Hydrotalcite-Modified Clinoptilolite as the Catalyst for Selective Catalytic Reduction of NO with Ammonia (NH3-SCR)

A series of clinoptilolite-supported catalysts, modified with hydrotalcite-like phase (HT) by co-precipitation, were prepared and tested in NH3-SCR reactions. It was found that deposition of HT on clinoptilolite increased conversion of NO within 250–450 °C, and that the positive impact on the catalytic activity was independent of HT loading. The promoting effect of clinoptilolite was attributed to Brönsted acid sites present in the zeolite, which facilitated adsorption and accumulation of ammonia during the catalytic process. Concentration of N2O in the post-reaction gas mixture reached its maximum at 300 °C and the by-product was most likely formed as a consequence of NH4NO3 decomposition or side reaction of NH3 oxidation in the high-temperature region. The gradual elimination of nitrous oxide, noticed as the material with the highest concentration of hydrotalcite phase, was attributed to the abundance of oligomeric iron species and the superior textural parameters of the material. UV-Vis experiments performed on the calcined samples indicated that Fe sites of higher nuclearity were generated by thermal decomposition of the hydrotalcite phase during the catalytic reaction. Therefore, calcination of the materials prior to the catalytic tests was not required to obtain satisfactory overall catalytic performance in NO reductions.


Introduction
Over the last decades, layered double hydroxides (LDHs), also called as "hydrotalcitelike anionic clays", have attracted considerable interest from the scientific community. The increasing attention directed at the application of LDHs in many fields results from the unique structural features and chemical composition of layered doubled hydroxides, which can be easily adjusted depending on the intended use. The general formula of layered double hydroxides is [M 1−x II M x III (OH) 2 ] [A x/n n− ]·mH 2 O, where M II and M III correspond to divalent and trivalent metal ions, respectively, while A n− represents nonorganic or organic interlayer anions [1]. The group of LDHs can be divided into natural and synthetic anionic clays. The natural hydrotalcite reflects a brucite-like structure, in which Mg 2+ cations are partially replaced with Al 3+ cations. The positive charge generated by this substitution is typically balanced by carbonate anions (CO 3 2− ), which co-exist in the interlayer space with water molecules [2]. Due to the fact that Mg 2+ and Al 3+ cations can be substituted by other chemical elements of similar atomic radius, a great number of LDHs with a wide range of Me 2+ /Me 3+ combinations can be prepared [3]. Furthermore, synthetic layered double hydroxides can be obtained by various procedures, e.g., solgel [4], rehydration [5], induced hydrolysis [6], or co-precipitation, which is the most under stirring conditions. Constant pH of 9.5-10 was adjusted by the introduction of 1 M solution of NaOH, which was added simultaneously with the mixture of metal precursors. Subsequently, the obtained precipitate was aged for 1 h at 65 • C in the mother solution. Afterwards, the formed solid was filtered, washed with the distilled water to remove the residual nitrates, and dried overnight at 80 • C. The prepared material was labeled as HT.
Preparation of clinoptilolite-supported catalysts with co-precipitated hydrotalcite phase started from the transformation of natural zeolite into the hydrogen form. The raw clinoptilolite (labeled as Clin) was protonated using 5 wt% of HCl solution. Typically, the material was introduced into the adequate volume of acid to obtain zeolite/HCl ratio of 1/3. The suspension was shaken for 2 h, filtered, and washed with distilled water. The shaking procedure was repeated three times, and afterwards the sample was dried at 100 • C in air. The obtained zeolitic support was labeled as H-Clin.
The catalysts investigated in this work were prepared by co-precipitation of hydrotalcitelike phase at constant pH directly on the surface of the protonated clinoptilolite. Firstly, 5 g of H-Clin were introduced into the aqueous solution of Na 2 CO 3 and the suspension was kept under vigorous stirring at 65 • C. In order to enhance the adhesion of the zeolitic surface, 2 cm 3 of propylene glycol were added dropwise into the solution. Co-precipitation of hydrotalcite was performed according to the same procedure as described for the HT sample. Due to high acidity of H-Clin, a higher amount of NaOH solution was required to maintain the desired basic pH of the reacting mixture. The amounts of metal nitrates were adjusted adequately to obtain 20, 25, and 30 wt% coverage of H-Clin with the hydrotalcite phase.

Characterization of the Catalysts
The chemical composition of the catalysts in relation to the content of Si, Al, Mg, Cu, and Fe was determined by inductively coupled plasma optical emission spectroscopy (ICP-OES, QTEGRA). Crystallinity and phase purity were analyzed by X-ray powder diffraction (XRD). The XRD patterns were obtained using a Panalytical Empyrean diffractometer. The diffractograms were collected using Cu Kα radiation source (λ = 1.54184 Å) at a tube current of 40 mA and a voltage of 40 kV in the scanning range of 2θ of 3-90 • . The recorded XRD data were analyzed using X'pert HighScore software plus (with database). The size of crystals of single-phase hydrotalcite was calculated according to the Debye-Scherrer equation, including a correction related to the instrument broadening. Besides this, the unit cell parameters of the material were determined by the method proposed by Rives [39]. Textural properties and specific surface area of the materials were analyzed by low-temperature N 2 sorption using a Micromeritics 3Flex Surface Characterization gas adsorption analyzer. Prior to the experiment, the samples were degassed under vacuum conditions at 90 • C for 1 h and afterwards, at 350 • C for 5 h. The specific surface area (S BET ) of the materials was calculated using the BET (Brunauer-Emmet-Teller) model, from the adsorption branch, according to the recommendations of Rouquerol [40]. Scanning electron microscopy (SEM) studies were carried out using Field Emission Scanning Electron Microscope JEOL JSM-7500 F equipped with an X-ray energy dispersive (EDS) system. SEI images were provided by the secondary electron detector. Thermogravimetric studies (TG) were performed to determine changes in the weight of the samples within 30-800 • C, with the temperature ramp of 10 • C·min −1 . Typically, the sample was placed on a platinum holder in the mixture of air and helium. Thermogravimetric and differential thermal analyses (TGA-DTA) consisted of progressively increasing the temperature to quantify the weight losses, which solid samples suffer. The procedure consisted of heating the sample to 800 • C with a temperature ramp of 10 • C/min using an air stream of 20 mL/min. Mettler Toledo TGA/SDTA 851E equipment was used for the analyses carried out. The characteristic chemical groups present in the materials were studied by FT-IR spectroscopy. The spectra were collected using a Perkin Elmer Frontier spectrometer in the wavelength region of 4000-400 cm −1 , with a resolution of 4 cm −1 . The coordination and aggregation of metal species introduced into the zeolites were investigated by ultraviolet diffuse reflectance spectra (UV-vis-DR). The analysis was carried out using a Cary 5 spectrophotometer, equipped with a diffuse reflectance accessory. The spectra were taken in the range of 200-800 nm, with a resolution of 2 nm.

Catalytic Tests
The catalytic performance of the prepared materials in NH 3 -SCR reaction was analyzed in a fixed-bed flow microreactor with a quartz tube under atmospheric pressure. Typically, 200 mg of the catalyst with 20-35 mesh was outgassed in a flow of nitrogen at 400 • C for 30 min. The material was cooled down to 100 • C and exposed to the gas mixture containing 800 ppm of NO, 800 ppm of NH 3 , 3.5 vol.% of O 2 , and He as an inert. The total gas flow was 100 mL·min −1 , which led to the GHSV of 30,000 mL·h −1 ·g −1 . The NH 3 -SCR tests were carried out in a temperature range of 150 • C to 450 • C with 50 • C as a step. Concentrations of the residual NO and N 2 O (the by-product of the reaction) in the outlet gas were analyzed continuously by the FT-IR detector (ABB 2000, AO series). The results were calculated based on the specific algorithm and collected as an xls file. This manner of the analysis did not provide FT-IR spectra of the post-reaction gas mixture; however, it did enable a relatively fast calculation of the experimental results. The conversion of NO was calculated according to the formula represented by Equation (1): where NO conv -NO conversion, C NO in -inlet concentration of NO, C NO out -outlet concentration of NO in the gas mixture.

