3.1. Modeling Effect under Altitude and Sea Level Conditions
The initial phase of the study focused on model calibration to reproduce the observed conversion efficiencies for CO and HC during steady-state tests conducted under warm sea-level and cold high-altitude conditions, as described in [
16]. The calibration tests are detailed in
Table 2 and
Table 3. In particular,
Table 2 displays the experimental data for warm sea-level conditions (0 m and 20 °C), and
Table 3 displays those corresponding to cold high-altitude conditions (2500 m and −7 °C).
Due to the absence of in these tests, the calibration was restricted to reactions excluding this species. Specifically, it focused on HC adsorption and desorption ( and ), CO (), and HC () oxidation reactions in the presence of . The calibration of kinetic constants for these reactions considered the effects of thermal transients on the oxidation and the adsorption-desorption equilibrium, as well as the influence of HC coverage on the reaction rate of the adsorption-desorption dynamics. This methodology facilitated a steady-state representation at test completion, distinguishing between HC oxidation and adsorption conversion efficiencies under varying environmental conditions.
In this initial part of the calibration, the objective function, defined by Equation (
5) and minimized using the simplex search method by Lagarias et al. [
42], represented the weighted sum of cumulative errors in conversion efficiency (
) for CO and HC. It considered the modulus of the error up to each time point (
t) for each pollutant species (
p).
The results of the CO and HC conversion efficiency of the experimental tests for both warm sea-level and cold altitude cases are shown in the contour maps in
Figure 1, which is analyzed in detail in [
16].
Figure 2 presents the modeling results of the steady-state tests under warm sea-level and cold high-altitude conditions. The comparison of the model results with experimental data, depicted in
Figure 1, points out its ability to simulate CO and HC conversion efficiencies accurately.
The comparison between
Figure 1a and
Figure 2a evidences how the model is able to capture the CO conversion behavior at the warm-sea level. The model successfully predicted the low reactivity fashion below 100 °C OC inlet temperature. Additionally, it accurately reproduced the enhancement in CO conversion efficiency and its sensitivity to variation in exhaust mass flow as temperature increased. Furthermore, the model identified the threshold in mass flow and temperature where 100% CO conversion was achieved.
Regarding the CO conversion efficiency under cold high-altitude conditions, as illustrated in
Figure 2c, the model reflected the changes in conversion efficiency, caused by modifying environmental conditions. Notably, it reproduced the increase in CO light-off temperature and the significant reduction in CO conversion efficiency at reduced exhaust mass flows, a trend more pronounced under cold high-altitude conditions than its warm sea-level counterpart.
The ability of the model to predict HC conversion efficiency under varying environmental conditions was further confirmed by comparing
Figure 2b,d with their corresponding experimental data (
Figure 1b,d). Notably, the model accurately predicted the dominance of zeolite adsorption at lower temperatures [
16]. Additionally, it captured the dependence of the conversion efficiency on both temperature and mass flow rate for oxidation reactions. However, the model exhibited lower sensitivity than the experiments to these factors.
The calibrated reactions allowed CO and HC elimination prediction across diverse conditions under CDC operation, emphasizing the
oxidation pathway for lean combustion scenarios and accounting for HC accumulation. Nonetheless, these reactions cannot account for the influence of
present in exhaust gases, as elaborated in
Section 2.1. To address this gap, a targeted calibration of reactions that occur in the presence of
was needed.
Therefore, the next phase of calibration focused on fine-tuning the reactions involving
within the catalyst, specifically targeting reactions
to
listed in
Table 4. The goal was to refine the predictive capability of the model regarding the catalytic processes influenced by
. A new objective function for this calibration phase was added to reflect the selectivities (
) of CO and HC to reactions involving
and
pathways. These selectivities were detailed in a preceding investigation by Piqueras et al. [
28], which examined the reactivity of an OC across different
concentrations in standard conditions. The objective of this calibration step was to ensure that the removal of CO and HC occurred in the presence of
. Selectivity, defined in Equation (
7), accounts for the contribution of each reaction (
) to the conversion of the individual species, calculated as the proportion of a change in concentration of a species due to a specific reaction to its total concentration change, which is the sum of all reaction contributions.
