail later. The PW analysis treats these two parameters as constant, and is therefore only appropriate for describing the higher exposure, non coverage dependent, ices. However, TST can be used to calculate the energy of desorption and pre-exponential factors for each individual sub-monolayer exposure, showing exactly how these parameters change as a function of coverage.
The threshold for the beginning of multilayer ice growth is identified by comparing the desorption profiles of different ice thicknesses (Fig. 6A for methyl acetate and Fig. S3A† for methyl propanoate) so that plots can be constructed to determine the order of desorption (Fig. 6B and S3B†) from the relative coverages at a common desorption temperature for each TPD trace. This allows the exposure at which the change from monolayer to multilayer ice growth occurs to be determined very easily.
The starting point of this analysis is the Polanyi–Wigner equation (eqn (1)):67,68
(1) |
(2) |
Rearranging this equation and taking logarithms, and noting that only relative coverage θrel can be measured in the experiments described here, eqn (2) becomes:
(3) |
The desorption order can then be obtained by plotting a graph of ln[I(T)] versus ln[θrel] for a series of TPD curves of varying initial exposure at a fixed temperature. The gradient of this plot gives the order of desorption, n. These plots are shown in Fig. 6B for methyl acetate and Fig. S3B† for methyl propanoate.
The two regimes seen in Fig. 6B clearly indicate monolayer and multilayer desorption, with the change from monolayer to multilayer desorption for methyl acetate occurring at ∼30 Lm (Fig. 6B) and that for methyl propanoate (Fig. S3B†) occurring at ∼25 Lm. The monolayer order of desorption for methyl acetate from Fig. 6B is equal to 1.95. A desorption order of 2 would suggest second order desorption which can only be achieved via recombinative desorption. Since we know from the RAIRS data that the methyl acetate is physisorbed molecularly on the surface, then we know that dissociative adsorption does not occur. Hence, this high order of desorption occurs due to repulsive intermolecular interactions that occur between the sub-monolayer adsorbates, as already discussed. For methyl propanoate, the plot in Fig. S3B† gives a monolayer order of desorption of 1.45. For the same reasons as for methyl acetate, this again is not a realistic value. In light of this, the order of desorption for the sub-monolayer coverages of both esters was set to n = 1, the ideal value for first order desorption, in agreement with analysis undertaken for other molecules.11,13,62 The orders of desorption for multilayer methyl acetate and methyl propanoate are close to zero (n = 0.02 and 0.14 respectively), as expected for multilayer desorption.
The calculated multilayer order of desorption was then used to determine the energies of desorption (Fig. 6C) and pre-exponential factors for multilayer methyl acetate (30 Lm to 150 Lm) and methyl propanoate (30 Lm to 150 Lm). Rearrangement of eqn (3) gives eqn (4):
(4) |
Hence a plot of ln[I(T)] − nln [θrel] versus 1/T gives the energy of desorption from the gradient of the graph. An example desorption energy plot for multilayer methyl acetate is shown in Fig. 6C. The multilayer desorption energy is determined to be 42.8 ± 0.7 kJ mol−1 for an exposure of 50 Lm. Determining the desorption energy for all multilayer exposures of methyl acetate allows an average multilayer desorption energy for both amorphous and crystalline methyl acetate to be calculated, as shown in Table 3. Crystalline multilayer values are determined by peak fitting the TPD data to separate the two phases. An example of the peak fitting for methyl acetate is shown in Fig. S4.† For methyl propanoate, it is only possible to determine a desorption energy for the crystalline multilayer, also shown in Table 3, since the ice becomes crystalline prior to desorption as already discussed. Once the order and energy of desorption have been calculated, these can then be put into the Polanyi–Wigner equation to calculate the pre-exponential factor for multilayer desorption. The calculated pre-exponential values are also given in Table 3.
Methyl acetate | Desorption order | Edes/kJ mol−1 | Pre-exponential factor, ν |
---|---|---|---|
a The desorption order for monolayer ices was set equal to 1, as described in the text.b The order of desorption of crystalline multilayer was assumed to be 0.c Literature values for Edes and ν were reported by Ligterink et al.13 using TST analysis on the TPD data from Zahidi et al.37 | |||
Monolayer (amorphous) | 1a | 57.1 ± 0.4 → 47.2 ± 0.3 | 3.1 × 1019±0.2 → 1.6 × 1019±0.1 s−1 |
Multilayer (amorphous) | 0.02 ± 0.04 | 43.5 ± 0.9 | 4.2 × 1032±0.4 molec cm−2 s−1 |
Multilayer (crystalline) | 0b | 45.8 ± 0.9 | 1.6 × 1032±0.4 molec cm−2 s−1 |
Ligterink et al13 | — | 64.9c | 4.1 × 1019 s−1 |
The PW analysis works well for multilayer ices but does not work for monolayer ices if the desorption energy and pre-exponential factor are coverage dependent. As already described, for both monolayer methyl acetate and methyl propanoate the desorption temperature decreases with increasing exposure, due to the presence of repulsive interactions. In this case, both the desorption energy and pre-exponential factor change with exposure, which means that eqn (4) cannot be used to determine the desorption energy accurately. Hence an alternative method of analysis must be used to determine the monolayer desorption energies and pre-exponential factors. As such, these parameters were determined using the TST method, as described in detail elsewhere.13,47
The TST method can be applied to the experimental data to first determine ν using the values of the translational and rotational degrees of freedom of the adsorbed species:13,47
(5) |
(6) |
(7) |
The 3D translational partition function is calculated as follows:
(8) |
For methyl acetate and methyl propanoate, the kinetic parameters are highly exposure dependent, with the sub-monolayer desorption energies and pre-exponential factors gradually decreasing as the exposure increases. Fig. 7 shows this exposure dependence for both methyl acetate and methyl propanoate, with the methyl acetate sub-monolayer energies (panel A) decreasing from 57.1 ± 0.4 kJ mol−1 (0.5 Lm) to 47.2 ± 0.3 kJ mol−1 (20 Lm) – a decrease of 10 kJ mol−1. For 30 Lm and above, the multilayer forms and the energy of desorption plateaus to reach the coverage independent value of 43.5 ± 0.9 kJ mol−1. The same trend is shown for the pre-exponential factors (Table 3 and Fig. 7B), with a decrease in the value of the pre-exponential factor for methyl acetate as the exposure increases from 0.5 Lm to 20 Lm and a constant value for multilayer ices (not shown).
