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H2S-modified Fe-Ti spinel: A recyclable magnetic sorbent for recovering gaseous elemental mercury from the flue gas as a co-benefit of the wet electrostatic precipitators Sijie Zou, Yong Liao, Shangchao Xiong, Nan Huang, Yang Geng, and Shijian Yang Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.6b05765 • Publication Date (Web): 22 Feb 2017 Downloaded from http://pubs.acs.org on February 24, 2017
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H2S-modified Fe-Ti spinel: A recyclable magnetic sorbent for
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recovering gaseous elemental mercury from the flue gas as a
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co-benefit of the wet electrostatic precipitators
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Sijie Zou, Yong Liao, Shangchao Xiong, Nan Huang, Yang Geng, Shijian Yang *
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Jiangsu Key Laboratory of Chemical Pollution Control and Resources Reuse, School of
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Environmental and Biological Engineering, Nanjing University of Science and Technology,
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Nanjing, 210094, P. R. China
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Abstract:
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The non-recyclability of the sorbents used to capture Hg0 from the flue gas causes a high
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operation cost and the potential risk of exposure to Hg. The installment of wet electrostatic
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precipitators (WESPs) in coal-fired plants makes the recovery of spent sorbents for recycling and
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the centralized control of Hg pollution possible. In this work, H2S-modified Fe-Ti spinel was
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developed as a recyclable magnetic sorbent to recover Hg0 from the flue gas as a co-benefit of the
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WESP. Although Fe-Ti spinel exhibited poor Hg0 capture activity in the temperature range of the
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flue gas downstream of the flue gas desulfurization (FGD), H2S-modified Fe-Ti spinel exhibited
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excellent Hg0 capture performance with an average adsorption rate of 1.92 µg g-1 min-1 at 60 oC
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and the capacity of 0.69 mg g-1 (5% of the breakthrough threshold) due to the presence of S22- on
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its surface. The five cycles of Hg0 capture, Hg0 recovery, and sorbent regeneration demonstrated
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that the ability of modified Fe-Ti spinel to capture Hg0 did not degrade remarkably. Meanwhile,
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the ultra-low concentration of Hg0 in the flue gas was concentrated to a high concentration of Hg0,
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which facilitated the centralized control of Hg pollution.
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Table of Contents
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1. Introduction
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As mercury emission from coal combustion is one of the most important sources of
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anthropogenic mercury emission,1-3 nations at the Minamata Convention agreed to control
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mercury emission from coal-fired plants.4 Hg species in the flue gas of coal-fired plants mainly
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present as particulate-bound mercury (Hgp), oxidized mercury (Hg2+) and elemental mercury
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(Hg0).5 Though Hg2+ and Hgp can be effectively removed by the flue gas desulfurization (FGD)
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and the electrostatic precipitator (ESP), the control devices in coal-fired plants cannot remove Hg0
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from the flue gas.6 Therefore, gaseous Hg0 is the main Hg species emitted by coal-fired plants to
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the atmosphere.7
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The strategy to control Hg0 emission from coal-fired plants now falls into the conversion of
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gaseous Hg0 to Hg2+ or Hgp.8, 9 The oxidation of Hg0 to Hg2+ can be achieved as a co-benefit of the
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selective catalytic reduction (SCR) catalyst,10, 11 which is installed to reduce NOx. Currently, the
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oxidation of Hg0 by the SCR catalyst is restricted for at least four reasons, including the lack of
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HCl in the flue gas, the interference of NH3 with Hg0 oxidation, Hg0 re-release in the FGD unit
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and the potential risk of exposure due to Hg2+ in the desulfurization gypsum.5, 8, 12, 13 The injection
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of sorbents upstream of the ESP for the conversion of gaseous Hg0 to Hgp is a potential
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commercial technology to control Hg0 emission from the flue gas.9, 14 As the ESP removes spent
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sorbents from the flue gas with a huge amount of fly ash particles, it is impossible to recover spent
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sorbents from the mixture collected by the ESP.15 Therefore, the injection of sorbents to control
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Hg0 emission from the flue gas is limited for at least three reasons, including the high operation
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cost because of the non-recyclability of the sorbent, the negative effect on the marketability of fly
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ash and the potential secondary emission of Hg during the utilization of the fly ash.16-19
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To recover spent sorbents for recycling and to achieve the centralized control of Hg pollution,
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the installation of a fabric filter (FF) downstream of the ESP was once suggested and in this setup,
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the sorbents would be injected between the ESP and the FF.15 As more than 99% of the fly ash
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particulates were collected by the ESP, the mixture collected by the FF consisted mainly of a
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small amount of ultrafine particulates and the sorbents which contained Hg. If the sorbents were
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magnetized, it was possible to recover spent sorbents for recycling and to achieve the centralized 4
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control of Hg pollution.17 Therefore, a large number of magnetic sorbents, including MagZ-Ag0,17,
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20
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and Co-MF 27 were developed to capture gaseous Hg0 in the flue gas. However, the installation of
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an FF merely to recover spent sorbents is particularly uneconomical.