Catalytic Tests Catalytic Performance of Fresh HT-Clinoptilolite
The samples of hydrotalcites co-precipitated on clinoptilolite were tested as the catalysts of selective catalytic reduction of NO with ammonia. NO conversion obtained for the samples is presented in Figure 1. Furthermore, concentration of N 2 O (as the by-product of NH 3 -SCR) at the reactor outlet is depicted in Figure 2. desired direct oxidation of ammonia. Therefore, the reaction probably dominated over NH3-SCR in the high-temperature range and was able to contribute to the production N2O [43]. The emission of N2O (a common by-product of NH3-SCR) during the reaction is a very important factor for the potential application of the catalyst in the industry. The selectivity towards the formation of N2O is a source of information on the side reactions occurring. It can be noticed from Figure 2 that the concentration of N2O for raw clinoptilolite and single-phase hydrotalcite did not exceed 40 and 100 ppm, respectively. In contrast, the yield of N2O was drastically elevated for HT_Clin samples. Interestingly, despite very similar activity in NO reduction in the high-temperature range, the emission of N2O porting material [18]. For this reason, it was expected that the presence of zeolite play a crucial role in the advantageous distribution of Fe-Cu oxides, since the reduction of N emissions with the increasing temperature has not been observed for single-phase H Therefore, the generation of mixed oxides on the surface of clinoptilolite could contribu to a higher selectivity of the catalysts to N2 and H2O above 300 °C.

Chemical Composition and Crystallinity of the Samples
The content of Si, Al, Mg, Fe, and Cu in the samples was measured by inductive coupled plasma-optical emission spectrometry (ICP-OES). The overview of the obtain data, expressed as wt% of each component, is presented in Table 1. It can be observed th the chemical composition of non-supported hydrotalcite is in agreement with the calc lated one. Besides, the quantity of Si and Al in the non-modified clinoptilolite, which giv an approximate Si/Al molar ratio of 4.4, corresponds to that reported in the literature [4 After modification with HCl, concentration of aluminum in the zeolite slightly decreas due to dealumination, which occurs normally after acid treatment [47]. Thereby, the init modification with HCl resulted in successful, controlled elimination of Al cations fro the zeolitic framework. According to Garcia-Basabe and co-workers [47], breaking Albonds and the successful extraction of Al by diluted acids does not affect the topology the zeolitic framework, however, it does result in a higher thermal stability and pore vo ume. What is more, Ghasemian et al. [48] reported the improved catalytic performance clinoptilolite in propane-SCR after the zeolite was leached with mild oxalic acid. The be eficial effect of pre-treatment with acid was ascribed to re-distribution and the increas It can be observed from Figure 1 that non-calcined, single-phase HT exhibited the lowest NO conversion and that the temperature of 50% NO conversion (T 50 ) for this catalyst was ca. 350 • C. Additionally, above this value, catalytic activity of the material considerably decreased. On the other hand, around 55% of NO was eliminated at 450 • C for clinoptilolite, even before the introduction of the active phase. Relatively high activity of this material in SCR reactions can be ascribed to the natural presence of iron species in its structure [28]. It can be noticed that combination of clinoptilolite and hydrotalcite phase drastically improved the activity of the single materials in NO removal. The conversion was observed to increase up to 300 • C, reaching the maximum of 95%, independently of the concentration of HT on clinoptilolite. Of interest is that the percentage coverage of the zeolite with LDH phase did not significantly influence the catalytic performance of the materials. NO conversion of HT_Clin 25 and HT_Clin 30 was almost identical in the entire temperature range, while HT_Clin 20 was slightly less active within 200-275 • C. Positive influence of the co-existence of HT-and zeolitic phase on NO elimination resulted most probably from two reasons: (1) clinoptilolite acted during the reaction as the source of Brönsted acid sites, which enabled efficient adsorption of ammonia during the reaction [41], and (2) hydrotalcite phase was a source of Cu 2+ and Fe 3+ sites of Lewis type, contributing to low-and high-temperature activity, respectively [42]. Additionally, the catalytic activity of the materials above 300 • C slightly decreased, which can be attributed to non-desired direct oxidation of ammonia. Therefore, the reaction probably dominated over NH 3 -SCR in the high-temperature range and was able to contribute to the production N 2 O [43].
The emission of N 2 O (a common by-product of NH 3 -SCR) during the reaction is a very important factor for the potential application of the catalyst in the industry. The selectivity towards the formation of N 2 O is a source of information on the side reactions occurring. It can be noticed from Figure 2 that the concentration of N 2 O for raw clinoptilolite and singlephase hydrotalcite did not exceed 40 and 100 ppm, respectively. In contrast, the yield of N 2 O was drastically elevated for HT_Clin samples. Interestingly, despite very similar activity in NO reduction in the high-temperature range, the emission of N 2 O for the materials was completely different. The increased generation of nitrous oxide was temperature-dependent, since below 300 • C it followed the order of HT_Clin 20 < HT_Clin 30 < HT_Clin 25, while above 300 • C was sorted as HT_Clin 30 < HT_Clin 20 < HT_Clin 25. Besides, one should note that the amount of the emitted N 2 O was almost identical for HT_Clin 20 and HT_Clin 25 within a range of 350-400 • C. What is more, the increase in N 2 O emission was observed only up to 300 • C, while within the range of 300-450 • C concentration of nitrous oxide visibly reduced, especially for HT_Clin 30. The explanation of the emission of N 2 O below 300 • C was proposed by Zhang and Yang [44]. The authors postulated that the source of nitrous oxide in the low-temperature NH 3 -SCR is ammonium nitrate (NH 4 NO 3 ), formed by the interaction of NH 3 and surface nitrates on the catalyst surface at the initial level of the process. Decomposition of NH 4 NO 3 is followed by reaction (R1): High-temperature (300-450 • C) formation of N 2 O may be associated with the Lewis acidic sites originating from Cu and zeolite support. As it was reported elsewhere, the aforementioned acidic sites are prone to form NH from oxidative dehydrogenation of NH3. The former further reacts with NO from feed gases produce N 2 O [45]. Considering the level of NO conversion of the most active catalysts at and above 300 • C, and the amount of the formed N 2 O by-product, such an explanation has its confirmation in the experimental results.
Generally, it can be observed that the coverage of clinoptilolite with HT noticeably influenced concentration of N 2 O above 300 • C. This observation can be explained by the possible decomposition of hydrotalcite phase, taking place between 300 and 350 • C, simultaneously with the catalytic reaction. Thermal treatment of layered doubled hydroxides results in the formation of mixed metal oxides, beneficially distributed within the supporting material [18]. For this reason, it was expected that the presence of zeolite played a crucial role in the advantageous distribution of Fe-Cu oxides, since the reduction of N 2 O emissions with the increasing temperature has not been observed for single-phase HT. Therefore, the generation of mixed oxides on the surface of clinoptilolite could contribute to a higher selectivity of the catalysts to N 2 and H 2 O above 300 • C.

