Goethite nanoparticle aggregation: effects of buffers, metal ions, and 4-chloronitrobenzene reduction

Amanda M. Stemig a, Tram Anh Do a, Virany M. Yuwono a, William A. Arnold b and R. Lee Penn *a
aDepartment of Chemistry, 207 Pleasant St SE, Minneapolis, MN 55455, USA. E-mail: rleepenn@umn.edu; Fax: +01 612 626 7541; Tel: +01 612 624 6000
bDepartment of Civil Engineering, 500 Pillsbury Dr SE, Minneapolis, MN 55455, USA. E-mail: arnol032@umn.edu; Fax: +01 612 626 7750; Tel: +01 612 625 8582

Received 24th October 2013 , Accepted 7th July 2014

First published on 31st July 2014


Abstract

Iron mineral systems are effective at transforming highly oxidized contaminants in natural and engineered systems. The rate at which the contaminant degrades may be influenced by the amount of available mineral surface area. This study used dynamic light scattering and cryogenic transmission electron microscopy to monitor changes in the aggregation state of goethite nanoparticles before and after reaction with 4-chloronitrobenzene (4-ClNB). The effects of buffer identity, buffer concentration, and adsorbing metal identity on the goethite nanoparticle suspension characteristics and reactivity were monitored. Results demonstrate that buffers, which serve to hold pH nearly constant over the course of a reaction, are not benign additives in batch reactors. In fact, the identity and concentration of the buffer used strongly influences the rate of 4-ClNB degradation by surface-associated ferrous ion. Increasing buffer concentration resulted in more compact goethite nanoparticle aggregates, and slower 4-ClNB degradation was observed. In addition, the rate of degradation changed dramatically with changing buffer identity, with rates of reaction changing by an order of magnitude when switching from 4-(2-hydroxyethyl)-1-piperazineethanesulfonic acid (HEPES) to tris(2-hydroxyethyl)amine (TEA). Finally, of the three metal ions selected (Ca(II), Fe(II), and Co(II)), the addition and adsorption of the two transition metals resulted in a dramatic decrease in the average nanoparticle aggregate size. Furthermore, oxidation of the adsorbed Fe(II), via O2 or 4-ClNB reduction, yielded decreases in zeta potential and increases in aggregate size. This work demonstrates that small changes in reaction parameters have a large effect on the rate of contaminant degradation through changes in nanoparticle aggregation state.



Nano impact

Little is known about how natural and synthetic chemical species affect the reactivity of nanoparticles under environmentally relevant conditions. Specifically, aggregation state is predicted to strongly impact the accessible reactive surface area, and aggregation state is sensitive to solution conditions. It is essential to elucidate the links between reactivity and the aggregation states of nanoparticles. This work, which primarily focuses on the reductive degradation of 4-chloronitrobenzene by iron(II) adsorbed onto goethite surfaces, demonstrates that both the rates of degradation of environmental contaminants and the extent of nanoparticle aggregation are intimately linked. Changes to how reactors are prepared can dramatically affect the rates of reaction, the degree to which the goethite surfaces are charged, and the aggregation state of the iron oxide nanoparticles. Variables such as the buffer employed, as well as its concentration, as well as other additives, such as metal ions added, can result in substantial differences in experimental rate constants. This work combines quantification of degradation rates with quantification of aggregation state, including some analysis of direct images of aggregates in vitrified solution via cryogenic transmission electron microscopy.

Introduction

Groundwater is an important fraction of the water supply throughout the United States. In 2005, 20% of water used in the United States was withdrawn from groundwater.1 Many oxidized organic compounds, including chlorinated solvents, nitroaromatic compounds, and pesticides are present as contaminants in groundwater.2,3 These chemicals have been designed with highly oxidized components in their structures, making them not only effective for their intended use but also stable in oxic environments. These compounds are frequently found as persistent contaminants in groundwater systems and, thus, pose an exposure risk to humans and wildlife.4–9 More than thirty years after the passage of the Comprehensive Environmental Response, Compensation, and Liability Act (i.e. Superfund), groundwater contamination still presents a challenge, in terms of remediation and the return of water resources to unrestricted use.10 While stability in oxic environments facilitates the transport of pollutants between soil and groundwater phases, the presence of oxidized functional groups suggests that reduction provides a means for the breakdown or remediation of these compounds.

In groundwater, a reductant known to reduce oxidized contaminants is Fe(II) associated with an iron mineral surface. Iron oxides such as ferrihydrite, goethite, magnetite, hematite, and lepidocrocite are ubiquitous in the environment and readily adsorb Fe(II) ions.11 Degradation reactions of oxidized pollutants have been shown to be both efficient and rapid in these systems.12–19 This is due to the formation of reactive capacity after association of the Fe(II) ions with the iron mineral.20,21 The amount of adsorbed Fe(II),13,16,22 suspension pH,13,16,23,24 and the adsorption of other constituents12,18,19,22,25–27 each affect the formation of reactive sites and dramatically alter the rate of contaminant reduction.

The number of reactive sites is directly related to specific surface area. Surface area increases with decreasing particle size, which means, on a mass normalized basis, the smallest mineral nanoparticles will contribute the most surface area.28 Nanoparticles, however, are highly susceptible to aggregation, which can physically block access to reactive sites. This effect was shown by Vikesland et al.,29 who demonstrated that by increasing the ionic strength of the suspension, magnetite nanoparticles aggregated, and the observed rate of carbon tetrachloride loss decreased.

The goal of this research is to elucidate the link between the aggregation state of iron oxide nanoparticles and their reactivity. Such nanoparticles may be present naturally11 or introduced in an engineered remediation scheme.30–33 4-Chloronitrobenzene (4-ClNB) was selected as a model contaminant due to its previous use as a probe compound34–39 and its nitro group represents relevant classes of environmental contaminants (explosives and pesticides).40

In addition to measuring kinetics of pollutant degradation, this study investigates changes in nanoparticle aggregation in situ by using dynamic light scattering (DLS) and cryogenic transmission electron microscopy (cryo-TEM). DLS measures the intensity of scattered light from suspended objects, enabling dynamic assessment of aggregation state. The working hypothesis is that larger aggregates will have more points of internal contact and thus, less surface area accessible to the surrounding solution for the degradation of environmental contaminants. An alternative hypothesis is that electron shuttling from one primary crystallite to another may result in faster kinetics than expected based on accessible surface area.41,42 Cryo-TEM enables the direct imaging of vitrified samples, which can be collected at any point during a reaction and thus serve as snapshots of the aggregation state during an experiment. Together, DLS and cryo-TEM enable quantitative characterization of aggregation state before, during, and after reaction.

