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Visualizing Arsenate Reactions and Encapsulation in a Single Zero-Valent Iron Nanoparticle Lan Ling, and Wei-Xian Zhang Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.6b04315 • Publication Date (Web): 12 Jan 2017 Downloaded from http://pubs.acs.org on January 12, 2017
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Visualizing Arsenate Reactions and Encapsulation in a Single Zero-Valent Iron Nanoparticle
Lan Ling and Wei-xian Zhang* State Key Laboratory for Pollution Control School of Environmental Science and Engineering Tongji University 1239 Siping Road Shanghai, China 200092
*To whom correspondence should be addressed. Email:
[email protected], Phone: +8621-15221378401, Fax: +86-21-6598 0041.
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ABSTRACT
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A nanostructure-based mechanism is presented on the enrichment, separation and immobilization
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of arsenic with nanoscale Zero-Valent Iron (nZVI). The As-Fe reactions are studied with
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Spherical Aberration Corrected Scanning Transmission Electron Microscopy (Cs-STEM). Near
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atomic-resolution (99.9%) for 30 minutes prior to
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the experiment. The iron nanoparticles for the STEM analysis were collected from batch reactors
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containing 10 ppm As(V) with pre-determined doses of iron nanoparticles (e.g., 0.2–5 g/L ).
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Batch reactors were sealed with screw caps and mixed on a shaker table at ambient temperature
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(approximately 22 °C). The collected nZVI particles were rinsed twice with high-purity nitrogen
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purged ethanol and stored in a nitrogen-purged sample vial for solid reactions before the STEM
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analysis.
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Methods. Electron microscopy characterizations are performed on a FEI Titan™ G2 80-300,
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which is a STEM (scanning transmission electron microscope) integrated with corrected electron
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optics. The system is equipped with a FEI X-FEG high brightness Schottky field emission source
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(brightness 1.8 × 109 A/cm² srad at 200 kV, beam current 1,300 pA in 0.2 nm spot), a CEOS
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hexapole/transfer doublet design aberration corrector, High-Angle Annular Dark-Field
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(HAADF) and Bright-Field (BF) detectors, an Electron Energy-Loss Spectrometer (EELS)
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(Gatan, UK), Energy Filtered TEM (EFTEM, Quantum SE/963 200 kV) and the FEI
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ChemiSTEM system.19, 20
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3D-ET and XEDS analysis are achieved with the FEI SuperX operated at a beam current of ~0.8
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nA and a probe size of ~0.2 nm at 200 KV. Each spectrum image of 512×512 pixels is acquired
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over a 10 min duration. The tilt series of XEDS images are collected from −64° to +64° with a 2°
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tilt increment. Data processing is achieved using the Inspect3D software (FEI) with a built-in
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algorithm of simultaneous iterative reconstruction technique (SIRT). 3D dataset of segmentation
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is then realized with the Amira software.23
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RESULTS AND DISCUSSION
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nZVI, an engineered nanomaterial has been increasingly used in environmental remediation and
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hazardous waste treatment.13−17, 24−27 For example, numerous reports have documented its
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effectiveness in detoxifying halogenated hydrocarbons in groundwater.28−32 Figure 1 presents
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images of nZVI (more are available in the Supporting Information, Figure S1). A fresh nZVI
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particle is spherical with diameter typically in the range of 20–100 nm. The BF and HAADF
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images (Figure 1a and 1b) provide complementary views of the core-shell structure. As shown in
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the high-resolution TEM images (Figure. 1c and 1d), nZVI has a classical core-shell structure,
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that is, an individual nanoparticle has local or nanoscale crystalline structures, comprises of an
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Fe(0) core and separates from other nanoparticles by a thin (2−5 nm) interfacial layer of iron
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oxides. Short-range lattice arrangements and some defective structures on the shell surface are
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also apparent from the high-resolution TEM micrographs (Figure 1d). The extremely thin
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dimension, disordered and defective nature of the oxide layer offer efficient electron passage and
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high reactivity via tunneling effects and defect channeling. 33 The core-shell structure bestows
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the nanoparticles with the reductive characteristics of Fe(0) and coordinative properties of iron
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oxides, offers a unique and powerful combination for the separation and sequestration of arsenic
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and heavy metal ions.13-17, 21, 22
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Figure 1. STEM images of clean nanoscale zero-valent iron (nZVI). (a) Bright Field (BF); (b)
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High-Angle Annular Dark-Field (HAADF). (c) and (d) are high-resolution TEM images.
