Environ. Sci. Technol. 2010, 44, 4472–4478 Ni(II) Sorption on Biogenic Mn-Oxides with Varying Mn Octahedral Layer Structure MENGQIANG ZHU,* MATTHEW GINDER-VOGEL,† AND DONALD L. SPARKS Department of Plant and Soil Sciences, Delaware Environmental Institute, University of Delaware, 152 Townsend Hall, Newark, Delaware 19716 Received March 29, 2010. Accepted April 26, 2010. Biogenic Mn-oxides (BioMnOx), produced by microorganisms, possess an extraordinary ability to sequester metals. BioMnOx are generally layered structures containing varying amounts of Mn(III) and vacant sites in the Mn layers. However the relationship between the varying structure of BioMnOx and metal sorption properties remains unclear. In this study, BioMnOx produced by Pseudomonas putida strain GB-1 was synthesized at either pH 6, 7, or 8 in CaCl2 solution, and Ni(II) sorption mechanisms were determined at pH 7 and at different Ni(II) loadings, using isotherm and extended X-ray absorption fine structure (EXAFS) spectroscopic analyses. Our data demonstrate that Ni(II) sorbs at vacant sites in the interlayer of the BioMnOx and the maximum Ni(II) sorption capacity increases as the formation pH of BioMnOx decreases. This relation indicates that the quantity of BioMnOx vacant sites increases as formation conditions become more acidic, which is in good agreement with our companion study. Contents of the vacant sites were quantitatively estimated based on maximum Ni(II) sorption capacity. Additionally, this study reveals that imidazole groups are involved in Ni(II) binding to biomaterials, and have a higher Ni(II) sorption affinity, but a lower site density compared to carboxyl groups. determines the maximum Pb(II) sorption capacity of synthetic birnessite (12). In addition, layer Mn(III) that surrounds vacant sites in birnessite may affect heavy metal (e.g., Zn(II) and Pb(II)) sorption geometry for better charge compensation (8). As a biogeochemically relevant metal, Ni(II) is often associated with birnessite in the environment and has been found incorporated into Mn octahedral layers (2, 3). It also adsorbs at vacant sites via triple-corner sharing (TC) and at edge sites via tridentate-edge sharing (TE) and double-corner sharing (DC) (2, 13). The distribution of each Ni sorption species depends on the presence of vacant sites and experimental conditions. High pH favors Ni(II) structural incorporation whereas low pH favors Ni(II) TC adsorption at vacant sites (2, 10, 13). Ni(II) TE sorption only occurs at the edge sites of triclinic birnessite which does not contain vacant sites (10); whereas, Ni(II) DC sorption is also detected at the edge sites of δ-MnO2 at high Ni(II) loadings (2). Biomaterials, including microbial cells and/or extracellular polymeric substances (EPS), have abundant anionic functional groups, such as carboxyl, phosphoryl, sulfuryl, hydroxyl, and amine functional groups (14). Extended X-ray absorption fine structure (EXAFS) spectroscopy has demonstrated that carboxyl and phosphoryl groups are generally responsible for heavy metal binding on biomaterials (15–17) although other functional groups occasionally contribute (18). Heavy metal binding to specific functional groups depends on the type of microorganism, metal loadings, pH, and metals (15, 16). To the authors’ knowledge, spectroscopic data describing Ni(II) sorption on bacterial biomaterials has not been reported. Since Ni(II) is commonly associated with naturally occurring birnessite, we chose Ni(II) to investigate sorption on BioMnOx produced by Pseudomonas putida strain GB-1 at pH 6, 7, or 8 in CaCl2 solutions using sorption isotherms and Ni K-edge EXAFS spectroscopy. The three BioMnOx contain varying amounts of vacant sites and concentrations of layer Mn(III) according to their structural characterization (6). This study provides direct spectroscopic analyses to describe the correlation of Ni(II) sorption to the number of vacant sites and layer Mn(III) concentration. Additionally, we describe the types of organic functional groups involved in Ni(II) binding to biomaterials. Introduction