Paper # 070EN-0400 Topic: Environmental aspects of combustion 8th U. S. National Combustion Meeting Organized by the Western States Section of the Combustion Institute and hosted by the University of Utah May 19-22, 2013 Mercury Oxidation by Halogens under Air-Fired and Oxygen-Fired Conditions Ignacio Preciado, Tessora Young, and Geoffrey Silcox Department of Chemical Engineering, University of Utah Salt Lake City, Utah 84112, USA Gas-phase mercury oxidation by halogens under air-fired and oxygen-fired (27% O2 in CO2) conditions was studied in a bench-scale, laminar, methane-fired, 300 W, quartz-lined reactor. The experiments provided data on the extents of elemental mercury oxidation in the presence of various flue gas components including chlorine, bromine, SO2, and NO. A wet conditioning system and a Tekran 2537A mercury analyzer were used to determine mercury speciation and concentrations. Under the same experimental conditions and for both halogens, oxy-firing produced modest increases in mercury oxidation. Extents of oxidation at chlorine concentrations of 100 to 500 ppmv (as HCl) ranged from 6 to 21% for oxyfiring and from 4 to 15% for air-firing. Oxidation by bromine at concentrations of 10 to 50 ppmv (as HBr) ranged from 43 to 69% for oxygen-firing and from 15 to 46% for air-firing. Under both firing conditions, the addition of NO (below 250 ppmv) had little or no effect on mercury oxidation by chlorine or bromine; and the addition of SO2 (below 400 ppmv) had no impact on oxidation by chlorine. 1. Introduction Oxy-fuel combustion is being considered as a promising path to CO2 capture and sequestration, especially for coal-fired power plants since its cost can potentially be less than or comparable to that of conventional air-fired combustion with amine-based CO2 capture (Okawa et al., 1997; Nsakala et al., 2001). The fate and analysis of mercury in oxy-fired systems have not been fully investigated. The fate of mercury under oxycombustion conditions is important, not only because of emissions, but also because of downstream corrosion. Trace amounts of mercury may lead to embrittlement and cracking of aluminum heat exchangers that are used in the cryogenic separation and compression of CO2 (Santos, 2009; Santos, 2010). Limited and to some extent uncertain data on mercury speciation in oxycombustion systems have been published. Some experimental data have indicated that elevated CO2 concentrations potentially enhance mercury retention on fly ash, while high O2 concentrations may promote mercury vaporization and emission (Qiu et al., 2007). Additional mercury oxidation has been observed in oxycombustion as a result of mercury chlorination (Ueno et al., 2008). Suriyawong et al., (2006) evaluated pulverized subbituminous coal under oxygen-carbon dioxide mixtures (20% O2/80% CO2 and 25% O2/75% CO2) to estimate the effects of O2 - CO2 coal combustion on submicron particle formation and mercury speciation. It was found that 10 to 20 % of the mercury in the coal was oxidized and the extent of mercury oxidation was unaffected by changing from air- to oxy-firing. Zhuang et al., (2011) have evaluated different Hg measurement techniques under oxy-combustion conditions. They found that for flue gas with high CO2 concentration, modifications to continuous mercury monitors (CMM) may be needed to eliminate biases caused my mass flow controllers or impinger solutions in the flue gas conditioning system. Varied impinger chemistry under oxycombustion conditions suggests Hg sampling using wet-chemistry methods, such as Ontario Hydro, may bias measured gas-phase Hg concentrations due to the high concentrations of CO2. The homogeneous oxidation of mercury has been extensively studied at the University of Utah under air and oxy-firing conditions (Senior et al., 2009; Silcox et al., 2010, Van Otten at al., 2011). Experiments were performed in a bench-scale, methane-fired, quartz-lined reactor, in which quench rate and flue gas compositions (which included halogens such as chlorine and bromine) were varied. Mercury measurements were performed using a Tekran 2537A analyzer coupled with a wetchemical speciating and conditioning system. In the absence of SO2, preliminary results with oxy-firing conditions (air was replaced with a mixture of 27 % oxygen, balance carbon dioxide) showed a dramatic effect in oxidation of mercury by chlorine. At 400 ppm chlorine (as HCl equivalent), oxidation levels were around 80 % vs. 5 % oxidation obtained under air-firing tests for the same chlorine concentration. Oxidation levels with bromine at 25 and 50 ppm (as HBr equivalent) ranged from 80 to 95 % and were about the same for oxy- and air-firing conditions. Subsequent work has not reproduced