Open Access Article
Xinlin Xie,
Jibin Yuan,
Lei Liu,
Hanzi Liu* and
Zhiqiang Sun
*
Hunan Engineering Research Center of Clean and Low-Carbon Energy Technology, School of Energy Science and Engineering, Central South University, Changsha 410083, China. E-mail: liuhz@csu.edu.cn; zqsun@csu.edu.cn
First published on 15th December 2025
The selective catalytic reduction of ammonia (NH3-SCR) is a promising technology for abating nitrogen oxides (NOx), yet its application at high temperatures is severely hampered by the over-oxidation of ammonia, leading to a trade-off between NOx conversion and N2 selectivity. Herein, we construct a series of Fe-exchanged ZSM-5 catalysts with controlled Fe loadings (0.05–0.5 wt%) to decouple the competing reaction pathways. The optimized 0.1Fe@ZSM-5 catalyst achieves 83.0% NOx conversion at 700 °C and maintains exceptional stability for over 120 h under harsh conditions, representing a significant performance enhancement. Mechanistic investigations combining kinetic modeling and in situ spectroscopy reveal a dual kinetic regime, governed by the size of the Fe species. Catalysts with low Fe loadings favor the standard SCR pathway via stable NH4+ and
intermediates, whereas catalysts with higher loadings and larger Fe nanoparticles promote the undesirable oxidation of ammonia to NOx. The result identifies that the optimal catalytic sites for high-temperature SCR rely on a delicate balance, activating ammonia for the desired reaction while suppressing its subsequent over-oxidation. These findings provide new implications for advanced catalyst design by tuning the active site structure to navigate competing reaction kinetics.
Keywords: Selective catalytic reduction; NH3 oxidation; Kinetics modeling; Brønsted acid site; N2 selectivity.
The catalytic oxidation of ammonia over metal-based catalysts has been studied extensively, both for its abatement as a toxic pollutant and for its potential in chemical synthesis, yielding products such as N2, NO, and N2O.10–12 The ammonia activation is facilitated by metal–oxygen sites via abstraction of a H+ proton, where the stronger oxidizability of the metal–oxygen bonds plays a crucial role. For instance, iron oxides possess a relatively low Fe–O bond energy, enabling the activation of NH3. In the case of NH3-SCR, rational ammonia oxidation is beneficial, as it accelerates the initial dehydrogenation to form the
intermediate, which couples with NO to produce N2. However, under excessively oxidizing conditions, lattice oxygen can drive the progressive dehydrogenation of adsorbed
. This process leads to the formation of highly reactive NH* or N* radicals, which are subsequently oxidized to NOx, thereby lowering the N2 selectivity and suppressing the catalytic performance for the desired NOx reduction.13,14 This inherent trade-off between NH3 conversion and N2 selectivity poses a challenge for NH3-SCR reactions on activated metal oxide surfaces.
Fe-based zeolites are energetically favored for stable NO reduction and high N2 selectivity, owing to their inherent spatial confinement and shape-selective properties.7 Previous studies have focused on the kinetics and mechanisms of the interaction between NOx and NH3.15,16 According to acid–base principles, the exchange of Fe ions into the zeolite framework generates Brønsted acid sites associated with Fe–OH moieties, which are recognized as critical for the initial adsorption and activation of NH3, thereby facilitating N–N bond coupling.17,18 However, an excessive concentration of these exposed acid sites can trigger the over-oxidation of ammonia. Current research often investigates how the catalyst's lattice structure, oxidation state, and acid site distribution influence NO conversion and N2 selectivity, with the reaction pathway of NH2NO* being a key intermediate.19–22 Recent work has demonstrated the local coordination structure of the metal sites in dictating the diffusion pathways of dehydrogenated species, where van der Waals forces can create a barrier effect that suppresses the egress of intermediates leading to side reactions.23 The disparity between Fe–O and Si–O bond lengths makes the Fe catalytic center particularly sensitive to local defects, which in turn alters the Fe–Fe and Fe–O coordination environments and the structure of the Fe–OH acid sites. By tailoring the oxidative properties and coordination environment of the catalytic Fe centers, one can modulate the product selectivity and reaction network through synergistic kinetics. Therefore, establishing a quantitative descriptor that correlates Fe–Fe/O coordination numbers and acid properties helps to fundamentally decouple the competing pathways of NO reduction and NH3 oxidation.
