Subscriber access provided by Nottingham Trent University
Energy and the Environment
Cr(III) adsorption by cluster formation on boehmite nanoplates in highly alkaline solution Wenwen Cui, Xin Zhang, Carolyn I. Pearce, Ying Chen, Shuai zhang, Wen Liu, Mark H. Engelhard, Libor Kovarik, Meirong Zong, Hailin Zhang, Eric D. Walter, Zihua Zhu, Steve Heald, Micah P Prange, James J. De Yoreo, Shili Zheng, Yi Zhang, Sue B. Clark, Ping Li, Zheming Wang, and Kevin M. Rosso Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.9b02693 • Publication Date (Web): 23 Aug 2019 Downloaded from pubs.acs.org on August 26, 2019
Just Accepted “Just Accepted” manuscripts have been peer-reviewed and accepted for publication. They are posted online prior to technical editing, formatting for publication and author proofing. The American Chemical Society provides “Just Accepted” as a service to the research community to expedite the dissemination of scientific material as soon as possible after acceptance. “Just Accepted” manuscripts appear in full in PDF format accompanied by an HTML abstract. “Just Accepted” manuscripts have been fully peer reviewed, but should not be considered the official version of record. They are citable by the Digital Object Identifier (DOI®). “Just Accepted” is an optional service offered to authors. Therefore, the “Just Accepted” Web site may not include all articles that will be published in the journal. After a manuscript is technically edited and formatted, it will be removed from the “Just Accepted” Web site and published as an ASAP article. Note that technical editing may introduce minor changes to the manuscript text and/or graphics which could affect content, and all legal disclaimers and ethical guidelines that apply to the journal pertain. ACS cannot be held responsible for errors or consequences arising from the use of information contained in these “Just Accepted” manuscripts.
is published by the American Chemical Society. 1155 Sixteenth Street N.W., Washington, DC 20036 Published by American Chemical Society. Copyright © American Chemical Society. However, no copyright claim is made to original U.S. Government works, or works produced by employees of any Commonwealth realm Crown government in the course of their duties.
Page 1 of 43
Environmental Science & Technology
1
Cr(III) adsorption by cluster formation on boehmite nanoplates in
2
highly alkaline solution
3
Wenwen Cui1,2,3, Xin Zhang1,*, Carolyn I. Pearce4, Ying Chen1, Shuai Zhang1,5, Wen
4
Liu6, Mark H. Engelhard6, Libor Kovarik6, Meirong Zong1,7, Hailin Zhang1,2,3, Eric D.
5
Walter6, Zihua Zhu6, Steve Heald8, Micah P. Prange1, James J. De Yoreo1,5, Shili
6
Zheng2, Yi Zhang2, Sue B. Clark1,9, Ping Li2,*, Zheming Wang1,*, and Kevin M.
7
Rosso1,*
8
1 – Physical & Computational Science Directorate, Pacific Northwest National
9
Laboratory, Richland, Washington 99354, USA
10
2 –National Engineering Laboratory for Hydrometallurgical Cleaner Production
11
Technology, Key Laboratory of Green Process and Engineering, Institute of Process
12
Engineering, Chinese Academy of Sciences, Beijing, 100190, China
13
3 – University of Chinese Academy of Sciences, Beijing, 100049, China
14
4 – Energy & Environment Directorate, Pacific Northwest National Laboratory,
15
Richland, WA, USA
16
5 – Department of Materials Science and Engineering, University of Washington,
17
Seattle, Washington 98195, USA
18
6 – Environmental Molecular Sciences Laboratory, Pacific Northwest National
19
Laboratory, Richland, Washington 99354, USA
20
7 – School of Earth Sciences and Engineering, Nanjing University, Nanjing, Jiangsu 1
ACS Paragon Plus Environment
Environmental Science & Technology
21
Province, 210023.
22
8 – Advanced Photon Source, Argonne National Laboratory, Lemont, IL 60439, USA
23
9 – The Voiland School of Chemical and Biological Engineering, Washington State
24
University, Pullman, Washington, USA
2
ACS Paragon Plus Environment
Page 2 of 43
Page 3 of 43
Environmental Science & Technology
25
Abstract.
26
The development of advanced functional nanomaterials for selective adsorption in
27
complex chemical environments requires partner studies of binding mechanisms.
28
Motivated by observations of selective Cr(III) adsorption on boehmite nanoplates (-
29
AlOOH) in highly caustic multicomponent solutions of nuclear tank waste, here we
30
unravel the adsorption mechanism in molecular detail. We examined Cr(III) adsorption
31
to synthetic boehmite nanoplates in sodium hydroxide solutions up to 3 M, using a
32
combination of XRD, Raman, XPS, STEM, EELS, HR-AFM, TOF-SIMS, Cr K-edge
33
XANES/EXAFS, and EPR. Adsorption isotherms and kinetics were successfully fit to
34
Langmuir and pseudo-second-order kinetic models, respectively, consistent with
35
monotonic uptake of Cr(OH)4- monomers until saturation coverage of approximately
36
half the aluminum surface site density. High resolution AFM revealed monolayer
37
cluster self-assembly on the (010) basal surfaces with increasing Cr(III) loading,
38
possessing a structural motif similar to guyanaite (β-CrOOH), stabilized by corner-
39
sharing Cr-O-Cr bonds and attached to the surface with edge-sharing Cr-O-Al bonds.
40
The selective uptake appears related to short-range surface templating effects, with
41
bridging metal connections likely enabled by hydroxyl anion ligand exchange reactions
42
at the surface. Such a cluster formation mechanism, which stops short of more laterally
43
extensive heteroepitaxy, could be a metal uptake discrimination mechanism more
44
prevalent than currently recognized.
45
INTRODUCTION
46
Given the growing preponderance of functional nanomaterials intended for unique 3
ACS Paragon Plus Environment
Environmental Science & Technology
Page 4 of 43
47
applications, it is increasingly important to fundamentally understand the basis for their
48
selective interaction with other species in complex chemical environments1-6. One such
49
category of interaction having diverse impacts is the adsorption of metals. For example,
50
the persistence of toxic heavy metals in the environment poses major risks to
51
ecosystems and human health7-11. Most nanomaterials of a given composition can now
52
be specifically tailored in terms of particle size, shape, and surface functionalization,
53
suggesting the potential for new metal-selective sorbents for the protection or
54
remediation of water resources7, 12-15. Such a strategy offers flexibility in design and
55
operation, better sustainability and cost-effectiveness relative to standard methods such
56
as chemical precipitation16, 17, ion exchange18, 19, photocalysis20, membrane filtration7,
57
21-24
58
inexpensive, simple binary metal (oxyhydr)oxides, such as those of iron14,
59
aluminum29-32, titanium7, 33, and magnesium7, 34 show great promise for this purpose.
60
Their high density of surface OH groups and their high attainable surface area in
61
nanomaterial forms enables a high selectivity and capacity for heavy metal adsorption35.
62
In particular, nanosized boehmite (γ-AlOOH) is one sorbent of interest for a variety
63
of selective metal uptake applications including Cr,36 V,32, 37 Hg,38 As,39 Pb,40 Cd,41 and
64
even organic pollutants39, 42. Boehmite is a layered structure material crystallizing in
65
the orthorhombic space group Cmcm and typically possessing a tabular
66
pseudohexagonal or rhombic habit. The dominant basal (010) surface of layers contain
67
alternating oxygen and hydroxyl groups that aggregate the layers via hydrogen bonding.
68
The resulting platelet habit depends on the interplay between relatively stable (100) and
and use of electrochemical techniques24. Because they are chemically stabile and
4
ACS Paragon Plus Environment
25-28,
Page 5 of 43
Environmental Science & Technology
69
(101) edge surfaces, with both edges present in hexagonal nanoplates, whereas only
70
(101) edges are present on rhombic nanoplates43-45. Hence this structure type offers a
71
variety of oxo and hydroxo functional groups for selective metal binding on both basal
72
and edge surfaces.
73
The fact that boehmite can tightly and selectively bind metals, even in extremely
74
complex chemical environments, has no better demonstration than through its known
75
chemical associations found in caustic nuclear waste. For example, at the U.S.
76
Department of Energy’s Hanford site, where vast quantities of nuclear fuel reprocessing
77
waste containing high concentrations of aluminum and sodium hydroxide are stored46-
78
51,
79
dictate its overall chemical behavior46, 47. In these caustic multicomponent solutions the
80
adsorption mechanism is not well known, nor is the basis for its selectivity for Cr(III).
81
Cr(III) has been proposed to adhere to the boehmite surface either as a nano-to-micron
82
sized precipitate or as an adsorbed complex, the latter of which may or may not then
83
ultimately lead to its incorporation as a substituent for Al in the boehmite structure47.
nanosized boehmite appears to selectively bind metals such as Cr(III) that then
84
Using this system as inspiration, the present work examines Cr(III) adsorption on
85
nanoboehmite in concentrated sodium hydroxide solution, to help advance a more
86
detailed understanding of selective uptake mechanisms in complex environments. In
87
caustic sodium hydroxide both the surface structure of nanoboehmite and the speciation
88
of Cr(III), beyond the expectedly dominant tetrahydroxyanion Cr(OH)4
89
comprehensively known, although recent modeling work has begun to examine the
90
structure at boehmite surfaces in concentrated electrolytes44. It is thus not clear whether 5
ACS Paragon Plus Environment
52-54,
are not
Environmental Science & Technology
91
Cr(III) adsorption at alkaline conditions will bear any mechanistic correspondence with
92
the precedent already established for acidic to circumneutral pH regime. For example,
93
using the iron oxyhydroxide goethite (-FeOOH), an X-ray absorption spectroscopic
94
investigation of Cr(III) at pH 4 suggested the importance of inner-sphere surface
95
complex formation and polymerization catalyzed by the oxide surface55. It was
96
proposed that the surface structure acted as a template to precipitate Cr(III)
97
oxyhydroxide as isostructural α-CrOOH, which at higher coverages converted to
98
growth of the γ-CrOOH polymorph55. But the extent to which such a mechanism is also
99
relevant at highly alkaline conditions is unknown. In particular, this study seeks to
100
answer to the following two questions:
101
(1)
What is the loading capacity and kinetics of Cr(III) adsorption on
102
nanoboehmite in sodium hydroxide solutions?
