Dongdong Song,
Xunzhe Shao,
Menglong Yuan,
Li Wang*,
Wangcheng Zhan,
YangLong Guo,
Yun Guo* and
Guanzhong Lu
Laboratory for Research Institute of Industrial Catalysis, East China University of Science and Technology, Shanghai, China. E-mail: wangli@ecust.edu.cn; yunguo@ecust.edu.cn; Fax: +86 21 6425 3703; Tel: +86 21 6425 3703
First published on 1st September 2016
The selective catalytic oxidation of ammonia to nitrogen (NH3–SCO) was investigated over MnOx–TiO2. The physicochemical properties of MnOx–TiO2 were characterized by XRD, O2-TPD, NH3-TPD, H2-TPR and XPS, and the reaction mechanism was studied by in situ DRIFTS. The addition of Mn into TiO2 accelerated the support phase transformation and the formation of Mn–O–Ti bonds. MnOx(0.25)–TiO2 showed the best performance in NH3–SCO, for which complete conversion of NH3 was obtained at 200 °C with the temperature window (180–300 °C) for N2 yield > 80%. The formation of Mn–O–Ti provided abundant oxygen vacancies which promoted the adsorption and dissociation of molecular oxygen to form active oxygen species. The finely dispersed MnOx species on the support favored NH3 adsorption. N2O was produced over the whole temperature range while NOx was produced only at high temperatures (>250 °C). N2O was formed from the combination of two HNO species at low temperatures, whereas it was formed from NH3 and nitrate/nitrite species reaction at high temperatures.
4NH3 + 4NO + O2 → 4N2 + 6H2O |
In order to efficiently remove NO, the application of over stoichiometric NH3 results in NH3 slip at low temperature. The concentration of NH3 slip of SCR units has been regulated to less than 10 ppm in China. Catalytic oxidation, with a low level of energy consumption and high purification efficiency, is a promising technology for NH3 emission control. Due to the variety of products in NH3 oxidation, such as N2, NOx (NO, NO2), N2O, the selective catalytic oxidation (SCO) of NH3 (NH3–SCO) to N2 is a potential technology to control NH3 slip without secondary pollutants.
Supported noble metals and transition metal oxides work well in NH3–SCO. Higher NH3 conversion at less than 180 °C could be obtained on Ag/Al2O3,1 CuO/RuO2,2 Pt/CuO/Al2O3,3 and Ir,4 but the N2 selectivity needs to be further improved. Compared with supported noble metal catalysts, transition metal oxide catalysts, CuO,5 Fe2O3,6 NiO,7 V2O5,8 exhibit higher N2 selectivity at rather high temperatures (300–400 °C). Exploring the activity of metal oxides at low temperatures makes possible their practical application in the future.
The presence of Mn4+/Mn3+ type redox couples,9 the tunnel structure and active lattice oxygen species10 contribute to the excellent performance of manganese oxides in oxidation. Due to excellent SO2 tolerance11 and oxygen sensitivity,12 TiO2 is usually used as the support. So MnOx/TiO2 catalysts have been studied for low-temperature selective catalytic reduction of NH3 (NH3–SCR).13
Several mechanisms of the SCO process have been suggested. Three major reaction pathways have been proposed. The imido mechanism suggests that the intermediate species are the imido (NH) and nitrosyl (HNO) species,14 and N2 comes from their reaction. The hydrazine (N2H4) mechanism proposes that N2H4 arises from two amide species (NH2), and then N2 from N2H4 oxidation.15 The key step of the above mechanisms is NH3 dehydrogenation. The internal selective catalytic reduction (i-SCR) mechanism focuses on the reaction between NH3 and NOx species.16 The mechanism varies with the properties of the catalysts.
In this paper, a series of MnOx–TiO2 catalysts were prepared by the sol–gel method and their catalytic performance in NH3 selective oxidation was investigated. XRD, Raman, N2 adsorption–desorption, ICP, O2-TPD, H2-TPR and XPS were used to characterize the physicochemical properties of the samples, and in situ DRIFT was applied to understand the oxidation reaction process. The correlation between the activity and physicochemical properties was investigated.
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Powder X-ray diffraction (XRD) measurements of the catalysts were carried out using a Bruker/D8 X-ray diffractometer (Bruker, Germany) with Cu Kα radiation (λ = 0.154056 nm) at 40 kV and 40 mA. The patterns were taken over the 2θ range from 10° to 80° at a scan speed of 6° min−1.