In this study, we report the synthesis and robust catalytic performance of a series of Fe-exchanged ZSM-5 catalysts. By developing a comprehensive kinetic model that couples the primary SCR reaction with parasitic NH3 oxidation, we demonstrate that the ion-exchanged Fe loading directly affects the high-temperature NH3–NO–O2 reaction system. Among the catalysts studied, 0.1Fe@ZSM-5 achieved a NO conversion of 83.0% and maintained exceptional stability for over 120 h at 700 °C in the presence of SO2 and water vapor. This performance represents a 15.2% enhancement in high-temperature de-NOx activity at 850 °C compared to our previous work. Mechanistically, we reveal that the exposed Fe nanoparticles facilitate the consumption of NH3-coordinated Lewis acid sites, promoting NH3 adsorption and activation on the Brønsted acid sites for the SCR reaction. Simultaneously, these nanoparticles catalyze further dehydrogenation of
intermediates at elevated temperatures, which leads to the undesired over-oxidation of ammonia to NO.
Transmission electron microscopy (TEM) revealed the microstructural features of 0.5Fe@ZSM-5 (Fig. 1c, S1 and S2). The large-scale image displays the characteristic morphology of the MFI framework. High-resolution TEM (HR-TEM) reveals distinct Fe2O3 nanoparticles anchored on the zeolite framework, evidenced by clear lattice fringes corresponding to the (110) and (104) planes (Fig. 1e and f). Furthermore, energy-dispersive X-ray spectroscopy (EDS) elemental maps (Fig. 1g) show a homogeneous distribution of the framework elements (Si, Al, and O), whereas Fe is concentrated in discrete locations, consistent with the presence of nanoparticles.
Atomic-resolution scanning transmission electron microscopy (AC-STEM) was used to probe the iron species in 0.1Fe@ZSM-5 at the atomic scale. The images (Fig. 1h–j and S3) revealed numerous distinct bright dots and ∼1.5 nm particles, demonstrating that 0.1Fe@ZSM-5 is composed of both dispersed Fe atoms and nanoparticles (NPs). Electron energy loss spectroscopy (EELS) was subsequently conducted to analyze the oxidation state of the Fe species. The Fe L3 and L2 edges from three EELS line scans exhibited identical positions at 708.7 and 721.5 eV, respectively, consistent with the Fe3+ reference (Fig. 1k).26 The combined results confirm the presence of small nanoparticles containing Fe3+ species on 0.1Fe@ZSM-5.
The O 1s XPS spectra (Fig. 2b) were deconvoluted into three distinct components, corresponding to lattice oxygen (Olattice) at a binding energy of 530.2 eV, surface-adsorbed oxygen (Osurface-adsorbed) at 531.7 eV, and adsorbed hydroxyl groups (Ohydro) at 532.6 eV.34,35 It is worth noting that the parent HZSM-5 exhibits a large proportion of Osurface-adsorbed which is associated with –Al/Si bonds.36 While surface-adsorbed oxygen was the predominant species across all samples (49–54%) from parent HZSM-5 or metal oxides,36–38 the concentration of lattice oxygen exhibited a notable, non-monotonic trend with increasing Fe content. For 0.1Fe@ZSM-5, it has the highest value of lattice oxygen of about 33.1%, and concurrently displayed the lowest concentration of adsorbed hydroxyl groups (14.9%). However, 0.5Fe@ZSM-5 shared the equivalent amount of lattice oxygen and adsorbed hydroxyl groups (both 20.7%). The variation suggests that moderate Fe incorporation promotes the generation of lattice oxygen while excessive Fe loading may bring hydroxyl enrichment, which enables the catalyst to obtain higher N2 selectivity.
