Determination of Chemical Speciation of Arsenic and Selenium in High-As Coal Combustion Ash by X-ray Photoelectron Spectroscopy: Examples from a Kentucky Stoker Ash.

Knowledge of the chemical speciation of arsenic and selenium in coal fly ash is essential in the evaluation of the environmental behavior of fly ash disposed in a landfill in a natural environment. In this study, a series of high-As coal fly ash from stoker boilers were collected to determine the chemical forms of arsenic and selenium. The ash surface chemical characteristics and the speciation of arsenic and selenium were characterized by X-ray photoelectron spectroscopy and X-ray-induced Auger electron spectroscopy. The results indicate that the surface enrichment ratio for selenium (63.3-309.5) is higher than that of arsenic (1.2-21.2). The Wagner chemical-state plot of arsenic indicates that As is mainly present as As(V) bonded to oxygen ligands, that is, the [AsO4]3- anion; Se is found predominantly as elemental Se (62.0-83.3%), followed by selenite (16.7-38%). The extreme enrichment of both arsenic and selenium arsenic is controlled by iron oxides in the coal fly ash.

Introduction

Metalloid arsenic and selenium are known volatile elements of environmental concern, which can be potentially released from coal-fired power plants.[1] During high-temperature combustion, volatile elements arsenic and selenium in coal may be completely vaporized and significantly condensed onto the fly ash surface.[1,2] Coal combustion byproducts (fly ash) are considered to be a main potential source of trace elements for the environment.[3,4] One of the concerns regarding As and Se in coal fly ash is their natural leaching into the environment when the ash is disposed in landfills or ash ponds.[4] The leaching behavior of arsenic and selenium in fly ash is largely controlled by their chemical speciation.[4−6] Arsenic in coal fly ash occurs mainly as pentavalent arsenate [As(V)] with minor trivalent arsenite [As(III)], which might be associated with glass, iron (oxyhydr) oxides, and calcium arsenate;[7−10] these As-bearing chemical species in fly ash are stable under oxic environment but might be mobile and bioavailable under anoxic conditions.[10] Compared to the inert elemental selenium (Se0), the oxidation state of Se such as selenite [SeO32–, Se(IV)] and selenate [SeO42–, Se(VI)] is labile and highly soluble.[11] In general, in an oxidizing alkaline environment, selenium is much more mobile and soluble.[6]

Coal fly ash is a complicated heterogeneous material, mainly consisting of glassy materials with minor mineral phases and unburned carbon.[12] The chemical speciation of arsenic and selenium in the fly ash can be determined by indirect and direct methods. Direct determination of the chemical speciation of arsenic and selenium in coal fly ash is an important but difficult task because of their low concentration and heterogeneity in fly ash. Hower et al.[13] used high-resolution transmission electron microscopy (HRTEM) combined with energy-loss spectroscopy to demonstrate that the nanocarbon particles can host heavy metals and metalloids including Hg, As, Se, and Pb. Synchrotron X-ray absorption spectroscopy (XAS) is a primary technique to detect the chemical species of metal(loid)s in coal or coal fly ash.[6,8] However, access to this energy spectroscopy technique is not easy, and it can be expensive. In addition to TEM and XAS, X-ray photoelectron spectroscopy (XPS) is the other well-established nondestructive surface analysis technique for characterizing the surface chemical state of metal(loid)s in the fly ash.[7,14−16] The presence of peak at 48.5 eV could be assigned to As 3d for arsenic oxides in coal fly ash.[15] Goodarzi[7] indicated that As5+ is the dominant form of arsenic in several Canadian coal fly ashes, and As was found to be greatly enriched on the surface of fly ash. Yan et al.[17] assigned two peaks of Se 3d to elemental Se (56 eV) and SeO2 (60 eV) in the cooled aerosol particles generated from lab-scale coal/coke combustion experiments. However, XPS may not give accurate information on the chemical state of one element because the binding energy values for the specific chemical state of some elements vary in a relatively wide range. For example, the binding energies of As(V)–O bonds are 44.9, 45.6, and 46.8 eV for Na2HAsO4·H2O, FeAsO4·2H2O, and As2O5, respectively.[18] More accurate determination of the chemical state of elements can be obtained by a two-dimensional Wagner chemical-state plot.[18−20] The Wagner plot, which combines the data of core-level binding energy with the kinetic energy of the Auger transition, has been successfully used to identify the chemical state of elements in heterogeneous natural samples and to avoid ambiguous results.[18,20,21] Therefore, it might be a practical method to clearly identify As and Se species in coal fly ash.