X-ray photoelectron spectroscopy (XPS) analysis was performed using an ESCALAB 250Xi (Thermo Fisher Scientific, USA) with a monochromatic Al Kα source (hν = 1486.6 eV), operating at 150 W. The binding energy of adventitious C 1s (284.6 eV) was used as a reference.
Hydrogen temperature-programmed reduction (H2-TPR) experiments were carried out using a commercial system (PX200, PengXiang, China) equipped with a thermal conductivity detector. Ammonia temperature-programmed desorption (NH3-TPD) and oxygen temperature-programmed desorption (O2-TPD) were performed with the same apparatus. In H2-TPR, the samples (50 mg) were heated in 5 vol% H2/N2 (40 ml min−1) from room temperature to 850 °C at a ramp of 10 °C min−1. In NH3-TPD, the samples (50 mg) were preheated in N2 at 500 °C for 1 h before testing. After 5% NH3 adsorption saturation at 30 °C, N2 was introduced to remove physically adsorbed NH3. In O2-TPD, the outlet gas was recorded with an online mass spectrometer apparatus (HIDEN QIC-20, England). The samples (100 mg) were pretreated in 3% O2 in He stream (30 ml min−1) at 450 °C for 1 h, then cooled down to ambient temperature in He to get a stable MS baseline. In all the experiments the heating rate (10 °C min) was the same from 50 to 800 °C.
Raman spectra were obtained using a Renishaw inVia Reflex (Renishaw, England) spectrometer equipped with a CCD detector at ambient temperature and under moisture-free conditions. The excitation source was the 514.5 nm line of an Ar ion laser. The laser power was set at 3 mW.
The in situ DRIFTS was performed using a Nicolet 6700 FT-IR spectrometer (Thermo Fisher Scientific, USA) with an MCT detector. In the DRIFT cell with ZnSe windows connected to a gas flow system, the sample was pretreated at 400 °C in Ar for 1 h before each test. The background spectra were recorded at each temperature. 500 ppm NH3, 5% O2 and Ar balance were used in the experiments at a total flow rate of 50 ml min−1.
In order to exclude the effect of surface area on activity, the specific activities were calculated and are shown in Table 1. With the Mn loading increasing from 0.1 to 0.25, the specific activity increased from 0.7 to 3.6 (mmol (min−1 m−2) × 10−6) at 130 °C, while further increasing Mn loading had less effect on specific activity. Therefore, there was an optimum Mn amount (25%) for selective NH3 oxidation.
Catalysts | SBET (m2 g−1) | Pore size (nm) | Crystallite sizea (nm) | Mn contentb (wt%) | Specific activity (mmol (min−1 m−2)) × 10−6 |
---|---|---|---|---|---|
130 °C | |||||
a Calculated from the Scherer equation according to the (110) diffraction peak of TiO2.b Mn content of the catalyst determined by ICP-AES. | |||||
Pure TiO2 | 45.1 | 8.7 | 21.0 | — | 0.5 |
MnOx(0.1)–TiO2 | 74.2 | 5.0 | 8.8 | 8 | 0.7 |
MnOx(0.2)–TiO2 | 113.2 | 4.2 | 10.4 | 18 | 0.8 |
MnOx(0.25)–TiO2 | 46.6 | 6.2 | 11.7 | 27.8 | 3.6 |
MnOx(0.3)–TiO2 | 41.7 | 4.8 | 11.1 | 33.7 | 3.1 |
The N-containing product distribution (N2, NOx and N2O) is also shown in Fig. 1. N2O was produced even at low temperatures (>100 °C) with a yield lower than 10%; while the appearance of NOx occurred at high temperatures (>250 °C) with a yield of up to 20% at 350 °C. The yield of N2O decreased with the increase of NOx yield.
The XRD patterns of MnOx–TiO2 catalysts are presented in Fig. 2. This suggests that the support was in the form of anatase. With the introduction of Mn, the diffraction peaks of anatase weakened and the characteristic peaks of rutile gradually intensified. The MnOx(0.2)–TiO2 material exhibited complete rutile phase which indicated that Mn loading speeded up the anatase-to-rutile (A–R) transition. The doping of Mn caused the diffraction peak (2θ = 36.2°) to shift to higher angles compared with TiO2, which was attributed to lattice shrinkage due to the lower ionic radius of Mn4+ (0.060 nm) with respect to Ti4+ (0.068 nm).