The surface acidity of the Fe@ZSM-5 catalysts was further investigated using NH3-TPD. As shown in Fig. 2c, the low-temperature peaks at 100–300 °C are ascribed to weak acid sites, corresponding to NH3 release from the weaker Lewis acid sites associated with exchange metal ions.39 Meanwhile, the high-temperature peaks at 400–500 °C correspond to strong acid sites exhibiting thermal stability.39,40 Compared to HZSM-5, increasing the Fe loading shifts the high-temperature NH3 desorption peak from 447 °C to approximately 410 °C, indicating a reconstruction in the acid site structure. The total quantified acidity for each Fe@ZSM-5 sample is about 3 mmol g−1, comparable to that of HZSM-5. The surface acidity was detected by pyridine IR and the spectra (Fig. S4) reveal bands at 1450, 1545, 1625 and 1490 cm−1, which are assigned to Lewis sites, Brønsted sites, and a combination of Lewis and Brønsted sites (BNH4 + LNH3 acid), respectively.41 The quantitative analysis (Table S2) of Brønsted vs. Lewis (B/L) through pyridine-IR shows a marked decrease from 41.0 for HZSM-5 to 14.4–22.6 for Fe@ZSM-5, indicating a substantial reduction in Brønsted acidity and a relative increase in Lewis acidity upon Fe incorporation. Furthermore, the H2-TPR profiles in Fig. 2d reveal the reducibility of Fe@ZSM-5. With increasing Fe loading, the initial peak corresponding to the reduction of Fe2O3 to Fe3O4 was intensified,42 while the high-temperature region associated with the reduction of FeO particles to metallic Fe (Fe2+ to Fe0) decreased in intensity.43 This suggests that the Fe2+ observed in the XPS spectra may originate from the interaction between iron and the surrounding atoms.44 The results also imply that Fe3+ predominates as the stable species at higher loadings.
X-ray absorption fine structure (XAFS) was employed to probe the coordination environment of iron within the synthesized Fe@ZSM-5 catalysts. The normalized Fe K-edge X-ray absorption near-edge structure (XANES) spectra are presented in Fig. 2e. The absorption threshold (E0) for all samples is shifted to a higher energy relative to that of Fe foil, indicating that iron predominantly exists in an oxidized state.45 As the iron loading decreases, the XANES spectra exhibit a further shift toward higher energy and a broadening of the normalized peak. These features are characteristic of the oxidation of Fe to Fe3+, suggesting a higher average oxidation state in catalysts with lower iron content,46 aligning with the fitting results in the XANES spectra.
The Fourier-transformed (FT) EXAFS spectra of the Fe@ZSM-5 catalysts (Fig. 2f) exhibit a prominent peak at ∼2.5 Å, corresponding to the Fe–Fe scattering path. The intensity of this peak strengthens with increasing iron loading, while the intensity of the Fe–O scattering path at 1.8 Å concurrently diminishes. These trends indicate that higher iron loadings promote the formation of Fe nanoclusters. In contrast, lower loadings favor a coexistence of atomically dispersed Fe species and small nanoclusters. This structural model is corroborated by wavelet transform (WT) analysis (Fig. 2g), which clearly resolves the distinct scattering contributions from Fe–O and Fe–Fe paths. Quantitative EXAFS fitting provides further validation (Table S3). As the iron loading increases from 0.05 to 0.5 wt%, the Fe–Fe coordination number rises from 0.9 to 5.4, while the Fe–O coordination number decreases from 4.1 to 1.8. These results are in agreement with the structural evolution inferred from our XANES and WT analyses.