The chemical speciation of trace elements in coal fly ash is dependent upon feed-coal properties, combustion conditions, boiler types, air pollution control devices, etc.[2,7] Much of the detailed information on the chemical speciation of As and Se in coal fly ash has focused on pulverized-coal combustors[7,8,13] or fluidized-bed boilers.[5,7] Coal stoker boilers are also an important boiler type, which are widely used in a variety of applications.[22] Nevertheless, direct determination of the surface chemistry and chemical speciation of metal(loid)s in stoker ash is lacking. In this study, the surface chemical characteristics and speciation of As and Se in the stoker ash are studied using XPS and X-ray-induced Auger electron spectroscopy (XAES). As reported by Mardon et al.,[22] the concentration of As in the studied ash samples exceeded 1000 μg/g. On the basis of the bulk analysis, Mardon et al.[22] also suggested that arsenic in the stoker ash might be present as “a condensate on the surface of the Al–Si ash particles” or as “a component in a fine carbon fraction”. However, this speculation concerning the chemical speciation of arsenic in the fly ash lacked direct evidence. The extremely high-As stoker ash provides a good opportunity to study the chemical speciation of arsenic and selenium in fly ash. These samples in this study are designed to obtain more precise information on the chemical speciation of As and Se in the stoker fly ash using XPS and XAES. To the best of author’s knowledge, the research may be the first time the XPS–XAES technique has been used to characterize the chemical speciation of As and Se in coal fly ash. The results of this study also can provide not only important information on the modes of As and Se occurrences in fly ash but also a more practical option for researchers to identify As and Se species in other complex environmental samples compared to synchrotron-based analysis.

Materials and Methods

Sample Collection

Three stoker fly ashes, 93259 (first row of the hoppers), 93260, and 93261, were collected in July 2006 from three successive baghouse hoppers of the Eastern Kentucky University (EKU) heating boilers. The whole ash 93259 was screened at 60, 100, 200, 325, and 500 mesh, respectively.

Chemical Analysis

Bulk chemical analysis reported by Mardon et al.[22] was supplemented with a more detailed examination of the samples used in this study. In detail, the concentration of major element oxides and trace elements was determined for the screened ash samples in this study. Especially, supplementary determination of rare earth elements and selenium in all ash samples was also carried out in this study (Table S1). Mercury was determined using a Milestone DMA-80 analyzer (with a 0.005 ng detection limit) based on the methods of Dai et al.[23] Concentrations of other trace elements in the fly ash were determined by quadrupole-based inductively coupled plasma mass spectrometry (Thermo Fisher, X series II ICP-MS). In order to reduce the spectral interferences of the Ar-based polyatomic ions 40Ar35Cl and 40Ar38Ar to 75As and 78Se, respectively, the concentrations of As and Se in samples were determined by ICP-MS using collision/reaction cell technology, following the procedures outlined by Li et al.[24] Boron concentrations were also determined by ICP-MS after digestion of the solid sample (50 mg) using a mixture of H3PO4, HNO3, and HF; a 2% ammonia solution was injected into the spray chamber of the ICP-MS facility to eliminate the memory effect of boron.[25] Prior to ICP-MS analysis, all samples were digested using a closed vessel microwave digestion system (Milestone UltraClave).

Analysis of surface chemistry for the ash samples was performed on an XPS spectrometer (ESCALAB 250 Xi, Thermo VG Scientific) using a monochromatic Al Kα (1486.6 eV, 150 W) X-ray source. Survey scan analyses were carried out with a spot size of 500 μm2 area and a pass energy of 30 eV. High-resolution scan analyses of the ash samples were performed to obtain the spectra of C 1s, O 1s, S 2p, Fe 2p, Ca 2p, As 2p, As 3d, and Se 3d. The energy step size for the narrow scan analysis was 0.05 eV. The final high-resolution scan spectrum was obtained with at least three times of scan for each element. To compensate for the charging effects, all the spectra have been corrected to the C 1s spectra set to 284.8 eV.[26] Photoelectron lines after nonlinear background subtraction (Shirley) were fitted with Gaussian/Lorentzian functions using CasaXPS (version 2.3.13) software. In addition to the photoelectronic lines of As 3d and Se 3d, the X-ray-induced Auger lines of arsenic (As LMM) and selenium (Se LMM) were also examined. These data can be used to obtain the Auger parameter and the chemical-state plot to clearly distinguish the chemical states of As and Se in the fly ash samples.[18,19]

