Environ. Sci. Technol. 2008, 42, 4771–4776 Effect of Volatile-Char Interaction on the NO Emission from Coal Combustion M I N G Y U Y A O , † D E F U C H E , * ,† YANHUA LIU,‡ AND YINHE LIU† State Key Laboratory of Multiphase Flow in Power Engineering, School of Energy and Power Engineering, and School of Human Settlements and Civil Engineering, Xi’an Jiaotong University, Xi’an 710049, China Received August 4, 2007. Revised manuscript received January 18, 2008. Accepted April 15, 2008. To clarify the effects of volatile-char interaction on the redistribution of fuel-N to N2 during devolatilization and the reduction of NO through gas-solid reactions during combustion, two types of experiments were performed on a novel reactor. The separate combustion of volatile and char and the combustion of entrained pulverized coal, and the formation of NO was examined between 800 and 1100 °C by using four typical Chinese coals with different ranks. The effect of volatile-char interaction on fuel-N conversion to NO during combustion was elucidated through comparing the NO emissions from the two types of combustion experiments. The results show that the volatile-char interaction is more important in the redistribution of fuel-N to N2 during devolatilization than in the reduction of NO over 900 °C, and a contrary conclusion is obtained below 850 °C for all used coals. A specific parameter has been proposed to characterize the relative importance of the volatile-char interaction in the redistribution of fuel-N to N2 during devolatilization to the interaction in the reduction of NO to N2 during simulataneous combustion of volatile and char. The results are of significance for minimizing the NO formation in industrial combustion processes. 1. Introduction NO emissions from coal combustion are derived from both the coal nitrogen and the nitrogen in the combustion air. Three types of NO formation, thermal, prompt, and fuel, have been identified (1, 2). Coal contains 0.5-2 wt % nitrogen integrated in the organic coal structure. This nitrogen, known as fuel-N, is partly converted to NO during combustion, and becomes the major source of NO in pulverized coal combustion, accounting for more than 80% of the total NO emission (3, 4). To optimize combustion and minimize NO formation, a good understanding of the fuel-N conversion is required. The combustion of coal can be conceptually divided into two steps, that is, the devolatilization of coal followed by the reaction of the volatile and char with oxygen (1). The devolatilization is the thermal decomposition of the fuel resulting from the heating of the coal particles. The products * Corresponding author phone: +86-29-82665185; fax: +86-2982668789; e-mail: [email protected]. † State Key Laboratory of Multiphase Flow in Power Engineering, School of Energy and Power Engineering. ‡ School of Human Settlements and Civil Engineering. 10.1021/es071945k CCC: $40.75 Published on Web 06/04/2008 2008 American Chemical Society of devolatilization are char and volatile. Part of the nitrogen escapes as volatile-N in gas phase such as cyanic (CN) and amino (NH) compounds. The nitrogen retained in the residual char is called char-N. Thus, NO finally formed during coal combustion comes from the combustion of both volatile-N and char-N (5–7). However, char-N differs from volatile-N in the mechanism of NO formation during combustion. The NO from the combustion of volatile is formed through homogeneous reactions, whereas the NO formation from char-N involves a gas-solid heterogeneous oxidation and an important reduction step of NO back to N2 (8). One of the important objectives in coal combustion research is to develop a comprehensive model of NO formation. To do so, most investigators developed individual models for volatile-N and char-N and then their relative contributions to the total NO emission were evaluated (1, 9–11). Therefore, it is a common practice that volatile and char are combusted separately to investigate their relative contributions to the total NO emission (2, 9). However, separate combustion of volatile and char cannot represent the real process in industrial furnaces. Previous work has shown that volatile-char interaction can lead to drastic changes in char structure and properties during the pyrolysis of coal (13–15), and throughout the process of coal-N oxidation there are significant gas-solid reactions between volatile and char if they are not separated from each other. Therefore it is necessary to take into account the effect of volatile-char interaction to develop an even more