MnOx/γ-Fe2O3,21 Fe-Ti-Mn spinel,15, 22 Mn-Fe spinel,16, 23, 24 Fe-Ti-V spinel,
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Fe-Ti spinel
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In China, wet electrostatic precipitators (WESPs) have been gradually installed downstream of
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the FGD to meet the stricter emission standards of coal-fired plants for ultrafine particulates.
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Magnetic sorbents can be injected downstream of the FGD for gaseous Hg0 capture. Then, the
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recovery of spent magnetic sorbents is a practical co-benefit of the WESP (the procedure is
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illustrated in Figure S1 in the Supporting Information).18 However, the temperature window of
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most reported magnetic sorbents (especially metal oxides) for gaseous Hg0 capture (100-200 oC)
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do not match the temperature range of the flue gas downstream of the FGD (40-100 oC).16, 22, 23, 26
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In our previous work, magnetic pyrrhotite (Fe1-xS) was developed as a recyclable sorbent for the
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recovery of gaseous Hg0 in the flue gas as a co-benefit of the WESP.
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showed excellent gaseous Hg0 capture performance at low temperatures, it was almost a
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permanent magnet, with a permanent magnetization of 3.7 emu g-1 (its saturation magnetization
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was only 7.0 emu g-1). This characteristic affected the re-dispersion of recovered pyrrhotite for the
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future recycling.
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18
Although pyrrhotite
In our previous work, super-paramagnetized Fe-Ti spinel with a saturation magnetization value
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higher than 30 emu g-1 was developed to capture gaseous Hg0 in the flue gas at 200-300 oC.
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However, this material showed a poor activity for gaseous Hg0 capture at low temperatures. To
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improve the performance of Fe-Ti spinel for Hg0 capture at low temperatures, it was modified by
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pretreatment with H2S. Modified Fe-Ti spinel showed an excellent performance for gaseous Hg0
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recovery and could be recycled; therefore, Hg0 recovery using the modified Fe-Ti spinel as a
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co-benefit of the WESP may be a promising and cost-effective technology for achieving the
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centralized control of Hg emission from the flue gas.
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2. Experimental Section
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2.1 Sample preparation
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Fe-Ti spinel (Fe/Ti=2) was prepared by co-precipitation followed by calcination at 400 oC for 3
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h.26, 28, 29 Then, Fe-Ti spinel was modified through treatment with 600 ppm of H2S/N2 at 300 oC
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for 1 h, with a gas hourly space velocity (GHSV) of 1.2×105 cm3 g-1 h-1.
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2.2 Characterization
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The BET surface area, magnetization, X-ray diffraction pattern (XRD) and X-ray photoelectron
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spectra (XPS) were determined using a nitrogen adsorption apparatus (Quantachrome,
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Autosorb-1), a vibrating sample magnetometer (VSM, LakeShore 735), an X-ray diffractometer
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(Bruker-AXS D8 Advance) and an X-ray photoelectron spectroscopy (Thermo, ESCALAB 250),
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respectively.
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2.3 Elemental mercury recovery
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Hg0 capture was conducted on a fixed-bed quartz tube microreactor at 40-100 oC. The GHSV
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used was generally 1.5×106 cm3 g-1 h-1 (i.e., approximately 1.5×106 h-1), 20 mg of the sorbent was
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used, and the gas flow was 500 mL min-1. The simulated flue gas contained approximately 110 µg
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m-3 of gaseous Hg0, 5% O2 (when used), 8% H2O (when used), 80 ppm of SO2 (when used) and a
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balanced amount of N2. The gaseous Hg0 concentration was determined online using a cold vapor
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atomic absorption spectrophotometer (CVAAS, Lumex R-915+). Meanwhile, the formation of
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SO2 due to the oxidation of modified Fe-Ti spinel during Hg0 capture was determined online using
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a Fourier transform infrared spectrometer (FTIR, Thermo SCIENTIFIC, ANTARIS, IGS
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Analyzer). The temperature programmed desorption of Hg adsorbed on modified Fe-Ti spinel
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(Hg-TPD) under N2 and air atmospheres were both performed on the microreactor at a heating rate
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of 10 oC min-1 and a gas flow of 700 mL min-1. The leachability of Hg species from modified
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Fe-Ti spinel after Hg0 capture was determined using the toxicity characteristic leaching procedure
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(USA EPA) with 5.7 mL L-1 of glacial acetic acid (pH=2.88) as the extraction fluid.30
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The cycle of Hg0 capture, Hg0 recovery and sorbent regeneration was also performed on the
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fixed-bed microreactor. After the capture of Hg0 at 60 oC for 3 h with the GHSV of 3.0×105 cm3
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g-1 h-1 (i.e., 100 mg of modified Fe-Ti spinel and 500 mL min-1 of the gas flow), the Hg adsorbed
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on modified Fe-Ti spinel was recovered through thermal treatment at 300 oC for 40 min with a N2
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gas flow of 100 mL min-1. Next, the N2 gas flow was shifted to 600 ppm of H2S/N2 for 1 h to 6
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regenerate the spent modified Fe-Ti spinel. At last, the modified Fe-Ti spinel after the
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regeneration was recycled.