Chemical Composition and Crystallinity of the Samples
The content of Si, Al, Mg, Fe, and Cu in the samples was measured by inductively coupled plasma-optical emission spectrometry (ICP-OES). The overview of the obtained data, expressed as wt% of each component, is presented in Table 1. It can be observed that the chemical composition of non-supported hydrotalcite is in agreement with the calculated one. Besides, the quantity of Si and Al in the non-modified clinoptilolite, which gives an approximate Si/Al molar ratio of 4.4, corresponds to that reported in the literature [46]. After modification with HCl, concentration of aluminum in the zeolite slightly decreased due to dealumination, which occurs normally after acid treatment [47]. Thereby, the initial modification with HCl resulted in successful, controlled elimination of Al cations from the zeolitic framework. According to Garcia-Basabe and co-workers [47], breaking Al-O bonds and the successful extraction of Al by diluted acids does not affect the topology of the zeolitic framework, however, it does result in a higher thermal stability and pore volume. What is more, Ghasemian et al. [48] reported the improved catalytic performance of clinoptilolite in propane-SCR after the zeolite was leached with mild oxalic acid. The beneficial effect of pre-treatment with acid was ascribed to re-distribution and the increased strength of the acid sites of clinoptilolite. One of the characteristic features of clinoptilolite is the natural presence of iron incorporated into its framework, as confirmed by ICP-OES. Due to that characteristic, the material can exhibit relatively high NO conversion, even in its natural form. Deposition of the hydrotalcite phase resulted in a gradual reduction of Si concentration, delivered to the sample exclusively by the zeolitic support. Moreover, the observed decrease was linear with the increasing coverage of clinoptilolite with HT phase. In contrast, the content of Al exhibited reverse trend, as the result of the presence of aluminum in the deposited hydrotalcite and followed the order of HT_Clin_20 < HT_Clin_25 < HT_Clin_30.
XRD patterns obtained for the investigated materials are presented in Figure 3. Nonmodified zeolite exhibited diffraction maxima located at the 2θ positions of ca. 9 [49,50]. However, the reflections at 9.85, 22.31, 30.02, and 31.81 • suggested that some part of the aluminosilicate coexists with the crystalline phase of heulandite [23]. Besides, the diffraction maxima at 2θ of 16.61, 26.65, and 50.07 • indicated the appearance of stilbite and SiO 2 impurities, respectively [51]. The diffraction pattern of H-Clin showed a similar shape to that of the raw zeolite and the position of the reflections characteristic of heulandite/clinoptilolite phases remained unchanged.  [14,15,54] and suggested that the prepared hydrotalcite exhibited rhombohedral (3R) symmetry. Besides, the crystallite size calculated for HT from Debye-Scherrer formula varied in the range of 100-200 Å.
In the case of HT-modified clinoptilolite samples, all of the obtained XRD patterns displayed identical shape, regardless of the percentage coverage of the zeolite with HT. Both the position and the intensity of diffraction peaks characteristic of clinoptilolite were identical with that obtained for the non-modified material. Thus, the heulandite framework was not sensitive for the deposition of hydrotalcite phase. However, the appearance of new, relatively broad peaks of low intensity at 2θ of ca. 34.43 (009), 45.93 (018), and 60.03 (110)° can be interpreted as the successful formation of a hydrotalcite structure on the surface of clinoptilolite. Additionally, it should be emphasized that at 2θ < 25° the diffraction peaks characteristic of clinoptilolite and hydrotalcite could partially overlap with each other due to their presence at similar diffraction angles.

Textural and Surface Properties of the Samples
Low-temperature N2 sorption was conducted in order to analyze textural features of the investigated materials. The isotherms obtained for non-supported hydrotalcite and HT co-precipitated on natural zeolite are presented in Figure 4. The isotherm of raw clinoptilolite was of type IV (a), with the narrow H3 hysteresis loop, according to the IUPAC classification [55]. Such specification of the hysteresis loop is characteristic of the capillary density in the wedge-shaped mesopores. The monolayer-multilayer adsorption at p/p0 < 0.6 and capillary condensation in mesopores at p/p0 > 0.85 suggested that the zeolite contains also micropores [23,56]. Additionally, such type of isotherm is characteristic of the materials consisting of non-rigid aggregates of plate-like particles, which is in line with  In the case of the fresh hydrotalcite, a single crystalline phase was detected by the reflections positioned at 2θ of 11. 32, 22.74, 34.43, 38.72, 45.93, 60.03, and 61.44 • , corresponding to (hkl) planes given in the figure. Therefore, the prepared material is characterized by a multilayered hydrotalcite-like structure (ICDD 00-022-0700) [15]. The absence of other diffraction maxima in the pattern suggested that no secondary phases were formed during the preparation of the material. Since the background signals were not altered and the diffraction peaks attributed to HT were broad, the obtained material was characterized by a small crystallite size [52]. The Fe-and/or Cu-containing phases were not detected in the obtained XRD patterns, suggesting their incorporation into the structure of hydrotalcite. The unit cell parameters were calculated for the HT sample according to the method proposed by Rives [53]. According to the author, the parameter c represents three times the distance between the layers and strongly depends on the type and orientation of interlayer anions. It can be calculated using two methods: (1) from the position of the first diffraction maximum, (003), c = 3d(003) or (2) from the position of three first reflections, (003), (006), and (009), as the sum of d(003) + 2d(006) + 3d(009). In this work, the c parameter was calculated according to the manner (2) and was found to be 22.61 Å. Additionally, the c' parameter, calculated as c/3, enables the researcher to establish the type of anion in the interlayer space. Thereby, the c' value of ca. 7.52 Å confirmed the presence of CO 3 2− (where the mean distance between the anions equals 3.3 Å) [1,54]. Furthermore, parameter a of the unit cell describes the average cation-cation distances in the hydrotalcite layers, and hence it is strictly correlated with the ionic radius of the cations [15]. The parameter a is typically calculated from the first reflection at 2θ = 60 • (originating from the diffraction by (110) planes) according to the formula a = 2d(110). The calculated values of a = 3.08 Å and c = 22.61 Å are in good agreement with those reported in the literature [14,15,54] and suggested that the prepared hydrotalcite exhibited rhombohedral (3R) symmetry. Besides, the crystallite size calculated for HT from Debye-Scherrer formula varied in the range of 100-200 Å.
In the case of HT-modified clinoptilolite samples, all of the obtained XRD patterns displayed identical shape, regardless of the percentage coverage of the zeolite with HT. Both the position and the intensity of diffraction peaks characteristic of clinoptilolite were identical with that obtained for the non-modified material. Thus, the heulandite framework was not sensitive for the deposition of hydrotalcite phase. However, the appearance of new, relatively broad peaks of low intensity at 2θ of ca. 34.43 (009), 45.93 (018), and 60.03 (110) • can be interpreted as the successful formation of a hydrotalcite structure on the surface of clinoptilolite. Additionally, it should be emphasized that at 2θ < 25 • the diffraction peaks characteristic of clinoptilolite and hydrotalcite could partially overlap with each other due to their presence at similar diffraction angles.