Results and discussion

Crucial to continued work in this area is consistency in experimental work so as to facilitate meaningful comparisons between laboratories. A survey of a sampling (78 in total) of recent research articles in the field (Fig. 1)12–17,19–26,29,34–36,38,39,43–100 demonstrate substantial variation in the preparation of reactors for degradation reactions of environmental contaminants. Variations include buffer type, the order in which reagents (buffer, mineral, Fe(II), contaminant) are added, the number of equilibrations upon addition of reagents, the length of time allowed for equilibration, and number and identity of constituents present during each equilibration step. Buffer concentrations ranged from 0.4 to 100 mM, a mean of 32 mM, and median of 25 mM (with one extreme outlier of 1 M excluded from this analysis). Small differences in reaction conditions may be largely irrelevant or may fundamentally change the properties of the nanoparticle suspension such that comparisons of datasets become impossible. A goal of this work was to evaluate a subset of potentially important batch reactor variables so as to determine which variables of the experimental protocol do and do not facilitate quantitative and qualitative comparisons of reactivity in goethite nanoparticle systems.
image file: c3en00063j-f1.tif
Fig. 1 Graphical representation of iron mineral reactor preparation parameters from a sampling of 78 research articles. The buffer identity used in each study (note that the total exceeds 78 as multiple studies used various buffers) and the number of steps with equilibration periods in which the constituents are added (insert) were summarized to show the variation in procedures applied.

Goethite particle characteristics

The goethite particles employed here had dimensions of 63.7 ± 22.9 nm by 8.9 ± 3.9 nm as measured by TEM and surface area of 136.8 m2 g−1 as measured by N2 adsorption. The mineral identity was confirmed by X-ray diffraction. Additional details are in the ESI (Fig. S1, Table S1, and Fig. S2).

Buffer concentration and metal ions: pre-reaction

Aggregate sizes (from DLS) and zeta potentials (a surrogate for surface charge) in MOPS buffer before and after divalent metal ion addition are summarized in Table 1. In 20 mM MOPS buffer, the primary goethite particles form large aggregates. The value obtained using DLS, approximately 3000 nm, is near the upper limit for the DLS instrument, which means we can conclude only that the aggregates are large. However, the data point provides a basis for comparison to other conditions.
Table 1 Goethite aggregate sizes and zeta potentials measured using dynamic light scattering
Goethite only Goethite + 1 mM Fe(II) Goethite + 1 mM M(II)
MOPS concentration (mM) Diameter (nm) Zeta potential (mV) Diametera (nm) Zeta potential (mV) Diameterb (nm) Zeta potentialb (mV)
a Errors represent standard deviation from three measurements on a single sample. b For each pair of numbers, the first a measurement taken when the metal was added after the goethite and MOPS buffer had equilibrated for 18 hours (sample I) and the second is the measurement take when the metal was added after the goethite and MOPS buffer had equilibrated for 36 hours (sample II). c Average and standard deviation of nine separate preparations of goethite in 20 mM pH 7 MOPS. d Beyond the upper quantitative detection limit of the instrumentation.
5 96 ± 4 46
10 71 ± 4 42
20 3055d ± 1055c 30.9 ± 2.4c 260 ± 64 32 Fe(II): 240, 180 41, 38
Co(II): 180, 170 42, 41
Ca2+: 2300, 1700 22, 27
30 500 ± 150 17
40 640 ± 130 15
50 980 ± 540 9


The concentration of buffer present within a reaction system affects aggregation of the goethite nanoparticles. The effect of buffer concentration was tested in the presence of 1 mM Fe(II) but prior to 4-ClNB addition. MOPS buffer was selected for the buffer concentration experiments due to its frequency of use in past studies (Fig. 1).17,26,36 A general upward trend in aggregate size was observed via both DLS (Table 1) and cryo-TEM (Fig. 2) with increasing buffer concentration. For cryo-TEM analysis, goethite suspensions in 10, 20, and 50 mM were selected (6 images per concentration), and the images suggest that the average aggregate size is similar in 10 and 20 mM MOPS, but there is a significant size increase observed for goethite suspended in 50 mM MOPS. Despite the marked differences in size, the average aggregate density was statistically similar across all three buffer concentrations. Additional aggregate analysis revealed that a majority (>50%) of all nanoparticle contacts within an aggregate occurred along the major nanoparticle axis (Fig. 2; complete TEM analysis results in ESI, Fig. S3). Previous results have demonstrated that the goethite {021} are the reactive surfaces, which could mean that such side-by-side contacts may not significantly affect accessible, reactive surface area.34 Finally, zeta potential measurements clearly demonstrate a dramatic drop in surface charge as a function of increasing MOPS concentration. This parallels the increase in aggregate size as observed by DLS. With the observation that many of the particle–particle contacts occurs along the long-axis of the nanocrystals, one could hypothesize that MOPS molecules primarily adsorb onto the 110 type surfaces, resulting in a drop in surface charge for those surfaces. At pH 7, the particles are clearly positively charged, and the adsorption of deprotonated, negatively charged MOPS molecules results in a net drop in surface charge. If that drop in net charge primarily occurs via the 110 type surfaces, then aggregation across those surfaces may be promoted. Alternatively, MOPS may primarily adsorb onto the nanocrystal tips, resulting in steric repulsion between the tips, which could effectively promote aggregation in a side-by-side configuration.


image file: c3en00063j-f2.tif
Fig. 2 Representative cryo-TEM images of goethite aggregates before the reaction in MOPS buffer at concentrations of 10 mM (left), 20 mM (middle), and 50 mM (right). The table summarizes the size measurements, nanoparticle density calculations, and quantification of side to side nanoparticle contacts at each concentration (detailed image analysis results are included in Fig. S3).

Three M(II) ions were selected to determine their effect on goethite nanoparticle aggregate size and surface charge in 20 mM MOPS before the addition of 4-ClNB (Table 1). Two goethite suspensions were prepared for each metal ion. Both sample I and II were prepared in the same manner, except that the metal ion addition was delayed by 18 hours for sample II. The hard metal ion, Ca(II), did not significantly alter either the aggregate diameter nor surface charge of nanoparticles. The small change observed in zeta potential is consistent with limited adsorption of Ca(II) onto the iron mineral surface. Upon addition of the transition metal ions Fe(II) and Co(II), however, nanoparticle aggregation dramatically decreased and zeta potential increased, which is consistent with adsorption of these cations onto the mineral surface, ultimately resulting in dispersal of the particles. Both trends hold for delayed addition of metal ions as demonstrated by the sample II series. Overall, these results are consistent with expectations regarding the effect of surface charge on particle stability.