To investigate this high-temperature inactivation, we performed separate catalytic oxidation of NH3 in the presence of O2. The concentration of NOx produced from NH3 oxidation increased with both temperature and iron loading (Fig. 3c). This result shows that at high temperatures, NH3 oxidation becomes a dominant competing side reaction, consuming the reducing agent and thereby lowering the efficiency of NO reduction. Moreover, the lower NO concentration of pristine HZSM-5 further confirms this side reaction to the iron species. Combining the TEM and XAS results, we preliminary conclude that the iron nanoparticle size is an important factor in modulating the trade-off between NH3-SCR activity and NH3 oxidation.
The effect of gas hourly space velocity on the catalytic performance was explored (Fig. 3d). Increasing the space velocity led to a decrease in NO conversion. This was accompanied by a rise in unconverted NH3 at the outlet, while the concentrations of NO2 and N2O by-products did not change significantly. These results indicate that the drop in NO conversion at higher space velocities is due to the reduced NH3 conversion rather than the enhanced NH3 over-oxidation.
In addition, the long-term stability of the 0.1Fe@ZSM-5 catalyst was tested at 700 °C (Fig. 3e). The catalyst demonstrated robust performance over a 50 hour run, with NO conversion showing only a slight decrease from 79.5% to 77.0%. During this period, the outlet NO2 concentration increased from 4.1 to 7.5 ppm, while the N2O concentration remained stable. This suggests that the minor drop in NO conversion is linked to a slow side reaction where some NO is oxidized to NO2, which does not efficiently enter the fast SCR pathway.
Regarding practical application, we evaluated the long-term catalytic performance of synthesized 0.1Fe@ZSM-5 and HZSM-5 under exposure to 300 ppm SO2 and 8.3 vol% H2O at 700 °C. Under 300 ppm SO2, 0.1Fe@ZSM-5 deactivated gradually, with NO conversion decreasing from 83.0% to 78.5% over 50 h as shown in Fig. 4a. Introducing 8.3 vol% H2O accelerated deactivation and the conversion dropped to 60.1%. After both poisons were removed at 110 h, the catalyst partially recovered to 71.5%. For comparison, HZSM-5 showed a similar slight decline under SO2 alone, from 77.3% to 72.1% NO conversion. With both SO2 and H2O, the conversion decreased to 60.8% and did not recover after poison removal, indicating irreversible deactivation.
Further physicochemical analyses were performed after 120 h continuous reaction to probe the deactivation mechanism of 0.1Fe@ZSM-5. HAADF-STEM and EDS reveal dispersed Fe nanoparticles. Sulfur deposits distribute broadly on ZSM-5 with partial co-localization on Fe nanoparticles, while remaining overall dispersed. The 27Al MAS NMR spectra were used to track the evolution of the framework Al throughout the long-term hydrothermal ageing. As can be seen in Fig. 4d, the broad peak signal of dehydrated 0.1Fe@ZSM-5 is 4-coordinated corresponding to the Brønsted acidic Al(IV) site at 58 ppm. After SO2 + H2O ageing for 120 h, the signal intensity of the framework Al decreases, suggesting a dealumination process.48 The significant decline of the LNH3 peak from Py-IR clearly indicates the loss of Lewis acid sites after long-term poisoning (Fig. 4e). The O2-TPD patterns (Fig. 4f) of the as-prepared catalyst and after 120 h in SO2 and H2O confirm a severe loss of lattice oxygen (over 400 °C)49,50 and diminished oxygen mobility after exposure to SO2 and H2O. These observations indicate that sulfur deposition blocks active oxygen sites and suppresses lattice oxygen participation in the long-term test.