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Previous work has showed that nZVI can quickly remove both As(III) and As(V) from water and
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also possess large capacity (>200 mg As/g Fe) for arsenic encapsulation. 16 The reactions of
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arsenate with nZVI can be manifested with the distributions of oxygen, iron and arsenic in spent
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nZVI particles. Figure 2 presents the XEDS elemental mappings of As(Kα), Fe(Kα), O(Kα),
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XEDS line profiles, color overlays and spectra of selected areas acquired from a single nZVI
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nanoparticle reacted with arsenate. The nanoparticles were from a reactor after 48-hour reactions
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with 10 mg/L arsenate. After the reactions, the nZVI nanoparticles is slightly distorted due to
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iron dissolution and precipitation of iron hydroxides (Figure 2a). The Fe mapping (Figure 2b)
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shows footprint of iron with a dense metallic core. From Figure 2d, the ring of oxygen matches
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the lower intensity area of iron, reconfirming that the surface layer is rich in oxygen. The arsenic
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mapping (Figure 2c) on the other hand illustrates a distinctive ring of arsenic just on top of the
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Fe(0) core surface. This ring of arsenic is intense and locates exactly between the Fe(0) core and
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iron oxide shell, resulting from the reduction of As(V) and accumulation of As(0). Previous work
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with XPS showed that arsenic accumulated inside the particle is mostly the reduced As(0) and
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As(III),15, 16 we now prove that arsenic can fully penetrate the surface oxide layer.
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More detailed information on the intraparticle distributions of oxygen, iron and arsenic in a
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reacted nZVI particle is obtained from the XEDS line profiles (Figure 2a, Figure S2). The
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arsenic profiles, peak positions and heights offer valuable information on the rates of
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intraparticle mass transfer and reactions, also on the speciation [i.e., As(V), As(III) and As(0)]
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and total amount of arsenic in the nanoparticle. The iron abundance ascends rapidly within first
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4–5 nm and reaches a plateau at the depth of 8−9 nm under the particle surface. The Fe scan
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shows a sharp valley matching the location of the arsenic ring. The oxygen profile climaxes at
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about 3 nm from the water-nanoparticle interface just outside the Fe(0) core. This is consistent
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with the core-shell model that the outer surface iron is more oxidized with oxygen-rich oxides
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while the inner part is less oxidized with more Fe(II). From XEDS quantifications (Figure 2g-2j
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and Figure S2), the arsenic abundance in this thin layer is estimated at 19.44 wt% and accounts
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for more than half of the arsenic within the whole particle.
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Figure 2. High-resolution STEM-XEDS elemental mappings and XEDS quantifications of
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the Fe-As reactions. (a) HAADF image and XEDS line profiles, (b) Fe, (c) As, (d) O, (e)
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Fe+As, (f) Fe+As+O, (g-i) XEDS quantifications, and (j) XEDS spectra. Signals were collected
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from an iron nanoparticle after 48-hour reactions with 10 mg/L arsenate.
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Figure 3. 3D chemical mapping of spent nanoscale zero-valent iron after reactions with
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arsenate. (a) 3D elemental distributions of Fe (blue), O (green) and As (red). (b-j) are a series of
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mappings acquired from spent nanoscale zero-valent iron reacted with arsenate in the tilt range
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of +64° to -64°. The sample was from a batch reactor containing 10 mg As(V)/L and 0.5 g/L
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nZVI after 48 hours. A corresponding video of the 3D tomography can be found in the
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Supporting Information (Movie S1).