103
(2)
104
is there a catalytic templating role of the nanoboehmite surface)?
Does Cr(III) adsorb as isolated ions, clusters or epitaxial overlayers (i.e.,
105
To do so we examined the adsorption behavior of Cr(III) on ~38 nm boehmite
106
nanocrystals of thickness ~6 nm in caustic sodium hydroxide solutions from pH 13 to
107
3 M NaOH, the latter being similar to the alkalinity in Hanford nuclear waste.
108
Macroscopic adsorption isotherms and kinetics were determined using inductively
109
coupled plasma mass spectrometry (ICP-MS). Microscopic adsorption mechanisms
110
were explored at the nanoscale using a combination of X-ray diffraction (XRD), Raman
111
spectroscopy, X-ray photoelectron spectroscopy (XPS), X-ray absorption spectroscopy
112
(XAS), scanning transmission electron microscopy (STEM) with electron energy loss 6
ACS Paragon Plus Environment
Page 6 of 43
Page 7 of 43
Environmental Science & Technology
113
spectroscopy (EELS), high resolution-atomic force microscopy (HR-AFM), time-of-
114
flight secondary ion mass spectrometry (TOF-SIMS) and electron paramagnetic
115
resonance (EPR).
116
The integrated findings reveal that the adsorption of Cr(III) on nanoboehmite at
117
alkaline conditions initially proceeds via hydroxyl ligand exchange enabling inner-
118
sphere binding of Cr(OH)4- monomers. At higher loadings when the Cr(III)
119
concentration in solution was higher than 20 ppm these monomers polymerize into
120
clusters incipient to the guyanaite (β-CrOOH) structure. Hence, similar to observations
121
at acidic conditions, at alkaline conditions the adsorption selectivity and capacity of
122
nanoboehmite for Cr(III) appears linked to the catalytic effects of specific boehmite
123
surfaces.
124 125
EXPERIMENTAL METHODS
126
Chemicals and Materials
127
Aluminum nitrate (Al(NO3)3·9H2O, ≥98%), sodium hydroxide (NaOH, ≥98%), and
128
chromium nitrate (Cr(NO3)3·9H2O, ≥99%) were purchased from Sigma-Aldrich
129
Chemical Reagent Co. Ltd., USA. All chemicals were of analytical grade and used as
130
received without further treatment and purification. Deionized water was used
131
throughout the experiments.
132
Preparation of Boehmite Nanoplates
133
Boehmite nanoplates were synthesized by our previously reported hydrothermal 7
ACS Paragon Plus Environment
Environmental Science & Technology
134
method.56 Briefly, a 0.25 M aluminum nitrate solution was prepared by dissolving an
135
weighed amount of Al(NO3)3·9H2O in deionized water under stirring at room
136
temperature, and titrated with 1 M NaOH to adjust the pH of the solution to ~10.0. After
137
continuous stirring for 1 h, gel-like Al(OH)3 precipitates formed. The solid was
138
separated from the suspension by centrifugation and washed with deionized water three
139
times to remove all soluble salts.
140
In a 100 ml Teflon liner, a weighed amount of the Al(OH)3 gel solids were dispersed
141
into deionized water and the suspension pH was adjusted to ~12 using NaOH solution.
142
The concentration of gels (defined as the concentration of Al3+) was 0.5 M and the
143
volume of the solution was 80 mL. The Teflon container was sealed into a Parr steel
144
vessel and then was heated in an electric oven with a rotation device (10 rpm) at 200
145
oC
146
deionized water three times and dried at 80 oC overnight, and then was characterized by
147
XRD, Raman spectroscopy, scanning electron microscopy (SEM), and transmission
148
electron microscopy (TEM) to ensure phase purity.
149
Cr(III) Adsorption Measurements
for 48 h. The resulting white product was recovered by centrifugation, washed with
150
Batch Cr(III) ion adsorption experiments were performed in 50 mL centrifuge tubes.
151
Cr(NO3)3·9H2O was dissolved in NaOH solution with different concentrations (0.1, 0.2,
152
0.4, 0.5, 0.8, 1, 2, 3 M) to investigate the effect of NaOH concentration on Cr(III)
153
adsorption on boehmite. Cr(III) solutions with concentrations (1, 5, 10, 20, 50, 100, 200
154
mg·L-1) at pH of 13 were then prepared to measure the adsorption isotherm. Boehmite
155
(0.01 g) was added into 10 mL Cr(III) solution of various concentrations and shaken at 8
ACS Paragon Plus Environment
Page 8 of 43
Page 9 of 43
Environmental Science & Technology
156
room temperature, with specific time intervals for measurement. After agitation, the
157
supernatants were filtered through a syringe filter (0.45 m) and the residual Cr(III)
158
concentration in the solution was determined by inductively coupled plasma - optical
159
emission spectrometry (ICP-OES). The solids of Cr(III)-adsorbed boehmite were
160
washed with deionized water three times, dried at 80 oC and characterized to study the
161
mechanism of Cr(III) adsorption. The Cr(III) adsorbed boehmite samples with the
162
initial Cr concentration of 50 and 200 mg·L-1 were defined as Cr-B-1 and Cr-B-2,
163
respectively.
164
Solids Characterization
165
X-ray diffraction (XRD)
166
XRD patterns were recorded on a Philips X’pert Multi-Purpose Diffractometer (MPD)
167
(PANAlytical, Almelo, The Netherlands) equipped with a fixed Cu anode operating at
168
50 kV and 40 mA. XRD patterns were collected in the 5−80° 2θ range. Phase
169
identification was performed using JADE 9.5.1 from Materials Data Inc., and the 2012
170
PDF4+ database from the International Center for Diffraction Data (ICDD) database.
171
Raman spectroscopy
172
Raman spectra were collected using a Horiba LabRam HR spectrometer coupled with
173
an inverted optical microscope (Nikon Ti-E) with a 40X objective and a 632.8 nm HeNe
174
laser light source. Spectra were collected in the 150−4000 cm−1 range using three 60 s
175
exposure times.
176
Nitrogen Adsorption/Desorption Isotherms 9
ACS Paragon Plus Environment
Environmental Science & Technology
177
Nitrogen adsorption-desorption isotherms were collected by a surface area and porosity
178
analyzer (Micromeritics, ASAP 2020), and the Brunauer-Emmett-Teller (BET) surface
179
area was calculated from the linear part of the BET plot.
180
Scanning Electron Microscopy (SEM)
181
Morphology measurements were carried out using a Helios NanoLab 600i SEM (FEI,
182
Hillsboro, OR). All samples were sputter-coated with a thin layer of carbon prior to
183
analysis (∼5 nm) to ensure good conductivity and imaging.
184
Transmission electron microscopy (TEM)
185
As-prepared samples were dispersed in water with sonication for 5 min. Samples were
186
prepared by placing drops of solution onto the copper grid (Lacey Carbon, 300 mesh,
187
Copper grid, Ted Pella, Inc.). After drying under ambient conditions, the samples were
188
introduced into the FEI Titan TEM. The samples were imaged using an acceleration
189
voltage of 300 kV. SEM and TEM were also used to evaluate the size distribution of
190
as-synthesized boehmite samples. The width and thickness of the particles were
191
determined based on average values for more than 20 particles.
192
X-ray photoelectron spectroscopy (XPS)
193
Physical Electronics Quantera Scanning X-ray Microprobe was used to perform the
194
XPS measurements. Monochromatic Al Kα X-ray (1486.7 eV) was used as source for
195
excitation and a spherical section was used as the analyzer. The equipment has a
196
detection system with a 32-element multichannel. The sample was probed by directing
197
the X-ray beam perpendicular to the sample and the detector was at 45°. The spectra 10
ACS Paragon Plus Environment
Page 10 of 43
Page 11 of 43
Environmental Science & Technology
198
were collected using a pass-energy of 69.0 eV with a step size of 0.125 eV. The Ag3d5/2
199
line, showed a FWHM of 1.0 eV ± 0.05 eV using these conditions. The Cu 2p3/2 at
200
932.62 ± 0.05 eV and the Au 4f7/2 at 83.96 ± 0.05 eV features were used to calibrate the
201
binding energy scale. Charging was observed during the experiment which was
202
minimized by using low energy electrons at 1.5 eV, 20μA and low energy Ar+ ions. All
203
samples were prepared as pressed powders supported on a metal bar for the XPS
204
measurements. Scans were recorded from 0 – 1350 eV, with subsequent high-resolution
205
scans of the Al 2p, O 1s and Cr 2p regions obtained.
206
X-ray absorption spectroscopy (XAS)
207
Extended X-ray absorption fine structure (EXAFS) data at the Cr K-edge were acquired
208
in fluorescence mode on beamline 20-BM-B at the Advanced Photon Source. The
209
incident beam energy was selected using a Si (111) monochromator, and the X-ray
210
beam was focused to spot size of ~400 microns using a toroidal mirror. The
211
fluorescence signal was monitored using a multi-element, energy dispersive germanium
212
detector. Initial energy calibration was performed using a chromium foil. Slight changes
213
in monochromator energy were monitored and accounted for by simultaneously
214
measuring the spectra of the chromium foil as a reference standard. Al K-edge EXAFS
215
spectra were acquired at the Advanced Light Source (Berkeley, CA) at beamline 6.2.1.2.
216
To mount samples, powder was lightly pressed into indium foil and attached to a copper
217
sample holder using silver paint. A reference spectrum collected on corundum (α-Al2O3)
218
was used to calibrate the energy scale. Al K-edge EXAFS data were collected in total
219
electron yield (TEY) mode over the scan range from 1520 to 1850 eV. Both the Cr and 11
ACS Paragon Plus Environment
Environmental Science & Technology
220
Al K-edge EXAFS data were collected at room temperature and analyzed using the
221
Athena interface to the IFEFFIT program package57.
222
Scanning transmission electron microscopy (STEM) and electron energy loss
223
spectroscopy (EELS)
224
Microstructural investigation was performed with an aberration-corrected electron
225
microscope (FEI, Model Titan 80-300) in STEM mode. STEM images were taken at
226
300 keV in STEM mode with high angle annular dark field (HAADF) detector. Data
227
collection and analysis was performed on Gatan’s Digital Micrograph 1.9.4. The STEM
228
sample preparation was same as for TEM. The microscope is equipped with Gatan
229
Quantum ER energy filter for electron energy loss spectroscopy (EELS) analysis. EELS
230
measurements were performed at 300 kV in dual EELS mode and with the dispersion
231
of 0.1eV. The EELS data were recorded in the STEM mode with a probe size of 10 nm
232
to minimize the dose density and electron dose effects. All EELS spectra were recorded
233
in dual EELS mode, allowing to establish a reference zero-loss peak (ZLP) with high
234
accuracy. The high energy loss spectrum was recorded from 480 eV to 684.8 eV, to
235
cover the ionization energy ranges for the oxygen K-edge and the chromium L-edge.