the dramatic effects seen with chlorine. When SO2 at 500 ppm was included in the oxy-fuel tests, the ability of chlorine and bromine to oxidize mercury dropped dramatically. Mercury oxidation on the order of 40 -50 % were obtained with bromine at 25 and 50 ppm (as HBr equivalent) and between 10 - 20% for chlorine at 400 ppm (as HCl equivalent). This work will study the fate of mercury oxidation by halogens in the gas phase under oxy-fuel and air firing conditions with an optimized mercury sampling system in order to ensure unbiased measurement of mercury speciation in oxy-combustion flue gas. 2. Methods The reactor design used in this study is described in detail in Fry et al., (2007) and was developed to study the effects of halogens such as chlorine and bromine, and species such as NO and SO2 on homogeneous gas-phase mercury oxidation. The reaction chamber is a quartz cylinder, having a 47mm inner diameter and 135-cm length. The first 54 cm of the cylinder are enclosed by a Thermcraft high-temperature heater and the remaining section of the quartz tube was heated with four, individually controlled heating tapes. The later permitted the quench rate to be adjusted in order to produce time-temperature profiles representative of industrial boilers. A 300 W quartz burner was used to feed methane and oxidant into the reactor. All species were introduced through the flame to create radical species representative of those seen in combustion systems. The stoichiometric ratio and the total gas flow rate (gases were fed at 6 SLPM into the burner) were the same for both, air and oxy fuel conditions. A mixture of 27% O2 and 73% CO2was used in the oxy-firing combustion tests. The percentage of oxygen after combustion was monitored with an oxygen analyzer and maintained at 2.0 - 2.2 % for all experiments. 2 Mercury is fed to the system using a mercury vapor permeation tube that is heated in an oil bath and uses air as the carrier gas. The carrier gas is then diluted with the residual air or oxygen-carbon dioxide mixture and sent to the burner. For oxy-fired experiments, carbon dioxide and oxygen were regulated using mass flow controllers and blended before diluting the mercury stream. Calibration gases in air were used as sources of chlorine and SO2 (6000 ppm Cl2 and 6000 ppm SO2) and calibration gases in nitrogen were used as sources of bromine and NO (500 ppm Br2 and 6000 ppm NO). NO and SO2 were fed to the burner in select experiments involving chlorine or bromine. The concentration of NO was measured at the reactor exit by a NOx analyzer, and the flow rate through the burner was adjusted to give the desired concentration. At the exit of the reactor, the flue gases (gas temperature around 350C) were split and sent to a wet conditioning system. . One stream was fed to an acidic solution containing 4 wt% SnCl2 to reduce all oxidized mercury to its elemental form. This gas stream represented the total amount of mercury fed to the reactor. The other gas stream was fed to a solution containing 10 wt% KCl and 1 wt% Na2S2O3 to capture oxidized mercury. This stream indicated the elemental mercury concentration present in the system. Both sides then bubbled through 5% NaOH solutions to remove any acidic species, with the exception of CO2. Flow designs ensured all solutions were being continually refreshed within the quartz impingers. A Tekran mercury analyzer was used to measure the concentration of elemental mercury. A four port sampler controlled which stream the Tekran sampled. The difference between the total and elemental gas streams was the concentration of mercury oxidized in the reaction chamber. A schematic of the experimental system is presented in Figure 1. Figure 1. Experimental system for measuring elemental mercury. 3. Results and Discussion Chlorine (as Cl2), bromine (as Br2), NO and SO2 were added through the burner. Before these were added, the baseline mercury concentration was verified by a material balance. The mercury balance 3 considered total and elemental mercury, measured using the continuous emission monitor (CEM) and sample conditioning system, at the beginning and end of each experiment. Figure 2 shows a typical set of continuous measurements of mercury species as a function of time with chlorine addition (ppm as HCl). The concentrations of total (HgT) and elemental (Hg0) mercury are indicated; the mercury oxidation is evaluated for each condition and obtained by difference of the total (HgT) and elemental (Hg0) mercury concentrations. Effect of halogens on mercury oxidation Figures 3 and 4 show the mean percentage of mercury oxidation for chlorine and bromine injection under air- and oxy-firing conditions. Experiments were repeated to determine