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The nano-structure based encapsulation can be visualized via electron tomography, which can
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generate high-resolution 3D view of pollutant distribution in a single nanoparticle. To achieve
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3D visualization, a series of projection (2D) images of a single nanoparticle are acquired from a
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wide range of angles by tilting the sample relative to the probe. A full 3D visualization is then
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established using a cross-correlation algorithm for image shift, tilt alignments and simultaneous
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iterative reconstruction (FEI Inspect3DTM, details are provided in Supporting Information). 34-39
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A video of 3D electron tomography showing arsenic in a single nZVI nanoparticle is provided in
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the Supporting Information (Movie S1). Figure 3 presents a series of projection images from
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selected angles. The XEDS tilt series and the resulting 3D tomography (Movie S1) discover a
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distinct feature of the As-nZVI reactions, that is, a thin and continuous layer of arsenic (in red
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color, ~23 Å in thickness, Figure 3) is deposited beneath the iron oxide surface layer and just on
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top of the Fe(0) core after 48-hour reactions with 10 mg/L As(V) (Na2HAsO4). The distribution
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sphere of arsenic is larger than that of the iron core but smaller than the distribution ring of
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oxygen. This technique generates extraordinary details and insights unattainable from
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conventional 2D XEDS scans as the state-of-the-art Cs-STEM can obtain atomic resolution
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structural imaging as well as high-resolution (~ 1 nm3) 3D elemental mapping. Although
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previous work has suggested that arsenic can be reduced and immobilized by zero-valent iron,
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this work, for the first time visualizes the formation of a continuous layer of arsenic within nZVI
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nanoparticles. This clearly points to a large capacity and stability of nZVI for arsenic
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encapsulation.
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In direct contrast, configurations of the XEDS mapping and electron tomography on the
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arsenate-ferric hydroxide (FeOOH) reactions (Figure 4 and 5) show that the arsenate is attracted
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rather loosely to the surface, that is, the arsenic atoms are to a large degree detached from the
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surface. The cyan color in Figure 4 and 5 reflects the nature of blue (iron) (Figure 4a) and green
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(oxygen) (Figure 4b) mixtures, suggesting that the particle body consists of Fe and O with As
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floating on top and/or near the surface. There is no intraparticle diffusion or accumulation of
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arsenic inside the oxide nanoparticle. The atomic ratios of oxygen, iron and arsenic from XEDS
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Figure 4. High-resolution STEM-XEDS elemental mappings and XEDS line profiles of
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ferric hydroxide (FeOOH)-arsenate reactions. (a) Fe, (b) O, (c) As, (d) Fe+As+O, (e)
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HAADF image, (f) XEDS line profiles (quantifications and spectra are provided in Supporting
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Information, Figure S3). The sample was from a batch reactor with 10 mg/L As(V) and 0.5 g/L
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Fe. Reaction time was 48 hrs.
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quantification implies no arsenate reduction (Figure S3).11, 40 XEDS quantitative analysis shows
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that weight percentage of arsenic is in the range of 2.48% to 2.97% on the FeOOH surface and
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average 1.75% for the whole particle. Furthermore, arsenic distributes unevenly on the FeOOH
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surface as shown in the 3D tomography (Movie S2 and Figure S3). The 3D tomography thus
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Figure 5. 3D chemical mapping on arsenate-goethite (FeOOH) reactions. (a) 3D elemental
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distribution of Fe (blue), O (green) and As (red). (b-j) are a series of mappings acquired from
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spent FeOOH reacted with arsenate in the tilt range of +64° to -64°. The sample was from a
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batch reactor with 10 mg As(V)/L and 0.5 g/L Fe after 48 hours. A corresponding video of the 3D
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tomography is provided in the Supporting Information (Movie S2).
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provides direct confirmation of a widely held postulation that arsenic is attracted to the goethite
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surface by forming surface complexes.11, 40 It further confirms that arsenic covering on the oxide
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surface is far from continuous and the amount of arsenic on iron hydroxide (FeOOH) is much
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less than the continuous layer of arsenic in nZVI.
