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Scalable Graphene-based Membranes for Ionic Sieving with Ultrahigh Charge Selectivity
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Seunghyun Hong, Charlotte Constans, Marcos Vinicius Surmani Martins, Yong Chin Seow, Juan Alfredo Guevara Carrió, and Slaven Garaj Nano Lett., Just Accepted Manuscript • DOI: 10.1021/ acs.nanolett.6b03837 • Publication Date (Web): 22 Dec 2016 Downloaded from http://pubs.acs.org on December 26, 2016
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Ag/AgCl
1 C 2PDMS 3 4 5 6PDMS C 7 8 9b ClK+ Chigh 10 11 12 Clow 13 ~ (P P ) ∆c diffusion I diff + 14 15 16 17 18 19 20
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Nano Oxide Lettersd Graphene
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Scalable Graphene-based Membranes for Ionic
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Sieving with Ultrahigh Charge Selectivity
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Seunghyun Hong1, Charlotte Constans1,2,, Marcos Vinicius Surmani Martins1,3, Yong Chin Seow1, Juan
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Alfredo Guevara Carrió1,4, and Slaven Garaj1,2,5,6 *
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Nanostructured graphene-oxide (GO) laminate membranes, exhibiting ultra-high water flux, are excellent
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candidates for next generation nanofiltration and desalination membranes, provided the ionic rejection could be
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further increased without compromising the water flux. Using microscopic drift-diffusion experiments, we
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demonstrated the ultra-high charge selectivity for GO membranes, with more than order of magnitude
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difference in the permeabilities of cationic and anionic species of equivalent hydration radii. Measuring diffusion
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of a wide range of ions of different size and charge, we were able to clearly disentangle different physical
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mechanism contributing to the ionic sieving in GO membranes – electrostatic repulsion between ions and
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charged chemical groups; and the compression of the ionic hydration shell within the membrane’s nanochannels,
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following the activated behavior. The charge-selectivity allows us to rationally design membranes with
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increased ionic rejection, and opens up the field of ion exchange and electrodialysis to the GO membranes.
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KEYWORDS Graphene Oxide Membranes, Ionic Permeability, Surface Charges, Ion Exchange, Ionic Sieving
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Centre for Advanced 2D Materials, National University of Singapore, Singapore 117542 Department of Physics, National University of Singapore, Singapore 117551 3 Department of Materials Science and Engineering, National University of Singapore, Singapore 117575 4 Mackgraphe - Graphene and Nano-Material Research Center, Engineering School, Presbyterian University Mackenzie, Brazil 01397-001 5 NUS Nanoscience & Nanotechnology Institute, National University of Singapore, Singapore 117581 6 Department of Biomedical Engineering, National University of Singapore, Singapore 117583 2
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Graphene-based membranes with ultra-high water flux and ionic sieving properties attracted recently 9, 10
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significant attention, as a severe strain on the fresh water supply
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new materials for water purification and desalination. Nanostructured graphene-oxide (GO) membranes
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– scalable, inexpensive, thermally and chemically robust, and integratable with current technologies
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particularly enticing candidates for the next-generation, high-performance separation membranes
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GO membranes consist of stacked layers of impermeable graphene sheets, 𝐿 = 1 − 10 µm in size, spaced by
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𝑑 = 0.9 − 1.2 nm via functionalized, mostly oxygen-carrying groups
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into nanoscale domains, delimiting a percolative network of pristine graphene channels, which could
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accommodate a few layers of water exhibiting frictionless flow
precipitated a strong research interest in
3, 13
1, 3, 11-13
14-18
– are
10, 19-21
. The
. The chemical groups are coalesced
1, 22
. Previous experiments
3, 15, 16, 23-25
, measuring
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salt diffusion through centimeter-scale membranes over a period of hours, showed no permeation for ions
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with hydration rates above size cut-off of 𝑅/ ≈ 4.5 Å and mostly unvarying permeation rate for smaller ions.
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Those experiments, due to their nature, are ineffective in disentangling all the physical mechanisms
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contributing to the permeability, are unable to distinguish permeability of different constituting ions in the salt,
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and could be prone to artifacts due to external defects and tears over larger areas of the membrane. To
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understand intrinsic membrane properties, we implemented a highly sensitive drift-diffusion technique,
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revealing ultra-high charge-selectivity of the GO membranes.