Textural and Surface Properties of the Samples
Low-temperature N 2 sorption was conducted in order to analyze textural features of the investigated materials. The isotherms obtained for non-supported hydrotalcite and HT co-precipitated on natural zeolite are presented in Figure 4. The isotherm of raw clinoptilolite was of type IV (a), with the narrow H3 hysteresis loop, according to the IUPAC classification [55]. Such specification of the hysteresis loop is characteristic of the capillary density in the wedge-shaped mesopores. The monolayer-multilayer adsorption at p/p 0 < 0.6 and capillary condensation in mesopores at p/p 0 > 0.85 suggested that the zeolite contains also micropores [23,56]. Additionally, such type of isotherm is characteristic of the materials consisting of non-rigid aggregates of plate-like particles, which is in line with SEM results [55,57]. The isotherm of H-Clin showed similar shape to that of non-modified zeolite, suggesting that the textural parameters of the materials were probably identical. Similarly to clinoptilolite, the isotherm of non-supported hydrotalcite had a shape characteristic of the type IV (a) [55]. Furthermore, the H1 hysteresis loop confirmed the mesoporous texture of the prepared HT, with well-defined and cylindrical pores [15,52]. Low-temperature N 2 sorption for hydrotalcite co-precipitated on clinoptilolite is expressed by IV type isotherm, classified additionally as a subtype H1, starting at p/p 0 of around 0.8. Therefore, co-precipitation of HT resulted in the formation of additional mesopores of cylindrical-like shape [3]. As summarized in Table 2, the volume of mesopores in the HT_Clin samples increased linearly with the percentage coverage of clinoptilolite with HT. Therefore, the fluent rise of the isotherms obtained for the materials at p/p 0 > 0.85 can be explained by the contribution of new mesopores present in the deposited hydrotalcite-like phase. cylindrical-like shape [3]. As summarized in Table 2, the volume of mesopores in t HT_Clin samples increased linearly with the percentage coverage of clinoptilolite wi HT. Therefore, the fluent rise of the isotherms obtained for the materials at p/p0 > 0.85 c be explained by the contribution of new mesopores present in the deposited hydrotalcit like phase. SBET of the raw clinoptilolite (see Table 2) was 13 m 2 ·g −1 , which is typical for this m terial [24,58]. Vassileva and Voikova [57] postulated that such a low value of specific su face area can be linked with the adsorption of N2 molecules on the external surface of t material, since they cannot enter the internal pores of clinoptilolite. Additionally Spry skyy and co-workers [59] explained this effect by the presence of exchangable cation com plexes, which exist in the micropores of clinoptilolite and hinder diffusion of nitrogen in the inner structure of the zeolite. Alternatively, the authors suggested that the low N2 a sorption capacity can be related to the strong interactions between highly polar structur water molecules and micropores of clinoptilolite. Therefore, the volume of micropor determined for the sample is as well very low. After pretreatment with HCl, specific su face area of clinoptilolite increased to 47 m 2 ·g −1 , as the result of decationation and deal mination, both caused by acid leaching. Additionally, removal of pore-blocking speci enhanced textural features of the zeolite by the elevation of micro-and mesopore volum which is in line with higher SBET of the sample. Non-supported HT showed SBET of 2 m 2 ·g −1 , which was the highest among the investigated materials, due to well-develop mesoporosity. Moreover, the value was even higher than that reported in the literatu for co-precipitated hydrotalcites [15,54,60]. Furthermore, it can be observed that high sp cific surface area of hydrotalcite contributed to the slight increase in SBET determined f  S BET of the raw clinoptilolite (see Table 2) was 13 m 2 ·g −1 , which is typical for this material [24,58]. Vassileva and Voikova [57] postulated that such a low value of specific surface area can be linked with the adsorption of N 2 molecules on the external surface of the material, since they cannot enter the internal pores of clinoptilolite. Additionally Sprynskyy and co-workers [59] explained this effect by the presence of exchangable cation complexes, which exist in the micropores of clinoptilolite and hinder diffusion of nitrogen into the inner structure of the zeolite. Alternatively, the authors suggested that the low N 2 adsorption capacity can be related to the strong interactions between highly polar structural water molecules and micropores of clinoptilolite. Therefore, the volume of micropores determined for the sample is as well very low. After pretreatment with HCl, specific surface area of clinoptilolite increased to 47 m 2 ·g −1 , as the result of decationation and dealumination, both caused by acid leaching. Additionally, removal of pore-blocking species enhanced textural features of the zeolite by the elevation of micro-and mesopore volume, which is in line with higher S BET of the sample. Non-supported HT showed S BET of 256 m 2 ·g −1 , which was the highest among the investigated materials, due to well-developed mesoporosity. Moreover, the value was even higher than that reported in the literature for co-precipitated hydrotalcites [15,54,60]. Furthermore, it can be observed that high specific surface area of hydrotalcite contributed to the slight increase in S BET determined for HT_Clin samples, which varied from 88 to 103 m 2 ·g −1 , depending on the zeolite coverage. This effect can be attributed to the presence of additional mesopores originating from LDH phase.

Morphology of the Samples
The morphology of clinoptilolite, before and after modification with hydrotalcite and the non-supported LDH, was analyzed by means of scanning electron microscopy (SEM). As shown in Figure 5, the natural clinoptilolite used in the studies exhibited high level of crystallinity. One can notice that the zeolitic structure did not consist of individual grains, but randomly arranged, heterogeneous plate-like layers, peripherally covered with impurities. According to the literature [61], the observed splitting of the separated layers is typical for clinoptilolite. Additionally, such structural characteristics of zeolites is advantageous to obtaining uniform dispersion of the catalytically active species [61,62].

Morphology of the Samples
The morphology of clinoptilolite, before and after modification with hydrotalcite and the non-supported LDH, was analyzed by means of scanning electron microscopy (SEM). As shown in Figure 5, the natural clinoptilolite used in the studies exhibited high level of crystallinity. One can notice that the zeolitic structure did not consist of individual grains, but randomly arranged, heterogeneous plate-like layers, peripherally covered with impurities. According to the literature [61], the observed splitting of the separated layers is typical for clinoptilolite. Additionally, such structural characteristics of zeolites is advantageous to obtaining uniform dispersion of the catalytically active species [61,62].  Figure 6 shows SEM images of non-supported and clinoptilolite-supported hydrotalcite. It can be observed from the micrograph recorded for HT that the material is characterized by strong adhesion of the individual layers, which are poorly dispersed. Zulkifli and co-workers [63] reported similar structure of hydrotalcite prepared by coprecipitation, comparing it to the "sand-rose". Zhang et al. [64] explained that this kind of morphology is a consequence of the presence of adsorbed or structural water and nonbridging hydroxyl groups in the interlayer space. Therefore, the plate-like particles of HT can be easily attached to each other through hydrogen bonding. While hydrotalcite phase was co-precipitated on the surface of clinoptilolite, its specification noticeably changed, compared to the non-supported HT. The so-called "sand-rose" morphology of the  Figure 6 shows SEM images of non-supported and clinoptilolite-supported hydrotalcite. It can be observed from the micrograph recorded for HT that the material is characterized by strong adhesion of the individual layers, which are poorly dispersed. Zulkifli and co-workers [63] reported similar structure of hydrotalcite prepared by coprecipitation, comparing it to the "sand-rose". Zhang et al. [64] explained that this kind of morphology is a consequence of the presence of adsorbed or structural water and nonbridging hydroxyl groups in the interlayer space. Therefore, the plate-like particles of HT can be easily attached to each other through hydrogen bonding. While hydrotalcite phase was co-precipitated on the surface of clinoptilolite, its specification noticeably changed, compared to the non-supported HT. The so-called "sand-rose" morphology of the material was completely lost, and the particles of LDH exhibited uniform shape and size of crystals. What is more, their dispersion on the zeolitic support was strongly correlated with the coverage level. Additionally, one can notice that regardless the amount of co-precipitated HT, its particles were rather clustered on the plate-like particles of clinoptilolite. Interestingly, the highest agglomeration degree was observed for HT_Clin 25, in which the zeolite was almost completely covered with HT crystals.