Under NH3 + O2 atmospheric conditions, NH3 oxidation products on the catalyst surface can be primarily classified as N2 and NO, with selectivity varying as the temperature increases. Higher temperatures favor higher NO selectivity.
| 4NH3 + 3O2 → 2N2 + 6H2O | (1) |
| 4NH3 + 5O2 → 4NO + 6H2O | (2) |
![]() | (3) |
![]() | (4) |
![]() | (5) |
Experimental measurement data under NH3 + O2 conditions were analyzed by selecting data points where NH3 conversion remained below 15% to minimize diffusion effects on fitting accuracy. Here,
represents the NH3 surface coverage. After optimization, the rate constants for NH3 oxidation reactions at various temperatures yielded an activation energy of 98.3 kJ mol−1. The pre-exponential factor A and activation energy Ea for the NH3 oxidation process were subsequently determined by fitting the ln
kx vs. 1/T relationship according to the Arrhenius equation. We compare the experimental measurements and model calculations for NH3 conversion and NH3-to-NO oxidation selectivity under NH3 + O2 atmospheric conditions. The calculated results demonstrate good agreement with experimental data over the 500–850 °C temperature range (Fig. 5b and c).
Under NH3 + NO + O2 atmospheric conditions, the reaction rate of NO is governed by the synergistic interplay between the catalytic reduction of NO by NH3 and the concurrent catalytic oxidation of NH3 to form NO. This dual mechanism significantly influences the overall reaction kinetics, as demonstrated below:
| 4NO + 4NH3 + O2 → 4N2 + 6H2O | (6) |
| 4NH3 + 3O2 → 2N2 + 6H2O | (7) |
| 4NH3 + 5O2 → 4NO + 6H2O | (8) |
![]() | (9) |
![]() | (10) |
Subsequently, the experimental data obtained under NH3 + NO + O2 conditions were systematically analyzed. Given the relatively low SNCR efficiency observed below 850 °C, gas-phase NH3 + NO + O2 reactions were excluded from consideration in this temperature range. To minimize the influence of mass transfer limitations on fitting accuracy, experimental data points with NO conversion rates below 15% were specifically selected for kinetic analysis. Through optimization procedures, the rate constants for NO catalytic reduction reactions were determined at various temperatures. The pre-exponential factor (A) and activation energy (Ea) for the NH3 oxidation process were subsequently derived by fitting the ln(kx) versus 1/T relationship according to the Arrhenius equation, as presented in Table S4.
Compared to conventional SCR kinetic models, this work introduces a dual kinetic framework that explicitly incorporates NH3 surface oxidation as a competing reaction under high-temperature conditions. A key feature of this framework is the inclusion of the selectivity of NH3 toward NO formation as a temperature-dependent parameter, which allows quantitative evaluation of how the NH3 over-oxidation pathway influences the overall SCR performance. This integration provides a more accurate description of the experimental results (Fig. 5d). As the temperature rises, the model successfully captures the transition where the NO formation rate surpasses the N2 formation rate, revealing the increasing contribution of NH3 oxidation in determining overall selectivity. By incorporating this temperature-dependent selectivity, the dual kinetic model addresses a gap in prior SCR kinetic frameworks, which typically treat NH3 oxidation as a parallel but independent side reaction.
To explore the effect of NH3 catalytic oxidation on SCR-related intermediates, in situ DRIFT measurements combined with TPSR were performed on 0.1Fe@ZSM-5 from 400 to 850 °C (Fig. 5e). Following NH3 adsorption, broad N–H vibration peaks at 3259 and 2936 cm−1 are ascribed to the asymmetric stretching as vas(NH4+) on Brønsted acid sites, where three hydrogen atoms bond to oxygen ions in the AlO4 tetrahedra.51,52 The sharp peaks at 3581 and 3660 cm−1 are attributed to Si–OH–Al and Si–OH, respectively. In the lower wavenumber region, the peak at 1287 cm−1 corresponds to
vibrations, while features at 1186 and 1621 cm−1 are assigned to vas(NH3) on Lewis acid sites, and those at 1465 and 1762 cm−1 to NH4+ vibrations on Brønsted acid sites.53 Upon heating in an NH3–NO–O2 atmosphere to 600 °C, the intensities of
and NH4+ intermediates at 3259 and 1621 cm−1 decay rapidly, whereas
remains relatively stable, indicating that certain
and NH4+ species serve as the initial active sites in the SCR redox cycle during activation. Notably, as the temperature further increased from 600 to 850 °C, only the absorbance of NH4+ intermediates at 3259 and 2936 cm−1 decreased significantly, whereas the band at 1465 cm−1 remained relatively stable. This observation indicates that framework Brønsted acid sites participate more actively in the synergistic conversion of NH3 and NO at high temperatures. Moreover, the time-resolved DRIFT spectra of 0.1Fe@ZSM-5 during NH3 adsorption, O2 oxidation, and NO reduction at 800 °C (Fig. S6–S8) confirm the dynamic transformation of NH4+ species during the redox cycle.