236
High-resolution atomic force microscopy (HRAFM)
237
HRAFM images were captured by Cypher-ESTM AFM (Asylum Research, CA) with
238
amplitude-modulate mode within nuclease-free water (Ambion). ArrowTM-UHFAuD
239
(NanoWorld) cantilever was used to image Boehmite Cr-B-1. The offline data
240
processing was done with software SPIPTM (Image Metrology, Denmark). 12
ACS Paragon Plus Environment
Page 12 of 43
Page 13 of 43
Environmental Science & Technology
241
Time-of-fight secondary ion mass spectrometry (ToF-SIMS)
242
ToF-SIMS measurement was performed at Environmental Molecular Sciences
243
Laboratory (EMSL), which located at Pacific Northwest National Laboratory. A
244
TOF.SIMS5 instrument (IONTOF GmbH, Münster, Germany) was used. A 25 keV
245
pulsed Bi3+ beam was used as the analysis beam to collect SIMS spectra. The Bi3+ beam
246
was focused to be ~5 µm diameter and scanned over a 200 200 µm2 area.
247
current of the pulsed Bi3+ beam (10 kHz) was about 0.56 pA, and data collection time
248
is ~96 s per spectrum. Mass resolution was in a range of 5000-7000, varying from
249
sample to sample due to sample roughness. A low energy (10 eV) electron flood gun
250
was used for charge compensation in all measurement. The ToF-SIMS sample
251
preparation was as follows: as-prepared samples were dispersed in water by a sonicator
252
for 5 min, and then the dispersed suspension was dropped on a silicon wafer, which
253
was then dried under ambient conditions prior to being introduced into the chamber.
254
Electron paramagnetic resonance (EPR) spectroscopy
255
All EPR measurements were performed on Bruker ELEXSYS E580 spectrometer. The
256
typical settings for the static spectra were microwave frequency = 9.32 GHz, sweep
257
width = 5000 G, time constant = 40.96 ms, sweep time = 82 s, power = 0.2 mW, field
258
modulation amplitude = 0.5 G. Temperature-dependent spectra were recorded after a
259
sample was equilibrated at a temperature for ten minutes. Absolute Cr3+ spin
260
concentration absorbed on boehmite was determined by comparing its double
261
integration to that of the spin standard at 125 K.
13
ACS Paragon Plus Environment
The
Environmental Science & Technology
262 263
RESULTS AND DISCUSSION
264
Characterization of Boehmite Nanoparticles
265
The XRD pattern of the as-prepared boehmite (Figure 1a) agreed well with the
266
powder diffraction file of pure boehmite (ICDD PDF # 00-74-1895)56; the strong
267
diffraction peak at the 2θ angle of 14.5° was assigned to (020) diffraction. As shown in
268
Figure 1b, the sample displayed Raman bands in the low wavenumber region (150-800
269
cm-1) at 343, 366, 455, 498 and 677 cm-1, which agree well with literature data for
270
boehmite and correspond to structural hydroxyl translational modes43, 58. Two broad
271
bands at 3078 and 3221 cm-1 in Figure 1c are attributed to the symmetric and
272
asymmetric stretches of these hydroxyl groups43, 47, 58.
273
SEM and TEM images (Figure 1d-f) show that the boehmite samples were all
274
rhombic nanoplates, which includes two dominant (010) basal surfaces terminated with
275
four (101) edge surfaces43, 44, 56. TEM images indicated that the mean size parallel to
276
[101] and average thickness along [010] (Figure 1g and 1h) were 38.3 and 5.7 nm,
277
respectively. It is noteworthy that this morphology and size of our synthetic material
278
are similar to boehmite particles found in radioactive tank waste at the Hanford site 59.
279
The results of nitrogen adsorption-desorption isotherms (Figure S1) were used to
280
calculate a BET surface area of 52.22 m2·g-1 for our material.
14
ACS Paragon Plus Environment
Page 14 of 43
Page 15 of 43
Environmental Science & Technology
281 282 283
Figure 1. Characterization of as-prepared boehmite: (a) XRD pattern, (b) and (c) Raman spectra, (d) SEM image, (e) and (f) TEM images; (g) size distribution and (h) thickness distribution.
284
Adsorption of Cr(III)
285
Overview of Cr(III) speciation and adsorption
286
Here we briefly summarize known relationships between Cr(III) speciation and its
287
adsorption mechanism, which are dominated by studies at low pH. Clearly critical is
288
the aqueous speciation of Cr(III), which is strongly pH dependent. At pH less than 2 it
289
exists as the bulky hydrated species Cr(H2O)63+ 60. Between pH 2 to 6.3 CrOH2+ is the
290
dominant hydroxo species52,
291
Cr2(OH)24+ and Cr3(OH)45+ also form in this pH range52, 61, 62. Cr(OH)3 solids precipitate
292
in the pH range from 6.3 to 11.552,
293
dominant52, 53. In our experiments, we could visually observe a trace undissolved Cr(III)
294
solid phase component when NaOH < 0.1 M. Above 0.1 M the solution is optically
295
very clear, consistent with complete dissolution of the Cr(III) precursor.
53,
but Cr(OH)2+ and polynuclear species such as
53,
and above this pH the Cr(OH)4 species is
15
ACS Paragon Plus Environment
Thus, to
Environmental Science & Technology
296
avoid precipitation, Cr(III) adsorption at alkaline conditions was performed in the
297
current study with its focus on pH 13 and above.
298
Previous adsorption work in the low pH range, where Cr(III) exists as cationic
299
species, shows that its adsorption can be viewed as an ion-exchange process with
300
protons33. For example, Cr(III) adsorption on lignin in the pH range 1.5~5.5 was well
301
described by a Langmuir isotherm and pseudo-second-order kinetics suggesting
302
monolayer chemisorption via cation exchange with surface H+ 63. Likewise, Cr(III)
303
adsorption on activated carbon at pH 3.7 was proposed to be a simple ion-exchange of
304
Cr(OH)2+ with –OH groups on the surface followed by formation of inner-sphere
305
complexes64. Adsorption of Cr(III) on titanate nanotubes at pH=5 also involved ion-
306
exchange with H+/Na+ in the interlayer33. Site-specific electrostatic attraction and
307
coordination of Cr(III) ions to material surfaces is an important control over its
308
adsorption behavior60, 61, 65. Thus, at highly alkaline conditions, it is possible that similar
309
ion exchange concepts, except in this case anionic ones, pertain to adsorption of
310
Cr(OH)4 on nanoboehmite.
311
Effect of NaOH concentration
312
Adsorption experiments were performed with varying NaOH concentration from
313
0.1 M to 3 M at an initial Cr(III) concentration of 50 mg·L-1. Aqueous Cr(III) speciation
314
as monomeric Cr(OH)4- is expected across this entire range. As shown in Figure 2, the
315
adsorption capacity for Cr(III) on boehmite nanocrystals was strongly affected by initial
316
solution pH, decreasing sharply with increasing NaOH concentration. The highest
317
adsorption capacity of Cr(III) was ~18 mg·g-1 at 0.1 M NaOH. 16
ACS Paragon Plus Environment
Page 16 of 43
Page 17 of 43
Environmental Science & Technology
318
To better understand the adsorption behavior, we selected pH 13 as the optimal pH
319
value for investigating the effects of other system variables such as the Cr(III)
320
concentration.
321 322 323
Figure 2. Effect of NaOH concentration on the Cr(III) adsorption on boehmite Adsorption isotherms
324
Adsorption experiments at pH 13 (0.1 M NaOH) with a series of Cr(III) solutions
325
at concentrations ranging from 1 to 200 mg·L-1, and a boehmite concentration of 1 g·L‑1
326
(10 mg boehmite in 10 mL Cr(III) solutions), were conducted at room temperature for
327
3 h. Both the Freundlich isotherm model and the Langmuir isotherm model were used
328
for the analysis of the obtained adsorption data as follows30, 41, 65: 1
329
The Freundlich isotherm model: ln 𝑄𝑒 = 𝑛ln 𝐶𝑒 + ln 𝐾𝐹
330
The Langmuir isotherm model: Qe = 1 + KLCeQmax
KLCe
(1) (2)
331
Where Ce is the equilibrium concentration of Cr(III) in solution (mg·L-1), Qe is the
332
equilibrium adsorption capacity (mg·g-1), KF (mg·g-1(mg·L-1)1/n) and n is the Freundlich
333
adsorption constant related to adsorption capacity and adsorption intensity, KL is the 17
ACS Paragon Plus Environment
Environmental Science & Technology
Page 18 of 43
334
Langmuir adsorption constant (L·mg-1), and Qmax is the maximum adsorption capacity
335
of the boehmite adsorbent (mg·g-1), respectively.
336
As shown in Figure 3 and Table 1, the Cr(III) adsorption data was better described
337
by the Langmuir isotherm model, with a substantially higher correlation coefficient (R2
338
value) of 0.998. Fits of this model indicate a maximum adsorption capacity (Qmax) of
339
19.85 mg·g-1. Based on the measured BET surface area 55.22 m2/g and measured mean
340
size and average thickness of the boehmite samples, and assuming adsorption site
341
densities equivalent to Al on the exposed surface, the corresponding theoretical
342
monolayer Qmax would be 40.46 mg Cr(III)/g AlOOH. Given that our measured Qmax is
343
less than half of this value, this implies lower Cr(III) sorption site densities, such as via
344
a sparse monolayer that is not structurally commensurate with the underlying boehmite
345
surface over long range.
