Xue
Zhang
and
Dadong
Shao
*
School of Environmental and Biological Engineering, Nanjing University of Science and Technology, Nanjing 210094, P R China. E-mail: shaodadong@126.com
First published on 20th July 2023
Seawater is a huge store of uranium, and the related uranium retraction technology has become a critical step in the sustainable development of nuclear power. For obtaining uranium U(VI) from seawater cheaply and environmentally, we introduced K2FeO4 during the polyamidoxime (PAO) preparation process in water to endow PAO with high antibacterial and low agglomeration properties. In this reaction, only water was used as the solvent with the goal of extracting U(VI) from seawater in a low-cost, pollution-free manner. Studies showed that the adsorption of U(VI) on K2FeO4@PAO conformed to a pseudo-second-order model, and the maximum adsorption capacity calculated by the Langmuir model was 137 mg g−1 at 298 K and pH 8.2. Moreover, K2FeO4@PAO showed high selectivity for U(VI) compared with a range of metal ions. K2FeO4@PAO also showed good recyclability, and the recovery rate only decreased by 3% after six cycles. In addition, antibacterial experiments indicated that K2FeO4@PAO could effectively inhibit the growth of Escherichia coli (E. coli) and Vibrio alginolyticus (V. alginolyticus) that are commonly found in seawater.
Polyamidoxime (PAO)-based materials can adsorb U(VI) due to the O and N atoms of PAO having the same distance and lone pair of electrons, and these are thus among the hot materials in U(VI) extraction research. Resulting from polyacrylonitrile's (PAN) low cost, good chemical stability, and easy industrial production, numerous adsorbents select it to prepare PAO-based materials for U(VI) recovery.16–18 There are many methods for synthesizing PAO in the laboratory. The classic synthesis method is –CN amidoximation, which can be divided into homogeneous and heterogeneous processes according to the solvent. The homogeneous method mainly involves the reaction of PAN and NH2OH in an organic solvent with dimethyl sulfoxide and N,N′-dimethyl formamide generally chosen in the laboratory. The heterogeneous method mainly involves the reaction of PAN with NH2OH in water and methanol/water solutions. Organic solvents are often required in this method, which makes it not only harmful to the environment but also increases the cost of U(VI) recovery, dramatically reducing the competitiveness of PAO in U(VI) extraction. Thus, we considered selecting water as a solvent during the amidoximation process. PAN, as a macromolecule material, is prone to agglomerate in water, leading to intramolecular bond accumulation without the reaction of its groups.19,20 In this work, K2FeO4 was adopted to inhibit the aggregation of PAN in water with an aim to obtain a higher conversion rate.
In the U(VI) extraction process, the interaction between U(VI) extraction materials and marine microorganisms should be considered in addition to improving the U(VI) recovery rate and cost.21,22 Seawater is a very harsh corrosive environment, which is typically characterized by high biological activity, with 106 colony-forming units (CFU) per mL level microbes (including bacteria and microalgae) found to exist in seawater. The microbes and their metabolisms affect material surface properties, which can eventually affect the U(VI) extraction performance. Thus, there is a necessity to design a novel adsorbent to achieve an antifouling goal.15,23,24 The corresponding standard electrode potentials of FeO42− both in acid (2.20 V) and alkali (0.72 V) media are higher than the well-known strong oxidant KMnO4 under the same conditions. This strong oxidation ensures the strong bactericidal ability of FeO42−. K2FeO4 can kill both Gram-positive and Gram-negative bacteria, fungi, viruses, and spores.25,26 The introduced K2FeO4 in PAN can inhibit the corrosion from marine microorganisms.
The structure of a material determines its properties, and ultimately affects its application optimizing the structure of a material is an effective way to enhance its properties and expand its application fields. Herein, we constructed the anti-biofouling nanoscale adsorbent K2FeO4@PAO for U(VI) recovery by introducing K2FeO4 during the amidoximation method with only water as a solvent (Fig. 1). The added K2FeO4 could overcome PAN agglomeration in water, so that PAN could well contact with NH2OH, which could help realize the economic and environmental recovering of uranium. Meanwhile, the high oxidation ability of K2FeO4 could exterminate bacterial. The obtained antibacterial K2FeO4@PAO particles exhibited a higher adsorption capacity and better anti-biofouling properties than PAO under the experimental conditions.
