Lidia
Lancellotti
a,
Antonio
Bianchi
a,
Alessandro
Kovtun
a,
Massimo
Gazzano
a,
Tainah Dorina
Marforio
b,
Zhen Yuan
Xia
c,
Matteo
Calvaresi
b,
Manuela
Melucci
*a,
Chiara
Zanardi
*ad and
Vincenzo
Palermo
*ad
aInstitute for Organic Synthesis and Photoreactivity, National Research Council (ISOF-CNR), via Piero Gobetti 101, 40129, Bologna, BO, Italy. E-mail: palermo@isof.cnr.it; manuela.melucci@isof.cnr.it; chiara.zanardi@unive.it
bDepartment of Chemistry ‘G. Ciamician’, Alma Mater Studiorum University of Bologna, via Selmi 2, 40126 Bologna, Italy
cDepartment of Industrial and Materials Science, Chalmers University of Technology, Gothenburg S-41296, Sweden
dDepartment of Molecular Sciences and Nanosystems, Ca’ Foscari University of Venice, via Torino 155, 30172 Venezia-Mestre, Italy
First published on 6th March 2024
Filters made of graphene oxide (GO) are promising for purification of water and selective sieving of specific ions; while some results indicate the ionic radius as the discriminating factor in the sieving efficiency, the exact mechanism of sieving is still under debate. Furthermore, most of the reported GO filters are planar coatings with a simple geometry and an area much smaller than commercial water filters. Here, we show selective transport of different ions across GO coatings deposited on standard hollow fiber filters with an area >10 times larger than typical filters reported. Thanks to the fabrication procedure, we obtained a uniform coating on such complex geometry with no cracks or holes. Monovalent ions like Na+ and K+ can be transported through these filters by applying a low electric voltage, while divalent ions are blocked. By combining transport and adsorption measurements with molecular dynamics simulations and spectroscopic characterization, we unravel the ion sieving mechanism and demonstrate that it is mainly due to the interactions of the ions with the carboxylate groups present on the GO surface at neutral pH.
The ability to induce selective ion transport in membranes could lead to valuable separations among multivalent (e.g. Ca2+, Mg2+, Pb2+, Cr3+) and monovalent (e.g. Na+, K+) metal ions, crucial for applications ranging from water desalination, softening, and purification to the extraction of rare elements.
In recent years, graphene oxide (GO) has emerged as one of the most promising materials for creating innovative membranes.9–15 These membranes can be fabricated through direct filtration of suspended GO nanosheets in water on porous substrates, resulting in highly ordered and uniform membranes with nanochannels formed between overlapped nanosheets.16–19 The application of an electric field has been found to induce selective migration of monovalent ions relative to divalent ones, offering new prospects for using GO membranes in ion separation applications.20–27 Several studies have demonstrated how ion migration can be modulated by the surface potential and influenced by an external electric field or changes in the polarity and field strength.20,28
While the mechanism behind the selective transport of ions within the nanochannels of membranes remains a subject of debate, it is generally accepted that it involves size exclusion and/or electrostatic interactions. The smaller diameters of monovalent cations (e.g. 3 and 4 Å for K+ and Na+, respectively) compared to those of multivalent cations (e.g. 6 and 8 Å for Ca2+ and Mg2+)29,30 explain the sieving mechanism based on steric effects. Various strategies have been developed to modify the interlayer spacing (d) of graphene-based structures, aiming to modulate their sieving activity. These strategies include physical confinement16 and alterations in the pH or ionic strength of the surrounding solution.31
Despite the advantages of GO-based membranes in inducing selective ion transport, their practical application has been limited to the laboratory scale due to constraints in producing compact and homogeneous filtering materials with surface areas larger than a few cm2, which are necessary for realistic water flows in real-world applications like water purification.