Results and Discussion

Chemical Compositions of Fly Ash

Results of bulk analysis of fly ash are listed in Table . The long version of the data table, which includes all the element concentration results, can be found in the Supporting Information (Table S1). In this study, Si, Al, C, and Fe are the dominant elements for the three raw fly ash samples, which are generally consistent with the mineralogical compositions of quartz, mullite, and hematite.[27] The concentration of arsenic is significantly higher than the reported values (typically in the range of 1–1000 μg/g) in most other coal fly ashes.[5,10,28] Selenium is also enriched in the raw fly ash (Table ). Further, as shown in Figure , there is a strong linear relationship between Fe2O3 and As, suggesting that the deposition of arsenic onto the fly ash surface may be associated with iron oxides.

Table 1

Major Element (Oxide wt %), Carbon, Sulfur, As (μg/g), and Se (μg/g) Data for Fly Ash Samples (Dry Basis)

sample number	SiO2	TiO2	Al2O3	Fe2O3	MgO	CaO	MnO	Na2O	K2O	P2O5	LOI (%)	C (%)	S (%)	As	Se
93259 whole ash	39.50	1.31	20.71	31.52	0.56	1.35	0.17	0.51	1.32	3.04	25.31	15.19	1.61	4876	256
93260 whole ash	39.66	1.33	20.26	29.87	0.54	1.32	0.19	0.64	1.36	4.85	25.34	17.61	1.50	8450	230
93261 whole ash	52.25	2.26	26.13	11.81	0.67	2.03	0.04	1.03	2.18	1.59	38.62	25.42	2.13	1378	200
93259 + 60 mesh	3.24	0.08	2.12	89.12	0.13	0.11	0.54	0.25	0.21	4.17	11.22	4.07	1.18	8022	222
93259 60 × 100 mesh	15.72	0.37	10.43	65.52	0.29	0.28	0.32	0.25	0.57	6.25	22.98	14.25	1.09	9379	305
93259 100 × 200 mesh	31.30	0.90	19.23	41.84	0.47	0.74	0.16	0.29	0.92	4.16	25.65	18.57	0.88	5768	321
93259 200 × 325 mesh	44.84	1.66	24.39	23.25	0.56	1.49	0.07	0.27	1.28	2.20	20.45	15.07	0.64	2856	288
93259 325 × 500 mesh	48.91	1.99	25.48	18.02	0.59	1.86	0.05	0.27	1.40	1.43	17.25	12.87	0.51	1663	225
93259 500 mesh	51.23	2.29	24.88	15.99	0.50	1.12	0.03	0.22	1.65	2.08	33.40	23.16	0.85	2033	260

Figure 1

Correlations between As and iron oxides (left) in the whole coal fly ash (bulk analysis) and correlations between the surface concentration of As/Se and the Fe content by XPS surface analysis.

Figure is a typical survey spectrum of fly ash (93259 60 mesh). The major chemical compositions in the fly ash sample determined by XPS are C, O, Si, Al, Fe, P, and S, corresponding to the binding energies of 285, 532, 104, 74, and 712 eV, respectively (Table ; Figure ). Minor elements (less than 1%, sometimes detected at the noise levels) specifically Ti, Na, Mg, and Ca are also identified. Main peaks of As 3d and Se 3d can be clearly observed at ca. 46 and 57 eV, respectively, in the high-resolution spectra (Figures and 6). Especially, in comparison with the element contents in the whole coal fly ash (bulk analysis), the mass percentage of As and Se in most ash surfaces is larger than 1 wt % (Table ), suggesting a significant surface enrichment. In addition, the correlation coefficient values between As versus Fe and Se versus Fe in the fly ash surface are 0.86 and 0.98, respectively (Figure ), indicating that Fe may play an important role in the As and Se surface retention.

Figure 2

Survey spectrum of fly ash (93259 60 mesh).