New characteristic peaks assigned to Mn2O3 and Mn3O4 were detected in the pattern of MnOx(0.3)–TiO2. The appearance of MnOx was due to the separation of Mn from TiO2.
In the typical sample of MnTiO3, the characteristic peaks could be observed at 684, 611, 465, 360, 336, 264, 236, and 202 cm−1 separately, and the intense Raman band at 684 cm−1 is regarded as a typical feature for MnTiO3.18 The strongest Raman band around 684 cm−1 is assigned to the highest frequency vibrational mode of octahedral MnO6, while the weak phonon modes below 300 cm−1 arise from lattice vibrations.19
With the addition of Mn, the characteristic peak of MnTiO3 at 684 cm−1 appeared. The peak intensified with increasing Mn loading amount up to 25 wt%; and a further increase in Mn loading, such as 30 wt%, led to the peak at 684 cm−1 being broadened which was due to overlapping with MnOx. Eight Raman active fundamentals, at 684, 610, 460, 360, 335, 262, 234, and 202 cm−1, were clearly observed for MnOx(0.25)–TiO2, which indicated the formation of MnTiO3. When taking the sensitivity of the Raman technique to the vibration of chemical bonds into account, it can be understood why MnTiO3 species could not be detected by XRD. It was seen from the Raman results that the formation of Mn–O–Ti supported the strongest interaction between TiO2 and Mn on MnOx(0.25)–TiO2.
Catalysts | H2 consumption (mmol g−1) | (Oα + Oβ)a | Mn3+/Mntotal | OS/(OL + OS) | Surface atom ratiob of Mn/Ti | |||||
---|---|---|---|---|---|---|---|---|---|---|
Total | a | b | c | d | e | |||||
a Obtained from O2-TPD.b Obtained from XPS. | ||||||||||
TiO2 | 0.04 | — | — | — | 0.04 | — | — | — | 0.16 | — |
MnOx(0.1)–TiO2 | 0.75 | 0.1 | 0.33 | 0.27 | — | — | 1 | 0.58 | 0.19 | 0.3 |
MnOx(0.2)–TiO2 | 2.11 | 0.3 | 0.99 | 0.75 | — | 0.05 | 2.9 | 0.59 | 0.25 | 0.7 |
MnOx(0.25)–TiO2 | 3.13 | 0.43 | 1.42 | 1.0 | — | 0.27 | 5.9 | 0.61 | 0.3 | 1.2 |
MnOx(0.3)–TiO2 | 3.20 | 0.34 | 1.38 | 0.98 | — | 0.5 | 2.6 | 0.56 | 0.27 | 1.7 |
A weak peak was observed for the reduction of TiO2 in the temperature range of 500–800 °C with 0.04 mmol g−1 total H2 consumption. With the presence of Mn, a peak with a shoulder at 100–450 °C was observed and intensified with an increase of Mn concentration. Combined with the ICP and the integral H2 consumption, it was known that the oxidation state of Mn was around +3 which indicated that MnOx was mainly in the form of Mn2O3. By de-convoluting the main reduction peak, three peaks were observed which represented the reduction of different species. Ettireddy20 assigned the peak at 215 °C to the reduction of anatase TiO2 closely interacted with MnOx, and the peak area correlated with the anatase TiO2 concentration. Although XRD results presented the A–R transformation of the support with the increase of Mn, the H2 consumption amount of peak a still kept increasing as shown in Table 2. So it excluded the possibility that peak a was from the reduction of the support, and it should be assigned to the reduction of Mn2O3 close to TiO2. The reduction of bulk Mn2O3 took place through a distinct two-step process: the first step involved the reduction of Mn2O3 to Mn3O4, and the second step was the reduction of Mn3O4 to MnO.21 The H2 consumption ratio confirmed the dominant Mn2O3 species, so peaks b and c were assigned to the reduction of bulk Mn2O3. The shoulder peak e at 400–550 °C was assigned to the reduction of Mn3O4, and XRD also confirmed the existence of Mn3O4 with the introduction of Mn loading up to 30 wt%.