MOPS concentration: effect on aggregate size and reaction rates

Fig. 3 shows both the rate constant for 4-ClNB degradation and the average pre-reaction aggregate size (determined by DLS and cryo-TEM) versus concentration of MOPS buffer. The maximum rate constant is observed for reactors containing 20 mM MOPS, and the rate constant decreases with further increases in buffer concentration. For MOPS concentrations less than 20 mM, the reaction rate decreased as the buffer concentration decreased. At 5 mM MOPS, the pH was less stable during the equilibration step and throughout the reaction, with the pH dropping by nearly one-third of a pH unit during equilibration and one-half a pH unit after reaction with 4-ClNB (Table S2). In contrast, at MOPS concentrations of 10 mM and higher, the pH dropped by one-tenth or less of a pH unit during the equilibration step. After reaction, the pH dropped by an additional tenth of a pH unit in the case of 10 mM MOPS reactor while the pH remained quite stable for MOPS concentrations of 20 mM and higher. The zeta potential measurements demonstrate a substantial difference between the 5, 10, and 20 mM MOPS reactors prior to addition of the 4-ClNB, most notable is the difference between the 10 and 20 mM reactors. This will influence the kinetics because the sorption of Fe(II) is strongly pH dependent at circumneutral pHs and because the reduction of the aromatic nitro group is dependent on pH.37,39,101 Conversely, at buffer concentrations at and above 20 mM, the buffering capacity is sufficient to maintain a pH of 7 throughout the reaction. Thus, we conclude that the results demonstrating decreased reactivity with increasing aggregate size is consistent with a loss in accessible surface sites for 4-ClNB degradation at the higher MOPS concentrations. In contrast, the lower MOPS concentrations do not provide adequate pH stability through the course of the reaction. Indeed, examination of the literature for results tracking ferrous ion adsorption to goethite, in combination with results from our laboratory using related conditions, demonstrates that the pH range of 6–7 is critical, with steep changes in ferrous ion adsorption as a function of modest changes in pH.75,102–108
image file: c3en00063j-f3.tif
Fig. 3 Average aggregate hydrodynamic diameter of goethite nanoparticles with 1.0 mM Fe(II) before reaction as a function of MOPS concentration as determined by DLS and cryo-TEM measurements (left axis). Observed rate of 4-ClNB degradation is plotted for each of the studied buffer concentrations and are connected by a line for ease of reading (right axis).

Buffer identity: effect on aggregate size and reaction rates

Buffers are commonly used to maintain a constant pH during a reaction, but their presence can result in substantial changes in aggregation state and surface chemistry,25 as seen in Table 1 for MOPS. Goethite nanoparticles suspended in solutions containing 1 mM Fe(II) and HEPES buffer were the most dispersed before reaction with 4-ClNB, and the aggregate sizes were 3–5 times larger for analogous suspensions prepared using MOPS and TEA buffers (Table 2). The zeta potentials, however, are similar for goethite particles in solutions prepared with the three buffers, indicating that the size differences are caused by a buffer-specific effect. In all cases, the introduction of 4-ClNB leads to a dramatic increase in size, accompanied by a decrease in zeta potential, and aggregate sizes after reaction in HEPES buffer were 3–5 fold smaller than in MOPS or TEA (Fig. 4; Table 2).
Table 2 Table displays the buffer molecular structure at pH 7 (and relevant pKa), the average nanoparticle aggregate size before the addition of 4-ClNB over the entire collection period (±SD), the average aggregate size over the 30 minutes after 4-ClNB addition (±SD), and the observed rate of 4-ClNB degradation (±95% CI)
Buffer pKa % in neutral amine form at pH 7 Pre-rxn size (nm) Pre-rxn zeta potential (mV) Post-4-ClNB spike size (nm) Post-4-ClNB spike zeta potential (mV) k obs, 4-ClNB (min−1)
a Beyond the upper quantitative detection limit of the instrumentation.
image file: c3en00063j-u1.tif 7.2 38.7 230 ± 37 38 4300a ± 2200 33 0.056 ± 0.001
image file: c3en00063j-u2.tif 7.6 20.1 72 ± 2 41 770 ± 340 38 0.091 ± 0.005
image file: c3en00063j-u3.tif 7.8 13.7 340 ± 39 41 2400 ± 720 34 0.009 ± 0.001



image file: c3en00063j-f4.tif
Fig. 4 Observed changes in the average hydrodynamic aggregate diameter upon injection of methanolic 4-ClNB into an Fe(II)-goethite suspension with 20 mM MOPS, HEPES, or TEA buffers as reported by DLS. Time zero represents 4-ClNB injection time, thus pre-reaction samples are given a negative time value. The dashed line at 3000 nm represents the upper quantitative detection limit of the instrumentation.

The observed differences in aggregate size may be explained by both the molecular and electronic nature of each buffer. At pH 7, the sulfate group on both MOPS and HEPES molecules is deprotonated, which allows for electrostatic interaction with the positively charged goethite surface. Because the zeta potential is similar for particles in all three buffers before the reaction, this suggests that pH and surface Fe(II), rather than buffer identity drives surface charge, and differences in aggregate size are intimately linked with the nature of the buffer molecules. If the sulfonate group is associated with the nanoparticle surface, the remainder of the molecule may act as a physical inhibitor to nanoparticle aggregation. The smaller nanoparticle aggregates suspended in HEPES buffer may be explained by steric hindrance because the HEPES molecules are larger. Another possibility is that the deprotonated amine group on the buffer sorbs to the surface, resulting in a net decrease in surface charge. The greater degree of aggregation in MOPS would then be due to greater adsorption, because more of the amine is deprotonated at pH 7 as compared to HEPES. (Attempts to quantify buffer sorption were unsuccessful.) Unlike MOPS and HEPES, TEA molecules are predominantly positively charged at near-neutral pH and thus unlikely to be sorbed onto the positively charged goethite surface. As such, the nanoparticles are more likely to form larger aggregates in TEA than in solutions containing MOPS or HEPES.