346 347 348 349
Figure 3. Cr(III) adsorption on boehmite with different initial concentration (a), Langmuir isothermal fitting model (b) and Freundlich isothermal fitting model (c) (boehmite 1 g·L-1, p H=13, room temperature, 3 h)
350 351 352
Table 1 Isotherm adsorption parameters for the Langmuir and Freundlich isothermal model fitting of Cr(III) adsorption on boehmite. (boehmite (1 g·L-1), pH=13, room temperature, 3 h) Qmax(mg·g-1)
KL(L·mg-1)
R2
19.85
0.317
0.998
n
KF
R2
Langmuir
Freundlich
18
ACS Paragon Plus Environment
Page 19 of 43
Environmental Science & Technology
2.425
3.715
0.850
353 354
Adsorption kinetics
355
Similarly at pH 13 (0.1 M NaOH), the adsorption kinetics were investigated with
356
an initial Cr(III) concentration of 100 mg·L-1 and boehmite loading of 1 g·L‑1, using
357
different equilibration times. Both pseudo-first-order and pseudo-second-order kinetic
358
models were used to fit the experimental data, according to35, 60, 66 log (𝑄𝑒 ― 𝑄𝑡) = log 𝑄𝑒 ―
359
The pseudo-first-order model:
360
The pseudo-second-order model:
t Qt
1
𝑘1
( )𝑡 2.303
1
= k Q2 + Qet 2 e
(3) (4)
361
where t (min) is time, Qe and Qt (mg·g-1) are the adsorption capacity at equilibrium and
362
at time t, respectively. k1 (min-1) is the second-order rate model adsorption constant, k2
363
(mg·g-1·min-1) is the second-order rate model adsorption constant, and V0 (mg·g-1·min-1)
364
is the initial adsorption rate which can be calculated by k2 and Qe.
365
The kinetic data for Cr(III) adsorption on boehmite is shown in Figure 4, along
366
with the pseudo-first-order and pseudo-second-order model fitting. The results suggest
367
that the pseudo-second-order kinetic model gave a better fit to the adsorption data and
368
consequently suggest that a chemisorption process34 adequately describes the measured
369
Cr(III) adsorption behavior (R2>0.998, Figure 4b, Table 2). Parameters obtained from
370
the pseudo-second-order kinetic model by plotting t versus t/Qt are given in Table 2.
19
ACS Paragon Plus Environment
Environmental Science & Technology
Page 20 of 43
371 372 373 374
Figure 4. Cr(III) adsorption on boehmite with different times (a), the Pseudo- Second -Order fitting model (b) and the Pseudo-First-Order fitting model (c) (boehmite 1 g ·L-1, pH=13, room temperature, initial concentration of Cr(III)=100 mg·L-1)
375 376 377
Table 2 Kinetics parameters of the pseudo-second-order kinetic model fitting of of Cr(III) adsorption on boehmite. (boehmite 1 g·L-1, pH=13, room temperature, initial concentration of Cr(III)=100 mg·L-1) The pseudo-firstorder kinetic model
The pseudo-secondorder kinetic model
378
Qe(mg·g-1)
k1
R2
9.643
0.0211
0.972
Qe(mg·g-1)
k2(mg·g-1·min-1)
R2
19.59
8.71×10-3
0.998
Nanoboehmite Characterization after Cr(III) Adsorption
379
Figure 5 shows that no new phases were detected in the XRD patterns of Cr(III)
380
adsorbed boehmite nanocrystals Cr-B-1 (50 mg·L-1) and Cr-B-2 (200 mg·L-1), and no
381
peaks for Cr(III)-based species were observed in both low and high wavenumber
382
regions of the Raman spectra. Therefore, any bulk crystalline Cr(III) species present,
383
such as by crystal nucleation and growth on the nanoboehmite surfaces, were
384
negligible.58
20
ACS Paragon Plus Environment
Page 21 of 43
Environmental Science & Technology
385 386 387 388
Figure 5. XRD patterns (a) and Raman spectra (b, c) of Cr(III)-adsorbed boehmite (Cr-B-1, Cr-B-2, boehmite 1 g·L-1, pH=13, room temperature, 3 h, initial concentration of Cr(III)=50, 200 mg·L-1, respectively)
389
However, surface-sensitive XPS spectra clearly showed that Cr adsorption had
390
indeed occurred, which were also used to provide information on surface binding sites
391
(Figure 6 and Table 3). Survey spectra (Figure 6a) show the presence of Cr on the
392
surface after adsorption. The Al 2p binding energy for boehmite both before and after
393
Cr adsorption was 73.9 eV, indicating that the local bonding environment of Al did not
394
change as a result of interaction with Cr (Figure 6b)48. The O1s binding energy for
395
boehmite (531eV) also did not change significantly upon Cr adsorption, which is
396
anticipated given that the oxygen binding environment in AlOOH and CrOOH is
397
similar67. The binding energies for the Cr 2p3/2 and Cr 2p1/2 peaks (Figure 6d) were
398
576.7 eV and 586.4 eV for Cr-B-1, and 576.8 eV, and 586.3 eV for Cr-B-2, respectively.
399
These binding energies confirm that Cr is present on the boehmite surface as Cr(III).
400
The atomic concentrations of Cr at the surface increased concurrently with decreasing
401
Al during the adsorption process (Table 3). The amount of Cr(III) on the boehmite
402
surface, as determined by XPS, is in qualitative agreement with the adsorption capacity
403
predicted by the Langmuir isotherm model in Table 1; given that in our XPS 21
ACS Paragon Plus Environment
Environmental Science & Technology
Page 22 of 43
404
measurement geometry the information depth was several Ångstroms into the surface,
405
quantitative comparison was not practical.
406 407 408 409
Figure 6. XPS full spectra (a), XPS spectra of Al 2p (b), O 1s (c) and Cr 2p (d) of pure boehmite and Cr(III) adsorbed boehmite (B, pure boehmite; Cr-B-1, Cr-B-2, boehmite 1 g·L-1, pH=13, room temperature, 3 h, initial concentration of Cr(III)=50, 200 mg·L-1, respectively).
410 411 412 413
Table 3 Atomic concentration and weight content of pure boehmite and Cr(III) adsorbed boehmite (B, pure boehmite; Cr-B-1, Cr-B-2, boehmite 1 g·L-1, pH=13, room temperature, 3 h, initial concentration of Cr(III)=50, 200 mg·L-1, respectively) Atomic concentration(%)
Weight content(%)
Samples Al
O
Cr
Al
O
Cr
B
26.4
68.6
0.0
38.0
58.8
0.0
Cr-B-1
24.2
67.1
2.0
33.6
54.1
5.7
Cr-B-2
22.3
65.6
3.5
30.8
53.7
9.3
414 415
We now turn our attention to high-resolution microscopic characterization of the
416
nanoboehmites after Cr adsorption. HAADF STEM images (Figure 7a) performed on
417
the Cr-B-1 sample indicate the presence of small Cr clusters on the boehmite surface.
418
Corresponding EELS data compared with that for Cr(III)2O3 and Na2Cr(VI)O4 22
ACS Paragon Plus Environment
Page 23 of 43
Environmental Science & Technology
419
standards confirm the trivalent oxidation state of Cr on the boehmite surface. For
420
example, the average L3 ionization energy loss was measured to be at 576.8 eV, which
421
matches the energy of the Cr(III)2O3 standard (Figure 7b), and is much lower than the
422
energy of Na2Cr(VI)O4 at 579.5 eV (Figure 7b). Thus, consistent with the XPS results,
423
EELS also shows that the adsorbed Cr species is present as Cr(III), not Cr(VI) for
424
example.
425 426 427
Figure 7. STEM HAADF image of Cr-B-1 (a) and EELS spectra of Cr-B-1, Cr2O3 and Na2CrO4 (b). Red circles indicate example locations of adsorbed Cr(III) species on the boehmite surface.
428
Given the expectations from the adsorption isotherm and XPS-based surface
429
analyses for approximately 50% surface coverage at maximum loading, attempts were
430
made to directly visualize the Cr distribution on the nanoboehmite surface. HRAFM
431
was performed before and after Cr adsorption. The observed size (40 nm) and thickness
432
(5 nm) of the as-prepared boehmite agreed well with the TEM and SEM measurements
433
(Figure 8a). The dominant basal (010) surface consistently showed minimal initial
434
microtopography and was therefore ideal for imaging at atomic resolution. The (010)
435
lattice was readily resolved (Figure 8b and 8c), revealing a rectangular surface unit cell
436
0.29 nm by 0.36 nm in dimension, which agrees well with expected values. In contrast, 23
ACS Paragon Plus Environment
Environmental Science & Technology
437
Cr(III)-reacted samples routinely showed additional features at the nanoscale. The (010)
438
plane for the Cr-B-1 sample was rougher, revealing small adsorbed patchy domains
439
(Fig. 8d). Based on the consistently uniform indications from XPS, STEM and EELS
440
that Cr(III) is on the surface, we thus make this assignment to these patches observed
441
in HRAFM. At high resolution, although the atomic structure of the surrounding (010)
442
surface could still be resolved (Figure 8e and 8f), no such ordered structure was readily
443
apparent while imaging the adsorbed patches. We thus assume that this indicates a lack
444
of substantial crystalline order within the adsorbed Cr(III) domains. Topographically
445
higher ‘brighter’ spots on the (010) surface at the margins of the patches are
446
conceptually consistent with adatom monomeric Cr(III)(OH)4 ions52, 53; their average
447
height, along with that of the patches themselves, is around 0.2 nm (arrows in Figure
448
8e and 8f). Collectively, the HRAFM images suggest that on nanoboehmite (010) Cr(III)
449
supplied in solution concentration of 50 ppm tends to adsorb as monomers that
450
segregate into poorly ordered single-layer clusters on the surface. It is also noteworthy
451
that surface coverages estimated by HRAFM agree well with coverages estimated both
452
by the measured adsorption isotherm and XPS-based surface concentrations, albeit here
453
limited to observations on just the (010) surface.
454 455
Figure 8. AFM images of as-prepared boehmite: (a) low resolution and (b) high resolution. The inset in 24
ACS Paragon Plus Environment
Page 24 of 43
Page 25 of 43
Environmental Science & Technology
456 457 458
panel (a) is zoomed-in on a single particle. (c) FFT of high-resolution image shown in panel (b), with arrows indicating boehmite lattice vectors. (d) Low-resolution image of Cr-B-1, (e) and (f) high-resolution image and corresponding phase image, respectively, of Cr-B-1.