Table 2

XPS Surface Chemical Composition of Coal Fly Ash (wt %) and the Surface ER

	surface analysis (wt %)															ER
	Si 2p	Al 2p	Fe 2p	P 2p	As 3d	Se 3d	C 1s	S 2p	Si	Fe	P	As	Se	C	S	Fe
93259 whole ash	15.05	7.93	2.27	1.68	1.01	2.20	35.88	4.2	1.1	0.1	1.8	1.7	136.6	3.3	3.6	22.05
93260 whole ash	11.44	4.42	1.96	3.08	1.99	0.86	41.50	4.8	1.5	0.2	3.5	9.9	81.2	5.7	7.8	20.89
93261 whole ash	11.44	5.67	0.61	1.08	0.48	0.79	45.82	5.8	1.1	0.2	3.8	1.2	63.3	4.4	6.6	8.26
93259 + 60 mesh	2.59	2.26	10.82	5.49	4.02	15.01	26.33	3.8	0.8	0.1	1.5	3.5	231.3	3.2	1.6	62.33
93259 60 × 100 mesh	7.59	4.72	4.42	4.03	3.07	4.03	44.21	2.0	1.2	0.1	1.7	12.5	163.5	3.6	2.1	45.83
93259 100 × 200 mesh	15.09	6.30	2.89	2.63	2.18	3.58	35.86	1.8	1.7	0.1	2.3	21.2	256.7	3.1	3.3	32.52
93259 200 × 325 mesh	18.29	7.24	3.18	1.94	1.63	3.41	31.87	2.3	1.6	0.3	3.6	14.3	234.4	3.8	6.5	16.26
93259 325 × 500 mesh	22.32	8.57	2.98	2.04	1.53	3.09	23.76	1.7	1.5	0.4	5.1	2.8	211.5	2.9	5.3	12.61
93259 500 mesh	14.56	5.36	2.80	1.92	0.74	2.51	42.87	2.3	1.5	0.6	5.2	13.2	309.5	4.5	6.7	11.18

Figure 3

As 3d signal and As LMM lines for selected fly ash samples detected by both XPS and XAES techniques. Black solid lines and dashed–dotted lines refer to best-fit and experimental curves, respectively. The peak assignment obtained by deconvolution is shown as red dashed lines and blue dashed lines. The Shirley background is added to each As 3d spectrum.

Figure 6

Se 3d high-resolution spectra for all the fly ash samples detected by XPS. Black solid lines and dashed–dotted lines refer to best-fit and experimental curves, respectively. The peak assignment obtained by deconvolution is shown as dashed lines in different colors. The Shirley background is added to each Se 3d spectrum. fwhm remains consistent during the fitting process (2.3–2.5 eV).

Comparison between XPS Surface Analysis and Bulk Analysis

In this study, the element contents in the fly ash surface determined by XPS are all normalized to Al. The method has been used in previous studies[14,15] because, during coal combustion, Al was a conservative element, therefore minimizing the variability in ash compositions and reflecting the differential enrichment behavior of elements.[14] To assess the surface enrichment of elements in fly ash, the enrichment ratio (ER) is calculated based on formula 1where MSi and MBi represent the mass concentration of each element in the ash surface (XPS analysis) and in the whole coal fly ash (bulk analysis), respectively. As shown in Table , the ER value of Si varies in the range of 0.85–1.67, suggesting that Si generally is evenly distributed throughout the whole ash.[14−16] For Fe, the ER value (<1) indicates that Fe is present much more in the interior than the outer surface.[29] However, although the ash surface is not enriched in Fe, Fe is a still major component on the surface of some of the fly ash particles, as discussed above. For C, S, P, As, and Se, the ER value is larger than 1, which is an indication of surface enrichment of these elements onto the fly ash surface. On the basis of the high ER values for Se (63–309), it can be inferred that extensive absorption/condensation of gaseous Se species onto the fly ash surface may occur in the post-combustion process. Note that although the concentrations of Se (200–321 μg/g) in the whole ash are much lower than that of As (1378–9379 μg/g), Se contents on the ash surface are higher than that of As (with the exception of the sample 93261) because of the more intense surface enrichment of Se in fly ash.

Chemical State of As

In this study, all the fly ash samples are subjected to XPS analysis to obtain the As 3d spectra and four of the samples are determined by both XPS and XAES techniques. Table summarizes the results of peak position for As 3d, As 2p3/2, As L2M45M45, As L3M45M45 lines, and Auger parameter. It should be noted that photoelectron lines of S 2s may overlap with As L2M45M45 (Figure ). To overcome this problem, Auger lines of As L3M45M45 are chosen to obtain the Auger parameters.[21] The selected XPS and XAES spectra of arsenic in coal fly ash are shown in Figure . The high-resolution spectra of As 3d for all the ash samples, after Shirley-background subtraction, are fitted with As 3d5/2 and As 3d3/2 doublet with a binding energy difference of 0.7 eV and an area ratio of 3:2.