A new error function was formulated based on the selectivities of each reaction for both the simulation and the reference case, as described in Equation (
8):
Equation (
9) shows the objective function to calibrate the model when
is present in the exhaust gases. The second term of this equation refers to the selectivity of CO to the oxidation with
(
) and the oxidation with ·OH (
). Complementary, it also accounts for the selectivity of HC to the oxidation with
(
) and the oxidation with ·OH (
).
The results corresponding to the OC operation with
are shown in
Figure 3, which compares the selectivities for CO and HC oxidation via
or ·OH with those reported by Piqueras et al. [
28]. As observed, to account for the presence of
in the exhaust gases for the studied OC, closely aligned with the reference.
With respect to CO reactivity, which is depicted in
Figure 3a,c, the model exhibited a high degree of consistency with the reference data in terms of selectivity. The selectivity towards ·OH, which is shown in
Figure 3c, indicated that at temperatures below 160 °C for low
concentrations and below 200 °C for high
concentrations. Above these temperature thresholds, introducing
led to a decrease in CO selectivity from ·OH to the
oxidation pathway.
Regarding the selectivity of HC oxidation, which is represented in
Figure 3b,d, it showed the same type of trend as observed with CO upon the introduction of
. However, it did not reach the selectivity levels for the ·OH pathway observed in CO. The influence of
on HC conversion is weaker at low temperatures due to the adsorption role. In parallel, the HC selectivity to the ·OH pathway decreases as temperature does, but this trend is more gradual and less affected by
concentration than for CO.
As a result of this calibration, the kinetic constants collected in
Table A1—
Appendix A were obtained. These constants include the activation energies and pre-exponential factors of the reactions involved and the accumulation capacity of HC and ·OH in each monolith channel.
3.2. CO Reactivity Analysis
For the CO case,
Figure 4 shows the percentage increase in CO conversion efficiency relative to the baseline results shown in
Figure 2a under warm sea-level conditions, as a function of the exhaust mass flow and catalyst inlet temperature. Each plot is devoted to 500, 1000, 5000, and 10,000 ppm of
molar fraction into the catalyst inlet gas, as previously detailed in
Section 2.
The findings indicated an enhancement in CO reactivity with increasing molar fractions of
, particularly evident within the low-temperature range under low flow conditions (around 100 °C and 35–50 kg/h). This effect extended to higher temperatures as the operating conditions transitioned to higher flow rates (around 150 °C with 60–70 kg/h). The improvement in conversion efficiency was most pronounced in the operating points with low conversion efficiency in the absence of
. As shown in
Table 2, these points were characterized by elevated CO concentrations and low temperatures, avoiding the oxidation by
.
The improvement in CO conversion efficiency consistently increased up to 5000 ppm in the molar fraction, resulting in a significant improvement above 60% at approximately 150 °C and an exhaust mass flow of 65 kg/h. This substantial increase differed from the 20% improvement observed at 1000 ppm and less than 10% at 500 ppm in molar fraction, accompanied by an expansion of the enhanced region to higher temperatures. However, the addition of 10,000 ppm of did not lead to a discernible improvement in reactivity beyond that achieved with 5000 ppm, being the enhancement stabilized at 60%. This trend indicated a saturation point beyond which further increases in concentration did not significantly impact reactivity.
The effect of introducing
on improving CO conversion efficiency was also observed under cold high-altitude conditions.
Figure 5 shows the percentage increase in CO conversion efficiency relative to baseline results shown in
Figure 2c, considering cold high-altitude scenarios influenced by exhaust mass flow and catalyst inlet temperature. Similar to the warm sea-level counterpart, the same molar fractions of
were introduced into the catalyst inlet gas. An enhancement band was observed at 150 °C in the low-to-mid mass flow range (30–60 kg/h) for the cases of 1000, 5000, and 10,000 ppm of
molar fraction. In contrast to the warm sea-level case, introducing 10,000 ppm further extends this band to the highest mass flow rates (70–80 kg/h).