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We measured the ionic permeability of a 3 µm thick GO membrane, mounted across an array of
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200×200 nm5 apertures in a 300 nm thick, free-standing, insulating SiNX layer on a Si substrate chip (Figure
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1a). By limiting the exposed membrane area to ~5 µm5 and keeping it relatively thick, we ensured there are
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no unintended cracks and defects that would skew the results . The GO membrane and its constituting GO
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crystallites were extensively characterized using atomic force microscopy, X-ray diffraction, Fourier transform
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infrared spectroscopy, etc. (see Supporting Information). The membrane chip was inserted in a custom-build
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fluidic cell, so that it separated two compartments, each subsequently filled with ionic solutions electrically
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contacted with Ag/AgCl electrodes. The electrodes were connected to a sensitive patch-clamp amplifier
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(Axopatch 200B), sourcing voltage at a sweep rate of 5 mV/5 s (step function) across the membrane and
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measuring ionic currents with 10 pA precision (no hysteresis was observed for such low rates). The
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polydimethylsiloxane (PDMS) gasket seal precluded ionic solution from leaking around the edges of the
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membrane.
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To discern the separate permeabilities of cations (𝑃8 ) and anions (𝑃; ) in the salt, we implemented the
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drift-diffusion technique to measure ionic currents driven by both the voltage and the concentration gradient
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(Figure 1b). The fluidic compartments were filled with different concentrations of a salt, and we could measure
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diffusive current across the membrane for zero applied voltage 𝐼diff ~ 𝑃8 − 𝑃; ∙ Δ𝑐. As we applied a voltage
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difference ∆𝑉 across the membrane, the added electrophoretic component to the overall current is
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𝐼drift ~ 𝑃8 + 𝑃; ∙ Δ𝑉 (Figure 1c). Measuring the two current components, we could deduce both 𝑃8 and 𝑃;
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permeabilities. Figure 1d shows representative current-voltage ( 𝐼 − 𝑉 ) curves, measured at a fixed
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concentration gradient: the slope of the curve is indicative of 𝐼drift ; whereas membrane potential 𝑉m = 𝑉(𝐼 =
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0) is indicative of 𝐼diff . More precisely, we extract the individual permeabilities by modeling the total current
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density 𝐽 ∆𝑐, ∆𝑉 across the membrane using the equation:
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𝐽=
J
𝑃J 𝑧J5
𝑧J 𝐹 ∙ Δ𝑉 𝐹 5 ∙ Δ𝑉 𝑋 f − 𝑋 p exp 𝑅𝑇 ∙ ∙ 𝑧J 𝐹 ∙ Δ𝑉 𝑅𝑇 1 − exp 𝑅𝑇
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For each ionic species X in the solution, 𝑃J is membrane permeability, 𝑧J is the valence, and 𝑋 R and 𝑋 S
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are the ionic concentrations in the feed and permeate chambers, respectively. Potential across the membrane
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∆V was adjusted for the electrodes’ redox potential; R is the universal gas constant; F is Faraday’s constant;
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and T is the temperature. For details on the model and the method, see Supporting Information.
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To elucidate the ionic selectivity of the GO membranes, we investigated the permeability of a wide
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selection of aqueous salt ions, with varying ionic charges and spanning a wide range of effective hydrated ionic
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volumes. Figure 2a depicts the permeation rates (p) of different cations (circle) and their corresponding Cl
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counter ions (squares) as a function of the cation’s hydration radii
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cation permeability decreases exponentially with increased hydration radius, followed by the sharp cutoff at
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𝑅H ≈ 4.6 Å; and (b) permeability of the negatively charged Cl ion is suppressed by an order of magnitude
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compared to the positive K and Rb ions, despite all those ions having very similar hydration volumes. We
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conclude that the two dominant mechanisms for the ion rejection in GO membranes are size exclusion due to
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compression of the ionic hydration shell in narrow channels
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. Two general trends are revealed: (a)
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, and electrostatic repulsion due to membrane
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surface charge (Figure 2b,c). The earlier diffusion experiments
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of all the salt ions, which is determined by the value for the least permeable species in a salt – for monovalent
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salts they were actually measuring permeability of the chlorine counter-ion, not cations. This led to apparent
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size-independent permeability for ions with hydration radii below the cut-off size defined by the channel
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height (implying rigid hydration shells around ions). Instead, by properly separating cations and anions, we
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observe the exponential dependence of the permeability on an ion’s hydration radius, consistent with the
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compressible hydration shell model, where coordinated water molecules could rearrange or detach
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themselves to allow passage of the hydrated ion through a narrow channel
measured the combined permeability
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.