Table 3

XPS and XAES Results of Peak Position for As 2p, As 3d, As 2p3/2, As L2M45M45, As L3M45M45 Lines, and Auger Parameter; Unit: eV

sample	2p	3d	3d5/2	L2M45M45	L3M45M45	α + hν
93259 60 mesh	1327	45.9	45.9	1254	1218	1263.35
93259 60 × 100 mesh	1328	46.4	45.9	1253	1217	1263.10
93259 100 × 200 mesh	1328	45.8	45.8	1253	1218	1263.28
93261 whole ash	1328	46.9	46.1	1253	1217	1263.44
93260 whole ash		46.9	46.1
93259 whole ash		45.8	45.6
93259 200 × 325 mesh		46.05	45.8
93259 325 × 500 mesh		46.1	45.7
93259 500 mesh		45.9	45.7
93261 whole ash		45.9	45.8

In general, the As 3d spectra show minor variations among all the samples. The binding energy values of As 3d5/2 are in the range of 45.7–46.1 eV, suggesting that arsenic might be present as As(V). The As L3M45M45 lines in the X-ray absorption near-edge structure (XANES) spectra are found between 1216 and 1218 eV. Consequently, the modified Auger parameter α′, defined based on the original Auger parameter (α) as Wagner suggested,[19] can be obtained based on formula 2where EK and EB represent the kinetic energy of the sharpest Auger line and binding energy of the most intense photoelectron line. The Auger parameter α′ is independent of charging effect and quite useful to identify the chemical state in insulator samples.[18,19,30] As shown in Table , arsenic in the fly ash samples has an Auger parameter of 1263.3 ± 0.2 eV. The calculated Auger parameter is plotted on the Wagner chemical-state plot as a series of diagonal lines.

The Wagner chemical-state plot for arsenic as well as several arsenic-bearing compounds from NIST XPS database[39] and published data[18,21,30] is depicted in Figure . In the chemical-state plot, it is observed that all the data points of the fly ash samples fall on a diagonal line with the Auger parameter of 1263.5 eV. These points of analyzed fly ash are close to scorodite (FeAsO4·2H2O) and Na2HAsO4 (points in the blue circle). On the basis of the arsenic chemical-state plot, other chemical states of arsenic, including As(III) oxides and AsO2–1, could be ruled out. This is a little different from the published data about the chemical forms of As in the coal fly ash. According to synchrotron-based XAS studies, Huggins et al.[8] indicated that there was a minor fraction (10–15%) of arsenic present as As(III) in 10 pulverized coal fly ash samples; Deonarine et al.[10] reported that 3–8% of total As occur as As(III) in two fly ash samples. In this study, arsenic in the stoker fly ash can probably be assigned to oxo-anion arsenate and might be associated with Fe oxides/hydroxides occurring as Fe(III)–AsO4. As can be seen from Figure , Fe 2p in the fly ash photoelectron spectroscopy exhibits a typical doublet because of spin–orbit coupling interactions. The peak of Fe 2p3/2, situated at 711.8 eV along with two satellites at the higher binding energy side of Fe 2p3/2 and Fe 2p1/2, is a typical spectrum of Fe(III) oxides and hydroxides.[20,26] The presence of metal (mainly Fe) oxides/hydroxides is also supported by the high-resolution scan spectra of O 1s (Figure ). The O 1s spectrum displays complex envelopes caused by different surface oxides species such as sulfates, phosphates, organics, and metal(loid)s oxides. A shoulder peak appearing at ca. 530 eV in the spectrum of fly ash 93250 60 mesh is much more obvious (Figure ) than that in the other ash samples. The shoulder peak for the 93250 60-mesh fly ash is a consequence of the high iron oxides content in the ash surface (Table ). Therefore, on the basis of the XPS and XAES analysis and the strong correlations between arsenic and iron (Figure ), arsenic in the studied stoker fly ash occurs as As(V) bonded to oxygen ligands, that is, the [AsO4]3– anion, and probably absorbed by iron oxides/hydroxides or incorporation into the Fe-bearing phases. It has been reported that Fe had strong correlations with As, forming As-/Fe-bearing compounds as independent minerals or As(V) sorbed to Fe(III) oxides/hydroxides in complex natural samples (mining wastes, stream sediments, and fly ash).[10,20,31] The chemical speciation of arsenic in this study generally agrees with fly ash samples from the Kingston fossil plant (Tennessee) that 95–100% of total As in the fly ash occurred as As(V) associated with iron (hydr)oxides and aluminosilicate glass.[32] Tian et al.[33] also demonstrated that arsenic occurred as As(V) in three different coal fly ash samples using XANES technology. Under a fully oxidized chemical environment, arsenate bonds strongly to iron oxide minerals as an inner-sphere complex as a bidentate, binuclear surface complex.[34] In addition, the formation of calcium arsenate in the fly ash could be excluded because of the very low contents of calcium in the ash surface.[2,5,7]