Fig. 1 Scheme for the fabrication and application of K2FeO4@PAO in the extraction of U(VI) from seawater. |
To study the effect of K2FeO4 on the PAO surface topologies, the microstructures of PAN and PAO prepared at different conditions were analyzed by SEM (Fig. 2A), with varying the addition amounts of K2FeO4 and PAN in the preparation process, as shown in Table 1. The SEM images indicated that the addition of 0.20 g K2FeO4 had no significant effect on PAO surface topologies, and the obtained K2FeO4@PAO was uniformly dispersed. As the mass of K2FeO4 increased, PAN agglomeration became more evident, and eventually, a PAN block was formed. The three reactions include the formation of –CN from unsaturated amine, the redox reaction between NH2OH and K2FeO4, and the conversion of –CN to –C(NH2)N–OH, which restrict and promote each other in water. When the amounts of PAN and NH2OH were much more than K2FeO4, the amidoximation reaction was the primary reaction in solution, and finally, uniform dispersed PAO particles were obtained. When the K2FeO4 amount was higher than PAN and NH2OH, the solution reaction was dominated by the redox reaction of K2FeO4 and NH2OH, which consumed most of the NH2OH and made it impossible to complete the conversion of –CN, instead forming –CN rings on the PAN macromolecular chains and thus creating bulk materials. Besides SEM, TEM was also applied to study the morphologies of PAO and K2FeO4@PAO. As shown in Fig. 2B, the single PAO presents a block form, but transformed into nanoscale particles (K2FeO4@PAO) after K2FeO4 was introduced. It was found that C, N, and O elements were uniformly distributed on PAO and K2FeO4@PAO surfaces by the TEM element mapping. Moreover, Fe was evenly distributed on the K2FeO4@PAO surface, proving that K2FeO4 recombined with PAO successfully. It is considered that the –C(NH2)N–OH unit in K2FeO4@PAO is the core of its application in U(VI) extraction. The adsorption capacity of K2FeO4@PAO for U(VI) gradually increased with increasing the PAN amount when the K2FeO4 amount was fixed at 0.20 g (Fig. S2A†) and decreased with increasing the K2FeO4 amount when the PAN amount was set at 2.00 g (Fig. S2B†). Therefore, the K2FeO4 amount should be well controlled during the K2FeO4@PAO preparation process. The aggregation of PAN could be significantly inhibited, and PAO particles with smaller particle sizes and better adsorption capability could be obtained at the composition of 0.20 g K2FeO4 and 2.00 g PAN. This reactant amount was selected in the following experiment.
Fig. 2 SEM images of K2FeO4@PAO with different K2FeO4 and PAO contents (A) and TEM image and EDS mappings of PAO and K2FeO4@PAO (B). The preparation conditions for K2FeO4@PAO are shown in Table 1. |
K2FeO4 (g) | PAN (g) | Name | |
---|---|---|---|
Fixed K2FeO4 series | 0.20 | 0.50 | 0.2:0.5 |
1.00 | 0.2:1 | ||
1.50 | 0.2:1.5 | ||
2.00 | 0.2:2 | ||
Fixed PAN series | 0 | 2.00 | 0:2 |
0.50 | 0.5:2 | ||
1.00 | 1:2 | ||
1.50 | 1.5:2 | ||
2.00 | 2:2 | ||
4.00 | 4:2 | ||
5.00 | 5:2 |
The effect of K2FeO4 on the PAO particle-size distribution was also studied. Dynamic light scattering (DLS) measurements showed that the PAO particle sizes were concentrated around 1600 nm (Fig. 3A). The particle diameter of K2FeO4@PAO was reduced ∼31% at 500 nm (Fig. 3B) compared with PAO. The introduced K2FeO4 could thus inhibit the agglomeration of PAN in water and promote the formation of nano-sized K2FeO4@PAO particles. The smaller K2FeO4@PAO particle size will help the adsorbent application in the target solution. The Tyndall phenomenon was used to further verify the size of the two particles. Here, if the particle is smaller than the wavelength of incident light, light scattering occurs. In this case, a light wave around the particle is observed and radiates around it, which is called scattered light and the Tyndall phenomenon is the scattering phenomenon of light. In terms of the macroscopic performance for the same incident light, if the particles are small, have a larger scattering angle, the scattered light has a weak flood angle, and its brightness is high, then the Tyndall phenomenon is obvious. If the particles are large, have a small scattering angle, the scattered light has a large flood angle, and a low centre brightness, then the Tyndall phenomenon is poor. As shown in Fig. S3,† the light-scattering angle of the particles of K2FeO4@PAO was large, the centre brightness was high, the flooding was small, and the Tyndall phenomenon was obvious. However, PAO had a poor particle size uniformity, and the light tended to be scattered by large particles. The light-scattering angle of the particles was small, the flooding area was large, the centre brightness was low, and the Tyndall path was dark.