The difference in the increase in CO conversion efficiency profiles with respect to the warm sea-level case was primarily attributed to high CO raw concentration in cold high-altitude conditions (see
Table 3). This limited the effectiveness of
in enhancing CO reactivity. At lower molar fractions of
, such as 500 ppm, the enhancement in conversion efficiency was negligible and limited to regions with low exhaust mass flow and temperature, where the concentration of CO and inhibition were reduced. However, as the
molar fraction increased, the enhancement region shifted towards higher exhaust mass flows, highlighting the role of the ·OH reaction pathway and the decrease in inhibition caused by CO consumption due to this carboxylic pathway. Higher
molar fractions made this effect increasingly apparent. Unlike warm sea-level conditions, high molar fractions of
did not lead to saturation effects in cold high-altitude conditions at every operating point due to the inherently lower initial reactivity of the catalyst in the absence of
. Therefore, significantly greater reactivity was observed when the
molar fraction was increased from 5000 to 10,000 ppm, especially in areas of high mass flow, which were highly affected by inhibition under CDC operation.
To elucidate the improvement in CO reactivity observed in the regions depicted in
Figure 4 and
Figure 5 and to understand the variability in the response to
introduction across different operating points, the analysis of the axial distribution of conversion efficiency throughout the catalyst was assessed. This involved identifying the regions of the OC that exhibited the highest reactivity at each operating point, as well as those areas most affected by the introduction of
. For this purpose, three sections along the length of the monolith were selected. First, the catalyst inlet cross-section corresponds to 4.66 mm from the inlet of the monolith. Then, the middle cross-section was 69.99 mm, and the outlet cross-section was 135.34 mm. The study prioritizes the cold high-altitude case for a more detailed examination, given its more notable increase in reactivity attributed to higher levels of inhibition under CDC operation.
Table 5 presents points A-E from
Figure 5 as representative of operating points corresponding to the region where a significant increase in reactivity was observed upon introducing
. These points are arranged in increasing order regarding inlet gas temperature and exhaust mass flow to the OC.
Thus,
Figure 6 presents the axial distribution of CO conversion efficiency along the monolith length for points A–E. Each subplot within
Figure 6 corresponds to a different
molar fraction at the catalyst inlet gas. The results for the CDC operation are shown in
Figure 6a revealed three different trends across the five operational points considered. At operating point A, no reactivity was observed across any section of the monolith due to the low inlet gas temperature (93 °C) and very high CO molar fraction (1194 ppm), resulting in significant inhibition. Points B and C exhibited higher inlet gas temperatures but also high CO molar fractions (616 ppm and 461 ppm, respectively). In these cases, some reactivity was observed, increasing along the monolith. As CO started to react at the inlet region of the monolith, its concentration decreased, thereby reducing inhibition in subsequent regions and enhancing overall reactivity along the monolith. In these scenarios, the entire length of the monolith contributed to the reaction, and an expanded catalyst volume would enhance CO conversion efficiency. Finally, points D and E, characterized by high inlet gas temperatures and low CO concentrations (low inhibition), demonstrated conversion efficiencies near 100%, with most conversion occurring at the inlet cross-section of the monolith.
Upon introducing 500 ppm in the
molar fraction, as shown in
Figure 6b, the conversion efficiency resulted largely consistent with the CDC scenario. Only minor differences at points B and C, with only a marginal increase in conversion efficiency in the initial cross-section of the monolith, contributed to increasing the reactivity along the whole monolith due to the early inhibition decrease. This enhanced conversion efficiency in the inlet region is attributed to the reaction pathways enabled by the presence of
, particularly through the formation of ·OH radicals on the catalytic surface. At this relatively low
concentration, the generation of these surface groups was limited, resulting in only a modest reactivity increase at the monolith inlet. Points D and E also experienced a boost in reactivity from the
presence at the inlet, with point D showing slightly higher reactivity. Compared to point E, it resulted in greater conversion efficiency due to its lower inlet mass flow and, hence, longer residence time. However, since both points already achieved near 100% conversion efficiency, no significant improvement was noted in the overall conversion efficiency increase map (
Figure 5a).