On the other hand, a well-established commercial filter type employs polymer hollow fiber modules, such as polyethersulfone (PES). These cost-effective modules are widely used for microfiltration. A typical filter consists of hundreds of hollow fibers (HF, Fig. 1a–c) of sub-millimeter diameter (300 μm in our case study) and nanometric lateral pores, determining the overall module cut-off (150 nm in our case study).
Fig. 1 (a) SEM image of PES hollow fibers with an inner coating of GO. On the left part of the image, some cracks due to fiber cutting are used to show the layered structure of the coating. The thickness of each layer is reported. Additional SEM images of uniform coating are presented in the ESI.† (b) GO-PS hollow fibers mounted in a filter. (c) The whole filter assembled. (d) Cartoon showing the filtering mechanism of the hollow fibers with purified water coming out of the lateral surface pores. (e) Cartoon showing the water flux and filtering action across the GO-HF multilayer (not in scale). |
In the standard cross-flow filtration mode, the feed solution flows inside the fiber and the purified water crosses the fiber section, exiting from the lateral surface pores, as schematized in the cartoons of Fig. 1d and e.
Recently, we demonstrated the feasibility of coating PES fibers with GO, resulting in a composite bilayer membrane (HF-GO, Fig. 1d and e). This membrane retains the microfiltration properties of PES-HF while also enabling the adsorption of small organic molecules. The adsorption occurs through the intercalation of molecules between stacked GO layers, as confirmed by X-ray diffraction (XRD) analysis before and after adsorption.32
HF-GO fibers offer a unique opportunity to create GO membranes with a large area (approximately ≈250 cm2 instead of just a few cm2) and to study ion sieving in scalable and commercially available devices. The cut-off of these commercial filters is smaller than the average size of GO nanosheets, and this offers a unique opportunity to self-assemble uniform coatings of GO with a large area inside these hollow fibers by simple filtration. The process continues until a uniform coating is obtained on the whole surface of each of the >200 microfibers in the filter, as demonstrated by permeability experiments.32 Leveraging these multilayer fiber-like filters, we investigate here the transport of monovalent (i.e. Na+, Li+, and K+) and divalent ions (i.e. Ca2+ Mg2+, and Pb2+) induced by an applied potential difference in HF-GO filters. The goal is to demonstrate that the selective ion transport observed in planar membranes is preserved in these large-scale filters and to understand the mechanism controlling the transport.
We study the activated ion transport in GO-HF membranes and compare it with that in planar GO membranes, with adsorption studies on GO powders, and with molecular dynamics and quantum mechanics calculations. These analyses highlight the combined effect of the ionic radius and chemical interactions with GO nanosheets as driving forces behind selective ion transport.
HF internally coated with GO were obtained according to a previously reported procedure.32 Briefly, 2 mg mL−1 of GO suspension (obtained by sonication in ultrapure water for 4 h) was filtered in cross-flow mode. Being the average lateral dimension of GO nanosheets larger than the fibers cut-off,33 the GO nanosheets adhered to the inner surface of the hollow fibers; the process of coating is self-limiting, given that areas already coated with GO will see a reduction in flux, while holes and leaks will attract a higher flux until they get uniformly coated by GO, creating an ordered membrane (Fig. 1e), and then stabilized by annealing at 80 °C. The uniformity and adhesion of the GO films stabilized in this way on the fibers were excellent, similar to what already demonstrated in previous work. GO-PES-coated fibers showed no release even after extensive filtration tests performed following a procedure described in ref. 32.
Good uniformity was confirmed by static ion permeability tests: in absence of any driving force, no diffusion of ions across the filter was observed, which could exclude the presence of cracks or leaks even at nanometric size (see also more details in the “Results” section). SEM images taken on different cut fibers also showed a uniform stable coating, see Fig. 1a; additional SEM images of the fiber cross section, taken along the fiber long axis, can be found in the ESI.† The thickness of the GO coating was tuned by reiteration of the GO filtration process (i.e., by increasing the volume of GO suspension filtered) reaching a thickness of up to 1.5 μm. Table S1† shows the relationship between the amount of GO injected into the filter (% w/w) and the thickness of the GO membrane of the PES fiber finally obtained, together with the acronym of the filter used hereafter.