Fig. 3 Size distributions (A and B), FT-IR spectra (C), TGA curves (D), and water contact angles (E) of PAO and K2FeO4@PAO. |
FT-IR and TGA were used to analyze the effects of K2FeO4 on the surface functional groups and thermal stability of PAO. As shown in Fig. 3C, The FT-IR spectra of K2FeO4@PAO and PAO were similar. In the K2FeO4@PAO spectrum, the peaks of N–H and O–H were at 3500–3000 cm−1, the peak of –CN was at ∼1668 cm−1, and the characteristic peak of N–O was at ∼932 cm−1, which were all consistent with the PAO infrared spectrum. Fig. 3D shows the TGA curves of PAO and K2FeO4@PAO. The first ∼4% weight losses of PAO and K2FeO4@PAO could be assigned to moisture loss. PAO and K2FeO4@PAO showed good thermal stability at 100–200 °C. The second weight loss at 200–500 °C was related to the cyclization dehydrogenation of PAO. PAO and K2FeO4@PAO then underwent severe oxidative cleavage at 500–700 °C.19
Static contact-angle experiments were used to quantify the surface hydrophilic property of PAO and K2FeO4@PAO. Before the test, each powder material was pressed into a tablet with a tablet press and the pressure of 20 MPa was maintained for 40 s. During the contact-angle measurement, 2 μL ultrapure water was injected for each test. Each sample was tested three times, and every test used a new sample to exclude residual effects. The results of the three tests are shown in Fig. 3E, whereby the average contact angles of PAO and K2FeO4@PAO were 34.8° and 40.3°, respectively. The lower water contact angles of PAO and K2FeO4@PAO indicated they both have good hydrophilicity, which would benefit their application in aqueous solution.
XPS was used to infer the binding states of the atoms and the electron distribution in K2FeO4@PAO and PAO by measuring the chemical shift of electrons in their layers (Fig. 4A). The high resolution of Fe 2p in the K2FeO4@PAO spectrum revealed the characteristic Fe 2p3/2 and Fe 2p1/227–29 of Fe signals located at 711.8 and 724.7 eV, respectively (Fig. S4†). A new peak appeared at ∼390 eV (Fig. S5†) related to XPS U 4f4 after U(VI) adsorption, revealing the high enrichment of U(VI) on PAO and K2FeO4@PAO surfaces. The XPS peaks of O 1s, N 1s, and C 1s were located at ∼532, ∼400, and ∼285 eV, respectively. The C 1s spectra (Table S1† and Fig. 4B) could be divided into five components at 284.6 ± 0.1, 285.3 ± 0.1, 286.4 ± 0.1, 287.4 ± 0.1, and 288.6 ± 0.1 eV corresponding to –CN, C–C, C–OH and –C(NH2)NOH, –CO, and –COO− groups of PAO and K2FeO4@PAO surfaces, respectively.30,31 As indicated in the N 1s spectra (Fig. 4C and Table S2†), the characteristic peaks with binding energies at 398.7 ± 0.1, 399.3 ± 0.1, and 400.5 ± 0.1 eV were attributed to the –CN, N–H, and –C(NH2)NOH bonds, respectively.31,32 The three fitting peaks in the O 1s spectra (Fig. 4D and Table S3†) belonged to –COO− (531.2 ± 0.1 eV), CO (532.3 ± 0.1 eV), and –OH (533.4 ± 0.1 eV), respectively.33,34 The XPS results showed that the chemical environments of PAO and K2FeO4@PAO were similar to each other, revealing that K2FeO4 did not affect PAO's chemical properties.