Similar trends in the desorption energies and pre-exponential factors are observed for methyl propanoate, with energy of desorption (Fig. 7A) and pre-exponential (Fig. 7C) values decreasing from 57 ± 0.1 kJ mol−1 and 7.7 × 10 19 s−1 (2 Lm) to 51 ± 0.1 kJ mol−1 and 4.4 × 10 19 s−1 (30 Lm) respectively.
The strong coverage dependence of the kinetic parameters for the lowest coverages is due to the repulsive interactions that govern the changing peak temperatures observed in Fig. 4A and 5A. These have been observed previously for COMs such as acetaldehyde, acetonitrile and benzene,11,12,48 as well as for other simple esters such as methyl formate and ethyl formate.10,62 From an astrochemical perspective, this coverage dependence is an important factor to consider when modelling the desorption of COMs from icy mantles, as a single set of kinetic parameters may not be sufficient to fully simulate the gas–grain mechanics, particularly when accounting for astronomical timescales of thousands of years.14–16
Although there have been several studies on the desorption behaviour of methyl acetate, only one monolayer energy of desorption has been reported and no values are available for the multilayer parameters. Ligterink et al. used TST and Redhead analysis to determine desorption energies for TPD data from previous studies across the literature,13 some of these values are presented in Table 4 for comparison with the coverage dependent parameters calculated in this work.13 For methyl acetate, they used TPD data from Zahidi et al. (values shown in Table 3).13,37 Their reported pre-exponential factor is similar to that calculated in this work, but their energy of desorption is considerably higher (an increase of 7.9 kJ mol−1). However, this is not unsurprising as the methyl acetate in that study is chemisorbed on Ni(111), whereas it is physisorbed on the HOPG surface used here.
Molecule | Mr | Edes/kJ mol−1 | Pre-exponential factor, ν/s−1 | Ref. |
---|---|---|---|---|
Acetonitrile | 43 | 48.3 → 44.7 | 3.9 × 1017 → 3.7 × 1017 | 69 |
50.0 → 35.0 | 1 × 1013 | 12 | ||
Acetaldehyde | 44 | 49.3 | 1.6 × 1018 | 13 |
36.7 | 7.7 × 1017 | 13 | ||
35.9 | 7.2 × 1017 | 13 | ||
Methyl formate | 60 | 38.0 | 2.2 × 1018 | 13 |
Methyl acetate | 74 | 57.1 ± 0.4 → 47.2 ± 0.3 | 3.1 × 1019±0.2 → 1.6 × 1019±0.1 | This work |
Ethyl formate | 74 | 45.7 | 1.3 × 1019 | 13 |
Methyl propanoate | 88 | 57.0 ± 0.1 → 51.0 ± 0.1 | 7.7 × 1019±0.1 → 4.4 × 1019±0.1 | This work |
The energy of desorption of crystalline methyl propanoate calculated in this work is 5.3 kJ mol−1 lower than that reported by Hudson et al.24 This difference is only just outside of the error bounds provided in that study. In that work, the energy of desorption was calculated via the construction of a Clapeyron plot from the vapour pressure of methyl propanoate. As such, the pre-exponential factor was not determined and can therefore not be compared to this work.
As there are no literature values for the kinetic desorption parameters of monolayer physisorbed methyl acetate or methyl propanoate, the values determined here have been compared to those of similar sized and functionalised molecules as well as the re-analysed data from Ligterink et al.13 These are presented in Table 4.
Starting by comparing the four esters (methyl formate, methyl acetate, ethyl formate, and methyl propanoate), there is a clear correlation between the kinetic parameters and molecular size, with the smallest (methyl formate) having the lowest desorption energy and pre-exponential factor. While methyl acetate and methyl propanoate have very similar energies of desorption for their respective lowest coverage, the pre-exponential factor for methyl propanoate is greater by over a factor of two, highlighting the importance of calculating and including both kinetic parameters in these studies, as opposed to assuming a standard value for the pre-exponential factor – a common practice in laboratory surface science studies. Acetonitrile and acetaldehyde values have also been included in Table 4 to show how smaller species compare. As expected, these generally have lower energies of desorption and pre-exponential factors.
Kinetic desorption parameters, such as those calculated in this work, have been previously used in astrochemical models to predict the desorption behaviour of ices under non-linear heating rates on timescales more relevant to the interstellar medium.70 These models demonstrate the importance of accurate kinetic parameters, with species such as methyl formate, glycolaldehyde and acetic acid desorbing on vastly different timescales under the same heating conditions despite being isomers of each other.70 With this in mind, the coverage dependence of the kinetic parameters for these esters (and similar species) can now be incorporated into these models to improve how the lowest coverages of COMs are treated in these simulations.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ra04466e |
This journal is © The Royal Society of Chemistry 2024 |