Chengwei Gaoa,
Baojun Lia,
Ning Chena,
Jie Ding*a,
Qiang Caib,
Jianmin Zhanga and
Yushan Liu*a
aCollege of Chemistry and Molecular Engineering, Zhengzhou University, 100 Science Road, Zhengzhou 450001, P. R. China. E-mail: liuyushan@zzu.edu.cn; jieding@zzu.edu.cn
bKey Laboratory for Advanced Materials of Ministry of Education, College of Materials Science and Engineering, Tsinghua University, Beijing 100084, P. R. China
First published on 26th April 2016
In this study, a novel series of ternary composites of halloysite nanotubes (HNT), Fe3O4 nanoparticles (NP), and graphene oxide (GO) was prepared via a facile co-precipitation process. After the simple heat treatment process, the Fe3O4/HNT@GO composite was converted to the Fe3O4/HNT@rGO composite (FHGC), which was investigated as a potential adsorbent for the removal of contaminants from water. This series of designed ternary systems FHGC-n (n = 1, 2, 3) was identified by SEM, TEM, HRTEM, FT-IR, powder XRD, Raman and X-ray photoelectron spectroscopy (XPS) analyses. As anticipated, for both the simulated organic contaminant species (RhB) and the inorganic contaminant species (As(V) ions) in water, the multifunctional FHGC exhibited good adsorption performance and easy separation. In each case of the FHGC series, the adsorption process for As(V) ions was less than 30 min, which is close to the best example in literature.
Herein, we report that one compelling choice for obtaining suitable dispersion properties in aqueous system is to construct organic–inorganic hybridized graphene-based composites.17 Currently, inorganic Fe3O4 nanoparticles (NP) are promising candidates because of several unique advantages, such as low cost, environmental friendliness and fine recyclability.10 Apart from being a material with good affinity for inorganic ions, Fe3O4 NP has also been explored for waste water treatment, such as the removal of As(V). In the recent literature, examples of graphene-based composites incorporated with Fe3O4 NP show favorable adsorption behaviors toward organic dyes and inorganic ions. In these cases, the presence of Fe3O4 NP hinders the re-stacking of graphene layers to modulate the dispersion properties of composites in aqueous systems, as well as the available area of graphene sheets.18 On the other hand, the graphene sheet as the substrate material modifies the Fe3O4 NP aggregation resulting from its magnetic nature. In comparison to the relatively tiny Fe3O4 NP, the size of natural clay halloysite nanotubes (HNT) is on the meso/macroscopic level, and they present negatively charged outer surfaces, and positively charged inner surfaces.19,20 After surface modification, the HNT@graphene composite is rendered a relatively large specific surface area and big pore volume to improve the total adsorption capacity,9 and incorporating HNT species into the Fe3O4@graphene binary system may produce larger tunnels to enhance the adsorption rate.22–24 It is also most likely beneficial for suppressing the aggregation of Fe3O4 NP. Hence, the ternary composite of graphene, HNT and Fe3O4 NP obtained by rational design can be an excellent candidate for the multifunctional adsorbent material for surface water and groundwater treatment. Such ternary systems may solve the problem of several pollutants coexisting in aqueous solution, and simplify the practical application process to reduce the costs.
Depth consideration is necessary before designing a facile hybridization process for these three species.25,26 Firstly, the GO sheet with the negatively charged outer surface27 and the nearly neutral rGO sheet,28 would hardly form a composite with HNT without suitable surface modification, because HNT also displays a negatively charged outer surface.29 Secondly, because of the magnetic feature of Fe3O4 NP, it easily aggregates and is dispersed with difficulty under mechanical mixing conditions.30 In our previous work, both HNT@rGO9 and Fe3O4@rGO10 binary composites were prepared by a convenient method triggered by the electrostatic self-assembly process, and displayed favorable adsorption performance in aqueous systems.