459
To gain more insight into the structure of these adsorbed Cr(III) domains we
460
performed ToF-SIMS surface analytical characterization. ToF-SIMS spectra of Cr(III)
461
adsorbed boehmite with the initial Cr(III) concentration of 1, 5, 10, 20, 50, 100, 200
462
mg·L-1 were obtained at the positive ion mode (Figure 9). Figure 9(a) shows the most
463
consistently intense Cr(III) ion peaks were
464
and Cr3O3+(m/z=203.81) in the m/z ranging from 45 to 210. The ToF-SIMS
465
measurement is based on an energetic sputtering process that more often tends to
466
deconstruct rather than construct metal clusters68.
467
Cr(III)-oxo fragments were consistently observed along with monomer fragments
468
suggests the likelihood of Cr-O-Cr clusters in the patchy domains on the surface as the
469
source material. More to this point, the relative abundances for the Cr2O2+ and Cr3O3+
470
multi-center secondary ions showed a systematic trend with the initial Cr(III) solution
471
concentration (Figure S2 and Figure 9b). Importantly, no Cr(III)-based clusters were
472
indicated to be present on the boehmite surface when the initial concentration of Cr(III)
473
was 1 ppm. Small amounts of Cr(III)-based dimers and trimers were detected when the
474
initial concentration of Cr(III) was 5 and 10 ppm. Many clusters were detected when
475
the initial concentration of Cr(III) was > 20 ppm. Hence the ToF-SIMS based analyses
476
suggest an uptake mechanism consistent with both the isotherm data and the HRAFM
477
images that entails Cr(III) monomer adsorption that assemble into surface clusters
478
systematically with increasingly higher surface Cr(III) loadings.
50Cr+(m/z=49.95),
Cr2O2+ (m/z=135.88),
Hence, the fact that multi-center
25
ACS Paragon Plus Environment
Environmental Science & Technology
479 480 481
Figure 9. ToF-SIMS (+) spectra (a) and relative abundance of CrxOy+ secondary ions (b) of Cr(III) adsorbed boehmite with different initial concentration of Cr(III) from 1 ppm to 200 ppm.
482
Given that the formation of Cr(III) clusters is likely, but that these clusters lack
483
long-range structural order, we used Cr K-edge XANES and EXAFS to obtain more
484
specific information on the local molecular environment around both Cr and Al at the
485
nanoboehmite surface. Cr K-edge XANES spectra for Cr-B-1 and Cr-B-2 were very
486
similar (Figure 10a). The spectra closely resemble those measured by Frommer et al.69
487
for a series of Fe-Cr-oxyhydroxides. The low energy contributions in the pre-edge
488
spectra are assigned to local transitions and the intensity of the first peak is the same
489
for Cr-B-1 and Cr-B-2, indicating similar distortion of the Cr coordination site. The
490
only difference between the XANES spectra for Cr-B-1 and Cr-B-2 is a slight decrease
491
in intensity of the higher energy pre-edge peak, likely related to non-local transitions to
492
neighboring Al in Al-Cr-oxyhydroxides (~5992.6 eV, shown in inset in Figure 10a).
493
This change can be explained by substituting some of the neighboring Al in Cr-B-1 by
494
Cr in Cr-B-2. Analysis of these non-local transitions suggests a lower amount of Cr26
ACS Paragon Plus Environment
Page 26 of 43
Page 27 of 43
495
Environmental Science & Technology
clustering in Cr-B-1.
496
For corresponding EXAFS analyses, Figure 10b shows the k3-weighted χ spectra
497
of Cr-B-1 and Cr-B-2, and the magnitude of the Fourier transformed spectra are shown
498
in Figure 10c. The first peak in the Fourier transform, which is the contribution of the
499
nearest-neighbor O atoms, is of similar height and position for both samples. Beyond
500
this intense Cr-O contribution, four weak but well-defined Cr-Me peaks are clearly
501
shown between 2 and 4 Å. The first and third Cr-Me distances are very close to the Me
502
shell distance in boehmite, as shown by the Al K-edge Fourier transform in Figure
503
10c43. Analysis of the data suggests that the key set of Cr-(Cr, Al) bond distances
504
pertaining to the adsorbed clusters are 3.01 Å, 3.45 Å, and 3.95 Å. It is noteworthy that
505
this set resembles but is distinct from those observed by Charlet and Manceau for small
506
surface clusters of Cr(III) templated onto goethite surfaces.55 (Charlet and Manceau
507
data shown in blue translated above the other Fourier transforms in Figure 10c). In that
508
study, α-FeOOH-like CrOOH cluster formation (Cr…Cr distance 3.45 Å) was enabled
509
by Cr(III) substitution into Fe(III) lattice positions on the surface (Fe…Fe distance 3.43
510
Å). In our case, however, boehmite Al…Al distances are 2.87 and 3.69 Å,70 suggesting
511
a Cr(III) cluster formation mechanism other than surface site substitution.
512
Comparison of our set of three key Cr-(Cr, Al) distances with those reported for
513
various bulk CrOOH polymorphs (Fig. S4), which are generally known to adopt bulk
514
topologies distinct from (Fe,Al)OOH polymorphs,71 revealed one prospect. Cr…Cr
515
distances reported for γ-AlOOH-like CrOOH are 3.05 and 3.98 Å55,
516
preclude our 3.45 Å observation. The γ-CrOOH mineral bracewellite entails Cr…Cr 27
ACS Paragon Plus Environment
72
but these
Environmental Science & Technology
517
distances of 2.97, 3.26, and 3.40 Å (Fig. S4c),73 and the α-CrOOH mineral grimaldiite
518
entails 2.97 and 4.77 Å (Fig. S4a),74 both generally incompatible with our observations.
519
The β-CrOOH mineral guyanaite, however, is based on a set of Cr…Cr distances (3.00,
520
3.51, and 4.30 Å) 75, 76 (Fig. S4b) sufficiently similar to those indicated by our collective
521
XAS information to suggest that a relaxed version of this CrOOH topology could be
522
representative of clusters on the boehmite surface.
523 524 525 526 527 528
Figure 10. (a) Cr K-edge XANES spectra with inset showing pre-edge region; (b) Cr K-edge k3weighted χ(k) spectra; (c) Fourier transform (FT) magnitude; for Cr K-edge Cr-B-1 (black solid line), Cr K-edge Cr-B-2 (red solid line), Al K-edge Cr-B-1 (black dotted line), Al K-edge Cr-B-2 (red dotted line) and Cr K-edge for Cr(III) sorbed on goethite from Charlet and Manceau55, translated above the other FTs for clarity.
529
Electron paramagnetic resonance (EPR), which is not surface specific but is highly
530
sensitive to Cr(III), was performed due to its ability to provide further information on
531
Cr-Cr interactions and interatomic distances within the adsorbed clusters. Figure 11
532
shows EPR spectra of pure boehmite versus Cr(III) adsorbed boehmite with varying
533
amount of chromium, with the broad Cr3+ signal located at a center of g = 1.984. The
534
weight percentage (wt%) of absorbed Cr(III) quantified by comparing to the EPR signal
535
of a standard solution 0.5 mM Cr(NO3)3 was plotted against the concentration of Cr(III)
536
in solution (Fig. 11b). A dramatic rise in Cr(III) uptake was observed for the solutions
537
between 1 and 20 ppm, followed by a slower increase between 20 and 100 ppm and a 28
ACS Paragon Plus Environment
Page 28 of 43
Page 29 of 43
Environmental Science & Technology
538
plateau between 100 and 200 ppm; consistent with the adsorption isotherm
539
investigation (Fig. 3a).
540
The linewidth of the EPR signal of regular crystals usually comes from the
541
interactions between the magnetic dipoles77, but for the paramagnetic species absorbed
542
inside regular crystals, the additional broadening effect may be caused by the
543
orientational and structural disorder of paramagnetic centers as well as the site-to-site
544
variation of the magnetic environment78. The EPR signal of absorbed Cr(III) on
545
nanoboehmite is relatively broad with a linewidth of 600 gauss at 0.1 wt% load,
546
suggesting the remarkable orientational, structural and magnetic variability of the
547
absorption sites. As shown in Figure 11c, the linewidth shows little difference when
548
the Cr(III) load increases from 0.1 wt% to 1.4 wt%.
549
According to a simplified treatment for the line broadening effect caused by dipolar
550
interactions between electron spins, the linewidth (full width at half-maximum height)
551
𝐵 can be calculated from the distance 𝑟𝑖𝑗 between the two spins i and j:79
552
𝐵 = (1.95 × 104)
〈∑
〉
𝑟𝑖𝑗 ―6
1/2
553
where B is in gauss and 𝑟𝑖𝑗 in Ångstroms. Therefore, for a base linewidth of 600 gauss
554
caused by site-to-site variation, we do not expect to observe a notable difference in
555
linewidth if the additional dipolar line broadening is much smaller than 600 gauss,
556
which in this case corresponds to an averaged spin-spin distance of 3.2 Å. This average
557
minimum distance of 3.2 Å between Cr(III) atoms provides additional insight regarding
558
the apparent structure of the sorbed Cr(III) clusters. Among the key Cr-(Cr,Al) 29
ACS Paragon Plus Environment
Environmental Science & Technology
559
distances inferred by EXAFS, the shortest (3.01 Å) may thus represent Cr-O-Al
560
interactions, likely an edge-sharing connection between Cr(III) in clusters to Al on the
561
nanoboehmite surface. To also achieve Cr-O-Cr bond lengths on the order of 3.45 Å,
562
such connections are more likely to be double corner-sharing. Both conditions are
563
compatible with the prospect of a β-CrOOH motif for the clusters directly bonded in an
564
inner-sphere fashion to the boehmite surface. Finally, it is noteworthy that the invariant
565
linewidth shown in Figure S3 indicates that the average minimum distance between
566
Cr(III) absorbed on nanoboehmite does not change with increasing Cr(III) loading.
567 568 569 570 571
Figure 11. EPR spectra of pure boehmite and Cr(III) adsorbed boehmite at different initial concentration of Cr(III) measured at 125 K (a); the weight percentage (wt%) of chromium absorbed in boehmite surface calculated as a function of the solution concentration (b) , and the Cr(III) EPR linewidth of different Cr(III)-boehmite samples (c).
572 573
The integrated findings converge upon a Cr(III) adsorption mechanism that
574
involves the surface-catalyzed self-assembly of adsorbed Cr(OH)4- monomers to form
575
clusters as a sparse monolayer at saturation coverages on the nanoboehmite surface.