Characteristic Chemical Groups in the Samples
The characteristic chemical groups present in the investigated materials were analyzed using FT-IR spectroscopy. Figure 7 shows the spectra recorded in the wavelength range of 4000-400 cm −1 , which can be divided into three characteristic regions: (1) 3800-3400 cm −1 , attributed to the O-H stretching vibrations; (2) 1700-700 cm −1 , corresponding to stretching Si-O and bending Al-Me-OH vibrations (where Me = cation of metal, for example Mg 2+ or Ca 2+ ), and to structural H 2 O molecules; (3) 700-450 cm −1 , ascribed to pseudo-lattice vibrations of the zeolitic framework or Al-O bonds in hydrotalcites [24,65]. Therefore, the peaks located at 3626 and 3444 cm −1 , present in all of the obtained spectra correspond to OH groups of water bonded to Me-OH units of hydrotalcite or/and ≡Al-OH-Si≡ in the zeolite [65,66]. According to the literature [66,67], ≡Al-OH-Si≡ surface groups and the framework ≡Al-OH and ≡Si-OH species are ion-exchange sites of the zeolites. Thus, the similar shape of the absorption bands for all of the materials confirmed that the hydrotalcite phase was deposited on the surface of clinoptilolite, and that no ion-exchange phenomena occurred through the performed modification. Additionally, the strong deformation mode at 1636 cm −1 corresponds to the presence of adjacent water molecules in the interlayer space of hydrotalcite or H 2 O in the internal structure of clinoptilolite [68,69]. Furthermore, the peak at 1381 cm −1 , detected only for non-supported hydrotalcite appeared due to the presence of carbonate ions bonded to the hydroxyl surface of HT [65]. The band at 1033 cm −1 , observable in the spectrum of HT results from the shift of the interlayer CO 3 2− ions to the so-called "free position", and it y the strong hydrogen bonding between the interlayer H 2 O and hydroxyl sheets of LDH [70]. Interestingly, the peaks corresponding to carbonate ions were absent for all of the HT_Clin samples, and the spectra obtained for clinoptilolite modified with HT phase were similar to those of raw zeolite. The band at 1220 cm −1 is attributed to the asymmetric stretching vibrations of the tetrahedral groups (MeO 4 ), while that at 1048 cm −1 is linked with the asymmetric stretching vibrations, sensitive to the content of Si and Al in the framework [24]. Hence, a slightly lowered intensity of the latter peak in the case of HT_Clin samples probably results from the decrease in Si and Al content in the materials, as confirmed by ICP-OES. The peak at 1015 cm −1 evidenced the presence of iron incorporated into the structure of the materials [71,72]. Last, but not least, the absorption bands at 794, 788, and 602 cm −1 appeared due to the asymmetric stretching vibrations of O-Me-O (where Me = Si or Al) [24]. Additionally, the peak at 445 cm −1 , detected for all of the obtained spectra, can be attributed to the bonds of Al-OH [24,65]. material was completely lost, and the particles of LDH exhibited uniform shape and size of crystals. What is more, their dispersion on the zeolitic support was strongly correlated with the coverage level. Additionally, one can notice that regardless the amount of coprecipitated HT, its particles were rather clustered on the plate-like particles of clinoptilolite. Interestingly, the highest agglomeration degree was observed for HT_Clin 25, in which the zeolite was almost completely covered with HT crystals.

Characteristic Chemical Groups in the Samples
The characteristic chemical groups present in the investigated materials were analyzed using FT-IR spectroscopy. Figure 7 shows the spectra recorded in the wavelength range of 4000-400 cm −1 , which can be divided into three characteristic regions: (1) 3800-3400 cm −1 , attributed to the O-H stretching vibrations; (2) 1700-700 cm −1 , corresponding to 1015 cm −1 evidenced the presence of iron incorporated into the structure of the materials [71,72]. Last, but not least, the absorption bands at 794, 788, and 602 cm −1 appeared due to the asymmetric stretching vibrations of O-Me-O (where Me = Si or Al) [24]. Additionally, the peak at 445 cm −1 , detected for all of the obtained spectra, can be attributed to the bonds of Al-OH [24,65].

Thermal Stability of the Samples
Thermogravimetric analysis was carried out to determine the number of steps and the temperature range of the weight loss during thermal treatment of the materials. The thermograms recorded for clinoptilolite-supported and single-phase HT are shown in Figure 8, while the percentage weight losses in the corresponding temperature regions are collected in Table 3. In general, the weight of the materials decreased during thermal treatment by the value of 15-43 wt%. One should note that the initial weight decreased by ca. 0.5 wt.% during equilibration at 30 °C in air. As presented in Figure 8a, thermal treatment of the single-phase hydrotalcite in the temperature range of 30-800 °C resulted in its gradual weight loss of ca. 41.5 wt%, which corresponds to that reported by Chmielarz et al. [14] for Co-and/or Cu-hydrotalcites. The behavior of the sample at the elevating temperature was characterized by two steps: (1) non-isothermal dehydration of hydrotalcite and elimination of small amount of weakly bonded CO2 within 30-200 °C and (2) removal of hydroxyl groups from the brucite-like layers and decomposition of volatile anions, such as carbonate between 200 and 400 °C [38,54]. Therefore, the peaks at 110 and 150 °C are

Thermal Stability of the Samples
Thermogravimetric analysis was carried out to determine the number of steps and the temperature range of the weight loss during thermal treatment of the materials. The thermograms recorded for clinoptilolite-supported and single-phase HT are shown in Figure 8, while the percentage weight losses in the corresponding temperature regions are collected in Table 3. In general, the weight of the materials decreased during thermal treatment by the value of 15-43 wt%. One should note that the initial weight decreased by ca. 0.5 wt.% during equilibration at 30 • C in air. As presented in Figure 8a, thermal treatment of the single-phase hydrotalcite in the temperature range of 30-800 • C resulted in its gradual weight loss of ca. 41.5 wt%, which corresponds to that reported by Chmielarz et al. [14] for Co-and/or Cu-hydrotalcites. The behavior of the sample at the elevating temperature was characterized by two steps: (1) non-isothermal dehydration of hydrotalcite and elimination of small amount of weakly bonded CO 2 within 30-200 • C and (2) removal of hydroxyl groups from the brucite-like layers and decomposition of volatile anions, such as carbonate between 200 and 400 • C [38,54]. Therefore, the peaks at 110 and 150 • C are related to the release of loosely, structurally and hydrogen-bonded H 2 O from the interlayer space. Furthermore, the stepwise decarbonation of the material is confirmed by the peak at 340 • C (isothermal) and in the region above 415 • C (non-isothermal) [73]. As depicted in Figure 8b-d and detailed in Table 3, the weight loss of HT_Clin samples was significantly lower than that of the pure HT. Thus, the zeolitic support could support the stability of hydrotalcite. However, this phenomenon could also result from lower amounts of HT being subjected to the decomposition compared to the single-phase LDH. It can be observed from the TG/DTG profiles of HT_Clin samples that the temperature of nonisothermal interlayer H 2 O elimination was shifted to 95 • C. This effect could be caused by the simultaneous removal of weakly bonded water molecules from clinoptilolite and the deposited HT phase. Furthermore, regardless of the coverage with hydrotalcite, all of the samples showed similar thermal behavior. Slightly lower values of the total weight loss recorded for HT_Clin 20 might be due to its lower concentration on the surface of clinoptilolite. The peaks appearing in the DTG curves at 270 and 360 • C correspond to the quasi-isothermal dehydroxylation from Al(OH) 3 and Mg(OH) 2 , respectively. Besides, decomposition of the interlayer carbonates took place between 395 and 410 • C [38,73]. Since the temperature range attributed to the decomposition of CO 3 2− was similar for all of the samples, it can be assumed that the stabilization of the carbonates in the co-precipitated HT was almost identical, regardless of the coverage degree. Last but not least, the peaks of very low intensity, located at 485, 510, and 460 • C for HT_Clin 20, 25, and 30, respectively, could be correlated with the presence of very small amounts of residual nitrates used for HT co-precipitation [38]. All in all, in our case, thermal decomposition of hydrotalcites resulted in the formation of the phase of mixed oxides of Fe and Cu, and the successive collapse of the LDH structure [15,73]. However, it should be noted that the temperature regions of the above-mentioned phase transitions are correlated with the chemical composition of HT (type of cations and interlayer anions) and may be varied for various types of LDHs. To sum up, the weight loss of the samples was related to dehydration, dehydroxylation of the brucite-like structure of hydrotalcite, elimination of weakly bonded CO 2 , and thermal decomposition of volatile anions, such as CO 3 2− .