Herein, we develop a more convenient co-precipitation procedure to obtain a series of new Fe3O4/HNT@rGO composite materials (FHGC-1, FHGC-2 and FHGC-3) without any surface modification. In this work, iron ions can be easily adsorbed onto GO and HNT to form nucleation centers because of the electrostatic interaction. Furthermore, Fe3O4 NP generated on the surface of both GO and HNT will eliminate the electrostatic repulsive forces between the two negatively charged components. In the case of FHGC-n (n = 1, 2, 3), the experiments for the removal of the organic dye rhodamine B (RhB) and the inorganic arsenic(V) ion were respectively investigated in aqueous systems. As we expected, because of the excellent adsorption behaviors and the simple operations of separation and recycling, multifunctional FHGC-n (n = 1, 2, 3) displayed good application prospects in wastewater treatment. In particular, FHGC-2 showed better adsorption performance toward simulated organic contaminant species than FHGC-1 or FHGC-3, while for the inorganic arsenic(V) ion removal, FHGC-1 was best.
qe = V(C0 − Ce)/m | (1) |
Ce/qe = 1/qmKL + Ce/qm | (2) |
log![]() ![]() ![]() | (3) |
In this study, the microstructure of FHGC-n (n = 1, 2, or 3) was determined by SEM, TEM and HRTEM analyses (Fig. 1). SEM results show that the Fe3O4 NP and the tubular HNT are distinctly dispersed on the rGO sheet (Fig. 1a–c). Further detailed evidence for the formation of the ternary composite was traced by TEM (Fig. 1d–g and S1†) and HRTEM (Fig. 1h) analyses. Although the morphologies of these three FHGC samples are very similar, the amount of Fe3O4 NP is visibly different in the three samples (Fig. 1d–g). The HNT and Fe3O4 NP are loaded onto the surface or intercalated between the rGO sheets; independent Fe3O4 NP and HNT are absent in these images of FHGC-n (n = 1, 2, or 3) composites. The morphology of the HNT is consistent with that of raw HNT (Fig. S1i†), while the morphology of Fe3O4 NP produced by using the facile co-precipitation process is irregular spheres with diameters of about several to 20 nm. Additionally, it is obvious that the dispersion of Fe3O4 NP onto graphene sheet is not quite homogenous. This may have originated from the distribution of the oxygen groups on the GO sheets, which could act as the nucleation centers to capture the Fe3+. On the other hand, the tendency of Fe3O4 NP toward aggregation is driven by their magnetic nature, which may also result in the non-homogeneous distribution of Fe3O4 NP on the graphene sheets. Moreover, in Fig. 1g, the distinctly resolved lattice (around 0.295 nm corresponding to the (220) plane of Fe3O4,35) and fine diffraction spots (inset, Fig. 1h),36 suggest that the irregular spherical-Fe3O4 NP were highly ordered crystals.
![]() | ||
Fig. 1 SEM images of (a) FHGC-1; (b) FHGC-2; (c) FHGC-3. TEM images of (d) FHGC-1; (e) FHGC-2; (f) FHGC-3; (g) Fe3O4 on HNT, the inset is the corresponding SAED pattern. (h) HRTEM image of Fe3O4. |
In this study, the FT-IR spectra of samples FHGC-n (n = 1, 2, 3) are very similar (Fig. S2a† and 2a); thus, only FHGC-2 is discussed in detail. As shown in Fig. 2a, the presence of rGO, Fe3O4 NP and HNT is undoubtedly demonstrated, as well as their combination in the FHGC. In comparison with the spectra of GO and rGO, the typical stretching vibrations of carboxyl groups (1715 cm−1) or epoxide groups (1090 cm−1) were absent in the FHGC-2 spectrum, suggesting the total conversion from GO to rGO.9,10 The peaks at 1571 cm−1 (CC) and 1086 cm−1 (C–O) in the spectrum of FHGC-2 were assigned to the stretching vibrations of rGO,37 while the typical peaks of HNT were present at 1640, 1040, 750 and 550 cm−1.10,20 The peaks at 567 and 416 cm−1 correspond to the Fe2+–O2− and Fe3+–O2− in the FHGC-2 spectrum, which also confirmed the presence of Fe3O4.9,21,31