While buffers such as MOPS, HEPES, and TEA enable adequate maintenance of pH, their presence is not passive with regard to mineral surface reactivity. The reduction of the nitro group to the amine requires the consumption of protons and the buffers provide a continuous source throughout the degradation process. The buffer identity, however, greatly affects the aggregation state of the goethite nanoparticles before the reaction with 4-ClNB is initiated. Thus, trends can be compared, but quantitative comparisons remain challenging with different buffers and buffer concentration.

Results tracking the reduction rate of 4-ClNB for reactors prepared with each of the three buffers are also reported in Table 2. The reaction is pseudo-first order in all buffers examined, and the rate in HEPES buffer solution is approximately 1.5 and 10 times faster than that in MOPS and TEA buffer solutions, respectively. This parallels the pre-reaction size trend. The largest aggregates (suspended in TEA) would be expected to have the smallest accessible surface area and the slowest rate of contaminant degradation, and the smallest aggregates (suspended in HEPES) would be expected to have the largest amount of accessible surface area and the fastest rate of degradation. Generally, the average hydrodynamic diameter increased dramatically upon injection of 4-ClNB dissolved in methanol (Table 2; Fig. 4). Greater size variation was observed when the nanoparticles were suspended in MOPS buffer (even considering that any value greater than 3000 nm is above the linear detection limit of the instrument). The variation in size is likely caused by turning the cuvettes over to re-suspend the settling particles. In the case of MOPS, the large variations may indicate breaking apart of loosely formed aggregates. Thus, the true size of the largest aggregates is difficult to quantify by DLS. It can be concluded, however, that the nanoparticle aggregates are dynamic throughout the degradation process and that the buffer greatly affects the average aggregate size and reactivity.

Metal identity: effect on aggregate size during reaction with 4-ClNB and oxygen

4-ClNB degradation was only observed in the Fe(II)-goethite system (Fig. S4). Reaction in the presence of Ca(II) was neither expected nor observed (data not shown), because Ca(II) is redox inactive. Co(II) is redox active, but the reduction of the aromatic nitro group was essentially zero over the first 45 minutes (the time period over which substantial 4-ClNB reduction occurred with Fe(II)) and significant loss of 4-ClNB by HPLC analysis was not detected until ca. 24 hours.

Upon the addition of methanolic 4-ClNB to goethite nanoparticle suspensions, the identity of the adsorbed metal ion impacted the aggregation state (Table 3). Goethite nanoparticles suspended with dissolved Co(II) remained well dispersed throughout the entire experiment (constant zeta potential), but no significant degradation of 4-ClNB, despite the hypothesized redox activity of Co(II) in this system, was observed. In contrast, goethite nanoparticles suspended in a solution containing Fe(II) remained well dispersed until the addition of the methanolic 4-ClNB, after which a substantial decrease in zeta potential and increase in aggregate size were observed as the 4-ClNB reacted. The drop in zeta potential in the Fe(II)-goethite system (from 38 mV before introduction of 4-ClNB to the system to 33 mV after) results from the oxidation of Fe(II) to Fe(III), and incorporation of the Fe(III) into the mineral phase as FeOOH thus reducing the surface charge. To see if the same effect would be observed with another oxidant, the systems were exposed to oxygen rather than 4-ClNB. For Fe(II), exposure to oxygen also results in increasing aggregate size and decreased zeta potential (Table 3; Fig. S5). Thus, oxidation of the Fe(II) clearly contributes to the observed increase in nanoparticle aggregate size. Co(II) is not oxidized under these conditions, and there are no changes to either the goethite aggregate size or surface charge.

Table 3 Effect of oxidant addition aggregate size and zeta potential for systems containing Fe(II) and Co(II)
4-ClNB Oxygen
Metal added Pre-rxn size (nm) Pre-rxn zeta potential (mV) Post-rxn size (nm) Post-rxn zeta potential (mV) Post-rxn size (nm) Post-rxn zeta potential (mV)
a Low oxygen exposure. The cap on the cell containing the suspension was opened for 15 seconds, re-closed, and the cell was gently turned over 7 times. b High oxygen exposure. The cap was opened, reclosed, and the cell shaken. This procedure was repeated for 5 minutes. c A stream of oxygen was bubbled through the sample for 10 minutes. d Beyond the upper quantitative detection limit of the instrumentation.
Fe(II) 180 38 7930d 33 1050,a 6910bd 33,a 23b
Co(II) 170 41 840 39 130c 40c


Experimental

Chemicals

All aqueous solutions were prepared with ultrapure water (18 MΩ cm resistivity, Milli-Q, Millipore). NaHCO3 (Sigma-Aldrich, 99.7–100.3%) and Fe(NO3)3·9 H2O (Aldrich, 98+%) were used in the synthesis of goethite nanoparticles. 3-(N-morpholino)propanesulfonic acid (MOPS, Sigma-Aldrich, ≥99.5%), 4-(2-hydroxyethyl)-1-piperazineethanesulfonic acid (HEPES, Sigma-Aldrich), and Tris(2-hydroxyethyl)amine (TEA, Baker Analyzed Reagent, >99.0%) were adjusted to pH 7 with HCl (BDH Aristar) or NaOH (Mallinkrodt Chemicals, 99%), vacuum filtered, and deoxygenated by nitrogen sparging (Matheson, grade 99.9998%). 4-chloronitrobenzene (4ClNB, 99%) was obtained from Acros Organics. Acetonitrile (HPLC grade) and ammonium acetate (Fluka Analytical, HPLC, ≥99.0%) were used in high pressure liquid chromatography (HPLC) analysis. FeCl2·4H2O (Fisher Scientific, 101.0%), CoCl2 (Mallinkrodt Chemicals, 98.8%), and CaCl2 (Fisher Scientific, 99%) were used to prepare metal ion solutions.

Goethite nanoparticle synthesis

Goethite nanorods were synthesized by Chun et al.34 Particle size distribution and X-ray diffraction pattern of the synthesized particles are provided in the ESI.

4-ClNB degradation reactions

Experiments were carried out in 50 mL serum bottles and were prepared in an anaerobic chamber (Coy Laboratory Products, 5% H2/95% N2) and sealed with a PTFE-lined aluminum crimp cap. Reactors contained approximately 0.325 g L−1 goethite nanoparticles and deoxygenated pH 7 MOPS, HEPES, or TEA buffer. The reactor was removed from the anaerobic chamber, sonicated on ice for two hours (AquaSonic 150HT, VWR Scientific), and returned to the anaerobic chamber. The solutions of 1.0 M CoCl2, CaCl2, and acidified FeCl2 were prepared in the glove bag and added to the serum bottle to yield a final concentration of 1.0 mM of the desired cation. The suspension was stirred along the longitudinal axis of the serum bottle on a magnetic stir plate (IKAMAG RO10power, IKA Works Inc.) and allowed to equilibrate for approximately 18 hours. The serum bottle was wrapped in aluminum foil to prevent degradation by photolysis. To initiate an experiment, a deoxygenated methanolic solution of 4-ClNB was added to the reactor to yield an initial concentration of 100 μM.