Compared with the support, the intensity of the peaks (Oα, Oβ) increased with the amount of Mn up to 25%, and the decrease in intensity was also observed on MnOx(0.3)–TiO2. The increased area of Oβ implied a strong interaction between TiO2 and MnOx which led to the enhancement in lattice defects and oxygen vacancies and promoted the adsorption/mobility/desorption of O22−/O−. The formation of Ti–O–Mn or MnTiO3 detected by Raman spectroscopy also confirmed the strong interaction between TiO2 and MnOx. Meanwhile, the peak at 200–300 °C attributed to the desorption of O2− becomes a little stronger, which was consistent with the XPS results that more surface oxygen species existed on the surface of MnOx(0.25)–TiO2.
The temperatures of the O2− desorption peaks increased as Mn substitution amounts increased. This demonstrated that the interactions of Mn–O bonds were strengthened so the desorption of O2− became difficult, which was in agreement with the result of H2-TPR.
Compared with TiO2, the NH3 desorption temperature at weak acid sites shifted to lower temperatures. The presence of Mn promoted the amount of acid sites which suggested that Mn was the source of acid. The maximum acid sites seemed to be obtained on MnOx(0.2)–TiO2, while further increasing Mn led to the decrease of the amount of acid sites which was attributed to the aggregation of manganese oxide.
By excluding the effect of surface area, the acid density is calculated and the results are shown in Fig. 6B. Unlike the results in Fig. 6A, the presence of Mn had no obvious effects on acid density until Mn loading was up to 0.25. A further increase of Mn loading up to 0.3 led to the decrease of acid density on the catalyst. The highest acid density was obtained on MnOx(0.25)–TiO2 which favored NH3 adsorption and activation.
As shown in Fig. 7A, two peaks can be distinguished in the XPS O 1s spectra. The peak at 529.5 eV was assigned to the lattice oxygen O2− (OL), and the peak at 531.5 eV was assigned to the surface oxygen (OS), such as O2−, O22− and O−, belonging to defect oxide and hydroxyl-like groups.24 The OS/(OL + OS) ratio of TiO2 was only 16%; with the introduction of Mn, the OS/(OL + OS) ratios of the catalysts increased to 30%. This indicated that Mn promoted the amount of surface oxygen on the catalysts. The OS/(OL + OS) ratio on MnOx(0.25)–TiO2 reached 30% which was 2 times higher than that on TiO2.
Fig. 7C shows the XPS spectra of Mn 2p in the MnOx–TiO2 samples. The Mn 2p peaks could be de-convoluted to three peaks, the peaks at 643.0–644.0, 641.0–641.9 and 640.2–640.7 eV corresponding to Mn4+, Mn3+ and Mn2+, respectively.25 It was interesting to note that Mn3+ was the dominant species in the samples with small amounts of Mn4+ and Mn2+ species. The ratio of Mn3+/Mntotal increased with the addition of Mn and reached a maximum on MnOx(0.25)–TiO2. The Mn4+ species were in the form of Mn–O–Ti, confirmed by Raman spectroscopy; while the Mn2+ species originated from Mn3O4 detected by XRD. With the increase of Mn loading, the surface atomic ratio of Mn/Ti increased accordingly which suggested the enrichment of Mn species on the catalyst surface. Mn 2p3/2 binding energy slightly shifted to high binding energy (641.2 eV to 641.7 eV) because the Mn species showed deviation of electron cloud by interacting with titanium species, leading to an enhancement in oxidative ability.26
According to the law of conservation of charge, a binding energy increase of one element must be accompanied by a binding energy decrease of another element in an isolated system. The shift of Ti 2p3/2 (458.3 eV to 457.8 eV) and O 1s (529.5 eV to 529.2 eV) also confirmed the existence of interaction between Mn and Ti.
The intensity of Lewis acid site bands became strong when the temperature increased from 50 °C to 140 °C, while further elevating the temperature up to 300 °C caused the disappearance of the bands. By comparing the band intensities of Lewis acid sites and Bronsted acid sites, it was found that ammonia mainly existed on Lewis acid sites and kept stable even at 250 °C.
When the temperature increased from 100 °C to 140 °C, two new weak bands at 1456 and 1510 cm−1 were observed which are ascribed to –NH deformation modes of imido (N–H) species32 and amide (–NH2),33 respectively. The appearance of these intermediates indicated adsorbed NH3 could be activated through the abstraction of hydrogen.
Meanwhile, two weak bands at 2213 and 2240 cm−1 were observed which can be assigned to N–N stretching modes of adsorbed N2O from the oxidation of ammonia.34 The appearance of N2O in the absence of O2 demonstrated the oxidation of NH3 by lattice oxygen.