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3. Results and Discussion
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3.1 Characterization
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3.1.1
XRD and BET surface area
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The XRD pattern of Fe-Ti spinel corresponded notably well to the standard curve of cubic
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maghemite (γ-Fe2O3, JCPDS 39-1346), and the characteristic peaks corresponding to other iron
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oxides and TiO2 could not be observed (Figure 1a). This result suggests that Ti was incorporated
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into the spinel structure.26 After pretreatment with H2S, the slight peaks corresponding to cubic
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pyrite (FeS2, JCPDS 42-1340) were observed in Fe-Ti spinel, suggesting that the transformation of
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Fe-Ti spinel to iron sulfide occurred during the H2S pretreatment.31 The lattice parameter of
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modified Fe-Ti spinel (0.8388 nm) was much higher than that of Fe-Ti spinel (0.8335 nm),
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suggesting that some Fe3+ cations in Fe-Ti spinel were reduced to Fe2+ cations due to the H2S
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pretreatment. 32
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The BET surface areas of Fe-Ti spinel and modified Fe-Ti spinel were 87.5 and 32.7 m2 g-1,
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respectively.
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3.1.2
Magnetization
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Fe-Ti spinel exhibited super-paramagnetism with a minimized coercivity and a negligible
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magnetization hysteresis (Figure 1b). Meanwhile, Fe-Ti spinel showed an excellent magnetization
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with a saturation magnetization of 31.0 emu g-1. After pretreatment with H2S, the
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super-paramagnetism of Fe-Ti spinel was retained. However, the saturation magnetization of
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Fe-Ti spinel decreased to 24.6 emu g-1 due to the partial transformation of Fe-Ti spinel to
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non-magnetic pyrite. Due to the super-paramagnetism, the magnetization of modified Fe-Ti spinel
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simultaneously disappeared as the external magnetic field was removed. Therefore, spent
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modified Fe-Ti spinel, which was recovered by the magnetic separation, could be well
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re-dispersed without aggregation for recycling.
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3.1.3
XPS analysis
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The XPS spectra of Fe-Ti spinel, modified Fe-Ti spinel and denuded modified Fe-Ti spinel in
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the spectral regions of Fe 2p, Ti 2p, O 1s and S 2p are shown in Figure 2. The Fe 2p 3/2 binding
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energies on Fe-Ti spinel mainly appeared at 711.2 and 712.4 eV (Figure 2a), which were assigned
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to Fe3+ in the spinel structure and Fe3+ bonded with -OH, respectively.
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energies on Fe-Ti spinel mainly appeared at 458.7 and 464.4 eV (Figure 2b), which were
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attributed to Ti4+.
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531.7 eV (Figure 2c), which were assigned to O2- in transition metal oxides and O2- in -OH,
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respectively.29
28
26
The Ti 2p binding
The O 1s binding energies on Fe-Ti spinel mainly appeared at 530.2 and
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Two new binding energies appeared at 707.6 and 713.3 eV on modified Fe-Ti spinel in the
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spectral region of Fe 2p 3/2 (Figure 2d), which were attributed to Fe2+ bonded with S22- and Fe2+
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bonded with SO42-, respectively.26, 33, 34 The Ti 2p binding energies on modified Fe-Ti spinel still
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appeared at 464.6 and 458.9 eV (Figure 2e), which were consistent with those on Fe-Ti spinel
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(Figure 2b). A new binding energy at 532.2 eV appeared on modified Fe-Ti spinel in the O 1s
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spectral region (Figure 2f), which was assigned to SO42-.26 The S 2p binding energies on modified
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Fe-Ti spinel mainly appeared at 170.1, 168.9, 164.2 and 162.9 eV (Figure 2g), which were
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assigned to HSO4- , SO42-, polysulfur and S22-, respectively. 18, 26, 33, 35, 36
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Iron sulfide is easily oxidized after exposure to air. To exclude the effect of iron sulfide
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oxidation, modified Fe-Ti spinel was bombarded with Ar+ ions. The Fe 2p 3/2 binding energies on
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denuded modified Fe-Ti spinel mainly appeared at 707.2, 709.1, 711.1 and 712.4 eV (Figure 2h),
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which were assigned to Fe2+ bonded with S2- or S22-, Fe2+ and Fe3+ in the spinel structure and Fe3+
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bonded with -OH, respectively.18 The presence of Fe2+ in modified Fe-Ti spinel was also
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supported by the XRD analysis. The binding energies of S 2p on denuded modified Fe-Ti spinel