Birnessite is the predominant naturally occurring Mn-oxide in most environmental settings (1). Birnessite in soils and sediments is often enriched with heavy metals and alkaline and alkali earth metals (1–3). Naturally occurring birnessite minerals have been believed to result from microbial Mn(II) oxidation which produces biogenic Mn-oxide (BioMnOx) (4). Naturally occurring birnessite minerals tend to be hexagonal; however, they are not identical and differ in Mn octahedral layer structure, that is, varying amounts of Mn(III) and quantity of vacant sites in Mn layers (1, 5). Coexisting cations (i.e., H+, Na+, Ca2+, and Ni(II)) present during bacterial Mn(II) oxidation affect the Mn octahedral layer structure of BioMnOx (6, 7). Due to positive charge deficiency, vacant sites are generally the most common sites on birnessite for heavy metal sorption; however, in the case of Ni(II) edge sites may play an important role in sorption (2, 8–11). Wet chemical studies suggest that the quantity of vacant sites * Corresponding author phone: (302) 831-1230; fax: (302) 8310605; e-mail: mzhu@udel.edu. † Current address: Calera Corporation, 14600 Winchester Blvd., Los Gatos, CA 95030. 4472 9 ENVIRONMENTAL SCIENCE & TECHNOLOGY / VOL. 44, NO. 12, 2010 Material and Methods Macro-Scale Experiments. Biosorbent Preparation. Biosorbents refer to the solid precipitates at the conclusion of bacterial Mn(II) oxidation, containing both BioMnOx and biomaterials (bacterial cells + EPS). Biosorbents were prepared by resuspending harvested and washed P. putida GB-1 biomaterial in 50 µM MnSO4 solutions containing 16.67 mM CaCl2 at pH 6, 7, and 8, respectively (6). Biosorbents were then centrifuged at 3000g to remove the majority of the EPS (6). The biosorbents are denoted as bs6, bs7, and bs8, BioMnOx in the biosorbents denoted as BMnO6, BMnO7, and BMnO8, and biomaterial in the biosorbents denoted as biom6, biom7 and biom8 for pH 6, 7, and 8, respectively. Prior to Ni(II) sorption, the biosorbents were washed four times in 10 mM HEPES buffer (pH 7) to remove residual ions. Dissolved Ca2+ in the biosorbent stock suspensions was analyzed by inductively coupled plasma atomic emission spectrometry (ICP-AES) and was less than 0.05 mM. The BioMnOx concentration in the biosorbent stock suspensions was colorimetrically measured after dissolving Mn-oxides with NH2OH · HCl (19). Harvested biomaterial, without Mn(II) addition, was also used to study Ni(II) sorption. EPS was not 10.1021/es9037066 2010 American Chemical Society Published on Web 05/14/2010 FIGURE 1. Sorption isotherms (Figure 1a) and linear Langmuir plots (Figure 1b) of Ni(II) sorption at pH 7 in 50 mM NaNO3 solution on biosorbents preformed at pH 6 (bs6), 7 (bs7), and 8 (bs8), and dissolved Ca2+ and Mn(II) at sorption equilibrium (Figure 1c). The sorption densities are normalized by dry-weight concentration of the biosorbents. The samples (a, b, c) circled in Figure 1a are subject to XAFS and XRD analyses. separated from the bacterial cells prior to sorption experiments. The dry-weight concentrations of the biosorbent and biomaterial stock suspensions were measured and used to normalize Ni(II) sorption capacities. Ni(II) Sorption Isotherms. Ni(II) sorption isotherms were determined at pH 7 with 10 mL total reaction volume in 15 mL polypropylene centrifuge tubes. Biosorbent stock suspensions were added to achieve final [Mntot] as 0.5 mM; the biosorbent dry-weight concentrations were 1.20, 1.33, and 1.55 g L-1, respectively, for bs6, bs7, and bs8. Sodium azide (1.5 mM) was added to inhibit potential physiological and oxidizing activities of P. putida GB-1 (20). The background electrolyte contained 50 mM NaNO3 and 10 mM HEPES. The buffer was used to prevent possible structural modifications of BioMnOx during pH adjustment (6, 21). An aliquot of Ni(NO3)2 stock solution (9.48 mM) was added to achieve initial Ni(II) concentrations ranging from 0.048 to 0.479 mM. For samples with high Ni(II) initial concentrations, the Ni(II) stock solution was added incrementally to prevent possible bulk precipitation. All