The adsorption performances of K2FeO4@PAO at different contact times were also studied. U(VI) adsorption on PAO and K2FeO4@PAO rose sharply in the first 2 h, and then increased slowly with further increasing the reaction time (Fig. 5B), reaching equilibrium within 8 h. The adsorption kinetics were analyzed by pseudo-first-order (qt = qe × (1 − exp(−k1t)), where qe and qt (mg g−1) are the adsorbed amounts of U(VI) at equilibrium time and time t (h), respectively, and k1t (1 h−1) is the pseudo-first-order kinetic constant) and pseudo-second-order (qt = qe × t/(1/(K′ × qe) + t), where K′ (g (mg h)−1) is the pseudo-second-order kinetic constant) models.36,37 The relevant these parameters coefficients are generalized in Table S4.† The adsorption process of U(VI) by K2FeO4@PAO and PAO conformed to the pseudo-second-order model and chemisorption was the primary adsorption mode for U(VI) adsorption on K2FeO4@PAO and on PAO. According to the relevant results of the pseudo-second-order model, the maximum adsorption capacities of U(VI) on K2FeO4@PAO and PAO were 26.9 and 10.9 mg g−1 at pH 8.2 and 298 K, respectively.
Given the above excellent U(VI) recovery performance of K2FeO4@PAO, its effect for U(VI) recovery in various environmental solutions was also studied. As shown in Table 2, K2FeO4@PAO could effectively extract most U(VI) from this complex system. Therefore, the real application of K2FeO4@PAO in extraction U(VI) from seawater was performed, and seawater was prepared with sea salt. We found that K2FeO4@PAO could effective uptake ∼57% of 5 mg L−1 U(VI) from seawater. Experimental results further confirmed the high efficiency of K2FeO4@PAO in the extraction of U(VI) from seawater.
Sample | C[U(VI)] (mg L−1) | ||
---|---|---|---|
Initial | Final | Adsorption (%) | |
Diluted U(VI) sloution | 20 | 10.62 | 46.90 |
15 | 7.07 | 52.87 | |
10 | 5.04 | 49.60 | |
5 | 2.85 | 43.00 | |
Running water | 20 | 13.39 | 33.05 |
15 | 8.65 | 42.33 | |
10 | 6.40 | 36.00 | |
5 | 2.87 | 42.60 | |
Seawater | 20 | 14.51 | 27.45 |
15 | 8.78 | 41.47 | |
10 | 5.78 | 42.20 | |
5 | 2.17 | 56.60 |
Adsorption isotherms was used to depict the adsorption capacities of K2FeO4@PAO and PAO at three different temperatures (i.e. 298, 308, and 318 K). As shown in Fig. 5C and D, with increasing the U(VI) initial concentration and temperature, the adsorption capacities of K2FeO4@PAO and PAO for U(VI) increased. Langmuir (Cs = b × Cs,max × Ceq/(1 + b × Ceq), where Ceq is the equilibrium concentration of U(VI) after adsorption, Cs,max (mg g−1) and b (L mg−1) are the maximum adsorption capability of the adsorbent and the Langmuir constant, respectively) and Freundlich (Cs = K × C1/ne, K (mg g−1) and 1/n are the constants indicative of the adsorption capability and intensity, respectively) models were used to fit the experimental data, and the mechanism of the adsorption process is discussed.36,37 According to the R2 values in Table S5,† the Langmuir isotherm model could better describe the experimental data, suggesting there was no interaction between the adsorption sites, and the U(VI) adsorption process on K2FeO4@PAO was a monolayer adsorption. The Cs,max value K2FeO4@PAO for U(VI) at pH 8.2 and 298 K was calculated to be 137 mg g−1.
According to the adsorption results, the adsorption capacity of PAO prepared in water was lower than that reported when prepared in organic reagents.38–40 From the perspective of economic cost and environmental protection, obtaining PAO in water is more conducive to the long-term development of PAN as a material for extracting U(VI) from seawater. More importantly, the PAO's preparation in water has not been reported yet. PAN is widely used in U(VI) recovery, mainly because its surface contains a large number of –CN groups, which can be converted into –C(NH2)NOH by chemical reaction with NH2OH in solution and –C(NH2)NOH can coordinate with U(VI) to recover uranium. However, one cannot ignore that PAN is easy to agglomerate and most –CN is not reacted with NH2OH in water, resulting in PAO having a low adsorption capacity for U(VI). Here, K2FeO4@PAO nanoparticles were obtained after K2FeO4 was introduced into the PAN transformation process. Compared with PAO, the adsorption capacity of K2FeO4@PAO was significantly increased, indicating that PAN reacted more fully with NH2OH and the amount of –C(NH2)NOH on its surface increased.