576
Although the clusters are poorly ordered, the collective data allow for some conclusions
577
to be made regarding their structure. The local structure around Cr(III) is octahedral
578
and coordinated to both oxy and hydroxo groups. Both the EXAFS data and the ToF30
ACS Paragon Plus Environment
Page 30 of 43
Page 31 of 43
Environmental Science & Technology
579
SIMS results confirm the presence of Cr-O-Cr moieties. In addition, because both the
580
EPR data and the EXAFS data strongly suggest average nearest-neighbor Me…Me
581
distances greater than 3 Å, the local structure around the Cr atoms on boehmite is likely
582
not the same as that implied by the measured Cr2On secondary ions which, near their
583
energetic minimum, would contain Cr…Cr distances less than 2.3 Å80. The shortest Cr-
584
Cr bond distance (RCr…Cr) according to EPR is 3.2 Å, thus, the shorter EXAFS bond
585
distance (3.05 Å) likely corresponds to RCr-Al in edge-sharing Cr-O-Al octahedra that
586
connect the Cr(III) clusters to the nanobohemite surface. The observed Cr(III)-
587
(oxyhydr)oxide clusters appear dominated by corner-sharing Cr-O-Cr octahedral
588
linkages RCr-Cr of 3.45 Å and 3.95 Å.55, 72
589
Although it is difficult to posit a definite structure for the adsorbed Cr based on the
590
data assembled so far, analysis of the topologies of guyanaite and the boehmite (010)
591
surface showed a nearly heteroepitaxial lattice match in which two successive Cr atoms
592
along [100] share edges with two successive Al sites in a [101] column on the surface.
593
Such a structure, based on a strained guyanaite motif bound to the surface as depicted
594
in Figure 12, is compatible with the collective data set. Ongoing work entails molecular
595
simulations to test the veracity of this model.
31
ACS Paragon Plus Environment
Environmental Science & Technology
596 597
Figure 12. Proposed structure model for Cr(III) adsorption on boehmite (010).
598
The cluster formation mechanism is likely specific to these highly alkaline The high activity of the OH- anion is such that it is readily available as a
599
conditions.
600
metal-coordinating ligand both at the boehmite surface and in solution. We suggest that
601
the adsorption mechanism is based on an OH- ligand exchange process at the interface,
602
resulting in: (i) stabilization of inner-sphere Cr(OH)4- monomers on the boehmite
603
surface; and then (ii) their self-assembly polymerization into corner-sharing Cr-O-Cr
604
linkages that then stabilize the observed β-Cr(III)OOH-like clusters. Analogous to the
605
H+ ion exchange mechanism proposed for Cr(III) cation adsorption at low pH,
606
adsorption and polymerization of Cr(III) tetrahydroxyanions on the surface at high pH
607
may be mediated by OH- anion exchange processes.
608
In addition to answering our stated science questions, the insights obtained here
609
contribute more generally to the understanding of heavy metal adsorption on metal
610
(oxyhydroxide) nanomaterials in caustic environments, including in complex
611
radioactive liquid wastes, currently stored in tanks and awaiting processing at DOE 32
ACS Paragon Plus Environment
Page 32 of 43
Page 33 of 43
Environmental Science & Technology
612
nuclear legacy sites, such as Hanford.
613
ASSOCIATED CONTENT
614
Supporting Information
615
The Supporting Information is available free of charge on the ACS Publications website
616
at XXX.
617
Nitrogen adsorption-desorption isotherms curves of boehmite, ToF-SIMS and EPR
618
spectra of various Cr(III) adsorbed boehmite samples.
619
AUTHOR INFORMATION
620
Corresponding Authors
621
* Email:
[email protected](X. Z.),
[email protected](P. L.),
622
[email protected] (Z. W.), and
[email protected] (K. M. R.)
623
ORCID
624
Xin Zhang: 0000-0003-2000-858X
625
Zihua Zhu: 0000-0001-5770-8462
626
Kevin Rosso: 0000-0002-8474-7720
627
Notes
628
The authors declare no competing financial interest.
629
ACKNOWLEDGMENTS
630
The authors thank PNNL scientists Odeta Qafoku and Charles T. Resch for the help on 33
ACS Paragon Plus Environment
Environmental Science & Technology
631
the BET and ICP-MS measurements. This work was supported by IDREAM
632
(Interfacial Dynamics in Radioactive Environments and Materials), an Energy Frontier
633
Research Center funded by the U.S. Department of Energy (DOE), Office of Science,
634
Basic Energy Sciences (BES). A portion of this research was performed using EMSL,
635
a national scientific user facility sponsored by the DOE Office of Biological and
636
Environmental Research and located at PNNL. PNNL is a multiprogram national
637
laboratory operated for DOE by Battelle Memorial Institute under Contract DE-AC05-
638
76RL0-1830. WWC thanks the support from the China Scholarship Council.
639
REFERENCES
640
1.
641
onto Self-Assembled Monolayers: A Model System for the Study of Interactions of
642
Colloidal Particles and Organic Surfaces. Langmuir 1997, 13, (2), 119-121.
643
2.
644
Engineered Nanomaterials in Vascular plants. Environ. Sci. Technol. 2012, 46, (17),
645
9224-39.
646
3.
647
Organic/Inorganic Composite Nanoparticles: Tuning Full Color Spectrum. Chem.
648
Mater. 2012, 24, (17), 3415-3419.
649
4.
650
Treatment. J. Environ. Anal. Toxicol. 2012, 02, (07), 1000154.
651
5.
652
D. M.; De'Angeli, S. M.; Vick, S. C.; Fan, H., A novel family of structurally
653
characterized lithium cobalt double aryloxides and the nanoparticles and thin films
654
generated therefrom Chem. Mater. 2003, 15, (20), 3903–3912.
655
6.
656
Nanoparticles into Active Nanostructures. iScience 2019, 11, 272-293.
Fan, H.; López, G. P., Adsorption of Surface-Modified Colloidal Gold Particles
Miralles, P.; Church, T. L.; Harris, A. T., Toxicity, Uptake, and Translocation of
Sun, Z.; Bai, F.; Wu, H.; Boye, D. M.; Fan, H., Monodisperse Fluorescent
Wang, X., Nanomaterials as Sorbents to Remove Heavy Metal Ions in Wastewater
Boyle, T. J.; Rodriguez, M. A.; Ingersoll, D.; Headley, T. J.; Bunge, S. D.; Pedrotty,
Wei, W.; Bai, F.; Fan, H., Surfactant-Assisted Cooperative Self-Assembly of
34
ACS Paragon Plus Environment
Page 34 of 43
Page 35 of 43
Environmental Science & Technology
657
7.
Hua, M.; Zhang, S.; Pan, B.; Zhang, W.; Lv, L.; Zhang, Q., Heavy metal removal
658
from water/wastewater by nanosized metal oxides: a review. J. Hazard. Mater. 2012,
659
211-212, 317-31.
660
8.
661
metal pollution from mines in China: pollution and health risk assessment. Sci. Total
662
Environ. 2014, 468-469, 843-53.
663
9.
664
heavy metals via dietary intake of foodstuffs from the wastewater irrigated site of a dry
665
tropical area of India. Food Chem Toxicol 2010, 48, (2), 611-9.
666
10. Qiu, B.; Wang, Y.; Sun, D.; Wang, Q.; Zhang, X.; Weeks, B. L.; O'Connor, R.;
667
Huang, X.; Wei, S.; Guo, Z., Cr(vi) removal by magnetic carbon nanocomposites
668
derived from cellulose at different carbonization temperatures. J. Mater. Chem. A 2015,
669
3, (18), 9817-9825.
670
11. Qiu, B.; Guo, J.; Zhang, X.; Sun, D.; Gu, H.; Wang, Q.; Wang, H.; Wang, X.;
671
Zhang, X.; Weeks, B. L.; Guo, Z.; Wei, S., Polyethylenimine facilitated ethyl cellulose
672
for hexavalent chromium removal with a wide pH range. ACS Appl. Mater. Interfaces
673
2014, 6, (22), 19816-24.
674
12. Huang, J.; Cao, Y.; Shao, Q.; Peng, X.; Guo, Z., Magnetic Nanocarbon Adsorbents
675
with Enhanced Hexavalent Chromium Removal: Morphology Dependence of Fibrillar
676
vs Particulate Structures. Ind. Eng. Chem. Res. 2017, 56, (38), 10689-10701.
677
13. Rodriguez, A. T.; Li, X.; Wang, J.; Steen, W. A.; Fan, H., Facile Synthesis of
678
Nanostructured Carbon through Self-Assembly between Block Copolymers and
679
Carbohydrates. Adv. Funct. Mater. 2007, 17, (15), 2710-2716.
680
14. Huang, X.; Hou, X.; Song, F.; Zhao, J.; Zhang, L., Facet-dependent Cr(VI)
681
adsorption of hematite nanocrystals. Environ. Sci. Technol. 2016, 50, (4), 1964-1972.
682
15. Huang, X.; Hou, X.; Zhang, X.; Rosso, K. M.; Zhang, L., Facet-dependent
683
contaminant removal properties of hematite nanocrystals and their environmental
684
implications. Environ. Sci. Nano 2018, 5, (8), 1790-1806.
685
16. Balladares, E.; Jerez, O.; Parada, F.; Baltierra, L.; Hernández, C.; Araneda, E.;
686
Parra, V., Neutralization and co-precipitation of heavy metals by lime addition to
Li, Z.; Ma, Z.; van der Kuijp, T. J.; Yuan, Z.; Huang, L., A review of soil heavy
Singh, A.; Sharma, R. K.; Agrawal, M.; Marshall, F. M., Health risk assessment of
35
ACS Paragon Plus Environment
Environmental Science & Technology
687
effluent from acid plant in a copper smelter. Miner. Eng. 2018, 122, 122-129.
688
17. Chen, Q.; Yao, Y.; Li, X.; Lu, J.; Zhou, J.; Huang, Z., Comparison of heavy metal
689
removals from aqueous solutions by chemical precipitation and characteristics of
690
precipitates. J. Water Process Eng. 2018, 26, 289-300.
691
18. Moosavirad, S. M.; Sarikhani, R.; Shahsavani, E.; Mohammadi, S. Z., Removal of
692
some heavy metals from inorganic industrial wastewaters by ion exchange method. J.