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We postulate that the high charge selectivity of the GO membranes is a result of the negatively charged
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nanochannels in a GO membrane, due to the protonable oxygen groups. This leads to the expulsion of the
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negatively charged Cl ions from nanochannels, and suppression of the anionic permeability, as predicted by
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the electric double layer (EDL) model . Permeability of Cl ions in monovalent salts remained independent of
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counterions (Rb , K , Na , Li ); and the cation selectivity 𝑆8 = 𝑃8
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(Figure 2d). Interestingly, the EDL model breaks down in the case of chloride salts with divalent and trivalent
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cations, and P(Cl ) reverts to the value predicted for uncharged channels (Figure 2a,d). We attribute this effect
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to correlation-induced charge inversion , where multivalent ions overcompensate monovalent surface groups,
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leading to a sharp drop, or even an inversion, of the effective surface charge. A similar effect has been
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observed previously in highly charged protein channels
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channels .
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+
+
+
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+
𝑃8 + 𝑃; reached values in excess of 95%
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, such as bacterial porin OmpF, and in narrow silica
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To further investigate the ionic selectivity of GO membranes, we performed a series of drift-diffusion and
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ionic conductivity measurements using KCl aqueous solutions for a range of pH and molarity values. Figure 3a
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shows current-voltage (I-V) curves at same salt concentration on both sides, 𝑐KCl = 10 mM, measured for
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different pH values (see also Figure S3a). At this low molarity, nonlinear nature of the I-V curves at larger
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voltages is likely due to overlimiting currents driven by the concentration polarization at the surface of the
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membrane . The ionic conductance of the membrane was calculated from the slopes of the I-V curves in the
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Ohmic regime at low voltage (Figure 3b). The increase in pH (reduction in hydronium concentration) leads to
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increased dissociation of the carboxyl and hydroxyl groups within the GO sheets:
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Graphene-OH ⇄ Graphene-O; + H8
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This leads to an increase in negative surface charge density in the graphene nanochannels, and is reflected in
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an increased conductance and current rectification. The ionic currents associated with the excess hydronium
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(H3O ) or hydroxide (OH ) ions are subtracted as shown in Figure S4a. At higher pH, we also observe an increase
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in 𝑃 K 8 , a decrease in 𝑃 Cl; and an increase in cation selectivity 𝑆8 (Figure 3c), all consistent with the
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increase in the nanochannels’ charge.
+
-
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The strong surface charge effects were revealed in the membrane’s conductance 𝐺[ variation with the
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electrolyte concentration c (Figure 3d). Starting from 𝑐 = 1 M, the observed 𝐺[ immediately deviates from
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the expected linear regime for a charge-neutral membrane (black solid line), indicating the compression of the
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EDL in the nanochannels even at high ionic strengths. In contrast, the charge effects were previously observed
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to dominate the conductance in solid-state constrictions only at much lower salt concentrations
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that the cation selectivity, as deduced from ionic permeabilities, could reach as high a value as 𝑆8 = 96% at
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low salt concentration (Figure 3e,f).
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. We note
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To gain insight into the surface charge-driven ionic transport, we applied mean-field theoretical model
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based on the Poisson-Boltzmann and Navier-Stokes equations (see the Supporting Information for more
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details). The model fits the observed pH and molarity dependence of both the conductivity and the charge
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selectivity well (Figure 3), assuming the ions flow in pristine graphene nanochannels with an effective height of
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ℎG = 0.9 nm, an effective width in the range of 𝑤G ~50 nm, an effective channel length of 𝐿eff = 0.4 mm
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and a constant density of active site on the sidewalls corresponding to one protonable charged site per 2 nm
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(Figure S6). A crucial assumption of the model is the infinite-slip boundary condition for the water flow at the
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top and bottom graphene surfaces, and no-slip condition at the oxidized sidewalls. The large slip-length is
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consistent with the effect of frictionless water flow, as reported in GO membranes . The other possible
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geometries could not replicate the observed pH and molarity dependence of the conductance (see Supporting
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Information). We employed the same set of parameters to concurrently simulate all the independent
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experiments. The parameters deduced from the model are within the range expected for the GO membrane,
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despite crude the approximations. Although this continuous-media model has a limited scope at nanometer
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length scales, it has been shown to capture the relevant physics and to give sufficient semi-quantitative insight,
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where the intermolecular and steric interactions are renormalized into the effective hydrodynamic
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dimensions
36, 39
.
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In conclusion, we have shown that the ion-rejection in graphene-oxide membranes is driven as much by
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the electrostatic repulsion (defined by the nanochannel surface charge) as it is by the activated size-exclusion
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(defined by the nanochannel height). Hence, the engineering of the surface charge of the membrane offers a
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new venue for increasing the overall salt rejection, without constraining the water flux. We have demonstrated
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that the GO membranes exhibit ultra-high charge selectivity, reaching up to 96%, driven by the negative surface
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charge of the oxygen-carrying functional groups in the membrane’s nanochannels. Coupled with their high-
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durability and scalability, the GO membranes are well positioned for applications in high-performance ion
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exchange and electrodialysis technologies.