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mainly appeared at 161.7, 162.7 and 163.9 eV (Figure 2k), which were assigned to S2-, S22- and
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polysulfur, respectively.33, 34 However, the binding energy at 713.3 eV in the spectral region of Fe
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2p 3/2 corresponding to Fe2+ bonded with SO42-, the binding energy at 532.2 eV in the spectral
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region of O 1s corresponding to SO42-, and the binding energies at 168.9 and 170.1 eV in the
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spectral region of S 2p corresponding to SO42- and HSO4- could not be observed on denuded
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modified Fe-Ti spinel (Figure 2h, 2j and 2k). These results suggest that S2-, S22- and polysulfur 8
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directly resulted from the reaction between gaseous H2S and Fe-Ti spinel,31, 37-39 while SO42-
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indirectly resulted from the oxidation of S2- and S22- on the surface due to the exposure of
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modified Fe-Ti spinel to air. Therefore, the reaction between Fe-Ti spinel and H2S can be
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approximately described as: 37-39
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2H 2 S+2Fe 3+ =O → FeS 2 +Fe 2+ -O+H 2 O
(1)
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H 2 S+Fe 2+ =O → FeS+H 2 O
(2)
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FeS 2 → FeS+S 0
(3)
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The percentages of S species on modified Fe-Ti spinel and denuded modified Fe-Ti spinel,
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which were determined from the XPS analysis, are shown in Table 1. Table 1 shows that the
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percentages of S2- and S22- on modified Fe-Ti spinel were much lower than those on denuded
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modified Fe-Ti spinel, suggesting that most S2- and S22- on modified Fe-Ti spinel were oxidized to
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SO42- due to the exposure to air.40 However, the percentage of polysulfur on modified Fe-Ti spinel
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was only slightly less than that on denuded modified Fe-Ti spinel, suggesting that polysulfur was
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relatively stable on modified Fe-Ti spinel during exposure to air. This result was probably due to
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the strong binding energy of S-S.
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3.2 Elemental mercury capture
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The average rates of Hg0 capture by Fe-Ti spinel and modified Fe-Ti spinel at 40-100 oC were
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determined from the breakthrough curves (Figure 3) and are listed in Table 2. The average rates of
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Hg0 capture by Fe-Ti spinel were all less than 0.1 µg g-1 min-1 at 40-100 oC. However, the average
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rates of Hg0 capture by modified Fe-Ti spinel were in the range of 1.09-1.88 µg g-1 min-1, which
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were 12-169 times those of Fe-Ti spinel. This result suggests that the Hg0 capture performance of
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Fe-Ti spinel at low temperatures obviously improved after pretreatment with H2S.
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There is generally a low concentration of SO2 and a high concentration of water vapor in the
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flue gas downstream of the FGD, which often inhibit Hg0 capture by sorbents.16, 41 Therefore, the
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effect of SO2 and H2O on Hg0 capture by modified Fe-Ti spinel was investigated (Figure 3c). The
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average rates of Hg0 capture by modified Fe-Ti spinel in the presence of 8% H2O and 80 ppm of
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SO2 were generally close to those in the absence of H2O and SO2 (Table 2). This result suggests 9
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that the presence of H2O and SO2 did not show a remarkable inhibition on Hg0 capture by
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modified Fe-Ti spinel.
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As Hg0 capture is placed downstream of the FGD, the emission of SO2 due to the oxidation of
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modified Fe-Ti spinel is a serious concern. Figure S2 in the Supporting Information shows that the
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concentrations of gaseous SO2 formed during Hg0 capture by modified Fe-Ti spinel were
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generally less than 3 ppm at temperatures below 80 oC. This result suggests that the oxidation of
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modified Fe-Ti spinel to gaseous SO2 during Hg0 capture was negligible below 80 oC.
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As modified Fe-Ti spinel after Hg0 capture was collected with the fly ash from the WESP by
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water washing, the leachability of Hg species from modified Fe-Ti spinel was investigated.
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Although the initial amount of mercury adsorbed onto modified Fe-Ti spinel was approximately
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32.1 µg (100 mg of modified Fe-Ti spinel), neither Hg0 nor Hg2+ were observed in the extraction
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fluid of the glacial acetic acid solution. This result suggests that the leaching of Hg species from
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modified Fe-Ti spinel was negligible.