Speciation of Metals in the Samples
UV-Vis-DR spectroscopic studies enabled us to analyze speciation and distribution of transition metals present in natural zeolite or introduced onto clinoptilolite's surface via hydrotalcite co-precipitation. Figure 9a shows UV-Vis-DR spectra recorded for the parent and hydrogen forms of clinoptilolite. It can be observed that the raw clinoptilolite exhibited two strong absorption bands, which confirmed the presence of iron incorporated into the zeolitic structure [47]. The first band, centered at around 240 nm is attributed to ligand-to-metal charge transfer (LMCT, O 2-→ Fe 3+ ) transitions of isolated Fe 3+ species, tetrahedrally coordinated in the extra-framework positions [74]. It can be observed that

Speciation of Metals in the Samples
UV-Vis-DR spectroscopic studies enabled us to analyze speciation and distribution of transition metals present in natural zeolite or introduced onto clinoptilolite's surface via hydrotalcite co-precipitation. Figure 9a shows UV-Vis-DR spectra recorded for the parent and hydrogen forms of clinoptilolite. It can be observed that the raw clinoptilolite exhibited two strong absorption bands, which confirmed the presence of iron incorporated into the zeolitic structure [47]. The first band, centered at around 240 nm is attributed to ligand-tometal charge transfer (LMCT, O 2− → Fe 3+ ) transitions of isolated Fe 3+ species, tetrahedrally coordinated in the extra-framework positions [74]. It can be observed that distribution of iron in the zeolite slightly changed after protonation, since the first absorption maximum was shifted to 260 nm. This result is likely caused by oligomerization of Fe 3+ in the octahedral positions and formation of extra-framework Fe x O y species, primarily existing in the form of dinuclear complexes, such as [HO-Fe-O-Fe-OH] 2+ [75]. A similar effect was observed by Chemielarz et al. [43] for acid-modified vermiculite. Furthermore, the presence of oligonuclear Fe x O y was confirmed by the band at 325 nm, present in the spectra of both Clin and H-Clin samples. The very weak and broad signal, detected in the spectra above 400 nm, is associated with aggregated Fe 2 O 3 particles located near the pore openings or on the zeolite surface [74,76]. spectra of both Clin and H-Clin samples. The very weak and broad signal, detected in the spectra above 400 nm, is associated with aggregated Fe2O3 particles located near the pore openings or on the zeolite surface [74,76].
The UV-vis-DR spectra obtained for clinoptilolite-supported and single-phase hydrotalcite are presented in Figure 9b. The very intense absorption maximum at 200 nm, observed in the spectrum of HT, corresponds to the charge transfer from oxygen O 2-to the monomeric Cu 2+ ions and tetrahedral Fe 3+ cations. Additionally, the existence of [Cu 2+ -O 2--Cu 2+ ] and FexOy oligomers contributed to the increased intensity of the band within 250-350 nm [76]. The flat shape of the spectrum of HT suggested that transition metals were present in the sample exclusively in the form of isolated cations and oligomers and no other phases were formed, which is in agreement with XRD studies. Co-precipitation of HT on the surface of clinoptilolite resulted in a significant decrease in the absorption bands' intensity, which was linear to the coverage of the zeolite with hydrotalcite phase. Such a phenomenon could be caused by the fact that clinoptilolite was the major phase of the analyzed materials. It was observed that the position of the absorption maxima corresponded to that of HT. However, the presence of a narrow peak in the spectrum of HT_Clin 30 located at 200 nm and absent for the other HT_Clin samples suggested that the material with the highest concentration of hydrotalcite phase is the most abundant in the isolated species of Fe and Cu. Moreover, the broad bands appearing for all of the materials in the region of 250-325 nm confirmed that hydrotalcite phase probably did not interact with the zeolitic framework and formed a uniform, oligomeric layer consisting of oxygen and transition metals.

Discussion
The results presented in this work indicate that new NH3-SCR catalysts can be successfully prepared by co-precipitation of hydrotalcite phase on natural zeolite. However, there are some important aspects, which considerably influenced satisfactory catalytic performance of such materials.
Chemical composition of the materials is one of the most important aspects which influences their catalytic performance. In the investigated HT_Clin samples, the mass ratio of Fe:Cu was maintained on the approximate level of 2:1 and the loading of the catalytically active metals increased following the order of HT_Clin 20 < HT_Clin 25 < The UV-vis-DR spectra obtained for clinoptilolite-supported and single-phase hydrotalcite are presented in Figure 9b. The very intense absorption maximum at 200 nm, observed in the spectrum of HT, corresponds to the charge transfer from oxygen O 2− to the monomeric Cu 2+ ions and tetrahedral Fe 3+ cations. Additionally, the existence of [Cu 2+ -O 2− -Cu 2+ ] and Fe x O y oligomers contributed to the increased intensity of the band within 250-350 nm [76]. The flat shape of the spectrum of HT suggested that transition metals were present in the sample exclusively in the form of isolated cations and oligomers and no other phases were formed, which is in agreement with XRD studies. Co-precipitation of HT on the surface of clinoptilolite resulted in a significant decrease in the absorption bands' intensity, which was linear to the coverage of the zeolite with hydrotalcite phase. Such a phenomenon could be caused by the fact that clinoptilolite was the major phase of the analyzed materials. It was observed that the position of the absorption maxima corresponded to that of HT. However, the presence of a narrow peak in the spectrum of HT_Clin 30 located at 200 nm and absent for the other HT_Clin samples suggested that the material with the highest concentration of hydrotalcite phase is the most abundant in the isolated species of Fe and Cu. Moreover, the broad bands appearing for all of the materials in the region of 250-325 nm confirmed that hydrotalcite phase probably did not interact with the zeolitic framework and formed a uniform, oligomeric layer consisting of oxygen and transition metals.