At desired reaction times, 0.5 mL samples of the suspension were filtered with a 0.2 μm nylon membrane. The concentration of 4-ClNB was quantified by an Agilent 1100 Series system equipped with an ultraviolet detector. A 20 μL sample was injected onto a Zorbax SB-C18 column (4.6 mm × 150 mm, 5 μm). The 70[thin space (1/6-em)]:[thin space (1/6-em)]30 acetonitrile[thin space (1/6-em)]:[thin space (1/6-em)]ammonium acetate (10% v/v acetonitrile/ammonium acetate 1 g L−1, pH 7) mobile phase was operated at a flow rate of 0.7 mL min−1 for a total separation time of 7 minutes. The absorbance at 254 nm was monitored. The retention time of 4-ClNB was 4.42 minutes, and 4-chloroaniline (the ultimate degradation product of the reduction) eluted at 3.22 minutes.

Nanoparticle characterization

XRD. Nanoparticle composition was analyzed by XRD using a PANalytical X-Pert PRO MPD X-ray diffractometer equipped with a cobalt source, iron filter, and an X-Celerator detector over the range 20–105° 2θ at a scan rate of 0.0235° per second with an effective 90 seconds per step. The resulting patterns were compared to the reference powder diffraction files (PDFs) of ferrihydrite (#29-0712), magnetite (#19-0629), and goethite (#29-0713).
Zeta potential. A 2.5 mL sample of prepared goethite suspension was removed from the anaerobic chamber and placed in a Brookhaven Instruments Corporation ZetaPALS Zeta Potential Analyzer 90Plus/BI-MAS Multi Angle Particle Sizing Option DLS instrument where the zeta potential was measured. Data collection parameters consisted of: 5 runs of 20 cycles each, estimated sample size of 3000 nm, sample concentration of 0.32 mg mL−1, 25 °C, aqueous suspension, pH 7, and Smoluchowski zeta potential model.
DLS. A 2.5 mL sample of goethite suspension was transferred to an air-tight quartz cuvette inside the anaerobic chamber from a prepared reactor prior to 4-ClNB introduction. The sample was removed from the chamber and placed into the DLS instrument where the hydrodynamic diameter was continuously measured for approximately 30 minutes. To make measurements during reaction, the 4-ClNB solution was injected into the cuvette and the hydrodynamic diameter was measured for an additional 30 to 60 minutes. Run parameters consisted of triplicate measurements of a sequence of 9 runs (20 second run duration, total analysis time of 9 minutes), a dust filter value of 500, the assumption that the particles are thin shells, sample temperature of 25 °C, laser wavelength of 657 nm, and a detection angle of 90°. Every 9 minutes, the cuvette was taken out of the instrument and gently inverted twice to prevent particle sedimentation. The hydrodynamic diameters reported are the number-based mean diameter of the aggregates. Reported pre-reaction sizes are the average and standard deviation over the first 30 minutes while the post-reaction sizes are the final average hydrodynamic diameter recorded after 4-ClNB addition, unless noted otherwise.
Cryo-TEM. Approximately 3 μL of goethite nanoparticles suspended in MOPS buffer was applied to a 3 mm 200-mesh lacey carbon coated copper grid (SPI Supplies). The grid was blotted with filter paper in a 100% humidity environment for 2 seconds to create a thin film of suspension inside a controlled humidified chamber (Vitrobot Mark IV, FEI Company). The grid was plunged into a well of liquid ethane and transferred under liquid nitrogen to a cryo-TEM holder and analyzed by a FEI Technai F30 TEM. Images were analyzed using ImageJ 1.44p equipped with additional plugins from the MBF ImageJ for Microscopy Collection. Angles between adjacent particles were measured and counted for each aggregate to determine the frequency of side-to-side contacts. The particle density was determined by enclosing the aggregate in a polygon in which all corners pointed out, converting the image to black (background) and white (nanoparticles), and counting the number particle pixels in relation to the number of total polygon pixels. Results for each concentration are reported as the average of six representative images.

Conclusions

The size of goethite nanoparticle aggregates is dramatically reduced by adsorption of a transition metal ion, which imparts a positive charge to the surface. Only Fe(II) was found to promote the degradation of 4-ClNB, and oxidation of the added Fe(II) by 4-ClNB or oxygen resulted in increased aggregation. The different oxidants (atmospheric oxygen, pure oxygen, or 4-ClNB reduction) all led to increases in aggregation state. Thus, it appears that the oxidant identity is not a factor in aggregate size increase, but rather the fact that oxidation occurs.

Results also demonstrate aggregation state of goethite nanoparticles is affected by the chemical conditions in the reactor which in turn affects reactivity with contaminants. The buffer selected to maintain reactor pH and the buffer concentration used both alter the average nanoparticle size and, by extension, the surface area available for 4-ClNB degradation. Both the electronic and structural nature of the buffer molecule can explain the observed trends of both the goethite aggregate size and observed rates of 4-ClNB degradation. Zwitterionic buffers with spatial charge separation are better at preventing nanoparticle aggregation and yield faster rates of degradation than buffers with only a central positive charge.

In addition, the concentration of the buffer played a role in both the aggregation state and, to a greater extent, the rate of 4-ClNB degradation. At high buffer concentrations, the aggregates were larger and more densely packed on average (due to buffer association with the surface as evidenced by changes in zeta potential) than those suspended in lower buffer concentrations. This increase in packing is the hypothesized source of the decreased rate of 4-ClNB degradation. If the buffer concentration was not sufficient to maintain a stable pH, effects on the extent of Fe(II) sorption, and thus reactivity of the nanoparticles were observed. These dramatic effects of buffer identity and concentration on aggregation state and degradation rate calls into question the appropriateness of using biological buffers within batch reactors to simulate the reactivity of nanoparticles in natural aquatic systems. It appears that if it is desired to it will be necessary to use carbonate buffer to understand how nanoparticles react and aggregate in the environment.

Acknowledgements

The authors would like to thank the University of Minnesota and the National Science Foundation (NSF-1012193) for financial support. Parts of this work were carried out in the Characterization Facility, University of Minnesota, a member of the NSF-funded Materials Research Facilities Network (http://www.mrfn.org) via the MRSEC program.