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3.3 Mechanism for elemental mercury capture
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Figure 4 shows the XPS spectra of modified Fe-Ti spinel after Hg0 capture in the spectral regions
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of Fe 2p, Ti 2p, O 1s, S 2p and Hg 4f. After the adsorption of Hg0 onto modified Fe-Ti spinel,
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there were no obvious changes in the spectral regions of Fe 2p, Ti 2p and O 1s (Figures 4a, 4b and
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4c). However, a new, slight peak at 161.8 eV appeared in the spectral region of S 2p (Figure 4d),
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which was attributed to S2-.18 The binding energies of Hg 4f mainly appeared at 101.0 and 105.1
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eV (Figure 4e), which were assigned to HgO or HgS.22, 25, 33, 34
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The chemical adsorption of Hg0 onto Fe-Ti spinel was often attributed to the Mars-Maessen
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mechanism, which can be approximately described as follows: 14, 26
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Hg 0 (g) → Hg 0 ( ad )
(4)
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Hg 0 (ad) +2Fe 3+ +O 2- → HgO+2Fe 2+
(5)
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4Fe 2+ +O 2 → 4Fe 3+ +2O 2-
(6 )
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Reaction 4 shows the physical adsorption of gaseous Hg0 on the surface. Then, physically
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adsorbed Hg0 is oxidized by Fe3+ on the surface to HgO (i.e., Reaction 5). Reaction 6 shows the 10
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regeneration of Fe3+ on the surface through oxidation by gaseous O2. As the oxidation ability of
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Fe3+ on Fe-Ti spinel was very poor at low temperatures, Fe-Ti spinel showed a poor performance
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for the chemical adsorption of Hg0 (Figure 3a). As the oxidation ability of Fe3+ on Fe-Ti spinel
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obviously increased at increasing reaction temperatures, Fe-Ti spinel showed a moderate activity
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for Hg0 adsorption at 200-350 oC (Figure S3).26
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The chemical adsorption of Hg0 onto modified Fe-Ti spinel can also be attributed to the
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Mars-Maessen mechanism, and the potential oxidants for the oxidation of physically adsorbed Hg0
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were Fe3+, polysulfur, S22- and gaseous O2. As Fe-Ti spinel showed a poor performance for Hg0
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capture at low temperatures, Fe3+ on modified Fe-Ti spinel was ruled out. Table 2 shows that the
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average rates of modified Fe-Ti spinel for Hg0 capture at 40-100 oC under N2 atmosphere were all
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close to those in the presence of O2. Thus, gaseous O2 was ruled out. Elemental sulfur (i.e.,
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polysulfur) showed a poor performance for Hg0 capture at low temperatures due to the strong
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binding energy of S-S (Figure S4).18, 42 Thus, polysulfur was ruled out. Therefore, the oxidant on
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modified Fe-Ti spinel for the oxidation of physically adsorbed Hg0 could only be S22-, and the
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formed Hg species was HgS. Then, the chemical adsorption of Hg0 onto modified Fe-Ti spinel can
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be approximately described as follows:
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Hg 0 (g) → Hg 0 ( ad )
(4)
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2Hg 0 (ad) +S 22 → HgS+S
(7)
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Table 1 demonstrates that the percentage of S22- on modified Fe-Ti spinel slightly decreased
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after the chemical adsorption of Hg0 and that a small amount of S2- appeared. As the performance
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of modified Fe-Ti spinel for the chemical adsorption of gaseous Hg0 was much better than that of
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Fe-Ti spinel, the ability of S22- on the surface to oxidize the physically adsorbed Hg0 was much
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better than that of Fe3+ on the surface.
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3.4 Comparison of modified Fe-Ti spinel with other magnetic sorbents
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Table 3 compares the Hg0 capture performance of modified Fe-Ti spinel with those of other
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reported magnetic sorbents. The capacity of modified Fe-Ti spinel for Hg0 capture was
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approximately 0.69 mg g-1 at 60 oC with the breakthrough threshold of 5% (Figure S5 in the 11
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Supporting Information), and the average rate of Hg0 capture by modified Fe-Ti spinel was 1.92
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µg g-1 min-1 at 60 oC. This performance was much better compared to MagZ-Ag0,17, 20 Mn-Fe
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spinel,16, 23 Fe-Ti-Mn spinel,15 Co-MF
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from modified Fe-Ti spinel was negligible because the formed Hg species was HgS, which was
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much better than Mn-Fe spinel, 16 Fe-Ti-Mn spinel 15 and Co-MF
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water soluble HgSO4 or HgCl2). Moreover, the magnetization of modified Fe-Ti spinel was much
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higher than that of pyrrhotite,18 so the separation of modified Fe-Ti spinel from the mixture
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collected by the WESP was much easier than when pyrrhotite was used. In summary, modified
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Fe-Ti spinel showed the best performance for capturing Hg0 from the flue gas (Table 3).
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3.5 Elemental mercury recovery and the recycle of sorbent
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and pyrrhotite.18 Meanwhile, the leaching of Hg species
27
(the formed Hg species were
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The simplest method to recover Hg from modified Fe-Ti spinel was thermal treatment. Figure 5
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shows the Hg-TPD profiles of modified Fe-Ti spinel after Hg0 capture. The amount of Hg0
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desorbed, which was determined from the integration of the Hg-TPD profile, was approximately
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equal to the amount of Hg0 adsorbed, which was determined from the integration of the
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breakthrough curve. These findings suggest that most of the Hg adsorbed on modified Fe-Ti spinel
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could be thermally desorbed. The Hg-TPD profile under a N2 atmosphere showed a strong
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desorption peak at 190 oC and a tailing desorption peak at 270 oC (Figure 5). However, the
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Hg-TPD profile under an air atmosphere showed three desorption peaks at 190, 270 and 350 oC.