exact prediction model of NO formation during coal combustion for the minimization of NO emission (16, 17). Currently, little is known about the effect of volatile-char interaction on the conversion of fuel-N to NO. Using a novel reactor, this study is focused on the relative contributions of volatile-N and char-N to the total NO emission and the effect of volatile-char interaction during the coal combustion. The results demonstrate that the volatile-char interaction has a drastic effect on the conversion of fuel-N during combustion through two ways: the fuel-N redistribution during devolatilization and the reduction of NO during the combustion of volatile and char. 2. Experimental Section Radicals formed during devolatilization surrounding the char can greatly affect the reactions of char-N. Recent studies (13–15) have confirmed that volatile-char interaction during pyrolysis at elevated temperatures leads to a drastic change in the releases of fuel-N. It was believed that the volatile-char interaction would make more fuel-N release as N2 during devolatilization through the gas-solid reactions (4, 16–20). In addition, the reduction of NO could be enhanced by the volatile-char interaction during the simultaneous combustion of volatile and char (22, 23). The fate of the fuel-N is schematically illustrated in Figure 1. Figure 1 implies that the volatile-char interaction could help reduce the NO formation through the redistribution of fuel-N to N2 during devolatilization and the reduction of NO during the combustion that follows. The conversion of fuel-N to NO without volatile-char interaction is assumed to be X0. The conversion of fuel-N to NO with volatile-char interaction taking effect only during devolatilization is expressed by X1, and the separate combustion of volatile and char can exemplify this conversion. X2 is assumed to denote the conversion of fuel-N to NO with volatile-char interaction taking effect only during combustion, and the combustion of entrained pulverized coal can exemplify this conversion. VOL. 42, NO. 13, 2008 / ENVIRONMENTAL SCIENCE & TECHNOLOGY 9 4771 FIGURE 1. Simplified scheme to represent the fate of fuel-N in theory. x1 and x2 are defined as the volatile-char interaction coefficients to describe the effect of the interaction on NO abatement: x1 ) X0 ; X1 x2 ) X0 X2 (1) Two types of experiments were designed in order to clarify the relative contributions of char-N and volatile-N to NO emission from the combustion of coal and the effect of volatile-char interaction on fuel-N conversion. In the first type of experiment, NO emission from char-N and volatile are quantified separately. A novel setup was established for the experiments, as shown in Figure 2. The quartz reactor was located in the furnace. The electrical heating created approximately isothermal conditions. Temperature could be adjusted continuously. A 0.1 g coal sample was used throughout all experiments. The sample was loaded in the microfeeder (5) in advance, and the helium gas flow (800 mL/min) entrained the coal particles into the reactor that had been heated to a predetermined temperature within two minutes, as shown in Figure 2. The exiting tube was fixed and the sample tube could be pushed forward by a stepping motor to keep a given distance between the bottom of exiting tube and the surface of sample bulk, so that a constant feeding rate could be maintained. Quartz cotton of 3 cm thick was placed in the inner tube (9) at about 10 cm to its exit. Once coal particles entered the reactor volatiles were released and char was formed. The volatiles were able to pass through the quartz cotton and entered the outer tube of reactor, but the char was retained on the quartz cotton. When an experiment was started, the O2 stream (200 mL/ min) was switched to Line b in Figure 2 to oxidize the volatiles. The O2 stream was switched to Line a in order to oxide the char formed as soon as devolatilization had been finished. Experiments continued until the complete combustion of char. The purity of the O2 and He used was more than 99.999%. The concentration of NO from the combustion of volatile and char was measured in succession by a GASMETTM DX4000 FT-IR gas analyzer. The profile of NO emissions from the separate combustion of volatile and char is shown in Figure 3a. Ts represents the time when O2 is switched and char-N began to combust. The two peaks in the NO profile suggest that there should be two NO sources, the first arises from the nitrogen in the volatile matters, and the second arises from the fixed nitrogen in char. The