Notes and references

  1. N. J. Barber, U.S. Geological Survey Fact Sheet 2009-3098, 2009, p. 2 Search PubMed.
  2. C. A. Eddy-Miller, T. T. Bartos and M. L. Taylor, U.S. Geological Survey Scientific Investigations Report, 2013, p. 45 Search PubMed.
  3. K. L. Smalling, J. L. Orlando, D. Calhoun, W. A. Battaglin and K. M. Kuivila, U.S. Geological Survey Data Series 707, 2012, p. 40 Search PubMed.
  4. P. J. Squillace, J. C. Scott, M. J. Moran, B. T. Nolan and D. W. Kolpin, Environ. Sci. Technol., 2002, 36, 1923–1930 CrossRef CAS.
  5. R. J. Gilliom, Environ. Sci. Technol., 2007, 41, 3408–3414 CrossRef CAS.
  6. D. W. Kolpin, J. E. Barbash and R. J. Gilliom, Environ. Sci. Technol., 1998, 32, 558–566 CrossRef CAS.
  7. J. D. Fallon, Geological Survey Fact Sheet 066-00, 2000, 4 p Search PubMed.
  8. K. L. Smalling, G. M. Fellers, P. M. Kleeman and K. M. Kuivila, Environ. Toxicol. Chem., 2013, 32, 2026–2034 CrossRef CAS PubMed.
  9. R. W. Gale, M. J. Tanner, M. S. Love, M. M. Nishimoto and D. M. Schroeder, U.S. Geological Survey Open-File Report 2013-1046, 2013, 31 p. and supplemental tables Search PubMed.
  10. National Research Council, Alternatives for Managing the Nation's Complex Contaminated Groundwater Sites, Washington, DC:The National Academies Press, 2013 Search PubMed.
  11. R. M. Cornell and U. Schwertmann, The Iron Oxides: Structure, Properties, Reactions, Occurences and Uses, Wiley-VCH, 2nd edn, 2003 Search PubMed.
  12. R. A. Maithreepala and R.-A. Doong, Environ. Sci. Technol., 2004, 38, 6676–6684 CrossRef CAS.
  13. K. Pecher, S. B. Haderlein and R. P. Schwarzenbach, Environ. Sci. Technol., 2002, 36, 1734–1741 CrossRef CAS.
  14. M. Elsner, S. B. Haderlein, T. Kellerhals, S. Luzi, L. Zwank, W. Angst and R. P. Schwarzenbach, Environ. Sci. Technol., 2004, 38, 2058–2066 CrossRef CAS.
  15. C. L. Chun, R. M. Hozalski and W. A. Arnold, Environ. Sci. Technol., 2005, 39, 8525–8532 CrossRef CAS.
  16. J. E. Amonette, D. J. Workman, D. W. Kennedy, J. S. Fruchter and Y. A. Gorby, Environ. Sci. Technol., 2000, 34, 4606–4613 CrossRef CAS.
  17. T. P. Klupinski, Y.-P. Chin and S. J. Traina, Environ. Sci. Technol., 2004, 38, 4353–4360 CrossRef CAS.
  18. E. J. O'Loughlin, K. M. Kemner and D. R. Burris, Environ. Sci. Technol., 2003, 37, 2905–2912 CrossRef.
  19. R. A. Maithreepala and R.-A. Doong, Environ. Sci. Technol., 2004, 38, 260–268 CrossRef CAS.
  20. M. Elsner, R. P. Schwarzenbach and S. B. Haderlein, Environ. Sci. Technol., 2004, 38, 799–807 CrossRef CAS.
  21. A. G. B. Williams and M. M. Scherer, Environ. Sci. Technol., 2004, 38, 4782–4790 CrossRef CAS.
  22. D. Colón, E. J. Weber and J. L. Anderson, Environ. Sci. Technol., 2008, 42, 6538–6543 CrossRef.
  23. K. M. Danielsen and K. F. Hayes, Environ. Sci. Technol., 2004, 38, 4745–4752 CrossRef CAS.
  24. T. P. Klupinski and Y.-P. Chin, Environ. Sci. Technol., 2003, 37, 1311–1318 CrossRef CAS.
  25. A. Buchholz, C. Laskov and S. B. Haderlein, Environ. Sci. Technol., 2011, 45, 3355–3360 CrossRef CAS PubMed.
  26. J. A. Hakala, Y.-P. Chin and E. J. Weber, Environ. Sci. Technol., 2007, 41, 7337–7342 CrossRef CAS.
  27. J. A. Hakala and Y.-P. Chin, J. Agric. Food Chem., 2010, 58, 12840–12846 CrossRef CAS PubMed.
  28. J. J. Erbs, B. Gilbert and R. L. Penn, J. Phys. Chem. C, 2008, 112, 12127–12133 CAS.
  29. P. J. Vikesland, A. M. Heathcock, R. L. Rebodos and K. E. Makus, Environ. Sci. Technol., 2007, 41, 5277–5283 CrossRef CAS.
  30. J. Narr, T. Viraraghavan and Y.-C. Jin, Fresenius Environ. Bull., 2007, 16, 320–329 CAS.
  31. D. H. Phillips, T. V. Nooten, L. Bastiaens, M. I. Russell, K. Dickson, S. Plant, J. M. E. Ahad, T. Newton, T. Elliot and R. M. Kalin, Environ. Sci. Technol., 2010, 44, 3861–3869 CrossRef CAS PubMed.
  32. N. Savage and M. S. Diallo, J. Nanopart. Res., 2005, 7, 331–342 CrossRef CAS.
  33. J. Theron, J. A. Walker and T. E. Cloete, Crit. Rev. Microbiol., 2008, 34, 43–69 CrossRef CAS PubMed.
  34. C. L. Chun, R. L. Penn and W. A. Arnold, Environ. Sci. Technol., 2006, 40, 3299–3304 CrossRef CAS.
  35. A. Hartenbach, T. B. Hofstetter, M. Berg, J. Bolotin and R. P. Schwarzenbach, Environ. Sci. Technol., 2006, 40, 7710–7716 CrossRef CAS.
  36. J. Klausen, S. P. Tröber, S. B. Haderlein and R. P. Schwarzenbach, Environ. Sci. Technol., 1995, 29, 2396–2404 CrossRef CAS PubMed.