Before use, 1 L of 10−5 M aqueous solution of KCl was used to wash each filter in a dead-end configuration, i.e., in the same direction used later for ion transport. Each filter was then stored in this same electrolytic solution to tune the ionic conductivity when applying the electric field to activate ion migration. Some filters were treated and stored with HCl instead of KCl, as discussed below.
Tank 1 contained the electrolytic solution (0.1 M solution of the salt under investigation), while tank 2 contained ultrapure water (resistivity >18 MΩ cm). The two tanks were set at the same height to avoid any artefacts due to differences in pressure, which could influence transport behaviour. A constant potential of −1.0 V was applied to the electrode in tank 2, while the electrode in tank 1 was grounded. The variation of the conductivity of solution in tank 2 was tested every 10 min by performing measurements by electrochemical impedance spectroscopy (EIS), connecting interdigitated gold electrodes (DropSens-Metrohm) to the Frequency Response Analyzer (FRA) filter of the Autolab PGSTAT12 (Metrohm-Ecochemie). Frequency scans were performed over the range of 0.1–100 kHz with a signal amplitude of 50 mV. The DC bias was temporarily stopped during the collection of the EIS signal to avoid any interference; the impedance values were converted into conductivity values according to a methodology previously reported34 and, ultimately, to the total amount of ions transported to tank 2. The amount of ions transferred after 120 min was measured by atomic spectroscopy measurements (see Section 2.6). Three replicates were performed for each experiment. The linear correlation between the values of conductivity measured and the concentration of ions in solution was confirmed using a calibration curve (Fig. S2†).
The quantification of Li+, Ca2+, Mg2+, and Pb2+ was obtained by inductively coupled plasma optical emission spectroscopy (ICP-OES) performed with a PerkinElmer Optima 4200 DV simultaneous spectrometer. The sample introduction system used a pneumatic nebulizer coupled with a glass spray chamber. Four standard solutions for each cation were prepared starting from a 1000 mg L−1 standard solution to calculate the calibration plot of each element.
160 ns of MD simulations were carried out, fully sampling the behaviour of the cations in the inter-layer regions. Periodic boundary conditions (PBC) were employed to simulate infinite sheets. The analysis of MD simulations was performed with CPPTRAJ, a post-processing tool implemented in Amber18.40 The effect of the electric field was simulated using the “external electric field” implementation present in Amber18. An intensity of 1 V cm−1 was applied along the X-axis. The affinity of the ions for the GO sheets was computed using the MM-GBSA (Molecular Mechanics-Generalized Born Surface Area) algorithm.
In the absence of an applied potential, no spontaneous transport of ions was observed in the GO-coated filters and the ion concentration in tank 2 stayed null (Fig. S3 in the ESI†), demonstrating that even the thinnest GO coatings were uniform enough to block any ion transport in the absence of an external driving force. Even after long exposure, atomic spectroscopy analysis did not show the presence of Na+ and Ca2+ in tank 2, indicating that their concentration was under the limit of detection of the technique. Instead, we observed ions diffusing freely in the reference samples prepared without GO coating, the cut-off of the pristine fibers (150 nm) being much larger than the size of the ions, allowing tank 1 and tank 2 to reach an equal concentration (Fig. S3†). This evidence confirmed that the GO deposition approach used yielded a continuous coating on each fiber of the filter with no gaps or micro-cracks that would cause spontaneous leak of ions from tank 1 to tank 2.
After these initial checks, we activated ion transport by applying a potential of −1 V to electrode 2, while electrode 1 was grounded (Fig. 2a). The conductivity of the solution in tank 2 was monitored every 10 min by EIS, as described above. Fig. 3a shows, as an example, the variation of the conductivity due to the transport of Na+ in three different filters: after about 30 min, the conductivity of the solution increased, ultimately reaching a plateau after about 100 min. Besides the in situ measurements of ion concentration with EIS, the total number of ions ultimately present in tank 2 after 120 min was also quantified ex situ by atomic spectroscopy measurements to avoid possible artefacts due to other ions present in the solution influencing the total conductivity.