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The observed pattern of arsenic in the nZVI nanoparticle reflects the net result of the arsenic
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diffusion and reactions within the unique nanostructure. As presented earlier, nZVI consists of
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two nanomaterials. The core is zero-valent or metallic iron, which serves as a reductant for
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arsenite and arsenate reduction. The surface layer of iron oxides is formed from spontaneous
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oxidation of Fe(0) and can be represented with an average stoichiometry of iron hydroxide
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(FeOOH).15,16 Furthermore, the nZVI shell consists of a mixed Fe(II)/Fe(III) phase close to the
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Fe(0) interface and a predominantly Fe(III) at the outer surface of nZVI, resulting in a clear
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phase junction. Thus nZVI possesses the combinatorial properties of zero-valent iron and iron
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oxides. The iron oxide layer is polar and/or charged in water, offers electrostatic attractions and
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sorption sites to both cations and anions in water while the core supplies electrons or the
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reducing capability for further diffusion, reduction and deposition of arsenic and heavy metals
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such as Ni and Cu. The intraparticle diffusion of arsenic is highly favored since the core region
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has the highest concentration of Fe(0) for the arsenic reduction and immobilization. The grain
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boundary provides additional support to the observed arsenic diffusion in nZVI particle, that is,
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arsenic atoms diffuse preferably along the defective, high energy, and non-equilibrium
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polycrystalline grain boundary of iron oxides 41,
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patterns presented in Figure 2 and 3 are also consistent fully with results from previous XPS
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characterizations.15, 16
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Atomic-resolution STEM images of nZVI and a conceptual model on the sorption, precipitation
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and reduction of arsenic by nZVI are illustrated in Figure 6. As shown in Figure 6a and 6b, the
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reacted nZVI particle retains the classical core-shell structure. Furthermore, short-range lattice
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arrangements in the shell area are also apparent from the high-resolution STEM micrographs
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with individual iron atoms clearly identified under the HAADF model. nZVI formed from
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The iron, arsenic and oxygen distribution
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sodium borohydride reduction of ferric chloride has a body-centered cubic structure (bcc) in the
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space group Oh9
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orientation in unprocessed HAADF image. Higher magnification image (inset in Figure 6a)
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provides further evidence that a dense core displayed along (111) zone axis. The bright columns
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are the iron atoms and show subtle details about the shape and faceting of the nanocrystals. The
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intensity line profile (in red color, Figure 6a) measured across the periodical arrangements
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clearly signals individual atoms (highlighted with the blue circles). A HAADF intensity peak
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matches precisely to an atomic column. This is further evidenced by the corresponding electron
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diffraction patterns.
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The high-resolution STEM images of nZVI provide remarkable details on the atomic
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arrangements within the core-shell structure and complement previous work of XPS and EXAFS. 15,
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16
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of iron structure model in the (111) lattice plane with the lattice constant a of 2.405 Å. The
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interatomic spacing along this direction is measured at 1.70 Å, in good agreement with the
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calculated interatomic spacing along direction, that is,
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XEDS, this surface layer is enriched with arsenic as a result of the reductive deposition. The
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observed difference of peak intensity is likely caused by the substitution or replacement of iron
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for the arsenic atoms. 43, 44
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As shown in the conceptual model (Figure 6c), formation of the thin layer of arsenic between the
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Fe(0) core and iron oxide shell offers the most direct evidence on the nano-encapsulation and
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proves that the outer layer, especially the Fe(0)/oxide interface is the frontline for the As-Fe
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reactions. Evidence obtained in this work has important implications on applications of iron
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nanoparticles for arsenic separation and immobilization. The total capacity of nZVI for arsenic
15, 33
Figure 6a shows the structure of spent nZVI predominantly along (111)
In the Annular Dark Field (ADF) image (Figure 6b), the seven red points illustrate a unit-cell
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√
=1.70 Å. As observed from
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removal is the sum of surface sorption and immobilization by the Fe(0) reduction. Since the
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driving force for arsenic diffusion in nZVI is chemical reduction and successive encapsulation,
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the chemical reduction of arsenic is much greater than that of the surface sorption with capacity
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for arsenic immobilization governed primarily by and proportional to the amount of Fe(0).