The phase structure of FHGC-2 is described in detail and shown in Fig. 2b (the XRD patterns of FHGC-1 and FHGC-3 are shown in Fig. S2b†). As expected, the disappearance of the GO peak at 9.7° and the presentation of two broad rGO peaks centered at 24.3 and 43.6° indicate the complete reduction of GO to rGO,38 while the peaks at 24.8° and 35.0° originate from HNT.10,20 The positions and relative intensities of the diffraction peaks match well with the standard Fe3O4 (JPPDS no. 19-0629, 30.1° (220), 35.4° (311), 43.0° (400), 57.2° (511), and 62.6° (440)).39 As shown in Fig. 2c and S3,† the D (1340 cm−1) band of the disordered carbons and the G (1580 cm−1) band of the sp2 hybridized carbon are present in the Raman spectra of FHGC-n (n = 1, 2, or 3), and are very close to those in the spectra of GO and rGO.40 In addition, the increased D band intensity of the FHGC-n (n = 1, 2, 3) results from the apparent structural interactions of the ternary system (Fe3O4 NP, HNT and rGO sheet).41,42
Importantly, XPS analysis is a quite useful tool for identifying the details of elemental composition in material science. Herein, the XPS spectra of FHGC-n (n = 1, 2, or 3; Fig. 2d and S4†) distinctly show the carbon (C 1s), oxygen (O 1s), iron (Fe 2p), silicon (Si 2p), and aluminum (Al 2p). The observation of Si 2p (75.42 eV) and Al 2p (103.42 eV) is evidence for proving the existence of HNT in the ternary system FHGC.10,43 As shown in Fig. 2e, S4b and e,† Fe 2p3/2 (711.27 eV) and Fe 2p1/2 (724.92 eV) are also visible in the high resolution Fe 2p scan. It is clear that the fitting peaks broaden with higher binding energy in Fe3O4 as a result of the existence of Fe2+ (2p3/2) and Fe2+ (2p1/2).9,21 Moreover, the O 1s peak is observed at 531.42 eV, belonging to the lattice oxygen of Fe3O4, while the weak shoulder peak at 710 eV also confirms the presence of Fe3O4.9,21 In addition, Fig. 2f, S4c and f† show that the typical C 1s peak occurs at 284.6 eV, while the peak located at 286.02 eV is commonly attributed to surface-adsorbed hydrocarbons and their oxidative forms (–COOH, epoxide). In the C 1s spectrum of FHGC-n (n = 1, 2, or 3), the peak centered at 288.72 eV originates from the carbon element in association with oxygen in the carbonate ions.9,21,44 The remaining smaller peaks at higher binding energies (785.6, 788.2, 802.1, and 805.2 eV) are satellite shake-ups of the assigned components.45
As we know, Fe3O4 NP are paramagnetic. In the control experiments, it is clear that each of the samples FHGC-n (n = 1, 2, and 3) designed is easily removed by one small magnet and can be re-dispersed into aqueous solution without aggregation. Hence, M–H measurements were performed to further prove the paramagnetic behavior of FHGC-n (n = 1, 2, or 3) at room temperature. In each magnetization curve of FHGC-n (n = 1, 2, or 3; Fig. S5a†), the magnetic saturation value is lower than that of pure Fe3O4 NP (FHGC-1: 17.07 emu g−1, FHGC-2: 14.07 emu g−1, and FHGC-3: 6.88 emu g−1).46 These results may be caused by the relatively low content of Fe3O4 NP in FHGC-n (n = 1, 2, or 3), where the existence of non-magnetic rGO and HNT decreases the density of the magnetic component. The Hc (Fig. S5b†) indicates that the FHGC-n (n = 1, 2, or 3) is a kind of soft magnetic material. FHGC-n (n = 1, 2 and 3) samples were selected to investigate the microstructure of the ternary system by the N2 adsorption–desorption test. As shown in Fig. S6a,† the FHGC-n samples are mesoporous, showing the specific surface areas of 107.3 (FHGC-1), 152.4 (FHGC-2), and 103.8 m2 g−1 (FHGC-3), with the most probable pore widths of 5.7, 4.2, and 6.0 nm, respectively (Fig. S6b†); the total pore volumes of FHGC-n are 0.240, 0.282, and 0.289 cm3 g−1, respectively, for pore widths ranging from 1.7 to 300 nm.
According to the reported graphene-based composite,9,10 both HNT and intercalated Fe3O4 NP prevented the rGO from restacking during the heat reduction process to effectively maintain the large surface areas and pore volumes. In addition, both rGO and HNT are good candidates for adsorbing organic material, and the separation process is definitely facile, as a result of the presence of magnetic Fe3O4 NP in the FHGC-n (n = 1, 2, or 3) ternary system. In this paper, the typical organic dye RhB was selected for the study of the absorption properties in water.