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Figure 1 The drift-diffusion experiment. (a) Schematics of the experimental setup: the graphene oxide
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membrane was mounted on a freestanding SiNx membrane with an 12×12 array of square-shaped windows,
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separating two electrolyte-filled reservoirs; Ag/AgCl electrodes in each reservoir are used to apply an electric
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potential across the GO membrane and to measure the ionic currents flowing through the membrane. (b and c)
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Depiction of the ionic flow across the membrane driven by the concentration gradient (diffusion), and by the
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voltage difference (drift), respectively. (d) The ionic current-voltage characteristic of the membrane for
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different salts, measured under the concentration gradient 0.1M/0.01M across the membrane.
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Figure 2 Charge-selective permeability. (a) Permeation rates (p) for different cations (circles) and
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corresponding chloride counter-ions (open and filled squares) as a function of hydrated radius (RH) of the
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cations. The filled square represents the chloride permeability when in RbCl solution, where the hydration radii
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are very similar for both ions – the two-headed arrow shows the permeation difference resulting purely from
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the charge-rejection effects. The solid blue line is a guide to eye. (b and c) Schematics of the dominant ion
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rejection mechanisms: size exclusion (b) and electrostatic repulsion (c). (d) The cationic selectivity of GO
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membranes for different salts, reaching values in excess of 90%. Inset: the permeation rates of chloride ions as
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a function of the valence of the position counter-ion in the salt, revealing the effect of the correlated charge
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inversion in the sub-nanometer channels.
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Figure 3 Molarity and pH dependence of conductance and ionic permeation. (a) Current-voltage (I-V) curves
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across the membranes at KCl salt concentration 𝑐KCl = 10 mM, measured for different pH values. (b)
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Conductance vs pH. (c) Permeation rates for potassium and chloride ions for different pH values. (d) The ionic
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conductance vs molarity (circles) deviates from the Ohmic behavior (full line), even at high salt concentrations,
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due to sub-nanometer channel heights. (e and f) Molarity dependence for the permeation rates (e), and for
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the cation selectivity (f). Dashed curves in all the graphs are fit to the mean-field model, discussed in the text.
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▪ ASSOCIATED CONTENT
2
Supporting Information
3
The Supporting Information is available free of charge on the ACS Publication website at DOI:
4 5 6 7 8 9 10 11 12
Physiochemical characterizations of graphene oxide nanosheets; Interplanar spacing expansion of graphene oxide membranes in water; Quantitative analysis of ion selectivity across the membranes; Effect of SiNx substrate on the ion permeation; Calculation of ionic conductance and surface charge density; pH-dependent ionic conductances and surface charge densities; Effects of excess hydronium or hydroxide ions; pH-dependent drift-diffusion measurements; Mean field model for ion transport in the nanochannels; Validation of the analytical continuum models; Ion strength-dependent ionic conductance and cation permselectivity ▪ AUTHOR INFORMATION
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Corresponding Author
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* E-mail:
[email protected] 15
Author Contribution
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H.S. and S.G. conceived the concept of the study. H.S. performed the experiments and analyzed the data
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together with C.C. and J.A.G.C. H.S., M.V.S.M., Y.C.S. and J.A.G.C. fabricated and characterized the membranes.
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The continuum model analysis was performed by C.C. The manuscript was written by H.S. and S.G. with
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comments and input from all authors.
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Notes
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The authors declare no competing financial interest.
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▪ ACKNOWLEDGEMENTS
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We acknowledge support from the National Research Foundation, Prime Minister’s Office, Singapore, under
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the NRF Fellowship Program (Award No. NRF-NRFF2012-09) and Competitive Research Program (Award No.
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NRF-CRP13-2014-03). The authors are grateful to Dr. Eugene Choo of ZEISS Advanced Imaging Centre
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(Singapore) for assisting the FIB preparation of nanopores.
27
▪ REFERENCES
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R. R. Science 2014, 343, (6172), 752-754. 10
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▪ Table of Contents
van der Heyden, F. H. J.; Stein, D.; Besteman, K.; Lemay, S. G.; Dekker, C. Phys. Rev. Lett. 2006, 96, (22),
Garaj, S.; Liu, S.; Golovchenko, J. A.; Branton, D. Proc. Natl Acad. Sci. 2013, 110, (30), 12192-6.
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grapehe-oxide layers
1 2 3 4
Nano Letters 16 hydration charged Page functional shell groups
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ion
ACS Paragon Plus Environment
Size selectivity
of 16
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ion
Charge selectivity