The relevant thermodynamic parameters,41 standard enthalpy change (ΔH°), standard Gibbs free energy change (ΔG°), and entropy change (ΔS°) of K2FeO4@PAO and PAO for U(VI) adsorption at three different temperatures (i.e. 298, 308, and 318 K) were investigated and are discussed, and the results are shown in Table S6.† The energy released or adsorbed in the chemical reaction process can be expressed by heat, called the heat of reaction, also known as the “enthalpy change” (ΔH°). ΔH° > 0 means that the adsorption of U(VI) on K2FeO4@PAO and PAO surfaces is an endothermic process, which is consistent with the improved U(VI) adsorption at higher reaction temperature. For a chemical reaction, the ΔG° value determines the reaction direction. The negative ΔG° value indicated that the adsorption of U(VI) on K2FeO4@PAO and PAO is a spontaneous process, which also confirmed the strong affinity between –C(NH2)NOH and U(VI).
To evaluate the stability of K2FeO4@PAO, the desorption–regeneration properties of K2FeO4@PAO were studied. Different concentrations and solvents were used to eluate K2FeO4@PAO. First, 0.5 mol L−1 HCl, HNO3, NaOH, and Na2CO3 were selected as eluting agents for the desorption of U(VI) from the K2FeO4@PAO surface. As shown in Fig. S6,† Na2CO3 showed the best resolution rate at 99%. Different concentrations (0.1–1 mol L−1) of Na2CO3 solution were used to eluate the K2FeO4@PAO. The elution results are shown in Fig. 6A, where it can be seen that the elution rate gradually increased with the increase in Na2CO3 concentration. When the Na2CO3 concentration reached 0.5 mol L−1, the solution elution rate could reach almost 100%, so 0.5 mol L−1 Na2CO3 solution could achieve effectively regenerate K2FeO4@PAO. The adsorption capability of the regenerated K2FeO4@PAO for U(VI) is shown in Fig. 6B. The adsorption capacity of K2FeO4@PAO only decreased by 3% after its regeneration and reuse six times.
Based on the complex compositions of seawater, the coexistence of ions in seawater can affect the U(VI) adsorption. With various metal ions coexisting in seawater (such as Na(I), Ba(II), Sr(II), Ni(II), Co(II), Zn(II), Cu(II), Mn(II), Pb(II), and Fe(III)), ICP-MS was used to detect the concentration of each ion and then to evaluate the selectivity of K2FeO4@PAO for U(VI). As depicted in Fig. 6C, the adsorption capacity of K2FeO4@PAO for U(VI) was higher than that of the other ions, indicating that K2FeO4@PAO had excellent selective adsorption capacity for U(VI) in the coexistence ion system. The recovery of U(VI) from anionic solutions was also investigated for K2FeO4@PAO. As shown in Fig. 6D, with the increase in ion concentration, the influence of HCO3− on U(VI) recovery was undeniable due to the formation of new U(VI) species. In natural seawater, the concentration of various anions is far lower than 0.1 mol L−1, which means that anions have little effect on recycling U(VI).42 K2FeO4@PAO was obtained by introducing K2FeO4 into PAN to inhibit PAN agglomeration in water. The overall structure and morphology of the adsorbent were optimized. The particle size of K2FeO4@PAO can reach the nanometre scale, and it can be evenly dispersed in solution, so that the adsorbent can better contact with U(VI) and promote the occurrence of chemical reactions. The introduced K2FeO4 did not damage the stability and selectivity of PAO. As we expected, the adsorption capability of K2FeO4@PAO was much higher than PAO in various U(VI) solutions. In K2FeO4@PAO, PAO ensures the excellent selectivity of K2FeO4@PAO for U(VI), and the nanoscale particle size enables K2FeO4@PAO to fully react with U(VI) in solution, ultimately ensuring that K2FeO4@PAO has better adsorption effect on U(VI) than other ions in complex systems. Furthermore, K2FeO4@PAO also showed good cycling and selectivity for U(VI). In summary, K2FeO4@PAO can not only reduce the cost of the PAO preparation process and make the process greener, but can also further optimize the surface structure of the PAO and improve its adsorption properties in a variety of environments.
Fig. 7 Adsorption of U(VI) by PAO (A) and K2FeO4@PAO (B) in solutions of different concentrations. m = 0.02 g, V = 50 mL, I = 0.1 mol L−1 NaCl. T = 298 ± 1 K, pH = 8.2 ± 0.1, contact time: 24 h; bactericidal rates against E. coli and V. alginolyticus of different particles (C). The K2FeO4@PAO materials were named according to the used amounts of K2FeO4 and PAN (Table 1). |
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Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d3lp00060e |
This journal is © The Royal Society of Chemistry 2023 |