We compared the ion transport of monovalent and divalent cations which are relevant for water purification, namely Na+, Li+ and K+ with Ca2+, Pb2+, and Mg2+; these tests where repeated three times for each ion (see typical results in Fig. S4†) using GO coatings with 1.5 μm thickness (HF-GO-5).
Significant differences of transport were observed for different ions (Fig. 3b), suggesting that the transport in the GO membrane cannot be explained by a simple electric drift, but should depend on the chemical interaction of ions with the GO membrane.
Thanks to the 2D shape of the GO nanosheets, each ion should travel a tortuous path within the nanosheets (Fig. 2c), which have an interlayer distance of ca. 8–10 Å; while traveling in this space, ions will interact strongly with the numerous chemical moieties present on the surface of the GO nanosheets, so any difference in GO–ion interaction will be amplified by the tortuous path, leading to different diffusion rates. As an example, a rough estimate assuming an average GO sheet size of 1 μm, a layer thickness of 1.5 μm and an interlayer spacing of 8 Å gives a tortuous path of ≈0.94 mm for the ions to cross the filter.
Ca2+ has a larger hydrated radius than Na+ and, for its chemical nature, can be coordinated by the oxidized moieties present on the GO nanosheets. The ability of GO membranes to discriminate monovalent cations from bivalent cations has been demonstrated previously for planar GO membranes;35,47 this fundamental feature is observed also in the GO-HF studied here, which are more suitable for real applications.48–51
The differences observed could be due to (1) different sizes of the ions, expressed as the hydrated radius, (2) different charge, which will cause different ion mobilities in an electric field, or (3) different interactions with the charged moieties present on the GO surface.
Previous studies attributed the different permeation of ions in GO membranes to the different ionic radii of monovalent and divalent ions.18,19,52–54 To check if this hypothesis is true in our systems, Fig. 3b (black symbols) shows the concentrations of ions in tank 2 vs. the dimension of the hydrated radii of the relevant cation measured at neutral pH. An exponential correlation is observed for most ions (red dashed line in the semi-log plot of Fig. 3b), in agreement with previous reports on planar membranes35 with some interesting exceptions. Indeed, Pb2+ shows a lower permeation than Na+, despite having a similar hydrated radius. Moreover, the amount of Li+ is significantly lower with respect to Ca2+, despite their radii being similar. These results indicate that the transport properties of GO could not be explained by the ionic radius or charge alone, but rather by a combination of different parameters.
Besides the hydrated radius and charge, we also checked for a correlation of the number of ions transported across GO with other atomic parameters, such as the Stokes radius of the ions or their charge density (calculated as ionic charge/ion volume) but found no clear correlation with these additional parameters.
Indeed, the presence of charged groups protruding out of GO can foster the formation of coordination complexes with stability that does not follow the order of classical complexes in bulk solutions. Shibahara et al. demonstrated a strong chelating effect of GO functionalized with iminodiacetic acid, where the ability to capture heavy ions was depending on the synergic effect of the chelating acid groups and the GO surface.12 Sun et al. also demonstrated a synergic effect of aminobenzene groups to stabilize the Na+ ions on pristine (non-GO) graphene for energy storage applications.13
It is well known that negatively charged moieties on GO can be protonated; Terrones et al. demonstrated that there are three equilibria in GO, two relative to carboxylic acids exhibiting different acidity (pKa1 ≈ 4.0 and pKa2 ≈ 6.0) and one relative to alcohols (pKa4 ≈ 10.0).55 Titration experiments performed by adding KOH to the solutions of our GO confirmed that the most significant deprotonation took place at pH = 6.0 in agreement with previous results. Thus, to unravel the role played by the chemical interactions induced by oxidized moieties present on GO nanosheets in the ion transport, we pre-treated the filter with HCl at pH = 5 to partially protonate the carboxylate groups and remove the negative charge present on it according to: GO-COO− + H+ ⇄ GO-COO-H. We then tested again the transport of Ca2+ and Na+ (red symbols in Fig. 3b) as a representative example of ions possessing or not the tendency to be coordinated by Lewis organic donors. Quite interestingly, the amount of Ca2+ transported through GO increased 800 times when the filters were treated with HCl, going from 1.18 × 10−2 μmol to 9.78 μmol. We ascribe this effect to the fact that protonated oxygenated groups are not available to coordinate Ca2+. The amount of Na+ decreased slightly, going from 0.52 μmol to 0.1 μmol.