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The desorption peak at 190 oC could be assigned to the decomposition of HgS.18, 43, 44 Figure 5
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also shows that the intensity of the desorption peak at 190 oC under the air atmosphere was much
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less than that under the N2 atmosphere. Figure S3 in the Supporting Information shows that Fe-Ti
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spinel exhibited a moderate performance for gaseous Hg0 capture at 200-350 oC and the
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adsorption of Hg0 onto Fe-Ti spinel in the presence of O2 was much better than that under the N2
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atmosphere. This result suggests that during the Hg-TPD process, there was a re-adsorption of Hg0,
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which resulted from the decomposition of HgS, onto Fe-Ti spinel. Moreover, the reduced intensity
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of the desorption peak at 190 oC under air may be mainly related to the promotion of the
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re-adsorption of Hg0 on Fe-Ti spinel in the presence of O2. Therefore, the desorption peak at 270
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o
C was assigned to the decomposition of HgO,15, 16, 44 which resulted from the re-adsorption of 12
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Hg0. Furthermore, the desorption peak at 350 oC may be attributed to the decomposition of
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HgSO4,44 which resulted from the oxidation of HgS. The complete desorption of adsorbed Hg
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from modified Fe-Ti spinel shifted approximately 50 oC to high temperature in the presence of O2
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(Figure 5). Thus, the recovery of Hg from modified Fe-Ti spinel was performed under a N2
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atmosphere and the temperature was selected at 300 oC.
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Figure 6 shows the breakthrough curves of Hg0 capture by modified Fe-Ti spinel during the five
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cycles of Hg0 capture, Hg0 recovery and sorbent regeneration. The efficiencies of modified Fe-Ti
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spinel for Hg0 capture during the 5 cycles were all close to 100%. These results suggest that the
294
ability of modified Fe-Ti spinel to capture Hg0 from the flue gas did not degrade remarkably.
295
Although the characteristic peaks corresponding to pyrite became more apparent in the XRD
296
pattern of modified Fe-Ti spinel after the 5 cycles due to the reduplicative pretreatment with H2S,
297
the characteristic peaks corresponding to spinel were still predominant in the XRD pattern (Figure
298
1a). This finding suggests that the spinel structure of modified Fe-Ti spinel did not change
299
remarkably after the five cycles and that modified Fe-Ti spinel still remained an excellent
300
super-paramagnetism with a saturation magnetization of 11.8 emu g-1 (Figure 1b). The inset
301
picture in Figure 1b indicates that modified Fe-Ti spinel after the 5 cycles can still be easily
302
magnetically separated from a mixture of 0.2 g of modified Fe-Ti spinel, 2.0 g of fly ash and 20
303
mL of deionized water. Furthermore, the concentration of gaseous Hg0 in the recovery process
304
(100 mg of modified Fe-Ti spinel, 100 mL of N2 and 300 oC) was much higher than 5000 µg m-3.
305
The high concentration of gaseous Hg0 in the recovery process may facilitate the centralized
306
control of Hg pollution. These results all suggest that modified Fe-Ti spinel can be recycled to
307
recover Hg0 from the flue gas.
308
4. Perspectives
309
The recovery of Hg0 by recyclable modified Fe-Ti spinel as a co-benefit of the WESP may be a
310
cost-effective technology for the centralized control of Hg0 emission from the flue gas. However,
311
the environmental benefit and cost-effect of this technology will become very low if most Hg
312
species present in the flue gas are Hgp and Hg2+, which are converted into fly ash and
313
desulfurization gypsum upstream of the WESP. The Hg species in the flue gas after coal 13
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combustion primarily consist of gaseous Hg0, and the conversion of Hg0 to Hg2+ or Hgp in the flue
315
gas is mainly related to the presence of HCl in the flue gas.45 Meanwhile, HCl in the flue gas also
316
causes the extensive corrosion of metal components and the formation of organic chlorinated
317
compounds.46 Therefore, the removal of HCl in the flue gas upstream of the SCR unit by the
318
injection of sorbents is suggested.
319 320
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Corresponding Author * School of Environmental and Biological Engineering, Nanjing University of Science and
323
Technology. Telephone: 86-18-066068302; E-mail:
[email protected].
324
Acknowledgements
325
This study was financially supported by the National Natural Science Fund of China (Grant No.
326
41372044) and the Natural Science Fund of Jiangsu Province (Grant No. BK20150036).
327
Supporting Information
328
The Supporting Information is available free of charge on the ACS Publications Website (DIO:
329
XXXX), and includes the average rates of gaseous Hg0 capture by γ-Fe2O3 and modified γ-Fe2O3;
330
the procedure of Hg0 recovery from the flue gas by magnetic sorbents as a co-benefit of the WESP;
331
the concentration of SO2 formed during Hg0 capture by modified Fe-Ti spinel; and breakthrough
332
curves of gaseous Hg0 capture by γ-Fe2O3, modified γ-Fe2O3, Fe-Ti spinel, elemental sulfur,
333
Mn-Fe spinel, Fe-Ti-Mn spinel, pyrrhotite and modified Fe-Ti spinel.