  37. D. Naka, D. Kim and T. J. Strathmann, Environ. Sci. Technol., 2006, 40, 3006–3012 CrossRef CAS.
  38. A. Neumann, T. B. Hofstetter, M. Lüssi, O. A. Cirpka, S. Petit and R. P. Schwarzenbach, Environ. Sci. Technol., 2008, 42, 8381–8387 CrossRef CAS.
  39. C. A. Schultz and T. J. Grundl, Environ. Sci. Technol., 2000, 34, 3641–3648 CrossRef CAS.
  40. R. P. Schwarzenbach, P. M. Gschwend and D. M. Imboden, Environmental Organic Chemistry, John Wiley & Sons, Inc., Hoboken, NJ, 2nd edn, 2003 Search PubMed.
  41. M. M. Scherer, B. A. Balko and P. G. Tratnyek, Mineral-Water Interfacial Reactions, 1999, pp. 301–322 Search PubMed.
  42. K. M. Rosso, S. V. Yanina, C. A. Gorski, P. Larese-Casanova and M. M. Scherer, Environ. Sci. Technol., 2010, 44, 61–67 CrossRef CAS PubMed.
  43. C. Gu, H. Jia, H. Li, B. J. Teppen and S. A. Boyd, Environ. Sci. Technol., 2010, 44, 4258–4263 CrossRef CAS PubMed.
  44. S.-H. Kang and W. Choi, Environ. Sci. Technol., 2008, 43, 878–883 CrossRef.
  45. Y.-S. Keum and Q. X. Li, Chemosphere, 2004, 54, 255–263 CrossRef CAS PubMed.
  46. W. Lee and B. Batchelor, Environ. Sci. Technol., 2002, 36, 5147–5154 CrossRef CAS.
  47. L. Yan and G. W. Bailey, J. Colloid Interface Sci., 2001, 241, 142–153 CrossRef CAS PubMed.
  48. A. Agrawal and P. G. Tratnyek, Environ. Sci. Technol., 1995, 30, 153–160 CrossRef.
  49. L. Wu, B. L. Beard, E. E. Roden, C. B. Kennedy and C. M. Johnson, Geochim. Cosmochim. Acta, 2010, 74, 4249–4265 CrossRef CAS PubMed.
  50. Y. T. He, J. T. Wilson and R. T. Wilkin, Geochim. Cosmochim. Acta, 2010, 74, 2025–2039 CrossRef CAS PubMed.
  51. K. Amstaetter, T. Borch, P. Larese-Casanova and A. Kappler, Environ. Sci. Technol., 2010, 44, 102–108 CrossRef CAS PubMed.
  52. X. Liang, R. P. Philp and E. C. Butler, Chemosphere, 2009, 75, 63–69 CrossRef CAS PubMed.
  53. H.-S. Kim, W.-H. Kang, M. Kim, J.-Y. Park and I. Hwang, Chemosphere, 2008, 73, 813–819 CrossRef CAS PubMed.
  54. P. Larese-Casanova and M. M. Scherer, Environ. Sci. Technol., 2008, 42, 3975–3981 CrossRef CAS.
  55. T. Peretyazhko, J. M. Zachara, S. M. Heald, B.-H. Jeon, R. K. Kukkadapu, C. Liu, D. Moore and C. T. Resch, Geochim. Cosmochim. Acta, 2008, 72, 1521–1539 CrossRef CAS PubMed.
  56. D. M. Cwiertny, R. M. Handler, M. V. Schaefer, V. H. Grassian and M. M. Scherer, Geochim. Cosmochim. Acta, 2008, 72, 1365–1380 CrossRef CAS PubMed.
  57. C. L. Chun, R. M. Hozalski and W. A. Arnold, Environ. Sci. Technol., 2007, 41, 1615–1621 CrossRef CAS.
  58. J.-Y. Lee, R. M. Hozalski and W. A. Arnold, Chemosphere, 2007, 66, 2127–2135 CrossRef CAS PubMed.
  59. D. Colón, E. J. Weber, J. L. Anderson, P. Winget and L. A. Suarez, Environ. Sci. Technol., 2006, 40, 4449–4454 CrossRef.
  60. E. Silvester, L. Charlet, C. Tournassat, A. Géhin, J.-M. Grenèche and E. Liger, Geochim. Cosmochim. Acta, 2005, 69, 4801–4815 CrossRef CAS PubMed.
  61. H. D. Pedersen, D. Postma, R. Jakobsen and O. Larsen, Geochim. Cosmochim. Acta, 2005, 69, 3967–3977 CrossRef CAS PubMed.
  62. R. A. Maithreepala and R.-A. Doong, Environ. Sci. Technol., 2005, 39, 4082–4090 CrossRef CAS.
  63. E. C. Butler, Y. Dong, L. R. Krumholz, X. Liang, H. Shao and Y. Tan, Aquatic Redox Chemistry, 2011, pp. 519–538 Search PubMed.
  64. P. Larese-Casanova, D. M. Cwiertny and M. M. Scherer, Environ. Sci. Technol., 2010, 44, 3765–3771 CrossRef CAS PubMed.
  65. R. S. Cutting, V. S. Coker, N. D. Telling, R. L. Kimber, C. I. Pearce, B. L. Ellis, R. S. Lawson, G. van der Laan, R. A. D. Pattrick, D. J. Vaughan, E. Arenholz and J. R. Lloyd, Environ. Sci. Technol., 2010, 44, 2577–2584 CrossRef CAS PubMed.
  66. C. A. Gorski, J. T. Nurmi, P. G. Tratnyek, T. B. Hofstetter and M. M. Scherer, Environ. Sci. Technol., 2010, 44, 55–60 CrossRef CAS PubMed.
  67. F.-B. Li, L. Tao, C.-H. Feng, X.-Z. Li and K.-W. Sun, Environ. Sci. Technol., 2009, 43, 3656–3661 CrossRef CAS.
  68. C. A. Gorski and M. M. Scherer, Environ. Sci. Technol., 2009, 43, 3675–3680 CrossRef CAS.
  69. N. B. Tobler, T. B. Hofstetter, K. L. Straub, D. Fontana and R. P. Schwarzenbach, Environ. Sci. Technol., 2007, 41, 7765–7772 CrossRef CAS.
  70. N. B. Tobler, T. B. Hofstetter and R. P. Schwarzenbach, Environ. Sci. Technol., 2007, 41, 7773–7780 CrossRef CAS.
  71. P. Larese-Casanova and M. M. Scherer, Environ. Sci. Technol., 2007, 41, 471–477 CrossRef CAS.