char came from the same coal sample as volatiles, and it was combusted intactly as it was prepared to keep the activity of char until being oxidized. Obviously, an interaction between volatile and char would exist in the inner tube during pyrolysis. However, since the volatile was separated from char and oxidized in a different place, there would be no interaction between the volatile and the char during this period. So the total NO emission in this type of experiments can be represented as X1 ) X0 x1 (2) X1 is the total conversion of fuel-N to NO from both volatile and char. Experiments of the second type involved the combustion of entrained pulverized coal. The gas for feeding coal particles was switched from pure He to He-O2 mixture. Volatile and char undergo simultaneous combustion. The profile of NO emission for the second type of experiments is shown in Figure 3b. The volatile was oxidized as soon as it was released from coal particles because of sufficient oxygen. But, there FIGURE 2. Schematic experimental setup: 1 compressed gas; 2 steady flow valve; 3 pressure valve; 4 flow meter; 5 microfeeder; 6 three-way valve; 7 electrical furnace; 8 feeding tube; 9 inner tube; 10 outer tube; 11 quartz cotton;12 gas analyzer. 4772 9 ENVIRONMENTAL SCIENCE & TECHNOLOGY / VOL. 42, NO. 13, 2008 FIGURE 3. NO emissions from the separate combustion of volatile and char (a) and the combustion of entrained pulverized coal (b). TABLE 1. Fuel Characteristics proximate analysis [wt%, dry] ultimate analysis [wt%, daf] coal code ash volatile matter fixed carbon C H N S Oa Shenmu Hejin Tongchuan Jiaozuo SM HJ TC JZ 7.9 24.09 27.00 19.04 33.6 17.10 14.43 5.86 58.5 59.00 58.57 75.24 79.14 65.92 62.65 75.61 4.56 3.32 3.05 2.25 1.65 0.87 1.10 0.73 0.90 0.44 2.26 0.73 13.75 5.36 3.93 1.64 a O determined by difference. was little chance for the volatile to react with char under this condition, and the effect of volatile-char interaction on the fuel-N redistribution during devolatilization could be ignored. Nevertheless, the NO formed from volatile-N could be reduced by char through the gas-solid heterogeneous reactions, so that the volatile-char interaction was ineluctable during the combustion of volatile and char, and the NO emission can be represented as follows: X2 ) X0 x2 XNO ) t0+∆t t0 F × CNO × 10-6 × dt ⁄ 22.4 M × Nd ⁄ 14 metal content, wt% (dry) sample ash (wt%, dry) Si Al Fe Ca Mg K Na Ti SM HJ TC JZ 7.9 24.09 27.00 19.04 4.18 11.69 13.21 9.52 1.31 8.44 8.74 6.26 0.46 0.88 1.81 0.81 1.06 1.08 0.94 0.89 0.10 0.18 0.15 0.15 0.02 0.20 0.04 0.24 0.23 0.22 0.76 0.19 0.06 0.32 0.32 0.27 (3) The total NO emission during experiments is the integral of NO concentration within a certain length of time. If XNO is used to represent the ratio of nitrogen converted to NO during combustion process within ∆t to the nitrogen contained in the sample, then ∫ TABLE 2. Ash and Metal Contents × 100% (4) where F ) volumetric flow, L/s; t0 ) time at which measurement begins; ∆t ) measurement duration, s; M ) sample weight, g; Nd ) nitrogen content in sample, % db; and CNO ) NO concentration in flue gas, µL/L. Four Chinese coals used for experiments were Jiaozuo, Tongchuan, Hejin, and Shenmu, which are denoted respectively as JZ, TC, HJ, and SM hereinafter. All the coal samples were air-dried at 105 °C for 24 h, then ground and sieved to a size of less than 150 µm. The ultimate and proximate analyses are listed in Table 1. Table 2 shows the ash and metal contents in the used coals. 3. Results and Discussion 3.1. NO Emissions from the Separate Combustion of Volatile and Char. Figure 4 shows the NO emissions from the separate combustion of volatile and char, that is, the emissions from the experiments of the first type, and the total conversion of fuel-N to NO (expressed by X1) is XNO from volatile plus that from char. The results show that the total NO emission from separate combustion of volatile and char is greater at lower temperatures, and reaches the highest at 800 °C for all samples. Some previous investigators reported that the total NO emission increased with increased temperature (22, 23), but their experiments were performed under the condition of simultaneous volatile and char combustion. It has been reported that there was abundant N2 release from coal during devolatilization, and the conversion of fuel nitrogen to N2 increased almost linearly with temperature (16–20). As such, the total NO emission in this study inevitably decreases because of the more conversion of fuel nitrogen to N2 at higher temperatures. It seems that the volatile-char