For comparison, variations in intermediates during exposure to an NH3 + O2 atmosphere at 400–850 °C were also examined under NH3 catalytic oxidation conditions (Fig. 5f). At 400 °C, the
intermediate at 1287 cm−1 is markedly lower than that in NH3 + NO + O2, but its intensity reverses and increases upon heating to 800 °C, confirming that dehydrogenation products of NH3 or NH4+ proceed via the
pathway in high-temperature oxidizing environments, while
remains relatively inert. For quantitative comparison, normalized absorbance changes of characteristic peaks with temperature are shown in Fig. 5g, suggesting that NH4+ likely participates in surface species consumption during NH3 oxidation. Drawing from these observations, we propose a molecular-level pathway governed by a dual kinetic regime (Fig. 5h). Under moderate temperature conditions, a favorable activation barrier promotes the dehydrogenation of NH3 to form
intermediates. These species subsequently undergo N–N coupling to yield NH2NO*, which decomposes into N2 following the conventional SCR pathway. Conversely, at temperatures exceeding 700 °C, the higher thermal energy shifts the reaction toward an undesirable oxidation route. In this regime, lattice oxygen induces the progressive dehydrogenation of adsorbed NH3 at acid sites through sequential N–H bond scission. This process generates highly reactive NH* or N* radicals that are ultimately oxidized to NOx.
To probe the influence of the iron nanoparticle size on the SCR mechanism, we performed in situ DRIFT experiments on the 0.05Fe@ZSM-5, 0.08Fe@ZSM-5, and 0.5Fe@ZSM-5 catalysts. Following NH3 adsorption at 200 °C (Fig. 6a–c), distinct changes in the DRIFT spectra were observed as the Fe loading increased from 0.05 to 0.5 wt%. Correlating with the XANES fitting results, which indicated increasing metallic Fe content at higher loadings, these spectral changes suggest that metallic Fe influences the NH3 adsorption behavior. Specifically, the intensity of the band corresponding to NH3 coordinated to Lewis acid sites decreased, while the band assigned to NH4+ ions at 1471 cm−1 grew substantially. This shift indicates that NH3 preferentially adsorbs at Brønsted acid sites in the presence of metallic Fe species, where it forms more stable NH4+ species. The enhanced stability at Brønsted sites suppresses the excessive oxidation of NH3 at high temperatures, thereby improving the selectivity toward N2 formation.54 Furthermore, the band at 3259 cm−1, attributed to NH4+ ions interacting with Brønsted acid sites of the zeolite, was attenuated, indicating a weaker interaction between the agglomerated iron species and the zeolite framework.
As the temperature was increased (Fig. 6d–f), the intensity of all ammonia-related bands decreased, indicating the progressive desorption of NH3 from the acid sites. Notably, the evolution of the surface species differed significantly with iron loading. For the low-loading 0.05Fe@ZSM-5 and 0.08Fe@ZSM-5 catalysts, the bands for NH3 adsorbed on Lewis acid sites were almost completely consumed by 700–850 °C, whereas the signals for NH4+ and
species persisted. This suggests that the latter are more thermally stable and likely serve as key intermediates in the redox reaction. In contrast, for the 0.5Fe@ZSM-5 catalyst, the bands corresponding to nitrosyl species at 1846 cm−1 were significantly more intense.55 Concurrently, the consumption of the NH4+ band at 3259 cm−1 was more pronounced, indicating that the larger iron nanoparticles promote the undesirable over-oxidation of ammonia to NO at high temperatures, which is in agreement with the observed SCR performance.
as a critical species in the NO reduction pathway, which competes with the NH3 oxidation route. These findings offer a new strategy for the rational design of robust catalysts for challenging industrial applications. The development of a stable catalyst structure, coupled with a more accurate kinetic model, paves the way for advancing high-performance deNOx technologies to meet stringent emission regulations.