Thus, protonated groups are beneficial for Ca2+ transport, while hindering Na+ transport, due to the coordination effect previously mentioned.
To better explain the differences in the ion transport observed for GO-HF, we compared these results with atomistic simulations and with other tests performed in different simpler geometries using GO planar filters or measuring ion adsorption on GO with no ion transport, as detailed below.
Fig. 4 (a) Cartoon showing the adsorption of ions on GO under static conditions. (b) Percentage of ions adsorbed upon exposing 0.1 M solution to GO nanosheets at different pH values. |
The concentration of the solution was the same as that used in the HF-GO filtration tests; the protonation of GO was varied by varying the pH through addition of HCl to the solution. Fig. 4b and Table S2† show the results obtained. Each data point is an average of three separate tests.
The results showed that the uptake of Ca2+ decreased significantly at acidic pH, suggesting that the protonation of GO oxygenated groups at low pH hinders their coordination with Ca2+, thus lowering the adsorption efficiency toward Ca2+, in agreement with the ion transport results. Pb2+ and Mg2+ showed a strong interaction with GO, which became weaker at low pH as well, even if the change results only evident at a low pH value due to the strong interaction with GO oxidized moieties.
Instead, the uptake of Na+ and K+ in GO was poor with no significant differences at all pH values, confirming their weak chemical interaction with GO nanosheets, as expected based on the poor tendency of these ions to be coordinated by oxygenated groups. This agrees with what observed from experiments carried out in the filters. The uptake of Li+ was instead significantly stronger, due to its better interaction with GO, also this is in agreement with the transport measurements.
We fully sampled the behaviour of the cations in the inter-layer regions (interactions with epoxides, hydroxyls, carboxylate and all the possible combinations). We evaluated the MM-GBSA binding energy for 5000 snapshots, sampling all the different positions that the cations can assume (Fig. S7 in ESI†). MD simulations demonstrated that both Na+ and Ca2+ interact significantly with the GO membrane. The adsorption energy of the divalent Ca2+ ion (−58.2 kcal mol−1) with the negatively charged membrane was higher than the monovalent Na+ ion (−39.3 kcal mol−1). The difference in the adsorption could be ascribed to the electrostatic interaction term (see Table S3†). In its favorite adsorption site (Fig. 5c), the monovalent Na+ ion interacts with a single carboxylate group, while the divalent Ca2+ ion can interact simultaneously with two carboxylates (Fig. 5d). This gives a much stronger electrostatic interaction for Ca2+ (−86.7 kcal mol−1) as compared to Na+ (−50.8 kcal mol−1). van der Waals interactions tend to destabilize the interaction for the larger Ca2+ ion (+28.9 kcal mol−1) more than for the smaller Na+ (+12.0 kcal mol−1), but this steric repulsion is not strong enough to counter the electrostatic attraction.
The spatial restriction between two GO sheets is crucial to entrap the ions, because in simulations with a single GO sheet, the ions were not stable on the nanosheet and could diffuse in the bulk water (see Table S4†). The average distance of the ion from the binding COO− groups (Fig. S5†) was roughly proportional to the ionic radius, but there was no clear correlation of such distance with the adsorption energy.