experiments were performed in triplicate. The suspensions were shaken at 120 rpm on an orbital shaker at room temperature (∼23 °C) for 36 h. The pH values were adjusted twice using 1 M NaOH prior to stabilization. At the end of the reaction, final pH values were measured to be 7.05 ( 0.04. The same procedure used in the Ni(II) sorption on biosorbents studies was used for Ni(II) sorption on the biomaterial study which is denoted as Ni-biom. The Ni(II)-sorbed biosorbents and biomaterial were collected by centrifugation and stored at -80 °C prior to further analyses. The supernatants were filtered with 0.22 µm cellulose filters, and the filtrates acidified with 5% HNO3 for Ni(II) and Ca2+ analyses using ICP-AES. Dissolved Mn(II) and Ni(II) from experiments with low initial Ni(II) were remeasured by inductively coupled plasma mass spectrometry (ICP-MS). Molecular-Scale Measurements. Ni(II) Sorption Reference Materials. A Ni(II) sorption standard (NiTr) on triclinic birnessite (TcBir), that is, Na-birnessite, was made by reacting 1 mM Ni(II) with 1 g/L TcBir in 0.1 M NaNO3 at pH 7. A Ni(II) sorption standard on δ-MnO2 (NiMnO2) was prepared by reacting 1 mM Ni(II) with 2 g/L δ-MnO2 in 0.1 M NaNO3 at pH 4. Synthesis of TcBir and δ-MnO2 were previously described in Zhu et al. (6). EXAFS spectra of a marine nodule (FeMn5DSRB) with Ni(II) incorporated into the Mn octahedral layers was provided by Prof. Sherman at the University of Bristol, UK (3). A Ni(II)-acetate (1:4) solution was prepared by mixing 0.2 M Ni(NO3)2 with 0.8 M NaAc at pH 6. Two Ni(II)-phytate (1:2 and 1:4) solutions were made by adding 0.1 M Ni(NO3)2 to 0.2 and 0.4 M sodium phytate at pH 4, respectively. Preparation of other references used in this study, such as a Ni(II) histidine solution and a Ni(II) aqueous solution, are described in McNear et al. (22). The Ni(II) histidine solution was used to represent Ni(II) bound to imidazole groups. Ni EXAFS Spectroscopy. Ni K-edge EXAFS spectra were collected from Ni(II) sorption samples in fluorescence mode with a Lytle detector on beamline X11A at the National Synchrotron Light Source (NSLS), Upton, NY. The beamline was equipped with a Si (111) monochoromator. EXAFS spectra of Ni(II) sorption standards were collected in fluorescence mode with a 30-element Ge detector on beam line 11-2 equipped with a Si (220) monochoromator, at the Stanford Synchrotron Radiation Lightsource (SSRL), Menlo Park, CA. EXAFS spectra from Ni(II) organic standards were collected in transmission mode at the NSLS. The samples were transferred to plastic holders sealed with Mylar films on both sides for the measurement. EXAFS spectra of a Ni(II) metal foil (E0 ) 8333.0 eV) were collected concurrently with samples for internal energy calibration. A 3 µm cobalt filter was placed between the Lytle detector and samples to reduce elastic and Compton scattering by samples. EXAFS spectra reduction, shell-by-shell fitting and linear combination fitting (LCF) were performed with SIXPack (23). Theoretical phase shift and amplitude files for EXAFS shell-by-shell fitting were created by FEFF 8.02 from an atomic cluster with a hydrated Ni(II) octahedral complex adsorbed at a birnessite vacant site (10). The amplitude reduction factor (S02), 0.94, was derived by fitting the first oxygen shell (CN ) 6, fixed) of a Ni(NO3)2 solution and was used for all of the other shellby-shell fitting. X-ray Diffraction. Synchrotron-based wide-angle X-ray diffraction (XRD) patterns were collected from unreacted VOL. 44, NO. 12, 2010 / ENVIRONMENTAL SCIENCE & TECHNOLOGY 9 4473 TABLE 1. EXAFS Shell-by-Shell Fitting of Ni(II) Sorption Samples and Standardsa R Red χ2 shell CN distance(Å) σ2(Å2) ∆E(eV) 0.0088 66.34 Ni-O Ni-Mn Ni-Mn 6.7(0.7) 2b 6b 2.05(0.01) 3.08(0.02) 3.48(0.02) 0.007(0.001) 0.006(0.003) 0.010(0.003) -1.99(1.34) -1.99(1.34) -1.99(1.34) 0.0104 77.88 Ni-O Ni-Mn Ni-Mn 6.6(0.7) 2b 2b 2.05(0.01) 3.06(0.02) 3.48(0.02) 0.007(0.001) 0.000(0.005) 0.004(0.001) -2.01(1.44) -2.01(1.44) -2.01(1.44) NiMnO2 0.0194 28.51 Ni-O Ni-Mn Ni-Mn 5.9(0.5) 7.0(1.0) 8.8(5.4) 2.05(0.01) 3.49(0.01) 