Discussion
The results presented in this work indicate that new NH 3 -SCR catalysts can be successfully prepared by co-precipitation of hydrotalcite phase on natural zeolite. However, there are some important aspects, which considerably influenced satisfactory catalytic performance of such materials.
Chemical composition of the materials is one of the most important aspects which influences their catalytic performance. In the investigated HT_Clin samples, the mass ratio of Fe:Cu was maintained on the approximate level of 2:1 and the loading of the catalytically active metals increased following the order of HT_Clin 20 < HT_Clin 25 < HT_Clin 30, which was in line with the increasing activity in NH 3 -SCR. According to the literature [28,33,77] the excessive loading of Fe in the catalysts leads to the agglomeration of the active phase, the formation of catalytically inactive Fe 2 O 3 , pore clogging, and decreased activity in the low-temperature range. In contrast, higher loading of Cu improves NO conversion below 300 • C due to the presence of CuO species [78]. Nevertheless, Wang et al. [79] found that, while Cu content is higher than 1.5 wt%, high-temperature activity drastically decreases. Thereby, it is expected that relatively high conversion of NO obtained for HT_Clin samples above 300 • C resulted mainly from well-optimized concentrations of Fe and Cu in the catalysts.
Furthermore, one of the crucial factors contributing to high NO conversion is the choice of appropriate support. The supporting material aims to provide high surface to separate catalytically active species and prevent the formation of big crystals. Considering NH 3 -SCR, specifically porous supports are required, in order to supply the catalyst with sufficient space for the reaction to proceed. In our study, we used a natural zeolite, clinoptilolite. The material is not only relatively cheap, but also exhibits very promising catalytic features, such as the presence of iron incorporated into its framework [51]. Our studies confirmed that application of clinoptilolite as the supporting material for LDH phase significantly increased NO conversion above 250 • C. The strong relationship between the presence of the zeolite and the improved elimination of nitrogen oxide can be correlated with Si-O(H)-Al groups, present in the support. The hydroxyl bridges, tetrahedrally coordinated Si-OH and Al-OH, are considered as the source of Brönsted acid sites, which act as the reservoir of NH 3 during NH 3 -SCR [80]. Thereby, the presence of zeolitic framework facilitated adsorption of ammonia and consequently, the proceeding of high-temperature Eley-Rideal mechanism, which assumes adsorption NH 3 and its reaction with NO x from the gas phase [81]. Besides, the acidic character of zeolites is strongly correlated with the Si/Al molar ratio [82]. According to Grajciar and co-workers [80], high-silica zeolites exhibit the lowest stability of Si-O(H)-Al sites, resulting in poor Brönsted acidity. Since the Si/Al molar ratio of clinoptilolite used in this study was relatively low, the enhanced activity of the supported samples could have resulted not only from the presence, but also from the characteristics of the Brönsted centers. Therefore, we concluded that in the case of HT_Clin catalysts, introduction of acid sites was one of the crucial factors determining a high conversion rate of NO. The presence of Cu and Al-O centers delivered to the system from thermal decomposition of hydrotalcite, similarly to the applied zeolite support, were however, a source of Lewis acidic sites, which are considered to favor beforementioned Eley-Rideal mechanism of nitrogen formation [83].
The presented studies indicated that the concentration of the active phase deposited on clinoptilolite did not influence significantly on the catalytic activity. All of the investigated materials exhibited NO conversion characteristic of bimetallic Fe-Cu catalysts, in which CuO contributes to low-temperature activity, while Fe improves high-temperature NO reduction [84,85]. As confirmed by ICP-OES, the concentration of iron in HT_Clin catalysts was higher than that of copper. Therefore, it can be assumed that the loading of Cu in the samples was too low to form sufficient amount of CuO aggregates and increase lowtemperature NO reduction. In contrast, the superior high-temperature activity of HT_Clin catalysts can be correlated with the abundance of oligomeric iron and monomeric copper species in the catalysts. According to the literature [86][87][88][89], the metallic active sites in Fezeolites show strong inhibition effects by NH 3 adsorption at low temperatures. Generally, there are two possible explanations for this phenomenon. First of all, ammonia molecules are strongly bonded to Fe centers at low temperatures, enabling coordination of nitrogen oxides on the active sites. Alternatively, and more likely, adsorption of NH 3 results in the reduction of Fe 3+ to Fe 2+ , which inhibits the Fe 3+ → Fe 2+ redox reaction and oxidation of NO during the catalytic cycle [84]. On the other hand, Brandenberger et al. [90] attributed high-temperature activity of Fe-zeolite catalyst to the presence of dimeric and oligomeric iron species. UV-Vis studies performed over the analyzed HT_Clin catalysts indicated the presence of such structures, regardless of the loading of co-precipitated LDHs. Nonetheless, thermal decomposition of the hydrotalcite phase during the catalytic reaction most likely resulted in the partial redistribution of the active phase. For this reason, we performed additional UV-Vis experiments over HT and HT_Clin catalysts calcined in air. The obtained results, presented in Figure S2, enabled us to predict the type of species produced by the materials during catalytic reaction. It can be observed that thermal treatment indeed changed the distribution of the active phase. Firstly, all of the absorption bands were shifted to a higher wavelength range, compared to the non-calcined samples. The spectrum of HT after calcination exhibited two strong absorption peaks located at 220 and 270 nm, which resulted from the presence of iron oxide [91] and copper oxide [92] nanoparticles, respectively. Furthermore, the intensity of the absorption bands detected for the calcined HT_Clin catalysts was significantly decreased. The spectra of both HT_Clin 20 and 25 were almost identical and differed slightly from that of HT_Clin 30, which confirms that speciation of the active phase was influenced by HT loading. Specifically, the absorption peak appearing for HT_Clin 30 suggested that the sample was the most abundant in oligomeric iron species. What is more, the flat shape of the spectra recorded for HT_Clin catalysts above 500 nm confirmed the absence of bulky particles of metal oxides. Hence, calcination of the hydrotalcite phase produced exclusively extraframework metallic sites (mono-and oligomeric) on the zeolitic support, which had a positive impact on their NH 3 -SCR activity within 200-450 • C. Importantly, it was found that the oligomeric iron sites not only contribute to high-temperature activity, but are also active in non-selective oxidation of NH 3 above 350 • C [90]. This postulate can partially explain the highest concentration of N 2 O observed for HT, HT_Clin 20 and 25. However, one should note that the emission of nitrous oxide was not very pronounced for HT_Clin 30. Furthermore, Pereda-Ayo and co-workers [85] analyzed the behavior of different copper species during NH 3 -SCR reactions. The authors found that Cu 2+ ions, likely formed in low-copper content catalysts, maintain high NO conversion above 300 • C. Considering the relatively low loading of Cu in HT_Clin catalysts and the obtained results of UV-Vis experiments, the most satisfactory catalytic performance of the examined materials within 300-350 • C resulted not only from the presence of polynuclear Fe x O y , but also monomeric Cu 2+ species.
Thermal decomposition of hydrotalcite phase during NH 3 -SCR can be confirmed by monitoring of CO 2 emissions in the post-reaction gas mixture. As presented in Figure S1, the concentration of carbon dioxide produced during the reaction over non-modified clinoptilolite was very low, or even below the detection limit of the instrument. Therefore, CO 2 appeared in the exhausts exclusively due to the decomposition of the hydrotalcite phase. In the case of HT and HT_Clin 20, the emission of CO 2 was maintained on a similar level, regardless temperature of the reaction. In contrast, for HT_Clin 25 and HT_Clin 30 the production of carbon dioxide reached its maximum at 300 • C and moderately decreased above this temperature. The observed phenomenon was linked with the decomposition of the interlayer carbonates, which takes place at approximately 300 • C, as confirmed by TG experiments. It is of considerable interest that the temperature of the highest emission level of CO 2 corresponds to that of the greatest yield of N 2 O. Therefore, the presence of carbon dioxide in the reacting gas mixture limited selectivity to the desired reaction products, especially in the case of HT_Clin 25 and 30. One possible explanation of this effect may be found in the kinetic diameters of the molecules present in the gas mixture.
Since an ammonia molecule is smaller than a CO 2 molecules, carbon dioxide could set some diffusion limits for NH 3 to be successfully adsorbed on the catalyst surface. However, more detailed research is required to determine the impact of the presence of CO 2 on the selectivity of HT_Clin catalysts to nitrous oxide.
In contrast to NO conversion, co-precipitation of hydrotalcite had a noticeable impact on the concentration of the emitted N 2 O. In general, there are a few varied reasons for such phenomenon. First of all, it was observed that the generation of nitrous oxide was higher for HT_Clin samples compared to HT in the entire temperature range. As proposed by Zhang and Yang [44], generation of nitrous oxide below 300 • C results from thermal decomposition of NH 4 NO 3 . Furthermore, Gao et al. [84] found that Brönsted and Lewis acidity promotes formation of ammonium nitrate on the zeolite-supported catalysts in the low-temperature region of NH 3 -SCR, which is followed by the reactions (R2-R4): Therefore, the introduction of acid sites originating from the zeolitic support not only promotes the conversion of NO, but also contributes to non-desired production of N 2 O. The increased concentration of N 2 O in the residual gas mixture can be also correlated with the competitive ammonia oxidation taking place on copper species [14]. Nevertheless, when the temperature of the reaction exceeded 300 • C, the concentration of nitrous oxide gradually decreased. Feng and co-workers [41] found that decomposition of NH 4 NO 3 is promoted by Brönsted acid sites, which participate in several steps of the reaction. Therefore, depending on the temperature region, introduction of acid sites originating from clinoptilolite could indirectly influence the N 2 O yield in different manners. Alternatively, the decreasing concentration of nitrous oxide above 300 • C can be linked with decomposition of hydrotalcite phase and formation of dispersed metal oxides, which limited the production N 2 O [93]. What is more, iron zeolites were confirmed to be active catalysts of N 2 O decomposition [74,[94][95][96]. Pérez-Ramírez et al. [96] found that the extra-framework oligonuclear iron species exhibit superior activity in the reaction compared to the isolated Fe 3+ . The authors ascribed this effect to higher affinity to oxygen, which is crucial fordirect decomposition of N 2 O. Likewise, Sun et al. [74] suggested that more clustered iron sites are required to provide surface oxygen for the reaction with gaseous N 2 O. Considering the cited studies, decomposition of the hydrotalcite phase during the catalytic reaction and generation of oligomeric iron species (see Figure S2) promoted partial decomposition of N 2 O. Nevertheless, despite all of the samples containing dimeric and oligomeric iron sites, one can notice that the decreased concentration of nitrous oxide in the high-temperature range was mostly pronounced for HT_Clin 30. Therefore, the active centers of HT_Clin 20 and 25 promoted oxidation of NH 3 to nitrous oxide rather than decomposition of the generated by-product. Another possible explanation of the lower N 2 O yield observed for HT_Clin 30 is the superior textural parameter possessed by the catalyst. As confirmed by N 2 sorption studies, the sample exhibited the highest mesopore volume among the materials, which improved the diffusion of the reacting molecules. What is more, a relatively high value of S BET of the sample facilitated dispersion of the metallic active centers. In fact, it can be observed that the single-phase HT sample showed even better textural characteristics than HT_Clin 30. Hence, NH 3 -SCR activity of HT was probably limited by the absence of supporting material, abundant in acidic centers, which can adsorb and accumulate ammonia molecules. Given these points, the deposited hydrotalcite phase and clinoptilolite structure acted synergistically, forming new, promising, and ecologically friendly catalysts for the reduction of NO via NH 3 -SCR.
The catalytic features of the investigated materials can be also evaluated basing on the comparison of their performance in NH 3 -SCR with other catalysts. Therefore, in Table 4 we have summarized NO reduction and N 2 O concentration obtained for various catalysts tested in the conditions similar to that applied in our study. In fact, low-temperature activity of the catalysts consisting of HT and clinoptilolite is lower compared to Fe-zeolites of MWW family and single-phase Co-Cu mixed oxides derived from LDH. However, in the case of HT_Clin 25 and 30, NO conversion at 200 • C was very similar to that of Fe-clinoptilolite prepared by post-synthesis method. The lower activity of the investigated materials is most likely caused by three reasons: (1) speciation of the active phase, (2) chemical composition of the samples, (3) omitting of the calcination step. Higher levels of low-temperature activity of the catalysts supported on MWW zeolites resulted from the presence of isolated Fe 3+ species in the framework and extraframework positions. Additionally, Mg 2+ cations, originating from hydrotalcite phase in HT_Clin samples, could partially hinder the adsorption of NH 3 at low temperatures and inhibit the catalytic reaction. Furthermore, better catalytic performance of mixed metal oxides obtained from LDH could be a consequence of higher loading of Cu and the fact that the material was calcined prior to the catalytic reaction. However, the abundance of copper in the cited catalyst led to significant decrease in hightemperature NO conversion, caused by side reactions of NH 3 -SCR catalyzed by Cu above 350 • C. Thereby, it is expected that the controlled introduction of copper into HT_Clin catalysts was beneficial to maintain satisfactory high-temperature activity. Last, but not least, clinoptilolite modified with Fe by standard, post-synthesis method showed similar catalytic performance to HT_Clin 25 and HT_Clin 30. Since Fe loading in the cited Fe-Clin catalyst was approximately 5 wt%, lower activity of HT_Clin 20 results from the content of the active phase in the sample. What is more, one should note that emission of N 2 O for the HT_Clin catalysts exceeded that of other materials summarized in Table 4. Hence, further research is needed to improve selectivity of the catalysts and hinder side-reactions of NH 3 -SCR by the optimization of the chemical composition and preparation procedure.  [27] a NO conversion and N 2 O concentration at 250 and 350 • C, respectively. b Catalysts prepared by one-pot synthesis method with Fe loading of approximately 5 wt%. c Catalyst prepared by co-precipitation of hydrotalcite, followed by calcination at 500 • C in which Cu = 11.9 wt%, Co = 5.8 wt%, and Mg = 14.6 wt%. d Catalyst prepared by co-precipitation of hydrotalcite, followed by calcination at 500 • C in which Cu = 11.9 wt%, Co = 5.8 wt%, and Mg = 14.6 wt%.