The presence of NH3 and O2 also led to the appearance of bridge nitrite (1234 cm−1) and monodentate nitrate (1277 cm−1)35 at 100 °C and bidentate nitrate36,37 (1540 cm−1) at even higher than 250 °C. A weak band at 1832 cm−1 assigned to nitrosyl (–HNO)38 species was observed which was from the interaction between –NH and oxygen atoms. Combined with the appearance of nitrite and nitrate species, it is proposed that nitrosyl (–HNO) could be further oxidized to nitrite and nitrate.
Gas-phase N2O (2213, 2240 cm−1) was found in the whole temperature range, while the band at 1612 cm−1 ascribed to the weakly adsorbed gas NO2 (ref. 39) was only observed at 250 °C. The activity test results also confirmed that the product distribution of N-containing species depended on the temperature. There are many researches on the form of N-containing species in exhaust. It is usually considered that N2 arises from the reaction between NH and HNO.40 There are two main ways to get N2O, one is from the interaction between two HNO species,41 and the other way is by the reaction between nitrate species and ammonia.42 NOx is usually considered as the decomposition product of adsorbed nitrate/nitrite species.43
The interaction of O2 with the in situ-formed NH3 species at 230 °C was investigated. The experiment was conducted as follows: prior to the introduction of O2, the catalyst was exposed to 500 ppm NH3 at 230 °C for 1 h, followed by purging with Ar for 30 min. The in situ DRIFT spectra of the catalyst were recorded as a function of time, and the results are shown in Fig. 10.
The intensities of Lewis acid site and Bronsted acid site bands decreased even after introducing O2 for 1 min; and this became obvious after 5 min. With further exposure for 10 min, the nitrate species (1234, 1276, 1544 cm−1) appeared. The changes in the first 5 min were ascribed to the reaction between adsorbed NH3 and O2, and the appearance of nitrate species showed that adsorbed NH3 could be further oxidized to nitrate species. Meanwhile, the bands (2211, 2240 cm−1) assigned to N2O were observed after introducing O2 for 1 min which then decreased with further exposure time. With the appearance of nitrate species, the weakly adsorbed gas NO2 species (1612 cm−1) were observed.
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Fig. 11 In situ DRIFT spectra of catalyst exposed to NH3 + O2 after NO adsorption at 160 °C or 250 °C. |
Bridge nitrite (1234 cm−1), monodentate nitrate (1270 cm−1), and bidentate nitrate (1547 cm−1) were observed after NO pretreatment, which indicated that NO could be oxidized to nitrite and nitrate by lattice oxygen at 160 and 250 °C.
After exposure to NH3 and O2 for 10 min at 160 °C, the bands of NH3 adsorbed on Lewis acid sites (1178, 1602 cm−1) appeared and the intensity increased with the exposure time. Meanwhile, the intensity of the bands of nitrite and nitrate species kept stable in the presence of NH3 and O2.
Unlike the experiment conducted at 160 °C, an obvious disappearance of nitrite and nitrate species was observed after adding NH3 and O2 for 20 min at 250 °C, and the appearance of N2O (2211, 2240 cm−1) after 15 min was observed. The findings suggested that N2O was the reaction product of NH3 and nitrite/nitrate species.
Based on the above results, NH3 was mainly adsorbed on Lewis acid sites (Fig. 8) and activated through hydrogen abstraction. The intermediates (–NH2, –NH) were further oxidized to HNO species, and two HNO species can convert to N2O at low temperatures (Fig. 9). Meanwhile adsorbed NH3 can be directly oxidized to nitrite/nitrate species (Fig. 10).
The performance of nitrite and nitrate species depended on the temperature (Fig. 11). With the nitrite and nitrate species disappearing, N2O was observed at 250 °C which suggested that N2O was formed from the reaction between NH3 and nitrite/nitrate species. Combined with the in situ DRIFT results, the reaction mechanism of NH3 selective oxidation is shown in Fig. 12.
NH3 adsorbed on the Lewis acid sites can convert to NH and NH2 species by dehydrogenization and HNO species by further oxidation; meanwhile it also can be oxidized to nitrite and nitrate species deposited on the surface. N2 was produced from the reaction between HNO and NH species. N2O was formed from the combination of two HNO species at low temperatures, while from the reaction between adsorbed NH3 and nitrite/nitrate species at high temperatures.
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