5.45(0.02) 0.006(0.001) 0.009(0.001) 0.010(0.001) 3.32(0.87) 3.32(0.87) 3.32(0.87) bs6a 0.0163 25.69 Ni-O Ni-Mn 5.6(0.7) 4.6(2.0) 2.08(0.01) 3.51(0.02) 0.007(0.001) 0.012(0.004) 5.56(1.38) 5.56(1.38) bs6b 0.0076 18.05 Ni-O Ni-Mn 5.9(0.5) 4.3(1.4) 2.07(0.01) 3.50(0.01) 0.007(0.001) 0.011(0.003) 4.14(0.97) 4.14(0.97) bs6c 0.0088 35.88 Ni-O Ni-Mn 6.1(0.5) 3.2(1.2) 2.07(0.01) 3.50(0.01) 0.007(0.001) 0.009(0.003) 3.72(1.09) 3.72(1.09) bs7a 0.0175 21.65 Ni-O Ni-Mn 5.7(0.7) 3.9(2.1) 2.06(0.01) 3.49(0.02) 0.007(0.001) 0.012(0.005) 2.71(1.52) 2.71(1.52) bs7b 0.0112 45.86 Ni-O Ni-Mn 5.8(0.6) 3.3(1.3) 2.06(0.01) 3.50(0.01) 0.007(0.001) 0.010(0.003) 3.72(1.19) 3.72(1.19) bs7c 0.0128 54.42 Ni-O Ni-Mn 5.7(0.6) 3.2(1.8) 2.06(0.01) 3.50(0.02) 0.006(0.001) 0.011(0.005) 2.89(1.35) 2.89(1.35) bs8a 0.0097 15.12 Ni-O Ni-Mn 5.6(0.5) 5.1(1.3) 2.07(0.007) 3.51(0.01) 0.006(0.001) 0.009(0.002) 4.59(1.06) 4.59(1.06) bs8b 0.0149 154.14 Ni-O c Ni-O Ni-Mn 4.3(1.5) 2.4(1.0) 3.2(2.3) 2.04(0.03) 2.17(0.05) 3.52(0.03) 0.002(0.003) 0.002(0.003) 0.010(0.006) 5.40(2.76) 5.40(2.76) 5.40(2.76) bs8c 0.0084 11.59 Ni-O Ni-Mn 6.0(0.5) 3.3(1.6) 2.07(0.01) 3.50(0.02) 0.007(0.001) 0.012(0.004) 3.71(1.04) 3.71(1.04) samples NiTr a Errors are in parentheses. Only O and Mn shells are considered in the fitting without including scattering paths from organic functional groups. The denotations of bs6a, bs6b, bs6c represent the three samples in pH 6 series (bs6), labeled in Figure 1a, for XAFS analyses. Notations for bs7 and bs8 are in the same way as bs6. These notations are applicable in other Tables and Figures. b Fixed during the fitting. c An additional O shell must be used to get a good fitting. and Ni(II)-sorbed wet biosorbents in transmission mode with an image plate on beam line 11-3 at SSRL. This method is described in detail in Zhu et al. (6). Results Sorption Isotherms and Dissolved Mn(II)/Ca2+. The maximum Ni(II) sorption capacity of the biosorbents decreases as biosorbent formation pH increases (Figure 1a). Negligible amounts of dissolved Mn(II) are observed in the system, except for the first two sorption data points on bs7 which is likely due to contamination during the Ni sorption experiment (Figure 1c). However, upon formation, the biosorbents do contain Mn(II), which decreases as the BioMnOx formation pH increases (6). The reason for the absence of Mn(II) is not clear. It may be due to the washing procedure which could desorb Mn(II) from the biomaterials and/or BioMnOx (11). The dissolved Ca2+ concentration increases as biosorbent formation pH increases (Figure 1c), implying that the biosorbents formed at a higher pH retain more Ca2+ during their formation. Increased Ni(II) loadings also increase the dissolved Ca2+ concentration, particularly for bs8. Since the dissolved Ca2+ concentration is high, even at low Ni(II) loadings, the majority of the dissolved Ca2+ is not caused by Ni(II) sorption but by cation exchange with Na+ (∼60 mM) in the background electrolyte. 4474 9 ENVIRONMENTAL SCIENCE & TECHNOLOGY / VOL. 44, NO. 12, 2010 X-ray Diffraction of Biosorbents. The presence of single (31/02) reflections (Supporting Information S1) demonstrate that all of the reacted BioMnOx are of hexagonal layer symmetry (5, 24). The washing procedure changes the layer structure of the unreacted BMnO8 from orthogonal layer symmetry (splitting of 31/02 reflection) to hexagonal layer symmetry (Supporting Information S1). This change results from layer Mn(III) migration out of the Mn octahedral layers and is likely caused by H+/Na+ exchange with Ca2+ during the washing steps (6, 21). Na+ may not be able to prevent migration of layer Mn(III) as well as Ca2+ due to its weaker sorption affinity (6). The (31/02) and (20/11) peaks broaden for the unreacted BioMnOx as the BioMnOx formation pH increases from 6 to 8 (Supporting Information S1), suggesting different layer structure, as characterized in the companion paper (6). Ni EXAFS Spectroscopy. Two Mn shells at Ni-Mn distances of ∼3.08 and ∼3.48 Å are derived from NiTr spectra fitting (Table 1 and Figure 2), which are attributed to