the range in the levels of oxidation, and these are shown as error bars in the figures. Figures 3 and 4 show an increase in mercury oxidation with increasing halogen concentration. Neither NO nor SO2 were added in these experiments. When comparing average values, Hg oxidation by chlorine was 50% higher for oxyfiring compared to air-firing. Oxidation by bromine was 2 to 4 times higher for oxy-firing. Sliger, Kramlich, and Marinov (2000) suggested that homogeneous Hg oxidation by halogens could be explained by this simplified mechanism Hg + X + M = HgX + M (1) HgX + X2 = HgX2 + X (2) where X = halogen and M = third body. The formation of HgX is the rate controlling step. A possible explanation for higher oxidation under oxy-firing conditions is that the CO2 molecule is more effective third body than N2. Carbon dioxide is more effective than N2 at removing energy from the HgX transition state complex, facilitating the formation of oxidized Hg species. As shown by Figures 3 and 4, bromine is a more powerful oxidant for mercury than chlorine, on an equivalent molar basis. Similar findings have been reported in full-scale power-plant tests (Benson et al., 2007 and Richardson et al., 2006). Bromine radical chemistry is very different from that of chlorine. HCl is the dominant chlorine species for temperatures between 200 and 1000 C. With bromine, HBr, Br2, and Br are all significant (Niksa et al., 2010). This drastically different halogen chemistry could account for the increased homogeneous oxidation seen with bromine. 4 Hg fed in the system = 25 g/m3 Mercury Oxidation. Air-firing, chlorine 35 30 Mercury concentration (g/m3 ) Hg baseline Hg baseline 25 20 HgT 100 ppm as HCl 200 ppm as HCl 500 ppm as HCl Hg0 15 10 Hg2+ = HgTotal - Hg0 5 0 10:48:00 12:00:00 13:12:00 14:24:00 15:36:00 16:48:00 18:00:00 Time Figure 2. Measured concentrations of total and elemental mercury for different chlorine concentrations under air firing conditions % Hg oxidation for air and oxy-firing tests 30 % Hg oxidation 25 20 15 10 5 0 0 100 200 300 400 500 600 Chlorine as HCl (ppm) Air-firing Oxy-firing Figure 3. Mercury oxidation for different chlorine concentrations under air and oxy-firing conditions 5 % Hg oxidation for air and oxy-firing tests 80 Hg = 25 g/m 3 % Hg oxidation 70 2.0 % O2 (dry) in flue gas 60 50 40 30 20 10 0 0 10 20 30 40 50 60 Bromine as HBr (ppm) Air-firing Oxy-firing (27% O2 - 73% CO2) Figure 4. Mercury oxidation for different bromine concentrations under air and oxy-firing conditions Effect of NO and SO2 on mercury oxidation Table 1 summarizes the results for mercury oxidation by chlorine and bromine when NO and SO2 were injected in the reactor. It can be observed that the addition of NO did not affect the Hg oxidation by chlorine or bromine under both firing conditions. On the other hand, Hg oxidation by chlorine remained basically unchanged when SO2 was injected under both, air and oxy firing conditions. Results regarding the effects of SO2 on gas-phase mercury oxidation by bromine are not reported due to inconsistent data. The inconsistencies are due to the aqueous-phase complexing of mercuric ion by the bromide ion to form the stable species HgBr4-2. The complex resists reduction by stannous chloride (Babi, Schaedlich and Schneeberger, 2002) and as a result no elemental mercury is produced for analysis by the atomic fluorescent analyzer used in this study. Figure 5 is a plot of the chlorine-SO2 data presented in Table 1 for the oxy-fuel tests. The red dotted lines correspond to the range of Hg oxidation when feeding 200 ppm of chlorine without SO2 in the system. Increasing the SO2 concentration from 0 to 400 ppmv had little or no effect on mercury oxidation by chlorine, within experimental error. 6 Table 1. Range of mercury oxidation when adding SO2 and NO under air and oxy firing tests Chlorine as HCl at 200 ppm Species Air firing Oxy firing ppm % Hg oxidation % Hg oxidation (range) (range) SO2 - 0 4-8 6 - 11.5 SO2 - 100 5-9 6 - 10 SO2 - 200 4-8 5.5 - 9.5 SO2 - 400 4-8 5-9 NO - 0 NO - 25 SO2 - 50 SO2 - 100 SO2 - 250 4-8 4-8 4-8 3-7 3-6 Bromine as HBr at 30 ppm Species Air firing ppm % Hg oxidation (range) NO - 0 30 - 39 NO - 50 29 - 38 NO - 100 30 - 40 NO - 250 31 - 43 - % Hg oxidation for oxy-firing tests 20 % Hg oxidation Hg = 25 g/m 3 2.0 % O2 (dry) in flue gas 15 10 Range of % Hg oxidation f or 200 ppm as HCl, without SO2 5 0 0 100 200 300 400 500 SO2 (ppm) Figure 5. Mercury oxidation by chlorine with the addition of SO2 under oxy-firing conditions 4. Conclusions Homogeneous mercury oxidation by halogens under oxy-firing conditions has been shown to be more effective than under air-firing conditions. 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