The enhancement effects were more pronounced when the
molar fraction was increased to 5000 and 10,000 ppm, as illustrated in
Figure 6c,d. At points B and C, the increase in reactivity resulting from the high molar fraction of
led to greater availability of ·OH radicals at the monolith inlet, consequently increasing the conversion efficiency to near 100% in these inlet regions. For operating points D and E, the enhanced reactivity improved conversion efficiency in the inlet region, but only marginally, as these points already face limitations due to mass transfer rather than reactivity. Furthermore, the elevated availability of ·OH radicals with this high
concentration promoted certain reactivity even at operating point A, despite its low temperature.
The findings depicted in
Figure 6 demonstrated that
predominantly influences the inlet cross-section of the monolith, with the observed variations in reactivity in subsequent sections resulting from alterations in CO concentration initiated in these inlet cross-sections. To understand why the impact of
presence was primarily taking place at the inlet of the monolith, it is crucial to examine the selectivity of CO reactions with
and ·OH across different operating points and cross-sections of the monolith.
Figure 7 represents the selectivity of CO to ·OH in the context of cold high-altitude conditions with 500 ppm (
Figure 7a,b) and 10,000 ppm (
Figure 7c,d) in
molar fraction, at the inlet and medium cross-sections of the monolith.
The reactivity of CO with ·OH varied significantly between the inlet and middle cross-sections. In particular, the selectivity to CO with ·OH was considerably higher in the inlet cross-section of the monolith for 500 ppm and 10,000 ppm in the molar fraction, approaching a value of 1 for most operating points, except in areas showing the most significant increases in conversion efficiency. This selectivity sharply declined along the monolith length, with much lower values in the middle cross-sections, reaching its peak at approximately 60% for 500 ppm and 80% for 10,000 ppm. These peaks in CO selectivity to ·OH occurred in regions with minimal increases in conversion efficiency. The areas of high selectivity in the middle cross-section aligned with areas of low temperature where there was no reactivity (point A) and, to a lesser degree, with areas of high temperature where conversion efficiency was already elevated without (points D and E). In both scenarios, reactivity in these areas remained low due to unfavourable conditions that avoided oxidation (point A) or oxidation that had already occurred in the inlet cross-section, leaving no residual CO to react (points D and E). This selectivity pattern may seem counterintuitive since the zones with the most pronounced improvements in conversion efficiency, namely points B and C, upon introduction, appeared least affected by the CO with ·OH reaction pathway. Moreover, the selectivity for this reaction was more significant with 500 ppm in the molar fraction than with 10,000 ppm.
This seemingly contradictory behavior can be elucidated by examining the interplay between oxidation reactions and inhibition dynamics, alongside the ·OH coverage, as guided by
Figure 8. This figure illustrates ·OH coverage at both 500 and 10,000 ppm, focusing on the inlet and middle cross-sections of the monolith under cold high-altitude conditions. At points D and E, the CO conversion efficiency was initially high even under CDC operation. Therefore, the presence of
in the exhaust gases did not alter significantly the reactivity with
. Consequently, as observed in
Figure 8a, the relatively abundance of
allowed for significant ·OH coverage.
However, at points B and C, the introduction of 500 ppm in the
molar fraction enhanced the CO reactivity via the ·OH pathway. Yet, this
concentration was insufficient to sustain high ·OH coverages, limiting the reaction rate, particularly in the inlet cross-section, as shown in
Figure 8a. With 10,000 ppm in
molar fraction, the ability to generate and maintain ·OH coverage improved significantly in the inlet section (
Figure 8c), leading to a substantial increase in CO concentration and decreased inhibition, thus facilitating the oxidation via the
pathway towards the rear end of the monolith. This resulted in high activity but low selectivity for the ·OH reaction, as shown in
Figure 7d.