693
Water Chem. Technol. 2015, 37, (4), 191-199.
694
19. Tavakoli, O.; Goodarzi, V.; Saeb, M. R.; Mahmoodi, N. M.; Borja, R., Competitive
695
removal of heavy metal ions from squid oil under isothermal condition by CR11 chelate
696
ion exchanger. J. Hazard. Mater. 2017, 334, 256-266.
697
20. Zhao, Z.; An, H.; Lin, J.; Feng, M.; Murugadoss, V.; Ding, T.; Liu, H.; Shao, Q.;
698
Mai, X.; Wang, N.; Gu, H.; Angaiah, S.; Guo, Z., Progress on the Photocatalytic
699
Reduction Removal of Chromium Contamination. Chem. Rec. 2018, 18, 1-11.
700
21. Ates, N.; Uzal, N., Removal of heavy metals from aluminum anodic oxidation
701
wastewaters by membrane filtration. Environ. Sci. Pollut Res. Int. 2018, 25, (22),
702
22259-22272.
703
22. Blöcher, C.; Dorda, J.; Mavrov, V.; Chmiel, H.; Lazaridis, N. K.; Matis, K. A.,
704
Hybrid flotation—membrane filtration process for the removal of heavy metal ions
705
from wastewater. Water Res. 2003, 37, (16), 4018-4026.
706
23. Ye, C.-C.; An, Q.-F.; Wu, J.-K.; Zhao, F.-Y.; Zheng, P.-Y.; Wang, N.-X.,
707
Nanofiltration membranes consisting of quaternized polyelectrolyte complex
708
nanoparticles for heavy metal removal. Chem. Eng. J. 2019, 359, 994-1005.
709
24. Rosa, M. A.; Egido, J. A.; Márquez, M. C., Enhanced electrochemical removal of
710
arsenic and heavy metals from mine tailings. J. Taiwan Inst.Chem.Eng. 2017, 78, 409-
711
415.
712
25. Xu, F.; Liu, Y.; Liu, C., A Generalized-Rate Model for Describing and Scaling
713
Redox Kinetics in Sediments Containing Variable Redox-Reactive Materials. Environ.
714
Sci. Technol. 2018, 52, (9), 5268-5276.
715
26. Liu, Y.; Xu, F.; Liu, C., Coupled Hydro-Biogeochemical Processes Controlling Cr
716
Reductive Immobilization in Columbia River Hyporheic Zone. Environ. Sci. Technol. 36
ACS Paragon Plus Environment
Page 36 of 43
Page 37 of 43
Environmental Science & Technology
717
2017, 51, (3), 1508-1517.
718
27. Gong, K.; Guo, S.; Zhao, Y.; Hu, Q.; Liu, H.; Sun, D.; Li, M.; Qiu, B.; Guo, Z.,
719
Bacteria cell templated porous polyaniline facilitated detoxification and recovery of
720
hexavalent chromium. J. Mater. Chem. A 2018, 6, (35), 16824-16832.
721
28. Qiu, B.; Gu, H.; Yan, X.; Guo, J.; Wang, Y.; Sun, D.; Wang, Q.; Khan, M.; Zhang,
722
X.; Weeks, B. L.; Young, D. P.; Guo, Z.; Wei, S., Cellulose derived magnetic
723
mesoporous carbon nanocomposites with enhanced hexavalent chromium removal. J.
724
Mater. Chem. A 2014, 2, (41), 17454-17462.
725
29. Baumer, T.; Hixon, A. E., Kinetics of europium sorption to four different aluminum
726
(hydr)oxides: Corundum, gamma-alumina, bayerite, and gibbsite. J. Environ. Radioact.
727
2018, 195, 20-25.
728
30. Dubey, S. P.; Dwivedi, A. D.; Sillanpaa, M.; Lee, H.; Kwon, Y. N.; Lee, C.,
729
Adsorption of As(V) by boehmite and alumina of different morphologies prepared
730
under hydrothermal conditions. Chemosphere 2017, 169, 99-106.
731
31. Granados-Correa, F.; Jimenez-Becerril, J., Chromium (VI) adsorption on boehmite.
732
J. Hazard. Mater. 2009, 162, (2-3), 1178-84.
733
32. Zhang, H.; Li, P.; Wang, Z.; Zhang, X.; Zheng, S.; Zhang, Y., In Situ Synthesis of
734
γ-AlOOH and Synchronous Adsorption Separation of V(V) from Highly Concentrated
735
Cr(VI) Multiplex Complex solutions. ACS Sustain. Chem. Eng. 2017, 5, (8), 6674-6681.
736
33. Liu, W.; Wang, T.; Borthwick, A. G.; Wang, Y.; Yin, X.; Li, X.; Ni, J., Adsorption
737
of Pb(2)(+), Cd(2)(+), Cu(2)(+) and Cr(3)(+) onto titanate nanotubes: competition and
738
effect of inorganic ions. Sci. Total Environ. 2013, 456-457, 171-80.
739
34. Cui, W.; Li, P.; Wang, Z.; Zheng, S.; Zhang, Y., Adsorption study of selenium ions
740
from aqueous solutions using MgO nanosheets synthesized by ultrasonic method. J.
741
Hazard. Mater. 2018, 341, 268-276.
742
35. Sari, A.; Tuzen, M.; Soylak, M., Adsorption of Pb(II) and Cr(III) from aqueous
743
solution on Celtek clay. J. Hazard. Mater. 2007, 144, (1-2), 41-6.
744
36. Granados-Correa, F.; Jimenez-Becerril, J., Chromium (VI) adsorption on boehmite.
745
J. Hazard Mater. 2009, 162, (2-3), 1178-84.
746
37. Li, P.; Zheng, S.; Qing, P.; Chen, Y.; Tian, L.; Zheng, X.; Zhang, Y., The vanadate 37
ACS Paragon Plus Environment
Environmental Science & Technology
747
adsorption on a mesoporous boehmite and its cleaner production application of
748
chromate. Green Chem. 2014, 16, (9), 4214-4222.
749
38. Zhang, Y.-X.; Jia, Y.; Jin, Z.; Yu, X.-Y.; Xu, W.-H.; Luo, T.; Zhu, B.-J.; Liu, J.-
750
H.; Huang, X.-J., Self-assembled, monodispersed, flower-like γ-AlOOH hierarchical
751
superstructures for efficient and fast removal of heavy metal ions from water.
752
CrystEngComm 2012, 14, (9), 3005-3007.
753
39. Zhang, M.; Gao, B., Removal of arsenic, methylene blue, and phosphate by
754
biochar/AlOOH nanocomposite. Chem. Eng. J. 2013, 226, 286-292.
755
40. Zhang, Y.-X.; Yu, X.-Y.; Jin, Z.; Jia, Y.; Xu, W.-H.; Luo, T.; Zhu, B.-J.; Liu, J.-
756
H.; Huang, X.-J., Ultra high adsorption capacity of fried egg jellyfish-like γ-
757
AlOOH(Boehmite)@SiO2/Fe3O4 porous magnetic microspheres for aqueous Pb(II)
758
removal. J. Mater. Chem. 2011, 21, (41), 16550-16557.
759
41. Granados-Correa, F.; Corral-Capulin, N. G.; Olguín, M. T.; Acosta-León, C. E.,
760
Comparison of the Cd(II) adsorption processes between boehmite (γ-AlOOH) and
761
goethite (α-FeOOH). Chem. Eng. J. 2011, 171, (3), 1027-1034.
762
42. Nordin, J.; Persson, P.; Laiti, E.; Sjöberg, S., Adsorption of o-Phthalate at the
763
Water−Boehmite (γ-AlOOH) Interface-Evidence for Two Coordination Modes.
764
Langmuir 1997, 13, (15), 4085–4093.
765
43. Zhang, X.; Huestis, P. L.; Pearce, C. I.; Hu, J. Z.; Page, K.; Anovitz, L. M.;
766
Aleksandrov, A. B.; Prange, M. P.; Kerisit, S.; Bowden, M. E.; Cui, W.; Wang, Z.;
767
Jaegers, N. R.; Graham, T. R.; Dembowski, M.; Wang, H.-W.; Liu, J.; N’Diaye, A. T.;
768
Bleuel, M.; Mildner, D. F. R.; Orlando, T. M.; Kimmel, G. A.; La Verne, J. A.; Clark,
769
S. B.; Rosso, K. M., Boehmite and Gibbsite Nanoplates for the Synthesis of Advanced
770
Alumina Products. ACS Appl. Nano Mater. 2018, 1, (12), 7115-7128.
771
44. Prange, M. P.; Zhang, X.; Bowden, M. E.; Shen, Z.; Ilton, E. S.; Kerisit, S. N.,
772
Predicting Surface Energies and Particle Morphologies of Boehmite (γ-AlOOH) from
773
Density Functional Theory. J. Phys. Chem. C 2018, 122, (19), 10400-10412.
774
45. Prange, M. P.; Zhang, X.; Ilton, E. S.; Kovarik, L.; Engelhard, M. H.; Kerisit, S.
775
N., Electronic response of aluminum-bearing minerals. J. Chem. Phys. 2018, 149, (2),
776
024502. 38
ACS Paragon Plus Environment
Page 38 of 43
Page 39 of 43
Environmental Science & Technology
777
46. Peterson, R. A.; Buck, E. C.; Chun, J.; Daniel, R. C.; Herting, D. L.; Ilton, E. S.;
778
Lumetta, G. J.; Clark, S. B., Review of the Scientific Understanding of Radioactive
779
Waste at the U.S. DOE Hanford Site. Environ. Sci. Technol. 2018, 52, (2), 381-396.
780
47. Chatterjee, S.; Conroy, M. A.; Smith, F. N.; Jung, H.-J.; Wang, Z.; Peterson, R. A.;
781
Huq, A.; Burtt, D. G.; Ilton, E. S.; Buck, E. C., Can Cr(iii) substitute for Al(iii) in the
782
structure of boehmite? RSC Adv. 2016, 6, (109), 107628-107637.
783
48. Huestis, P.; Pearce, C. I.; Zhang, X.; N'Diaye, A. T.; Rosso, K. M.; LaVerne, J. A.,
784
Radiolytic stability of gibbsite and boehmite with adsorbed water. J. Nucl. Mater. 2018,
785
501, 224-233.