interaction has more significant effect on the redistribution of fuel-N to N2 during devolatilization at higher temperatures, resulting in less NO emission. It can also be seen from Figure 4 that there is an obvious dependence of X1 on XNO from char, since XNO from volatile varies very insignificantly with temperature, especially when the temperature is over 1000 °C. It has been indicated that higher conversion of nitrogen to N2 is always associated with lower conversion to char-N, and XNO from volatile is independent of temperature when the temperature is high enough (19, 20, 24). The experimental results show that for HJ and TC coals the total NO emission X1 and XNO from char is increased remarkably at 1100 °C relative to the values at 1000 °C. As we know, various minerals in coal can exert an influence on the conversion of char-N to NO (25–27). It is assumed that the catalytic effect of minerals in HJ and TC coals on the conversion of char-N to VOL. 42, NO. 13, 2008 / ENVIRONMENTAL SCIENCE & TECHNOLOGY 9 4773 FIGURE 4. NO conversion from the separate combustion of volatile and char. FIGURE 5. Contribution of Char-N to NO emission. FIGURE 6. NO conversion from the combustion of entrained pulverized coal. NO becomes predominant at 1100 °C, resulting in more XNO from char, hence more X1. Figure 5 shows the contribution of char-N to total NO emission, i.e., the ratio of the NO emission from char to the total NO emission. Obviously, the NO emission from char of SM coal (bituminous) is less than the NO emission from volatile during 800-1100 °C, since it is always less than 35%. As for JZ coal (anthracite), char-N becomes the primary source of NO emission and the contribution of char-N is greater than 56% at all temperatures. Both HJ and TC are lean coals, and the contributions of char-N for these two coals are greater than SM but less than JZ. It can be concluded that the contribution of char-N to NO emission is greater for higher rank coals. In addition to coal rank, temperature can have a profound effect on the contribution of char-N to NO emission. At low temperatures (900 °C or below), char-N is the main source of NO emission, except for the coal with very high volatile content (SM coal for instance). As temperature increases, volatile-N becomes more important. At high temperatures, volatile nitrogen conversion is generally greater than that of char nitrogen, which is in agreement with previous work. It has been reported that the NO emission from volatile can be as high as 60- 80% of the total fuel NO emission under the conditions typical for pulverized coal systems (2). Besides, mineral matters in coal can change the redistribution of fuel-N between char and volatile and catalyze the oxidation of char, which has been verified by our demineralized 4774 9 ENVIRONMENTAL SCIENCE & TECHNOLOGY / VOL. 42, NO. 13, 2008 FIGURE 7. Conversion of fuel-N to NO from the two types of experiments. FIGURE 8. Values of r at different temperatures. experiments. It is suggested that the increase of char-N contribution to NO emission at 1000 °C or above for HJ and TC coals should be caused by the minerals in the two samples. 3.2. NO Emission from the Combustion of Entrained Pulverized Coal. It is well-known that the oxidation of fuel-N to NO and the reduction of NO occur simultaneously during coal combustion. Consequently, the NO emission is determined by the competition of the two processes. NO emission increases if the formation rate of NO is greater than its reduction rate, and vice versa. The conversion of fuel-N to NO during the combustion of entrained pulverized coal, i.e., the second type of experiment, is shown in Figure 6. It can be seen that the fuel-NO emission does not increase with increased temperature monotonously. The conversion of fuel-N to NO reaches its maximum at 900 or 1000 °C, and decreases beyond that temperature, which is attributable to more NO reduction over 1000 °C (28). In this type of experiment, the volatile-char interaction affects the NO formation only through enhancing the gas-solid reaction on the surface of char. The experimental results show that the effects of volatile-char interaction on the NO reduction can be significantly elevated at 1000 °C, so that the reduction rate of NO increases more quickly than the oxidation rate of fuel-N to NO. The comparison between the conversion of fuel-N to NO from the combustion of entrained pulverized coal (expressed by X2) and that from the separate combustion of volatile and char (X1) is shown in Figure 7. It can be seen that X2 is less than X1 