Ni(II) sorption (∼3.08 Å) at edge sites (TE) (10) and Ni(II) sorption at vacant sites (TC) or at edge sites (DC) (∼3.48 Å). The contributions of each of these shells are 0.53 ( 0.21 for TC and 0.47 ( 0.21 for TE and were determined by fixing the Mn coordination numbers (CNs) at 6 and 2, respectively (Table 1). When the Mn CNs are fixed at 2, representing both TE FIGURE 2. Shell-by-shell fitting of Ni(II) k-edge EXAFS spectra and radial structural functions (RSF) over a k range of 3-11 Å-1. Dotted lines and solid lines represent data and fitting, respectively. EXAFS of Ni-his, Ni-ace, and Ni-biom are not fitted. EXAFS fitting results for FeMn5SRDB can be found in Peacock and Sherman (10). The RSF peaks of Ni incorporation in Mn layers (IN), Ni tridentate sorption at edge sites (TE), and Ni triple-corner sorption at vacant sites (TC) are labeled. and DC modes, the fits result in unreasonably small Debye-Waller factors (σ2) (0.000 for TE and 0.004 for DC) although other parameters are similar (Table 1). Therefore, it is likely that the Mn shell at ∼3.48 Å is derived from a TC species. Peacock and Sherman (10) found that Ni(II) TE species exist only at edge sites of triclinic birnessite at pH 7. The presence of Ni(II) TC species on TcBir in this study suggests that our TcBir sample contains some vacant sites. For δ-MnO2, the high CN, ∼7.0, of the Mn shell at ∼3.49 Å (Table 2) and, ∼8.8, of the Mn shell at ∼5.45 Å indicate Ni TC adsorption at vacant sites rather than DC adsorption at edge sites (2). This is further confirmed by a two Mn-shell fitting of NiMnO2 spectra with CNs fixed at 2 and 6, representing DC and TC species (data not shown), and resulting in an unreasonable contribution factor (1.35) for TC. A higher Ni(II) loading on δ-MnO2 (10 mM Ni(II) with 2 g/L δ-MnO2) decreases the second shell amplitude in R space (data not shown), likely due to the Ni(II) DC sorption at edge sites (2). EXAFS fitting reveals a single Ni-Mn distance at 3.49 3.52 Å for Ni(II) sorption on the biosorbents (Table 1). Other atomic shells, such as carbon, nitrogen, etc., from biomaterials are not considered in the fitting. Inclusion of additional Mn shells in the fitting does not improve fitting results, indicating that Ni is neither present as TE sorption complexes nor incorporated into vacant sites of BioMnOx. The relatively high CNs of the Mn shell indicate TC rather than DC adsorption (Table 1). The results also demonstrate that the CNs of the Mn shell decrease with Ni(II) loadings (Table 1). LCF Analysis of Ni(II)-biomaterial. The EXAFS of the Nibiom was fit using linear combinations of Ni(II) reference compounds (Table 2 and Figure 3). Fitting the data with Ni-acetate and Ni-phytate (1:2 or 1:4) does not result in a satisfactory representation of the Ni-biom EXAFS spectra (Table 2 and Figure 3). Addition of Ni-his to the LCF analysis (Table 2 and Figure 3) improves the fitting accuracy, particularly in the k-range of 3.0-6.5 Å-1, and reduces Red χ2 from 0.162 to 0.099, whereas the inclusion of Ni-glycine leads to a Red χ2 of 0.138 (not shown). Fitting of the spectra without Ni-phytate (i.e., with Ni-ace and Ni-his only) does not reduce the fitting accuracy (Table 2 and Figure 3), indicating the phosphoryl group is not a necessary functional group to describe Ni binding in this biomaterial. Adding Niaqueous to the standards used in fitting does not further improve the accuracy of the LCF analysis (Table 2), indicating that Ni(II) is bound to the biomaterial in an inner-sphere fashion. The best fit of the unknown spectra, with the least number of components, is obtained from a combination of Ni-ace (f ) 0.635) and Ni-his (f ) 0.379) only (Table 2 and Figure 3). Both histidine and glycine are amino acids containing the NH2-CHR-CO2 molecular fragment. However, histidine TABLE 2. EXAFS Linear Combination Fitting of Ni(II) Sorbed on the Biomaterial (Ni-biom) and Biosorbents (from bs6a to bs8c) with Sorption Standards: Ni(II) Sorbed on δ-MnO2 (NiMnO2), Ni(II) Acetate Solution (Ni-ace), Ni(II) Histidine Solution (Ni-his), Ni(NO3)2 Solution (Ni-aqu) and Ni