Figure 4

Wagner chemical-state plot for arsenic in coal fly ash and in several arsenic-bearing compounds from NIST XPS database and published data.

Figure 5

XPS data of Fe 2p and O 1s high-resolution spectra for the 93259 60-mesh fly ash sample.

Chemical State of Se

Selenium is one of the most volatile elements during coal combustion.[17] Previous studies reported that Se in coal fly ash can be present as several chemical forms including elemental Se (Se0), selenite [SeO32–, Se(IV)], selenate [SeO42–, Se(VI)], and SeO2.[6,8,17] As discussed in Section , the maximum concentration of Se in the surface of fly ash is 309 times higher than the Se content in the whole ash. Therefore, the Se 3d signal is strong enough to be detected in spite of the Se concentration in the whole ash being below the limit of detection of XPS (0.1 wt %, 1000 μg/g). Detailed XPS patterns of Se 3d for all fly ash samples are shown in Figure . The Auger lines of Se L3M45M45, which are detected at the noise level, are not considered in this study. It is established that elementary Se, selenite, selenate, and SeO2 have peaks of Se 3d5/2 at 55.4 ± 0.7, 59.1, 59.4 ± 0.6, and 61.6 eV, respectively.[39]

As described in Figure , the Se 3d peak for fly ash samples has a main asymmetric peak at 57 ± 0.7 eV with a broad binding energy range extending from 62 to 54 eV, indicating that more than one chemical state of Se occurred in the fly ash.[37] The Shirley-subtracted high-resolution spectra of Se 3d are fitted with the Se 3d5/2–3d3/2 separation of 0.86 eV and full width at half-maximum (fwhm) of 2.3–2.5 eV. Two chemical states of Se could be observed in the Se 3d spectra (Table ). The first split doublet is assigned to elemental Se0 with a binding energy of Se 3d5/2 at 56.5 ± 0.2 eV; the second peak corresponds to selenite (SeO32–, Se(IV)) with a binding energy of 58.5 ± 0.4 eV. All the fitting results are listed in Table . The Se distribution in the fly ash samples is dominated by elemental Se (62.0–83.3%), followed by selenite (16.7–38%). Se(VI) selenate or SeO2 is not the major form because the oxidation state of hexavalent Se 3d5/2 corresponds to a higher binding energy than that of Se(IV). Therefore, the residual error for the fitting process is lowest when the Se 3d peak is fitted into elemental Se0 and selenite. The result is generally in agreement with Liu et al.[6] that elemental Se is the dominant form with minor Se oxy-anions. In an earlier HRTEM study of the fly ash samples (93261 whole fly ash), Silva et al.[27] observed that Se mainly occurred in the elemental form encapsulated by the carbonaceous matter. However, studies of other fly ash sources indicated that Se(IV) was the predominant phase.[8,9,32,33] The variations between the chemical forms of Se in different fly ash samples might be associated with the different boiler types (stoker boiler vs pulverized-coal combustor), ash components, and the air pollution control devices.

Table 4

Fitting Results of the High-Resolution Scan Spectra of Se 3d for All the Fly Ash Samples

	Se(0)		Se(IV)
sample	position (eV)	conc (%)	position (eV)	conc (%)
93259 whole ash	56.8	83.3	59.2	16.7
93260 whole ash	56.6	66.6	58.0	33.5
93261 whole ash	56.9	62.0	59.0	38.0
93259 + 60 mesh	56.1	76.8	57.9	23.2
93259 60 × 100 mesh	56.5	80.3	58.5	19.8
93259 100 × 200 mesh	56.3	75.6	58.2	24.4
93259 200 × 325 mesh	56.6	78.3	58.3	21.7
93259 325 × 500 mesh	56.4	67.1	58.3	32.9
93259 500 mesh	56.7	70.8	59.0	29.2