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Laboratory batch experiments have confirmed that arsenic removal capacity can reach as high as
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200 mg As/g Fe.15,16
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Figure 6. Atomic-resolution STEM images of spent nanoscale zero-valent iron (nZVI) and
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a conceptual model on arsenate-nZVI reactions. (a) Unprocessed High-angle Annular Dark-
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field (HAADF) image of a portion of a nanoparticle, inset is a higher-magnification view of the
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core area. The HAADF intensity line profile (in red color) measured across the periodical
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arrangements signals individual atoms (highlighted with the solid blue circles). (b) Annular
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Dark-Field (ADF) image shows that Fe atoms in the core area are predominantly in the body-
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centered cubic (111) lattice plane. (c) A conceptual model on the sorption, precipitation and
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reduction of toxic metals with nZVI.
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Additionally, the reduced arsenic, As(0) is very stable in the presence of Fe(0). This is critical for
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the immobilization and stabilization of toxic heavy metals such as mercury, arsenic, and
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radioactive materials.22 Our laboratory experiments showed the nZVI-bound arsenic is much less
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sensitive to solution pH changes. For example, optimal pH for arsenic sorption to iron oxides is
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less than 4 with little sorption observed above pH 8. With nZVI, high efficiency (>90%) can be
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maintained over a wide range of solution pH (~3−10) (Figure S4). The presence of Fe(0) thus
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serves as an enduring shield or long-term stabilizer, which inhibits oxidation, dissolution and
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leaching of pollutants.
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Reactions with solid surfaces are the principal mechanisms controlling speciation, distribution,
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transformation, bioavailability, ultimate fate and toxicity of environmental contaminants, thus
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are fundamental in environmental, geological and colloidal chemistry.
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knowledge on the surface reactions of most environmental contaminants is still limited, largely
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impeded by the lack of effective tools for direct and in situ observations. We demonstrate that for
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the first time, reactions of arsenic with iron nanoparticles can be “seen” via high-resolution 3D
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electron tomography at near atomic resolution. This technique offers new opportunities in the
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investigation of pollutant transformation and detoxification by generating simultaneous high-
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resolution structural characterization and high-accuracy identification and quantification of
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contaminants in the solid phase. 34, 35 With further improvements and refinements, this technique
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will undoubtedly expand our understanding on the intraparticle mass transfer, catalysis,
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transformation and detoxification of environmental toxins in the heterogeneous environmental
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media.
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ASSOCIATED CONTENT
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45, 46
Nevertheless, our
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Supporting Information
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Supporting Information is available free of charge via the Internet at http://pubs.acs.org.
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Movies S1-S2, Figures S1-S4, and more experimental details are available in the Supporting
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Information.
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ACKNOWLEDGEMENTS
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Financial support from the National Natural Science Foundation of China (NSFC Grants
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21307094, 21277102 and 21677107), the Collaborative Innovation Center for Regional
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Environmental Quality and the State Key Laboratory for Pollution Control and Resource Reuse
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are acknowledged.
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AUTHOR INFORMATION
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Corresponding author
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Email:
[email protected], Phone: +86-21-15221378401, Fax: +86-21-6598 0041.
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Notes
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The authors declare no competing financial interests.
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REFERENCES
288
1. Geen van, A.; Bostick, B. C.; Trang, P. T. K.; Lan, V. M.; Mai, N. N.; Manh, P. D.; Viet, P. H.;
289
Radloff, K.; Aziz, Z.; Mey, J. L.; Stahl, M. O.; Harvey, C. F.; Oates, P.; Weinman, B.; Stengel,
290
C.; Frei, F.; Kipfer, R.; Berg, M. Retardation of arsenic transport through a Pleistocene aquifer.
291
Nature 2013, 501, 204–208.
292
2. Fendorf, S.; Michael, H. A.; Geen van, A. Spatial and temporal variations of groundwater
293
arsenic in South and Southeast Asia. Science 2010, 328, 1123–1127.
ACS Paragon Plus Environment
19
Environmental Science & Technology
Page 20 of 25
294
3. Nickson1, R.; McArthur, J.; Burgess, W.; Ahmed, K. M.; Ravenscroft, P.; Rahmanñ, M.
295
Arsenic poisoning of Bangladesh ground water. Nature 1998, 395, 338.
296
4. Rodríguez-Lado, L.; Sun, G.; Berg, M.; Zhang, Q.; Xue, H.; Zheng, Q.; Johnson, C. A.
297
Groundwater arsenic contamination throughout China. Science 2013, 341, 866–868.