For the fabrication of Fe@ZSM-5, a suspension was created by mixing 10 g of HZSM-5 in 100 ml of distilled water, under intense stirring. The necessary quantity of iron acetylacetonate (Fe(C5H7O2)3) was dissolved in this mixture. Ensuing continuous magnetic agitation at 80 °C for 3 h facilitated the homogenization of the solution, which was then subjected to filtration and thrice rinsed with distilled water. The filtrate was air-dried at 110 °C for 12 h, followed by calcination in a muffle furnace at 800 °C for 5 h under ambient air conditions. The resultant catalyst particles were sieved to obtain a granule size range between 0.18 and 0.25 mm.
The catalytic performance for the NH3-SCR of NOx was evaluated in a continuous-flow quartz fixed-bed reactor over a temperature range of 400–850 °C. The standard feed gas consisted of 1000 ppm NH3, 1000 ppm NO, and 6 vol% O2, with N2 as the balance gas. The total flow rate was maintained at 2 L min−1 using mass flow controllers, corresponding to a gas hourly space velocity (GHSV) of 30
000 h−1. The effluent gas concentrations (NO, NH3, N2O, NO2, and O2) were continuously monitored using an online infrared (IR) gas analyzer. To comprehensively assess the catalyst, several experiments were conducted: (i) the effect of GHSV on NO reduction was systematically investigated; (ii) long-term stability tests were performed under standard reaction conditions; (iii) the catalyst's resistance to poisoning was evaluated in the presence of 300 ppm SO2 and/or 8.3 vol% H2O. Prior to data acquisition for each point, the system was allowed to reach a steady state, and the reported values represent the average of measurements taken over a 20 minute period. The NO reduction efficiency, N2 selectivity, and apparent reaction kinetics were calculated using the following equations:
![]() | (11) |
![]() | (12) |
![]() | (13) |
Hydrogen temperature-programmed reduction (H2-TPR) was conducted on an AutoChem II 2920 instrument to evaluate the reducibility of the catalysts. In a typical measurement, 100 mg of the sample was loaded into a U-shaped quartz tube. The catalyst was pretreated at 300 °C for 1 h under a flowing He atmosphere (heated at 10 °C min−1) to remove adsorbed water. After the sample was cooled to 50 °C, the gas flow was switched to a 10 vol% H2/He mixture (30 mL min−1). The temperature was then ramped to 800 °C at a rate of 10 °C min−1, and H2 consumption was continuously monitored with a thermal conductivity detector (TCD).
The acidic properties of the catalysts were characterized by ammonia temperature-programmed desorption (NH3-TPD) and oxygen storage and mobility were evaluated by oxygen temperature-programmed desorption (O2-TPD) using the same instrument. Prior to the analysis, 100 mg of the sample was pretreated in a He flow at 300 °C for 1 h (10 °C min−1 ramp) and cooled to 50 °C. For NH3-TPD, the sample was saturated with ammonia by exposure to a 10% NH3/Ar stream (25 mL min−1) for 1 h, followed by Ar purging for 1 h to remove physisorbed ammonia, and then heated to 800 °C at a rate of 10 °C min−1, monitoring the amount of desorbed NH3 using the TCD. In O2-TPD, oxygen saturation was achieved by exposing the pretreated sample to 10% O2/He (25 mL min−1) for 1 h, followed by Ar purging for 1 h and subsequent heating to 800 °C at 10 °C min−1.