Phytate (Ni-phy) Solution. Errors Are Shown in Parentheses Ni-aqu Ni-ace Ni-phy(1:2)a Ni-his 0.984 (0.011) 0.300 (0.100) 0.635 (0.028) Ni-biom 0.074 (0.037) 0.030 (0.037) Ni-his bs6a bs6b bs6c bs7a bs7b bs7c bs8a bs8b bs8c 0.448 0.259 0.261 0.298 0.265 0.193 0.350 0.153 0.250 (0.044) (0.034) (0.026) (0.038) (0.028) (0.029) (0.026) (0.030) (0.031) 0.448 (0.082) 0.575 (0.041) 0.417 (0.060) Ni-ace 0.134 0.326 0.378 0.326 0.359 0.508 (0.038) (0.029) (0.023) (0.032) (0.024) (0.025) 0.503 (0.025) 0.508 (0.027) 0.949 (0.010) 0.661 (0.099) 0.379 0.306 0.339 0.354 0.323 0.675 (0.033) 0.216 (0.089) 0.227 (0.065) Ni-biomb 0.582 0.585 0.639 0.624 0.624 0.701 0.350 0.656 0.758 (0.082) (0.063) (0.049) (0.070) (0.052) (0.054) (0.026) (0.055) (0.058) (0.030) (0.036) (0.033) (0.032) (0.319) NiMnO2 0.376 0.409 0.369 0.339 0.366 0.297 0.626 0.333 0.266 a Ni-phytate (1:4) is not as good as Ni-phytate (1:2) in the LCF and is not used. represent total Ni(II) bound to the biomaterials in the biosorbents. b (0.016) (0.013) (0.010) (0.014) (0.010) (0.011) (0.019) (0.011) (0.012) Red χ2 sum 0.206 0.170 0.162 0.102 0.117 0.099 0.100 0.093 0.984 0.949 0.961 1.01 0.981 1.00 1.00 0.996 Red χ2 sum 0.180 0.109 0.064 0.132 0.075 0.080 0.261 0.081 0.092 0.958 0.993 1.01 0.963 0.990 0.998 0.977 0.990 1.02 Sum of Ni-ace and Ni-his fractions to VOL. 44, NO. 12, 2010 / ENVIRONMENTAL SCIENCE & TECHNOLOGY 9 4475 FIGURE 3. Linear combination fitting of Ni-biom and Ni-biosorbent EXAFS spectra. Ni-biom is fitted with Ni(II) organic complexes: a, acetate + phytate; b, acetate + histidine; c, phytate + histidine; d, acetate + phytate + histidine; e, acetate + phytate + histidine + aqueous. Ni-biosorbents are fitted with Ni-his, Ni-ace and NiMnO2. The labels correspond to Table 2. The experimental data of the Ni-biom were plotted in red for a better comparison with fitting results. has much better fitting accuracy than glycine in the LCF analysis of Ni(II) sorption on the biomaterial. The probable reason is that histidine possesses an imidazole group which has high complexation affinity to heavy metals (26, 27). This suggests that the imidazole group is involved in the Ni(II) binding to the biomaterial. In this study, Ni(II) can bind to cell surfaces, EPS and/or even inside of the cells because P. Putida can uptake Ni(II) (28). LCF Analysis of Ni(II)-Biosorbents. LCF analysis using Niace, Ni-his and NiMnO2 were performed on Ni(II) sorption samples to evaluate the relative contributions of Ni(II) bound to carboxyl groups, imidazole groups, and vacant sites, respectively (Table 2 and Figure 3). Inclusion of Ni-aqu, Niphy, NiTr, and FeMn5SRDB does not improve the fitting accuracies. Good LCF fitting accuracies (Table 2 and Figure 3) with NiMnO2 further confirms that Ni(II) sorption occurs at vacant sites of BioMnOx. Our study does not reveal Ni(II) DC sorption at edge sites of BioMnOx, even at relatively high Ni(II) loadings. The Ni(II) sorption loadings on BioMnOx, histidine, and carboxyl groups are individually calculated based on LCF fractions (Table 2) and are nonlinear square fitted with the Langmuir adsorption equation (Figure 4 and Table 3). The maximum Ni(II) sorption capacity (qmax) of BioMnOx decreases as the BioMnOx formation pH increases, but the sorption affinity (k) dramatically increases on the BioMnOx formed at pH 8 (Table 3). Compared to Ni-his, Ni-ace exhibits a higher maximum sorption capacity, that is, a higher site density of the carboxyl group, but a lower Ni(II) sorption affinity (Table 3). As Ni(II) loading increases, Ni sorption densities on biomaterials continue to increase; however, Ni sorption densities on BioMnOx become constant for BMnO7 and BMnO8 (Figure 4a), suggesting sorption saturation. This results in smaller molar fractions of Ni bound to BioMnOx and subsequently causes the obtained CNs of the Mn-shell in the EXAFS shell-by-shell fitting to decrease as Ni loadings increase (Table 1). Mass Balance of Ca2+ and Ni(II). Since Ni(II) sorption on BioMnOx reaches a plateau on BMnO8 (Figure 4a), the increase in dissolved Ca2+ concentration is likely