334
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References:
336
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456 457 458
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459 460
Table 1. The percentages of S species on modified Fe-Ti spinel, denuded modified Fe-Ti spinel
461
and
462
/%
modified
Fe-Ti
spinel
Hg0
after
capture
total S
S2-
S22-
polysulfur
SO42-/HSO4-
modified Fe-Ti spinel
6.2
0
0.8
1.9
3.5
denuded modified Fe-Ti spinel
9.9
3.4
4.4
2.2
0
modified Fe-Ti spinel after Hg0 capture
6.3
0.1
0.7
1.9
3.6
463 464 465
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466
Table 2. Average rates of gaseous Hg0 capture by Fe-Ti spinel and modified Fe-Ti spinel
467
/µg g-1 min-1 40 oC
60 oC
80 oC
100 oC
Fe-Ti spinel
0.01
0.02
0.06
0.09
modified Fe-Ti spinel
1.69
1.88
1.57
1.09
modified Fe-Ti spinel under N2
1.61
1.84
1.60
1.07
modified Fe-Ti spinel with H2O and SO2
1.34
1.92
1.50
0.96
468 469
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470 471
Table 3. Comparison of the performance of modified Fe-Ti spinel for gaseous Hg0 capture with
472
those of other magnetic sorbents reaction rate
capacity for Hg0
reaction
Hg species
Magnetization
/µg g-1 min-1
capture/mg g-1
condition
formed
/emu g-1
0.74
0.013 (20%)
0.24
0.033 (25%)
MagZ-Ag0 Ar at 50-150 oC
amalgam
simulated flue
HgSO4 and
gas at 60 oC
HgO
simulated flue
HgSO4 and
gas at 60 oC
HgO
simulated flue
HgSO4, HgCl2
gas at 150 oC
and HgO
40.0
17, 20
Mn-Fe spinel 16, 23 Fe-Ti-Mn 0.25
29.6
0.075 (25%)
spinel 15 Co-MF 27
pyrrhotite 18
0.16
45.6
0.03 (35%)
24.4
simulated flue 0.28
0.22 (4%)
1.92
0.69 (5%)
gas at 60 oC
modified
HgS
7.0
HgS
24.6
simulated flue gas at 60 oC
Fe-Ti spinel 473 474 475
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476
Figure captions
477
Figure 1. (a), XRD patterns of Fe-Ti spinel, modified Fe-Ti spinel and modified Fe-Ti spinel after
478
the 5 cycles of Hg0 capture, Hg0 recovery and sorbent regeneration; (b), magnetization
479
characteristics of Fe-Ti spinel, modified Fe-Ti spinel and modified Fe-Ti spinel after the 5 cycles.
480
Figure 2. XPS spectra of Fe-Ti spinel, modified Fe-Ti spinel and denuded modified Fe-Ti spinel in
481
the spectral regions of Fe 2p, Ti 2p, O1s and S 2p.
482
Figure 3. Breakthrough curves of gaseous Hg0 capture by: (a), Fe-Ti spinel; (b), modified Fe-Ti
483
spinel; (c), modified Fe-Ti spinel in the presence of H2O and SO2; (d): modified Fe-Ti spinel
484
under N2 atmosphere. Reaction conditions: [Hg0] =100-120 µg m-3, [O2] =5%, [H2O] =8% (when
485
used), [SO2] =80 ppm (when used), sorbent mass=20 mg for modified Fe-Ti spinel and 100 mg for
486
Fe-Ti spinel, total flow rate=500 mL min-1 and GHSV=300000 or 1500000 cm3 g-1 h-1.
487
Figure 4. XPS spectra of modified Fe-Ti spinel after Hg0 capture in the spectral regions of Fe 2p,
488
Ti 2p, O1s, S 2p and Hg 4f
489
Figure 5. Hg-TPD profiles of modified Fe-Ti spinel after Hg0 capture under N2 and air
490
atmospheres.
491
Figure 6. Breakthrough curves of Hg0 capture by modified Fe-Ti spinel during the five cycles of
492
Hg0 capture, Hg0 recovery and sorbent regeneration.
493 494 495
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modified Fe-Ti spinel after the 5 cycles modified Fe-Ti spinel Fe-Ti spinel maghemite JCPDS 39-1346 pyrite JCPDS 42-1340 20
30
40
50
60
70
2θ/degree
a
b 496 497
Figure 1. (a), XRD patterns of Fe-Ti spinel, modified Fe-Ti spinel and modified Fe-Ti spinel after
498
the 5 cycles of Hg0 capture, Hg0 recovery and sorbent regeneration; (b), magnetization
499
characteristics of Fe-Ti spinel, modified Fe-Ti spinel and modified Fe-Ti spinel after the 5 cycles.