Conclusions
The presented study offers one of the first fundamental investigations into the synergistic effect between hydrotalcite-derived active phase and zeolitic support of NH 3 -SCR catalyst. We have presented a novel approach for the synthesis of NH 3 -SCR catalysts, and it was found that natural clinoptilolite improves distribution of the metallic active centers originating from hydrotalcite. Moreover, it supplies the prepared dual-phase catalytic system with the acid sites, which actively adsorbs ammonia during the reaction. As a consequence, the supported LDHs showed superior catalytic activity in NO reduction over the single-phase hydrotalcite. Additionally, we reported that the coverage of clinoptilolite with HT did not influence the conversion of NO. It did, however, affect the emission of N 2 O. The generation of nitrous oxide below 300 • C probably resulted from side reactions of NH 3 -SCR. Conversely, within the range 300-350 • C, it was ascribed to the decomposition of ammonium nitrates or competitive oxidation of NH 3 promoted by copper species. The presented experiments also indicated that calcination of hydrotalcite phase co-precipitated on the natural zeolite prior to NH 3 -SCR test is not required to obtain satisfactory NO conversion and can be conducted during the catalytic reaction. Since our results are encouraging, the most active samples should be tested under various reaction conditions (i.e., without NH 3 , with SO 2 present in the reacting gas, or using various concentrations of the components of the gas mixture). Thereby, our future studies on the clinoptilolite-hydrotalcite catalysts will concentrated on this point.

Supplementary Materials:
The following supporting information can be downloaded at: https: //www.mdpi.com/article/10.3390/ma15227884/s1, Figure S1: Concentration of CO 2 emitted during NH 3 -SCR performed over the investigated samples; Figure S2: UV-Vis spectra recorded for the calcined catalysts. Funding: Agnieszka Szymaszek-Wawryca would like to gratefully acknowledge financial support from National Science Centre (Grant Preludium 19, no. 2020/37/N/ST5/00186). Urbano Díaz acknowledges financial support from Government of Spain through the project PID2020-112590GB C21/AEI/10.13039/501100011033. The work of Monika Motak was supported by the program "Excellence initiative-research university" for AGH University of Science and Technology.