caused by Ni(II) sorption on the biomaterial. Ca2+ mass balance calculations demonstrate that the increased [Ca2+] of 0.047 (from 0.218 to 0.265) mol kg-1 biosorbent (Figure 1c) is close to the corresponding increase of 0.050 (from 0.098 to 0.148) mol Ni kg-1 biomaterial on the biom8 (Figure 4a). Using the same argument, it can be concluded from Figure 4b that most of the Ca2+ replaced by Ni sorption is initially bound to carboxyl sites rather than histidine, consistent with the view that the tightly bound Ca2+ can be attributed to strong binding to carboxyl groups (29). At low Ni loadings, the slight increase in [Ca2+], 0.015 (from 0.203 to 0.218) mol kg-1 biosorbent (Figure 1c) only accounts for a small portion of the corresponding Ni(II) sorption on bs8 (0.093 from 0.060 to 0.153 mol kg-1 biosorbent) (Figure 1a), which also occurs for all data points for bs6 and bs7. This indicates that most of the Ni(II) initially sorbs onto sites not occupied by Ca2+ before the BioMnOx is saturated by Ni(II). Consequently, Ca2+ does not substantially compete with Ni(II) for sorption on BioMnOx under the conditions of this study. Discussion In addition to BioMnOx, the biosorbents also contain bacterial cells and EPS. Nevertheless, these biomaterials are unlikely to alter the intrinsic reactivity of the negatively charged BioMnOx (30). The data also show that neither Ca2+ nor interlayer Mn are in substantial competition with Ni(II) for sorption on BioMnOx. Thus, the observed Ni(II) sorption FIGURE 4. Ni(II) sorption isotherms on BioMnOx (BMnO6, 7 and 8) and biomaterials (biom 6, 7, and 8) (a), and histidine and acetate (b). The sorption densities are calculated based on component molar fractions of EXAFS linear combination fittings. 4476 9 ENVIRONMENTAL SCIENCE & TECHNOLOGY / VOL. 44, NO. 12, 2010 TABLE 3. Langmuir Parameters Obtained from Least Square Fittings for Ni(II) Sorption Isotherms for Each Sorbent Component qmaxa kb R2 c qmaxa Ni-biomaterial bs6 bs7 bs8 0.183 0.185 0.188 36.0 27.6 20.7 a 0.066 0.049 0.040 103.2 86.4 123.4 Maximum sorption loading. b 0.993 0.995 0.999 c fvacd 0.232 0.203 0.159 94.5 56.0 618.0 0.841 0.953 0.985 0.104 0.092 0.074 Ni-ace 0.954 0.897 0.696 0.125 0.164 0.130 Sorption affinity parameter. c Fitting goodness. differences among the three BioMnOx are derived from their intrinsic structural characteristics, that is, vacant site and layer Mn(III) content (6). Since Ni(II) sorption on BioMnOx occurs at vacant sites only, the maximum Ni(II) sorption capacities are apparently determined by the vacant site quantity (12). The results also suggest that vacant site occupancies of BioMnOx increase as the formation conditions become more acidic, consistent with our structural study (6). Estimation of Quantities of Vacant Sites. Assuming both sides of all vacant sites are occupied by Ni(II) at maximum sorption loadings (8), the molar fractions of vacant sites are estimated based on the following equations (Table 3), fvac ) R2 NiMnO2 Ni-his bs6 bs7 bs8 kb qmax / 2 qmax / 2 + 1 in which qmax is the maximum sorption loading. All calculated fvac lie within the range of the two end members, ideal hexagonal (fvac ) 0.167) and triclinic birnessite (fvac ) 0) (21). As BioMnOx formation pH increases, the vacant site fraction decreases (Table 3), consistent with the structural characterization of BioMnOx (6). The vacant site content in BioMnOx has been implied based on Zn(II) sorption loadings by a similar methodology (9). This method directly measures contents of vacant sites and is therefore not impaired by particle size effects as compared with EXAFS multiplescattering fitting (24). However, this assumes that metals are sorbed only at vacant sites rather than other sites (2). Zn(II) may be a better candidate than Ni(II) because Zn has not been found to adsorb at edge sites. Additionally, metal sorption or experimental conditions should not create new vacant sites. Mn(III) Roles. Empirical bond valence calculations showed that Mn(III)-coordinated oxygen atoms encompassing a vacant site are more undersaturated than Mn(IV)coordinated