298
5. Radloff, K. A.; Zheng, Y.; Michael, H. A.; Stute, M.; Bostick, B. C.; Mihajlov, I.; Bounds, M.;
299
Huq, M. R.; Choudhury, I.; Rahman, M. W.; Schlosser, P.; Ahmed, K. M.; Geen van A. Arsenic
300
migration to deep groundwater in Bangladesh influenced by adsorption and water demand.
301
Nature Geosci. 2011, 4, 793–798.
302
6. Stuckey, J. W.; Schaefer, M. V.; Kocar, B. D.; Benner, S. G.; Fendorf, S. Arsenic release
303
metabolically limited to permanently water-saturated soil in Mekong Delta. Nature Geosci. 2016,
304
9, 70–79.
305
7. Senn, D. B.; Hemond, H. F. Nitrate controls on iron and arsenic in an urban lake. Science 2002,
306
296, 2373−2376.
307
8. Polizzotto, M. L.; Kocar, B. D.; Benner, S. G.; Sampson, M.; Fendorf, S. Near-surface
308
wetland sediments as a source of arsenic release to ground water in Asia. Nature 2008, 454,
309
505−509.
310
9. Yavuz, C. T.; Mayo, J. T.; Yu, W. W.; Prakash, A.; Falkner, J. C.; Yean, S.; Cong, L.;
311
Shipley, H. J.; Kan, A. T.; Tomson, M. B.; Natelson, D.; Colvin, V. L. Low-field magnetic
312
separation of monodisperse Fe3O4 Nanocrystals. Science 2006, 314, 964−967.
313
10. Roberts, L. C.; Hug, S. J.; Ruettimann, T.; Billah, M.; Khan, A. W.; Rahman, M. T. Arsenic
314
removal with iron(II) and iron(III) waters with high silicate and phosphate concentrations.
315
Environ. Sci. Technol. 2004, 38, 307−315.
ACS Paragon Plus Environment
20
Page 21 of 25
Environmental Science & Technology
316
11. Ona-Nguema, G.; Morin, G.; Wang, Y.; Foster, A. L.; Juillot, F.; Calas, G.; Brown Jr, G. E.
317
XANES evidence for rapid arsenic(III) oxidation at magnetite and ferrihydrite surfaces by
318
dissolved O2 via Fe2+-mediated reactions. Environ. Sci. Technol. 2010, 44, 5416–5422.
319
12. Su, C.; Puls, R. W. Arsenate and arsenite removal by zerovalent iron: kinetics, redox
320
transformation, and implications for in situ groundwater remediation. Environ. Sci. Technol.
321
2001, 35, 1487–1492.
322
13. Kanel, S. R.; Manning, B.; Charlet, L.; Choi, H. Removal of arsenic(III) from groundwater
323
by nanoscale zero-valent iron. Environ. Sci. Technol. 2005, 39, 1291–1298.
324
14. Leupin, O. X.; Hug, S. J. Oxidation and removal of arsenic (III) from aerated groundwater by
325
filtration through sand and zero-valent iron. Water Res. 2005, 39, 1729−1740.
326
15. Yan, W. L.; Vasic, R.; Frenkel, A. I.; Koel B. E. Intraparticle reduction of arsenite (As(III))
327
by nanoscale zerovalent iron (nZVI) investigated with in situ X-ray absorption spectroscopy.
328
Environ. Sci. Technol. 2012, 46, 7018−7026.
329
16. Yan, W. L.; Ramos, M. A. V.; Koel, B. E.; Zhang, W. X. As(III) sequestration by iron
330
nanoparticles: study of solid-phase redox transformations with X-ray photoelectron spectroscopy.
331
J. Phys. Chem. C 2012, 116, 5303–5311.
332
17. Ling, L.; Zhang, W. X. Environ. Sequestration of arsenate in zero-valent iron nanoparticles:
333
visualization of intraparticle reactions at angstrom resolution. Sci. Technol. Lett. 2014, 1,
334
305−309.