at 800 °C and greater than X1 at 900 °C or above. That is to say, more NO release from the combustion of entrained pulverized coal than from the separate combustion of volatile and char when the temperature is greater than 900 °C. The effects of temperature on X1 and X2 are different. X1 decreases with increased temperature below 1000 °C, and increases beyond 1000 °C for some coals. X2 increases with increased temperature below 1000 °C, and decreases beyond 1000 °C for all used coals. X1 may be equal to X2 between 800 and 900 °C. The effect of volatile-char interaction on the reduction of NO is least at 1000 °C and elevated at 1100 °C. The effect of volatile-char interaction on fuel-N redistribution to N2 during devolatilization increases with increased temperature when the temperature is lower than 1000 °C, but it might decrease beyond 1000 °C. 3.3. Effect of Volatile-Char Interaction. As mentioned above, x1 ) X0/X1 and x2 ) X0/X2. We define VOL. 42, NO. 13, 2008 / ENVIRONMENTAL SCIENCE & TECHNOLOGY 9 4775 r) x1 X 0 X 0 X 2 ) ⁄ ) x2 X1 X 2 X1 (5) r indicates the relative importance of the volatile-char interaction in the redistribution of fuel-N to N2 during devolatilization to the interaction in the reduction of NO to N2 during the combustion of volatile and char. The calculated results of r are shown in Figure 8. Obviously, coal rank has a profound effect on the NO formation. It seems that the volatile-char interaction during devolatilization is stronger as the coal rank increases between 900-1000 °C, but JZ coal is an exception. Beyond that temperature range, coal rank has a more complex effect on the value of r. It can be deduced that nitrogen content, nitrogen functionalities, mineral matters, etc., could have an effect on the interaction. More work is needed to clarify these effects. While r is greater than 1.0, the volatile-char interaction is more significant in the fuel-N redistribution to N2 during devolatilization than in the NO reduction through gas-solid reactions during combustion. A greater value of r means a more significant interaction during devolatilization as the first step of coal combustion. In fact, NO emission would decrease when combustion is conducted under conditions of departure from stoichiometry, for example in the case of bias combustion or staged combustion. Theoretically, while r is greater than 1.0, NO emission would be decreased to the greatest extent if the two steps of coal combustion can be distinctly separated and an adequate devolatilization process can be ensured. For example, NO emission can be decreased if coal is gasified first and the formed gas and residual char are sent to furnace at different points to complete combustion separately. If X2 is less than X1, i.e., r is less than 1.0, the volatile-char interaction is more significant in the reduction of NO during combustion than in the redistribution of fuel-N to N2 during devolatilization. So that, combustion was expected to be performed under stoichiometric conditions to decrease the conversion of fuel-N to NO when r is less than 1.0. In practice, stoichiometric excess and uniform air distribution are necessary to control NO emissions, and bias combustion or staged combustion are not recommended to decease NO emissions in this case. According to the above discussions and Figure 8, it can be concluded that 1000 °C is the most suitable temperature for controlling the NO emission from coal combustion under conditions of departure from stoichiometry (oxygen deficiency) for these four coals. For example, bias combustion or staged combustion technology can be applied over 900 °C. Stoichiometric excess and uniform air distribution are necessary to control NO emission below 850 °C because r is less than 1.0 for all coals. Acknowledgments The financial support from the Natural Science Fund of China (50676076, 50576071) is gratefully acknowledged. Literature Cited (1) Jones, J. M.; Patterson, P. M.; Pourkashanian, M.; Williams, A. Approaches to modeling heterogeneous char NO formation/ destruction during pulverized coal combustion. Carbon 1999, 37 (10), 1545–1552. (2) Pershing, D. W.; Wendt, J. O. L. Relative contributions of volatile nitrogen and char nitrogen to NO emissions from pulverized coal flames. Ind. Eng. Chem. Process Des. Dev. 1979, 18 (1), 60–67. (3) Wu, Z. H.; Sugimoto, Y.; Kawashima, H. Effects of demineralization and catalyst addition on N2 formation during coal pyrolysis and on char gasification. Fuel 2003, 82 (15-17), 2057–2064. (4) Zhao, Z. B.; Li, W.; Qiu, J. H.; Li, B. Q. Catalytic effect of Na-Fe on NO-char reaction and NO emission during coal char combustion. Fuel 2002, 81 (18), 2343–2348. 