Possible Enrichment Mechanisms for High-As/Se Fly Ash

The feed coal used in the EKU steam plant is low-S (0.8%), high volatile A bituminous coal; trace elements, such as As (133 μg/g), are enriched in the feed coal, whereas Se (1.25 μg/g) is not concentrated.[22] The extremely high concentration of arsenic and the great surface enrichment of Se in the fabric filter fly ash may, therefore, not be anticipated. However, as noted above, the chemical composition of fly ash is not solely determined by the feed coal chemistry. Combustion conditions, post-combustion process, and the air pollution control devices are also important factors affecting the element’s partitioning behavior.[1] It is known that the concentration of As and Se is closely associated with particle size distribution; both As and Se are found to be concentrated on the fine-grain ash particles.[2,5,35] As shown in Figure S1, examination of the sized ash showed an enrichment of Fe in the coarser fly ash particles. This can also be observed based on the variations of Fe content in the raw fly samples from different baghouse hoppers. From the first-row fly ash to the third-row fly ash, the contents of Fe decreased along with the decreasing ash particle sizes (Table ). Therefore, most of the Fe oxides are probably present as individual coarse particles, as indicated by the mesh sizes of the fly ash. Interestingly, the variations of arsenic also display an enrichment in the coarse fly ash particles (Figure S1). Further, the surface analysis by XPS reveals that both arsenic and selenium peak in the coarsest fly ash fractions (93259 60-mesh ash). This is not anticipated as many previous studies reported the preferential condensation or absorption of volatile species onto the smaller particles during the post-combustion process.[2,5,36] Obviously, combined with the data from XPS and XAES experiments, the large amounts of Fe oxides play an important role in the significant retention of As and Se in the stoker fly ash surface.

The partitioning of arsenic and selenium between the vapor and solids is largely associated with the interactions of gaseous species with ash particles in the post-combustion zone. During high-temperature coal combustion in the stoker boiler, arsenic and selenium in feed coal would mostly vaporize into gas phases, such as Se0 (g), SeO (g), SeO2 (g), As2O3 (g), AsCl3 (g), and As2O5 (g).[17] These metalloid vapor phases may be physically and/or chemically absorbed by the iron oxides. Seams and Wendt[37] found that a strong correlation relationship existed between the concentration of As/Se and Fe/Ca content in the size-segregated ash particles collected from a 17 kW laboratory combustor. They suggested that Fe and/or Ca provided active sites for surface reactions where Se reacted preferentially with Fe over Ca. Compared to other mineral components (CaO and Al2O3), Fe(III) oxides were found to have the best absorption capability to react with gaseous As2O3 (g), forming stable arsenates.[38] In this study, the distribution of Fe oxides among the sized-fraction fly ash samples reveals that most of the iron oxides having relatively larger particle sizes are collected in the first-row baghouse hoppers (Table ). Consequently, arsenic and selenium that are captured by iron phases have their highest concentrations in the coarsest fly ash surface.

Conclusions

The surface chemical characteristics of As-enriched coal fly ash samples were studied by XPS and XAES, especially focusing on the chemical forms of arsenic and selenium in fly ash. Although the concentration of Se (200–321 μg/g) is significantly lower than that of As (1378–9379 μg/g), Se is found to be more enriched in the fly ash surface with surface ERs being up to 309. Arsenic in the fly ash samples has a binding energy and a kinetic energy in the range of 45.7–46.1 and 1216–1218 eV, respectively. Consequently, the Auger parameter for arsenic is calculated as 1263.3 ± 0.2 eV. The Wagner chemical-state plot derived from the As 3d binding energy and As L3M45M45 kinetic energy can be effectively used to determine the chemical state of arsenic in fly ash. These results reveal that As is mainly present as As(V) bonded to oxygen ligands, that is, the [AsO4]3– anion in the coal fly ash. The Se 3d peak has the main asymmetric peak at 57 ± 0.7 eV with a broad binding energy range and two chemical forms of Se can be found: elemental Se (62.0–83.3%) with a binding energy of Se 3d5/2 at 56.5 ± 0.2 eV and selenite (16.7–38%) with a binding energy of 58.5 ± 0.4 eV. On the basis of the XPS data and strong correlations between the concentration of As and Se and the iron content, the extreme enrichment of both arsenic and selenium is probably controlled by iron oxides in the coal fly ash.