335
18. Watanabe, M.; Ackland, D. W.; Burrows, A.; Kiely, C. J.; Williams, D. B.; Krivanek, O.L.;
336
Dellby, N.; Murfitt, M.F.; Szilagyi, Z. Improvements in the X-ray analytical capabilities of a
337
scanning transmission electron microscope by spherical aberration correction. Microsc.
338
Microanal. 2006, 12, 515–526.
ACS Paragon Plus Environment
21
Environmental Science & Technology
Page 22 of 25
339
19. Kim, Y.; Tao, R.; Klie, R. F.; Seidman, D. N. Direct Atomic-Scale Imaging of Hydrogen and
340
Oxygen Interstitials in Pure Niobium Using Atom-Probe Tomography and Aberration-Corrected
341
Scanning Transmission Electron Microscopy. ACS Nano 2013, 7, 732–739.
342
20. Jiang, Y.; Wang, Y.; Sagendorf, J.; West, D.; Kou, X.; Wei, X.; He, L.; Wang, K. L.; Zhang,
343
S.; Zhang, Z. Direct atom-by-atom chemical identification of nanostructures and defects of
344
topological insulators. Nano Lett. 2013, 13, 2851–2856.
345
21. Ling, L.; Pan, B.; Zhang, W. X. Removal of selenium from water with nanoscale zero-valent
346
iron: mechanisms of intraparticle reduction of Se(IV). Water. Res. 2015, 71, 274−281.
347
22. Ling, L.; Zhang, W. X. Enrichment and encapsulation of uranium with iron nanoparticle. J.
348
Am. Chem. Soc. 2015, 137, 2788−2791.
349
23. Ling, L.; Zhang, W. X. Environ. Reactions of Nanoscale Zero-Valent Iron with Ni(II):
350
Three-Dimensional Tomography of the “Hollow Out” Effect in a Single Nanoparticle. Environ.
351
Sci. Technol. Lett. 2014, 1, 209−213.
352
24. Feitz, A. J.; Joo, S. H.; Guan, J.; Sun, Q.; Sedlak, D. L.; Waite, T. D. Oxidative
353
transformation of contaminants using colloidal zero-valent iron. Colloids and Surfaces A:
354
Physicochem. Eng. Aspects. 2005, 265, 88–94.
355
25. Joo, S. H.; Feitz, A. J.; Sedlak, D. L.; Waite, T D. Quantification of the oxidizing capacity of
356
nanoparticulate zero-valent iron. Environ. Sci. Technol. 2005, 39, 1263–1268.
357
26. Bishop, E. J.; Fowler, D. E.; Skluzacek, J. M.; Seibel, E. M.; Mallouk, T. E. Anionic
358
homopolymers efficiently target zero valent iron particles to hydrophobic contaminants in sand
359
columns. Environ. Sci. Technol. 2010, 44, 9069−9074.
ACS Paragon Plus Environment
22
Page 23 of 25
Environmental Science & Technology
360
27. Kim, J. Y.; Lee, C.; Love, D. C.; Sedlak, D. L.; Yoon, J.; Nelson, K. L. Inactivation of MS2
361
Coliphage by Ferrous Ion and Zero-Valent Iron Nanoparticles. Environ. Sci. Technol. 2011, 45,
362
6978–6984.
363
28. Schrick. B.; Hydutsky. B. W.; Blough. J. L.; Mallouk. T. E. Delivery vehicles for zerovalent
364
metal nanoparticles in soil and groundwater. Chem. Mater. 2004, 16, 2187–2193.
365
29. Liu. Y. Q.; Lowry. G. V. Effect of particle age (Fe-O content) and solution pH on NZVI
366
reactivity: H-2 evolution and TCE dechlorination. Environ. Sci Technol. 2006, 40, 6085–6090.
367
30. Tee, Y. H.; Bachas, L.; Bhattacharyya, D. Degradation of trichloroethylene and
368
dichlorobiphenyls by iron-based bimetallic nanoparticles. J. Phys. Chem. C 2009, 113, 9454–
369
9464.
370
31. Imran, A. New generation adsorbents for water treatment. Chem. Rev. 2012, 112, 5073–5091.
371
32. Leupin, O. X.; Hug, S. J. Oxidation and removal of arsenic (III) from aerated groundwater by
372
filtration through sand and zero-valent iron. Water Res. 2005, 39, 1729−1740.