After analyzing all cases, it was found that there is a significant correlation between the ·OH coverage and selectivity to this species, confirming that in operating points where conversion efficiency improved, most notably under cold high-altitude conditions, the reaction rate was limited by the capability to stabilize ·OH coverage. This explains why no saturation in conversion efficiency enhancement was observed with higher molar fractions at altitude. With 10,000 ppm of , the CO selectivity to ·OH was not saturated, indicating a higher selectivity for reactions with . However, the reaction with ·OH effectively reduced CO enough to decrease inhibition, thereby enabling reactivity with and achieving high CO conversion efficiency.
Moreover, at high temperatures, ·OH coverage neared saturation at the inlet. These areas did not benefit from further introduction. Conversely, low-temperature regions also reached ·OH saturation, but the prevailing temperatures were too low for significant reactivity, hence not benefiting from increased concentration. Therefore, it is evident that certain operating points do not gain from , whereas those that do require higher molar fractions for cold high-altitude conditions compared to warm sea-level conditions. This is mainly due to the higher CO molar fractions in these conditions, which necessitated higher molar fractions to stabilize sufficient ·OH coverage to guarantee the abatement of CO.
3.3. HC Reactivity Analysis
As regards the impact of
on HC reactivity,
Figure 9 shows an improvement in HC conversion efficiency under warm sea-level and cold high-altitude scenarios. This figure illustrates the percentage increase in HC conversion efficiency as a function of the mass flow rate of exhaust gas and the inlet temperature, particularly at high molar fractions of
(5000 and 10,000 ppm). It is observed that the most significant enhancements in HC conversion efficiency induced by
corresponded with the conditions that were also the most affected by
in terms of CO conversion efficiency, specifically at temperatures around 140 °C–150 °C and an exhaust mass flow ranging between 60 and 65 kg/h. However, in the case of HC, this improvement was less significant, as it aligned with zones where adsorption was dominant in the absence of
, leading to moderate HC conversion efficiencies, as shown in
Figure 2b,d.
Moreover, introducing
gradually increased the HC conversion under warm sea levels. This was manifested by the fact that introducing 5000 ppm in the
molar fraction (
Figure 9a) led to maximum improvements of around 10%, while introducing 10,000 ppm resulted in a maximum improvement exceeding 20%. On the other hand, in cold high-altitude conditions, the enhancement was only relevant with the introduction of 10,000 ppm of
, as shown in
Figure 9d, with conversion efficiency improvements exceeding 30% at point B, whereas introducing 5000 ppm (
Figure 9c) yields only negligible impact (maximum improvement of around 5%).
These results indicate that the impact of
on HC required a higher
molar fraction than in the CO case. It can be attributed to two complementary factors. Firstly, increased reactivity was facilitated by the reaction pathway between HC and ·OH, according to reaction
detailed in
Table 4. Given the inherently lower reactivity of HC compared to CO, significant coverage of ·OH was required, requiring higher molar fractions of
. Secondly, greater efficiency in the CO conversion reaction reduced the inhibition caused by this species, facilitating the oxidation of HC with
[
16].
Finally, the fact that the improvement in the efficiency of the HC reaction was more moderate compared to that of CO was because
promoted the HC oxidation but in parallel to the adsorption process, which still played a relevant role. This replacement of one reaction mechanism by another was reflected in the selectivity to the HC adsorption, which is depicted in
Figure 10 for warm sea-level conditions with 0 ppm of
(plot a) and with 10,000 ppm of
(plot b), and for cold high-altitude conditions with 0 ppm of
(plot c) and with 10,000 ppm of
(plot d).
The analysis of
Figure 10 showed a decrease in the selectivity for adsorption in HC upon the introduction of
. When 10,000 ppm of
were introduced, the selectivity adsorption significantly decreased in the area with temperatures around 140–150 °C and exhaust mass flow of 60 to 65 kg/h, falling from 100% with 0 ppm of
in both environmental conditions to 2% with 10,000 ppm of
for the warm sea-level case and to 39% for the cold high-altitude case. This replacement of adsorption by ·OH oxidation was the most significant phenomenon related to the effect of
on the HC conversion, not implying a particularly relevant change in the overall HC conversion efficiency.