  72. L. Zwank, M. Elsner, A. Aeberhard, R. P. Schwarzenbach and S. B. Haderlein, Environ. Sci. Technol., 2005, 39, 5634–5641 CrossRef CAS.
  73. S.-Y. Oh, D. K. Cha, B. J. Kim and P. C. Chiu, Environ. Sci. Technol., 2004, 38, 3723–3730 CrossRef CAS.
  74. K. B. Gregory, P. Larese-Casanova, G. F. Parkin and M. M. Scherer, Environ. Sci. Technol., 2004, 38, 1408–1414 CrossRef CAS.
  75. B.-H. Jeon, B. A. Dempsey and W. D. Burgos, Environ. Sci. Technol., 2003, 37, 3309–3315 CrossRef CAS.
  76. P. J. Vikesland and R. L. Valentine, Environ. Sci. Technol., 2002, 36, 512–519 CrossRef CAS.
  77. L. A. Totten, U. Jans and A. L. Roberts, Environ. Sci. Technol., 2001, 35, 2268–2274 CrossRef CAS.
  78. M. S. Elovitz and E. J. Weber, Environ. Sci. Technol., 1999, 33, 2617–2625 CrossRef CAS.
  79. E. C. Butler and K. F. Hayes, Environ. Sci. Technol., 1998, 32, 1276–1284 CrossRef CAS.
  80. J. Klausen, S. B. Haderlein and R. P. Schwarzenbach, Environ. Sci. Technol., 1997, 31, 2642–2649 CrossRef CAS.
  81. B. A. Holmén, M. I. Tejedor-Tejedor and W. H. Casey, Langmuir, 1997, 13, 2197–2206 CrossRef.
  82. M. Tong, S. Yuan, H. Long, M. Zheng, L. Wang and J. Chen, J. Contam. Hydrol., 2011, 122, 16–25 CrossRef CAS PubMed.
  83. Y. Xie and D. M. Cwiertny, Environ. Sci. Technol., 2010, 44, 8649–8655 CrossRef CAS PubMed.
  84. L. Tao, F. Li, Y. Wang and K. Sun, Clays Clay Miner., 2010, 58, 682–690 CrossRef CAS.
  85. A. G. B. Williams, K. B. Gregory, G. F. Parkin and M. M. Scherer, Environ. Sci. Technol., 2005, 39, 5183–5189 CrossRef CAS.
  86. S. Chakraborty, F. Favre, D. Banerjee, A. C. Scheinost, M. Mullet, J.-J. Ehrhardt, J. Brendle, L. Vidal and L. Charlet, Environ. Sci. Technol., 2010, 44, 3779–3785 CrossRef CAS PubMed.
  87. A. Neumann, T. B. Hofstetter, M. Skarpeli-Liati and R. P. Schwarzenbach, Environ. Sci. Technol., 2009, 43, 4082–4089 CrossRef CAS.
  88. F. Monteil-Rivera, L. Paquet, A. Halasz, M. T. Montgomery and J. Hawari, Environ. Sci. Technol., 2005, 39, 9725–9731 CrossRef CAS.
  89. Y.-H. Tee, L. Bachas and D. Bhattacharyya, J. Phys. Chem. C, 2009, 113, 9454–9464 CAS.
  90. C. L. Chun, D. R. Baer, D. W. Matson, J. E. Amonette and R. L. Penn, Environ. Sci. Technol., 2010, 44, 5079–5085 CrossRef CAS PubMed.
  91. J. T. Nurmi, P. G. Tratnyek, V. Sarathy, D. R. Baer, J. E. Amonette, K. Pecher, C. Wang, J. C. Linehan, D. W. Matson, R. L. Penn and M. D. Driessen, Environ. Sci. Technol., 2005, 39, 1221–1230 CrossRef CAS.
  92. K. M. Danielsen, J. L. Gland and K. F. Hayes, Environ. Sci. Technol., 2005, 39, 756–763 CrossRef CAS.
  93. R. B. Merola, E. D. Fournier and M. M. McGuire, Langmuir, 2007, 23, 1223–1226 CrossRef CAS PubMed.
  94. R. J. Hanoch, H. Shao and E. C. Butler, Chemosphere, 2006, 63, 323–334 CrossRef CAS PubMed.
  95. S. Dixit and J. G. Hering, Chem. Geol., 2006, 228, 6–15 CrossRef CAS PubMed.
  96. Q. Wang, N. Cissoko, M. Zhou and X. Xu, Phys. Chem. Earth, Parts A/B/C, 2011, 36, 442–446 CrossRef PubMed.
  97. R. Welch and R. G. Riefler, Environ. Eng. Sci., 2008, 25, 1255–1262 CrossRef CAS.
  98. G. V. Nano and T. J. Strathmann, J. Colloid Interface Sci., 2008, 321, 350–359 CrossRef CAS PubMed.
  99. S.-Y. Oh, D. K. Cha, B. J. Kim and P. C. Chiu, Environ. Sci. Technol., 2005, 24, 2812–2819 CAS.
  100. W. Lee and B. Batchelor, Environ. Sci. Technol., 2002, 36, 5348–5354 CrossRef CAS.
  101. P. G. Tratnyek and D. L. Macalady, J. Agric. Food Chem., 1989, 37, 248–254 CrossRef CAS.
  102. E. Liger, L. Charlet and P. Van Cappellen, Geochim. Cosmochim. Acta, 1999, 63, 2939–2955 CrossRef CAS.
  103. L. Charlet, E. Liger and P. Gerasimo, J. Environ. Eng., 1998, 124, 25–30 CrossRef CAS.
  104. L. Charlet, E. Silvester and E. Liger, Chem. Geol., 1998, 151, 85–93 CrossRef CAS.
  105. J. M. Zachara, S. C. Smith and J. K. Fredrickson, Geochim. Cosmochim. Acta, 2000, 64, 1345–1362 CrossRef CAS.
  106. B. R. Coughlin and A. T. Stone, Environ. Sci. Technol., 1995, 29, 2445–2455 CrossRef CAS PubMed.
  107. Y. Zhang, L. Charlet and P. W. Schindler, Colloids Surf., 1992, 63, 259–268 CrossRef CAS.
  108. B.-H. Jeon, B. A. Dempsey, W. D. Burgos and R. A. Royer, Colloids Surf., A, 2001, 191, 41–55 CrossRef CAS.

Footnotes

Electronic supplementary information (ESI) available. See DOI: 10.1039/c3en00063j
These authors contributed equally to this work.

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