500
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Fe-Ti spinel
Fe 2p
Fe-Ti spinel
Ti 2p
Page 26 of 30
O 1s
Fe-Ti spinel
458.7
711.2
724.8
530.2
712.4
719.3
464.4 531.7
730
725
720
715
710
705
468
466
464
462
460
458
456
536
534
532
530
Binding Energy/eV
Binding Energy/eV
Binding Energy/eV
a
b
c
Fe 2p
modified Fe-Ti spinel
725.2
modified Fe-Ti spinel
Ti 2p
modified Fe-Ti spinel
O 1s
530.4
711.2
712.4
528
458.9
719.9 713.3
531.7 532.2
464.6 707.6
730
725
720
715
710
705
468
466
464
462
460
458
456
536
534
532
530
Binding Energy/eV
Binding Energy/eV
Binding Energy/eV
d
e
f
S 2p
modified Fe-Ti spinel
denuded modified Fe-Ti spinel
Fe 2p
Ti 2p
denuded modified Fe-Ti spinel
168.9 722.0 720.2 724.1
164.2
170.1
714.2
162.9
174
172
170
168
166
164
162
160
730
725
720
464.6
715
710
705
468
466
464
462
460
Binding Energy/eV
Binding Energy/eV
g
h
i
162.7
532
456
161.7
163.9
531.5
534
458
S 2p
denuded modified Fe-Ti spinel
O 1s
530.4
536
458.9
709.1 711.1 707.2 712.4
Binding Energy/eV
denuded modified Fe-Ti spinel
528
530
528
174
172
170
168
166
164
Binding Energy/eV
Binding Energy/eV
j
k
162
160
501
Figure 2. XPS spectra of Fe-Ti spinel, modified Fe-Ti spinel and denuded modified Fe-Ti spinel in
502
the spectral regions of Fe 2p, Ti 2p, O1s and S 2p.
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-3
Hg concentration/µg m
100 80 o
o
40 C o 80 C
60 40
60 C o 100 C
0
0
Hg concentration/µg m
-3
120
20
120 o
100 80
0
60 40 20
50
100
150
0
200
50
-3 o
Hg concentration/µg m
o
40 C o 80 C
60 C o 100 C
60 40
0
-3
120
80
150
200
b
a
100
100
t/min
t/min
0
60 C o 100 C
0
0
Hg concentration/µg m
o
40 C o 80 C
20
120 o
100
o
40 C o 80 C
80
60 C o 100 C
60 40 20 0
0 0
50
100
150
0
200
50
100
150
200
t/min
t/min
c
d
504 505
Figure 3. Breakthrough curves of gaseous Hg0 capture by: (a), Fe-Ti spinel; (b), modified Fe-Ti
506
spinel; (c), modified Fe-Ti spinel in the presence of H2O and SO2; (d): modified Fe-Ti spinel
507
under N2 atmosphere. Reaction conditions: [Hg0] =100-120 µg m-3, [O2] =5%, [H2O] =8% (when
508
used), [SO2] =80 ppm (when used), sorbent mass=20 mg for modified Fe-Ti spinel and 100 mg for
509
Fe-Ti spinel, total flow rate=500 mL min-1 and GHSV=300000 or 1500000 cm3 g-1 h-1.
510
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511 0
Fe 2p
modified Fe-Ti spinel after Hg capture
0
modified Fe-Ti spinel after Hg capture
711.0
725.0
0
Ti 2p
modified Fe-Ti spinel after Hg capture
458.8
712.4
530.2
713.3
719.8
O 1s
532.2
464.5
531.7
707.4
730
725
720
715
710
705
468
466
Binding Energy/eV
464
S 2p
170
168
166
164
534
532
530
c
528
Hg 4f
101.0
105.1 164.0
536
456
b modified Fe-Ti spinel after Hg capture
168.9
172
458
0
0
modified Fe-Ti spinel after Hg capture
174
460
Binding Energy/eV
a
170.2
462
Binding Energy/eV
162.8 161.8
162
160
108
106
104
102
Binding Energy/eV
Binding Energy/eV
d
e
100
98
512 513
Figure 4. XPS spectra of modified Fe-Ti spinel after Hg0 capture in the spectral regions of Fe 2p,
514
Ti 2p, O1s, S 2p and Hg 4f.
515
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516
0
Hg concentration/ µg m
-3
517 1200 1000
under N2 under air
800 600 400 200 0 0
100
200
300
400
o
Temperature/ C
518 519
Figure 5. Hg-TPD profiles of modified Fe-Ti spinel after Hg0 capture under N2 and air
520
atmospheres.
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100 the first run the second run the third run the forth run the fifth run
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Ηg concentration/µg m
-3
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0 0
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50
100
150
200
t/min
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Figure 6. Breakthrough curves of Hg0 capture by modified Fe-Ti spinel during the five cycles of
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Hg0 capture, Hg0 recovery and sorbent regeneration.
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