373
33. Wang, C. M.; Baer, D. R.; Amonette, J. E.; Engelhard, M. H.; Antony, J.; Qiang, Y.
374
Morphology and electronic structure of the oxide shell onthe surface of iron nanoparticles. J. Am.
375
Chem. Soc. 2009, 131, 8824–8832.
376
34. Arslan, I.; Yates, T. J. V.; Browning, N. D.; Midgley, P. A. Embedded nanostructures
377
revealed in three dimensions. Science 2005, 309, 2195–2198.
378
35. Van Aert, S.; Batenburg, K. J.; Rossell, M. D.; Erni, R.; Van Tendeloo, G. Three-
379
dimensional atomic imaging of crystalline nanoparticles. Nature 2011, 470, 374–377.
380
36. Que, E. L.; Bleher, R.; Duncan, F. E.; Kong, B. Y.; Gleber, S. C. et al. Quantitative mapping
381
of zinc fluxes in the mammalian egg reveals the origin of fertilization-induced zinc sparks. Nat.
382
Chem. 2015, 7, 130–139.
ACS Paragon Plus Environment
23
Environmental Science & Technology
Page 24 of 25
383
37. Genc, A.; Kovarik, L.; Gu, M.; Cheng, H.; Plachinda, P.; Pullan, L.; Freitag, B.; Wang, C. M.
384
XEDS STEM tomography for 3D chemical characterization of nanoscale particles.
385
Ultramicroscopy 2013, 131, 24–32.
386
38. Zhang, B.; Su, D. S. Electron Tomography: three-dimensional imaging of real crystal
387
structures at atomic resolution. Angew. Chem. Int. Edit. 2013, 52, 8504–8506.
388
39. Prévot, G.; Nguyen, N. T.; Alloyeau, D.; Ricolleau, C.; Nelayah, J. Ostwald-Driven Phase
389
Separation in Bimetallic Nanoparticle Assemblies. ACS Nano 2016, 10, 4127–4133.
390
40. Wang, Y., Morin, G., Ona-Nguema, G., Juillot, F.,Guyot, F., Calas, G., Brown Jr., G. E.
391
Evidence for different surface speciation of arsenite and arsenate on green rust: an EXAFS and
392
XANES study. Environ. Sci. Technol. 2010, 44, 109−115.
393
41. Shan, Z.W.; Stach, E. A.; Wiezorek, J. M. K.; Knapp, J. A.; Follstaedt, D. M.; Mao, S. X.
394
Grain boundary–mediated plasticity in nanocrystalline nickel. Science 2004, 305, 654-657.
395
42. Kumar, K.S., Van Swygenhoven, H. & Suresh, S. Mechanical behavior of nanocrystalline
396
metals and alloys. Acta Mater. 2003, 51, 5743–5774.
397
43. Parent, L. R.; Robinson, D. B.; Woehl, T. J.; Ristenpart, W. D.; Evans, J. E.; Browning, N.
398
D.; Arslan, I. Direct in Situ Observation of Nanoparticle Synthesis in a Liquid Crystal Surfactant
399
Template. ACS Nano 2012, 6, 3589–3596.
400
44. Krivanek, O. L.; Chisholm, M. F.; Nicolosi, V.; Pennycook, T. J.;
401
N.; Murfitt, M. F.; Own, C. S.; Szilagyi, Z. S.; Oxley, M. P.; Pantelides, S. T.; Pennycook S. J.
402
Atom-by-atom structural and chemical analysis by annular dark-field electron microscopy.
403
Nature 2010, 464, 571−574.
404
45. Stumm, W.; Morgan, J. J. Aquatic Chemistry: Chemical Equilibria and Rates in Natural
405
Waters. (John Wiley & Sons, Inc. Hoboken, 1996).
ACS Paragon Plus Environment
24
Corbin, G. J.; Dellby,
Page 25 of 25
Environmental Science & Technology
406
46. Morel, F. M. M.; Hering, J. G. Principles and Applications of Aquatic Chemistry. (John
407
Wiley & Sons, Inc. Hoboken, 1993).
ACS Paragon Plus Environment
25