We quantitatively estimated the diffusion of Na+ and Ca2+: when the cations are in the inter-layer region, in the absence of an external electric field, the calculated diffusion constant for Na+ and Ca2+ was 2.6 and 1.8 × 10−11 m2 s−1, respectively. Such numbers are significantly smaller than what calculated in bulk water for Na+ and Ca2+ (6.63 and 1.28 × 10−9 m2 s−1, respectively).
When an external electric field with an intensity comparable to the experimental conditions (1 V cm−1) was applied in the simulation, the diffusion of Ca2+ was strongly reduced, going down to 0.42 × 10−11 m2 s−1 (4.5-fold reduction, see Table S4†), while the diffusion of the Na+ ion increased to 3.8 × 10−11 m2 s−1 (10-fold increase), in line with the experimental observations.
MD simulations suggest that, in the absence of an electric field, Ca2+ ions diffuse freely and can diffuse preferentially in areas with no blocking groups. When the electric field is applied, there is a preferential migration direction induced by the field and Ca2+ ions follow this direction, colliding with the functionalization, thus reducing their migration speed. As for Na+ ions, being smaller, this effect is less pronounced, and therefore an overall acceleration is observed in the presence of the electric field.
The model should be considered just indicative, given that the electric field is not always parallel to the nanosheets, and is partially shielded by the ions in solution. However, these results indicate that the external electric field could provide improved mobility for Na+ ions. On the opposite side, the diffusion of the Ca2+ ions is hindered.
The MD simulation and experimental results showed a crucial role of the carboxylate groups in the interaction between GO and ions. Thus, we decided to perform QM/MM calculation to evaluate quantitatively the binding energies between the carboxylate groups of GO nanosheets and the different ions (Fig. 5a).
Fig. 6 shows the correlation between the GO–ion dissociation energy (calculated by computation) and the amount of ions adsorbed by GO measured in the adsorption experiments.
Fig. 6 Relationship between the GO–ion dissociation energy calculated by simulations and the amount of ions adsorbed by GO measured in the batch adsorption experiment at neutral pH (also shown in Fig. 4). The dashed line is a guide for the eye. |
A good correlation between the computational and experimental data can be seen; ions with a weak interaction with GO, like Na+ and K+, can penetrate into GO and travel quite easily through the membrane. Ions with stronger interaction with GO, like Li+ and all divalent ions, can penetrate easily into GO but get stuck in specific adsorption sites of the membrane. This effect can be mainly ascribed to electrostatic interactions with the negatively charged groups of GO.
During their travel in the GO membrane, the ions will likely reside most of the time in correspondence of negatively charged groups (e.g. partially protonated COO− groups), eventually hopping from one group to the other and moving from tank 1 to tank 2.
Ca2+ ions have a strong interaction with such COO− groups, which will act as traps for the Ca, coordinating them in highly stable configurations. Upon protonation, such a trapping effect decreases, allowing the ions to better drift across the GO filter.
Na+ ions can also have weak interaction with GO, allowing them to pass in large quantities across GO jumping form one COO− to the other. Upon protonation, the amount of COO− available for such transport decreases, thus hindering slightly the Na transport. The different interactions of Ca2+ and Na+ would agree well with what observed in static batch adsorption tests (Fig. 4b) and with computational data (Fig. 5 and Table S3†).
These planar membranes featured selective filtration as well, with Na+ being transported much better than Ca2+.
MD calculations suggested that Ca2+ is a better intercalant than Na+ in GO, even if showing worse transport properties. Indeed, XPS confirmed the presence of more Ca2+ than Na+ inside GO: we found about 0.18 at% of Ca2+ and 0.03 at% of Na+ in the membranes after transport experiment driven by the electric field. There is more calcium than sodium in the GO, even if more sodium is transported across GO. Thus, there is no correlation between the presence of ions in GO and the amount transported, confirming what already observed by MD, i.e., the ions which are more strongly interacting with GO do not show good transport performance.