4776 9 ENVIRONMENTAL SCIENCE & TECHNOLOGY / VOL. 42, NO. 13, 2008 (5) Leppälahti, J. Formation of NH3 and HCN in slow-heating-rate inert pyrolysis of peat, coal and bark. Fuel 1995, 74 (9), 1363– 1368. (6) Leppälahti, J.; Koljonen, T. Nitrogen evolution from coal, peat and wood during gasification: Literature review. Fuel Process. Technol. 1995, 43 (1), 1–45. (7) Kidena, K.; Hirose, Y.; Aibara, T.; Murata, S.; Nomura, M. Analysis of nitrogen-containing species during pyrolysis of coal at two different heating rates. Energy Fuels 2000, 14 (1), 184–189. (8) KÖpsel, R. F. W.; Halang, S. Catalytic influence of ash elements on NOx formation in char combustion under fluidized bed conditions. Fuel 1997, 76 (4), 345–351. (9) Visona, S. P.; Stanmore, B. R. Modeling NOx release from a single coal particle I. Formation of NO from volatile nitrogen. Combust. Flame 1996, 105 (1-2), 92–103. (10) Muhr, H.; David, R.; Villermaux, J. Modeling NOx Release from a single coal particle II. Formation of NO from char-nitrogen. Combust. Flame 1996, 106 (3), 207–218. (11) Chaiklangmuang, S.; Jones, J. M.; Pourkashanian, M.; Williams, A. Conversion of volatile-nitrogen and char-nitrogen to NO during combustion. Fuel 2002, 81 (12), 2363–2369. (12) Tullin, C. L.; Sarofim, A. F.; Beer, J. M. Formation of NO and N2O coal combustion: the relative importance of volatile and char nitrogen. Proc. 12th Int. Conf. Fluidized Bed Combust., ASME 1993, 599–609. (13) Lachlan, J. M.; Tian, F. J.; Li, C. Z. Effects of volatile-char interaction on the formation of HCN and NH3 during the gasification of Victorian brown coal in O2 at 500°C. Fuel 2006, 85 (14-15), 2148–2154. (14) Li, C. Z. Some recent advances in the understanding of the pyrolysis and gasification behaviour of Victorian brown coal. Fuel 2007, 84 (12-13), 1664–1683. (15) Li, X. J.; Wu, H. W.; Hayashi, J.; Li, C. Z. Volatilisation and catalytic effects of alkali and alkaline earth metallic species during the pyrolysis and gasification of Victorian brown coal. Part VI. Further investigation into the effects of volatile-char interactions. Fuel 2004, 83 (10), 1273–1279. (16) Tan, L. L.; Li, C. Z. Formation of NOx and SOx precursors during the pyrolysis of coal and biomass. Part II. Effects of experimental conditions on the yields of NOx and SOx precursors from the pyrolysis of a Victorian brown coal. Fuel 2000, 79 (15), 1891–1897. (17) Hayhurst,A.N.;Lawrence,A.D.TheAmountsofNOx andN2Oformed in a fluidized bed combustor during the burning of coal volatiles and also of char. Combust. Flame 1996, 105 (3), 341–357. (18) Wu, Z. H.; Ohtsuka, Y. Key factors for formation of N2 from low-rank coals during fixed bed pyrolysis: pyrolysis conditions and inherent minerals. Energy Fuels 1997, 114, 902–908. (19) Tsubouchi, N.; Ohtsuka, Y. Nitrogen release during high temperature pyrolysis of coals and catalytic role of calcium in N2 formation. Fuel 2002, (18), 2335–2342. (20) Wu, Z. H.; Sugimoto, Y.; Kawashima, H. The Influence of mineral matter and catalyst on nitrogen release during slow pyrolysis of coal and related material: a comparative study. Energy Fuels 2002, 16, 451–456. (21) Wu, Z. H.; Sugimoto, Y.; Kawashima, H. Effect of demineralization and catalyst addition on N2 formation during coal pyrolysis and on char gasification. Fuel 2003, 82 (15-17), 2057– 2064. (22) Wang, W.; Brown, S. D.; Hindmarsh, C. J.; Thomas, K. M. NOx release and reactivity of chars from a wide range of coals during combustion. Fuel 1994, 73 (9), 1381–1388. (23) Harding, A. W.; Brown, S. D.; Thomas, K. M. Release of NO from the combustion of coal chars. Combust. Flame 1996, 107 (4), 336–350. (24) Tsubouchi, N.; Ohshima, Y.; Xu, C. B. Enhancement of N2 formation from the nitrogen in carbon and coal by calcium. Energy Fuels 2001, 15 (1), 158–162. (25) Liu, Y.; Che, D.; Xu, T. Effects of minerals on the release of nitrogen species from anthracite. Energy Sources, Part A 2007, 29 (3), 313–327. (26) Yan, X.; Che, D. F.; Xu, T. M. Effect of rank, temperatures and inherent minerals on nitrogen emissions during coal pyrolysis in a fixed bed reactor. Fuel Process. Technol. 2005, 86 (7), 739–756. (27) Yao, M. Y.; Che, D. F. Catalytic Effects of Minerals on NOx Emission from Coal Combustion. Energy Sources, Part A 2007, 29 (11), 1005–1016. (28) Rodriguez-Mirasol, J.; Ooms, A. C.; Pels, J. R. NO and N2O decomposition over coal char at fluidized-bed combustion conditions. Combust. Flame 1994, 99 (3-4), 499–507. ES071945K
© Copyright 2026 Paperzz