![]() | (14) |
![]() | (15) |
The catalyst bed thickness is h, Cx represents the component concentration of reactants/products (mol m−3), primarily CNH3, CNO, and CO2 in this study, and kx (mol m−2 s−1) represents the reaction rate constant for each component. Subsequently, the rate equation was established:
| rx = kxf(Cx) | (16) |
Specifically, for the NH3 + O2 catalytic oxidation process on 0.1Fe@ZSM-5, NH3 adsorption based on the Langmuir model and O2 effects were primarily considered.58 For the comprehensive NH3 + NO + O2 reaction process, referring to standard SCR kinetic models, the reaction orders for NH3, NO, and O2 are 0, 1, and 0.5, respectively.59 The O2 content in coal combustion flue gas is approximately 6 vol%, with concentrations being orders of magnitude higher than other reaction gases, allowing neglect of concentration changes due to reaction during calculations. Additionally, according to the Mear criterion, since the external diffusion rate of catalyst particles is much lower than the reaction rate, diffusion effects on the gas–solid reaction process in this study can be neglected.60
Considering the influence of reactant gas internal diffusion within catalyst particles, an effectiveness factor η was introduced:
![]() | (17) |
The Thiele modulus expression is given as
, where R represents the catalyst particle diameter (m). For molecular sieve catalysts with porous structure characteristics, the comprehensive diffusion coefficient Dx,eff (m2 s−1) of gas component x is not only influenced by molecular diffusion and Knudsen diffusion (assuming a zeolite pore diameter of 10 nm) but also requires porosity correction. For the catalytic NOx reduction reaction, the effectiveness factor ϕn approaches 1, indicating that the entire process is under surface reaction control. Other model-related parameter values are shown in Table S5.
| Dx,eff = ε2Dx | (18) |
Here, Dx,gas represents the diffusion coefficient of reaction gases in air. For NH3, the Fuller equation yields a calculated value of 0.198 cm2 s−1 under standard conditions, while the diffusion coefficient of NO molecules in air is 0.168 cm2 s−1 (with temperature corrections applied as needed). In actual reaction processes, gas–solid reactions compete with intraparticle diffusion
. The combined effects of intraparticle diffusion and the chemical reaction on the overall reaction rate can be determined through the effectiveness factor and Thiele modulus.
The procedure for conducting in situ UV-vis and DRIFTS analyses comprised the following steps: (1) NH3 adsorption: the chamber was purged with He at 500 °C for 1 h and then brought back to ambient temperature. Subsequently, a flow of 1000 ppm NH3/He was introduced, gradually elevating the temperature from 100 to 800 °C at 10 °C min−1. (2) NH3 oxidation: upon reaching adsorption equilibrium (typically within 1 h) at a set temperature, 6 vol% O2 was infused into the chamber for 30 min. (3) NH3–NO–O2 co-presence and pulse: following equilibrium establishment (usually within 30 min) at the required temperature, a mixture of 1000 ppm NO, 6 vol% O2, and 1000 ppm NH3 in He was simultaneously fed into the chamber at 800 °C. For pulse tests, specific gas components were selectively discontinued. For the temperature programmed surface reaction (TPSR), the reaction chamber was heated from 400 °C to 850 °C in 1000 ppm NO and 6 vol% O2 after exposure to 1000 ppm NH3/He for 1 h. In situ DRIFT spectra were recorded every 8 seconds, and the IR spectrum presented subsequently represents the average interference pattern across eight successive scans.
The acidity of the samples was determined by pyridine infrared spectroscopy (Py-IR) on a Bruker Vector 22 spectrophotometer. Prior to the tests, the samples were shaped into tablets and degassed under vacuum at 400 °C for 1 h. After cooling to room temperature (RT), the samples were saturated with pyridine and then desorbed at RT, 200, and 450 °C under vacuum for 30 min. The IR spectra were registered in the 1400–1700 cm−1 range.
Supplementary information (SI): containing additional performance and structural data, as well as in situ DRIFTS. See DOI: https://doi.org/10.1039/d5im00245a.
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