oxygen atoms (8). Consequently, vacant sites surrounded by a mixture of Mn(III) and Mn(IV) could exhibit stronger adsorption affinities for interlayer metal cations than vacant sites surrounded only by Mn(IV). The dramatic change in Ni(II) sorption affinities of the BioMnOx formed at pH 8 could be due to the high fraction of layer Mn(III), as found in the companion paper. The similarity of Ni(II) sorption affinity on the BMnO7 to BMnO6 is probably due to the presence of dissolved Mn(II), which interferes with Ni(II), thereby decreasing apparent Ni(II) sorption affinity on BMnO7. Ni Distribution Between Mn-oxides and Biomaterials. A large fraction of Ni(II) is associated with the biomaterial before BioMnOx is saturated by Ni(II) sorption. However, Zn(II) is not sorbed on P. putida MB-1 biomaterial until the BioMnOx is saturated (9). In the Zn study, BioMnOx is 25 wt.% of the total biosorbents (9), whereas the BioMnOx in the current study is only 2.8-3.6 wt.%. The high portion of 18.8 11.7 20.7 d 0.992 0.991 0.974 Molar fraction of vacant sites. Ni(II) binding to the biomaterials may be due to the high biomaterial content in this study. Additionally, Ni(II) has relatively weak sorption affinity to birnessite compared to other heavy metals, such as Pb(II), Cu(II) and Zn(II) (31), and thus, the high Ni(II) affinity of histidine groups can comparably compete with BioMnOx for binding Ni(II). Furthermore, the different Ni(II) sorption affinity of BioMnOx derived from a different Mn layer structure also affects heavy metal distributions on them. The distribution of heavy metals between the biomaterial and minerals depends on metal sorption affinities and the relative amounts of each component. Environmental Implications. Mn-oxides are major metal sequesters in many geochemical environments, such as the ocean floor, and can affect trace metal cycling. As a dominant environmental Mn-oxide phase, layer Mn-oxides may have a wide range of metal sorption properties, depending on their formation conditions, and can impose different impacts on their surroundings. For instance, Mn-oxides are not stable when redox conditions change in the environment. Once Mn-oxides are reduced and dissolved, the Mn-oxides having more vacant sites can accelerate heavy metal cycling due to their bearing more heavy metals. Even for large tunnel structure of Mn-oxides, such as todorokite (3 × 3 tunnel), vacant sites/Mn(III) may play a similar role in metal sorption because building units of the tunnel structure are also edgesharing Mn octahedral layers (1). Acknowledgments Mengqiang Zhu is grateful for a University of Delaware Institute of Soil and Environmental and Quality (ISEQ) Graduate Fellowship. The research was supported by Delaware EPSCoR with funds from the National Science Foundation Grant EPS-0447610 and the State of Delaware and USDA Grant 2005-35107-16105. Use of the NSLS was supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, under Contract No. DEAC0298CH10886. The beamline X11 is supported by the Office of Naval Research and contributions from Participating Research Team (PRT) members. Portions of this research were carried out at the Stanford Synchrotron Radiation Lightsource, a national user facility operated by Stanford University on behalf of the U.S. Department of Energy, Office of Basic Energy Sciences. The SSRL Structural Molecular Biology Program is supported by the Department of Energy, Office of Biological and Environmental Research, and by the National Institutes of Health, National Center for Research Resources, Biomedical Technology Program. Supporting Information Available X-ray diffraction patterns of biosorbents. This material is available free of charge via the Internet at http://pubs.acs.org. VOL. 44, NO. 12, 2010 / ENVIRONMENTAL SCIENCE & TECHNOLOGY 9 4477 Literature Cited (1) Post, J. E. Manganese oxide minerals: Crystal structures and economic and environmental significance. Proc. Natl. Acad. Sci. U.S.A. 1999, 96, 3447–3454. (2) Manceau, A.; Lanson, M.; Geoffroy, N. 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