We also used XPS to check if the ions transported damaged or modified the chemical structure of GO. The oxidation degree of the membranes was not affected by ion transport, the O/C ratio obtained from C 1s and O 1s XPS signals was within the narrow range between 0.38 and 0.40 in each membrane before and after the transport. The C 1s signals were almost identical in all samples. The analysis of C 1s signals showed only a small decrease of epoxy groups after the hydration of the membrane, while no difference in the composition was found between the hydrated GO membrane and the GO membrane after Na+ and Ca2+ passage. See the ESI† for more details.
The presence of ions can vary the interlayer distance (d) between the GO nanosheets, so we used XRD to detect the eventual intercalation of ions in GO. Measurements were done on three membranes used for transport of Na+ and for Ca2+, respectively; the results were compared with the GO membranes exposed to pure water (d = 8.2 ± 0.2 Å). Fig. 7a shows clearly that the migration of ions within the membrane led to an increase of d, but with a different extent according to the different ions: d increased to (8.6 ± 0.1) Å for Na+ and to (9.0 ± 0.1) Å for Ca2+.
As a further test, we checked if similar results could be obtained without the electric field using instead brute force to achieve transport in the form of high hydraulic pressure, as typically done in reverse osmosis filters. Indeed, upon filtration of massive amounts of solution (>20 ml as compared to 2 ml used for electric field tests), some ions do indeed pass through and reach tank 2 with some preferential transport selectivity of Na+ over Ca2+ (+77% of Na+ ions passed with respect to Ca2+). However, no significant variations of d were observed by simply applying mechanical pressure using a pump (Fig. 7b). XRD is a bulk-responsive analytical method, so not sensitive to eventual ions blocked on the surface of the GO; analysing, instead, the treated membranes with a surface technique like XPS, a significant amount of Ca2+ was found on the membranes (0.42 ± 0.05 at%, more than double of what observed using the electric field, Table S5†), indicating that the membrane, in the absence of an electric field, acts as a sieve blocking most Ca2+ on its surface and that the electric field is needed to achieve transport of ions in GO, again highlighting the critical role of electrostatic interactions between the ions and GO.
By combining experiments performed on ion transport and ion adsorption, together with molecular dynamics simulations, XPS and XRD characterization, we could demonstrate that the differences in ion transport can be ascribed only in part to the ionic hydrated radius; a significant effect is due to the strong interaction of the carboxylate groups present on GO with the travelling ions, enhanced by the confined geometry of the stacked GO nanosheets.
Ions which interact strongly with GO will easily penetrate in between the sheets, as in the case of Ca2+, but will not be able to diffuse rapidly through the GO coating. Protonation of the carboxylate groups will allow instead a faster diffusion of Ca2+. The adsorption of Pb2+ and Mg2+ is instead so efficient that it is not affected significantly by the partial protonation of oxygenated residues; the adsorptive efficiency of GO toward these cations decreases only at the lowest pH tested.56 GO could be used thus as an efficient scavenger of such ions for water purification, but not as a filter.
Monovalent ions can interact significantly with GO, but less than divalent ions. This difference is due mostly to electrostatic interactions with the charged carboxylate groups and only to a minor extent to steric effects due to the different ionic radii.
Na+ and K+ can travel easily within GO, interacting significantly but reversibly with the carboxylate groups. Li+ shows instead a stronger interaction with GO, which hinders its ion transport performance.
Besides providing fundamental insight into the transport mechanisms, this work provides new perspectives in the design of ion sieving devices based on commercially available building blocks (GO and PES filters), and scalable, low cost, and sustainable membrane fabrication procedures (water based, low energy demanding) to be applied in water softening and desalination, among the others.
Even if such filters still cannot be applied at the commercial level, this practical demonstration of performance and the better understanding of ion sieving mechanisms is, in our opinion, a significant step towards practical applications of GO-based membranes in water purification.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d3nr05874c |
This journal is © The Royal Society of Chemistry 2024 |