786
49. Anovitz, L. M.; Zhang, X.; Soltis, J. A.; Nakouzi, E.; Krzysko, A. J.; Chun, J.;
787
Schenter, G. K.; Graham, T. R.; Rosso, K. M.; De Yoreo, J. J.; Stack, A. G.; Bleuel,
788
M.; Gagnon, C.; Mildner, D. F. R.; Ilavsky, J.; Kuzmenko, I., Effects of Ionic Strength,
789
Salt, and pH on Aggregation of Boehmite Nanocrystals: Tumbler Small-Angle Neutron
790
and X-ray Scattering and Imaging Analysis. Langmuir 2018, 34, 15839−15853.
791
50. Nakouzi, E.; Soltis, J. A.; Legg, B. A.; Schenter, G. K.; Zhang, X.; Graham, T. R.;
792
Rosso, K. M.; Anovitz, L. M.; De Yoreo, J. J.; Chun, J., Impact of Solution Chemistry
793
and Particle Anisotropy on the Collective Dynamics of Oriented Aggregation. ACS
794
Nano 2018, 12, (10), 10114-10122.
795
51. Conroy, M.; Soltis, J. A.; Wittman, R. S.; Smith, F. N.; Chatterjee, S.; Zhang, X.;
796
Ilton, E. S.; Buck, E. C., Importance of interlayer H bonding structure to the stability
797
of layered minerals. Sci. Rep. 2017, 7, (1), 13274.
798
52. Rai, D.; Eary, L. E.; Zachara, J. M., Environmental chemistry of chromium. Sci.
799
Total Environ. 1989, 86, (1-2), 15-23.
800
53. Rai, D.; Sass, B. M.; Moore, D. A., Chromitim(III) Hydrolysis Constants and
801
Solubility of Chromium(III) Hydroxide. Inorg. Chem. 1987, 26, 345-349.
802
54. Rai, D.; Moore, D. A.; Hess, N. J.; Rosso, K. M.; Rao, L.; Heald, S. M.,
803
Chromium(III) Hydroxide Solubility in the Aqueous K+-H+-OH−-CO2-HCO 3 − -CO
804
3 2− -H2O System: A Thermodynamic Model. J. Solution Chem. 2007, 36, (10), 1261-
805
1285.
806
55. Charlet, L.; Manceau, A., X-ray absorption spectroscopic study of the sorption of 39
ACS Paragon Plus Environment
Environmental Science & Technology
807
Cr(III) at the oxide-water interface: II. Adsorption, Coprecipitation, and Surface
808
Precipitation on Hydrous Ferric Oxide. J. Colloid Interface Sci. 1991, 148, (2), 443-
809
458.
810
56. Zhang, X.; Cui, W.; Page, K. L.; Pearce, C. I.; Bowden, M. E.; Graham, T. R.;
811
Shen, Z.; Li, P.; Wang, Z.; Kerisit, S.; N’Diaye, A. T.; Clark, S. B.; Rosso, K. M., Size
812
and Morphology Controlled Synthesis of Boehmite Nanoplates and Crystal Growth
813
Mechanisms. Cryst. Growth Des. 2018, 18, (6), 3596-3606.
814
57. Ravel, B.; Newville, M., ATHENA, ARTEMIS, HEPHAESTUS: data analysis for
815
X-ray absorption spectroscopy using IFEFFIT. J. Synchrotron Radiat. 2005, 12, (Pt 4),
816
537-41.
817
58. Ruan, H. D.; Frost, R. L.; Kloprogge, J. T., Comparison of Raman spectra in
818
characterizing gibbsite, bayerite, diaspore and boehmite. J. Raman Spectrosc. 2001, 32,
819
(9), 745-750.
820
59. Peterson, R. A.; Buck, E. C.; Chun, J.; Daniel, R. C.; Herting, D. L.; Ilton, E. S.;
821
Lumetta, G. J.; Clark, S. B., Review of the Scientific Understanding of Radioactive
822
Waste at the U.S. DOE Hanford Site. Environ Sci Technol 2018, 52, (2), 381-396.
823
60. Miretzky, P.; Cirelli, A. F., Cr(VI) and Cr(III) removal from aqueous solution by
824
raw and modified lignocellulosic materials: a review. J. Hazard. Mater. 2010, 180, (1-
825
3), 1-19.
826
61. Lyubchik, S. I.; Lyubchik, A. I.; Galushko, O. L.; Tikhonova, L. P.; Vital, J.;
827
Fonseca, I. M.; Lyubchik, S. B., Kinetics and thermodynamics of the Cr(III) adsorption
828
on the activated carbon from co-mingled wastes. Colloids Surf., A 2004, 242, (1-3),
829
151-158.
830
62. Tahir, S.; Naseem, R., Removal of Cr(III) from tannery wastewater by adsorption
831
onto bentonite clay. Sep. Purif. Technol. 2007, 53, (3), 312-321.
832
63. Wu, Y.; Zhang, S.; Guo, X.; Huang, H., Adsorption of chromium(III) on lignin.
833
Bioresour Technol 2008, 99, (16), 7709-15.
834
64. Yazaydin, A. O.; Bowers, G. M.; Kirkpatrick, R. J., Molecular dynamics modeling
835
of carbon dioxide, water and natural organic matter in Na-hectorite. Phys. Chem. Chem.
836
Phys. 2015, 17, (36), 23356-23367. 40
ACS Paragon Plus Environment
Page 40 of 43
Page 41 of 43
Environmental Science & Technology
837
65. Egodawatte, S.; Datt, A.; Burns, E. A.; Larsen, S. C., Chemical Insight into the
838
Adsorption of Chromium(III) on Iron Oxide/Mesoporous Silica Nanocomposites.
839
Langmuir 2015, 31, (27), 7553-7562.
840
66. Wang, T.; Liu, W.; Xiong, L.; Xu, N.; Ni, J., Influence of pH, ionic strength and
841
humic acid on competitive adsorption of Pb(II), Cd(II) and Cr(III) onto titanate
842
nanotubes. Chem. Eng. J. 2013, 215-216, 366-374.
843
67. Kloprogge, J. T.; Duong, L. V.; Wood, B. J.; Frost, R. L., XPS study of the major
844
minerals in bauxite: gibbsite, bayerite and (pseudo-)boehmite. J. Colloid Interface Sci.
845
2006, 296, (2), 572-6.
846
68. Benninghoven, A., Chemical Analysis of Inorganic and Organic Surfaces and Thin
847
Films by Static Time‐of‐Flight Secondary Ion Mass Spectrometry (TOF‐SIMS). Angew
848
Chem. Int. Edit 1994, 33, (10), 1023-1043.
849
69. Frommer, J.; Nachtegaal, M.; Czekaj, I.; Kretzschmar, R., The Cr X-ray absorption
850
K-edge structure of poorly crystalline Fe(III)-Cr(III)-oxyhydroxides. Am. Mineral.
851
2010, 95, (8-9), 1202-1213.
852
70. Corbato, C. E.; T., T. R.; Christoph, G. G., Structure refinement of deuterated
853
boehmite. Clay. Clay Miner. 1985, 33, (1), 71-75.
854
71. Rosso, K. M.; Rustad, J. R., Structures and energies of AlOOH and FeOOH
855
polymorphs from plane wave pseudopotential calculations. Am. Mineral. 2001, 86,
856
312-317.
857
72. N. Thomas, A.; Eiche, E.; Göttlicher, J.; Steininger, R.; G. Benning, L.; M.
858
Freeman, H.; Dideriksen, K.; Neumann, T., Products of Hexavalent Chromium
859
Reduction by Green Rust Sodium Sulfate and Associated Reaction Mechanisms. Soil
860
Systems 2018, 2, (4), 58.
861
73. Milton, C.; Appleman, D. E. A., M. H.; Chao, E. C. T.; Cuttita, F.; Dinnin, J. I.;
862
Dwornik, E. J.; Ingram, B. L.; Rose, H. J., Merumite, a complex assemblage of
863
chromium minerals from Guyana. US Geol. Surv. Prof. Pap. 1976, 887, 1-29.
864
74. Christensen, A. N.; Hansen, P.; Lehmann, M. S., Isotope effects in the bonds of α-
865
CrOOH and α-CrOOD. J. Solid State Chem. 1977, 21, 325-329.
866
75. Christensen, A. N.; Hansen, P.; Lehmann, M. S., Isotope effects in the bonds of β41
ACS Paragon Plus Environment
Environmental Science & Technology
Page 42 of 43
867
CrOOH and β-CrOOD. J. Solid State Chem. 1976, 19, (3), 299-304.
868
76. Fujihara, T.; Ichikawa, M.; Gustafsson, T.; Olovsson, I.; Tsuchida, T., Powder-
869
neutron diffraction studies of geometric isotope and hydrogen-bonding effects in β-
870
CrOOH. J. Phys. Chem. Solids 2002, 63, (2), 309-315.
871
77. Van Vleck, J. H., The Dipolar Broadening of Magnetic Resonance Lines in
872
Crystals. Phys. Rev. 1948, 74, (9), 1168-1183.
873
78. Stoll, S., Chapter Six - CW-EPR Spectral Simulations: Solid State. In Methods
874
Enzymol., Qin, P. Z.; Warncke, K., Eds. Academic Press: 2015; Vol. 563, pp 121-142.
875
79. Walter, E. D.; Sebby, K. B.; Usselman, R. J.; Singel, D. J.; Cloninger, M. J.,
876
Characterization
877
Spectrometry and EPR Spectroscopy. .J. Phys. Chem. B 2005, 109, (46), 21532-21538.
878
80. Veliah, S.; Xiang, K.-H.; Pandey, R.; Recio, J. M.; Newsam, J. M., Density
879
Functional Study of Chromium Oxide Clusters: Structures, Bonding, Vibrations, and
880
Stability. J. Phys. Chem. B 1998, 102, 1126-1135.
of
Heterogeneously
Functionalized
881
42
ACS Paragon Plus Environment
Dendrimers
by
Mass
Page 43 of 43
882
Environmental Science & Technology
For Table of Contents Use Only
883 884
High resolution AFM images indicate the Cr(III) adsorption by cluster formation on
885
aluminum oxyhydroxide boehmite (γ-AlOOH) nanoplates in caustic environments.
886
43
ACS Paragon Plus Environment