Absorption was monitored using the UV-Vis absorption spectrometer. The typically strong absorption band of RhB was immediately decreased when FHGC-n (n = 1, 2, or 3) was added into the test solution (Fig. 3a and S7a†). For the samples FHGC-n (n = 1, 2, and 3), more than 70% RhB in water disappeared after 3 min, and then the adsorption process gradually slowed down (Fig. S7c and d†). These results show that the concentration of remaining RhB is substantially unchanged after 15 min (C0 = 1.0 × 10−5 M is the initial concentration of RhB; C represents the concentration of RhB at a given moment), indicating the adsorption rate is relatively fast, compared to that in recent literature.9,10,47 Because of the magnetic Fe3O4 NP in this ternary system, FHGC is easily separated by using a small magnet (Fig. S7b†), which is very important to avoid secondary pollution in the waste water treatment. Interestingly, FHGC-2 exhibits the highest adsorption rate and lowest residual concentration of RhB.
Moreover, the maximum adsorption amount of FHGC-2 (19.39 mg g−1) is higher than that of FHGC-1 (15.22 mg g−1) and FHGC-3 (16.56 mg g−1). As shown in Fig. 3b, each adsorption curve of the three FHGC cases is well fitted by the first-order reaction rate kinetic model, which is similar to the binary system FGNC or HGC that we reported previously.9,10 Control experiments with Fe3O4 NP, HNT, GO, and rGO as adsorbents were carried out to determine the advantages of the FGNC ternary system (Fig. 3c). In comparison to the performances of GO and rGO, HNT showed bad adsorption behavior for RhB, while RhB in water was scarcely adsorbed by the pure Fe3O4 NP. It is evident that the significant adsorption ability exhibited by the FHGC-n ternary system mainly resulted from the physical adsorption onto the rGO surface.
Normally, the ratio of rGO in the sample is the key factor for the maximum adsorption amount (Amax). In this work, although the weight content of rGO calculated is gradually increased (FHGC-1: 20%, FHGC-2: 25%, and FHGC-3: 32%), the presentation of FHGC-2 is the most dazzling of the FHGC samples. We found that FHGC-2 was well dispersed in water under ultrasonic conditions in 30 min, while the other two samples were still slurries and precipitated easily under the same conditions; this may be the reason for the special behavior in the case of FHGC-2. To further investigate the capability of FHGC-n ternary systems, the absorption experiment was repeated for FHGC-2 under the same conditions. After the first 20 min (Fig. 3d), FHGC-2 was separated from the system by the magnet and directly reimmersed into a new RhB aqueous solution (20 mL, 1.0 × 10−5 M); the second line is almost the same as the first one, illustrating a similar absorption, still efficiently executed. It is noteworthy that the adsorption rate was retained with increased separation–absorption cycles, even in the 9th cycle.
Notoriously, arsenic is one of the top 20 hazardous substances in the world, especially the inorganic arsenic species, which are more dangerous than the organic forms. Arsenate (As(V)) is easily enriched in the surface water to aggravate the pollution of drinking water48 and consequently, it has attracted worldwide attention to develop facile and cheap techniques for the remediation of arsenic contamination. In a recent study by our group, the Fe3O4@rGO dyad composite (FGNC) prepared by the colloid electrostatic self-assembly method indicated favorable behavior in the removal of the simulated inorganic contaminant As(V) (Na3AsO4, Freundlich parameter n = 3.40).9 Herein, Na3AsO4 aqueous solution was again selected as the simulated As(V) water pollutant for the adsorption experiment of FHGC-n (n = 1, 2, or 3) samples. The adsorption results under neutral conditions are displayed (Fig. 4, S8 and Table S2,† pH ≈ 7). As illustrated in Fig. 4a, the equilibrium adsorption capacity (qe, mg g−1) increased visibly with increasing original concentration of As(V). For the FHGC-n (n = 1, 2 and 3) samples, both the Langmuir and Freundlich isotherm models were applied to analyze the adsorption equilibrium data of simulated inorganic contaminant As(V). Interestingly, sample FHGC-1, with the highest content of Fe3O4 NP (Fig. 4b and S8†), has a similar fine value of R2 in the Langmuir and Freundlich models, and the adsorption process on a homogeneous surface is possibly either a monolayer adsorption or a multilayer adsorption. In contrast, in sample FHGC-2 and FHGC-3, the monolayer adsorption process is only reasonable (Fig. 4b).
As we know, under neutral environmental conditions the major form of As(V) is the anionic species (including H2AsO4− and HAsO42−); therefore, there is a relatively strong electrostatic repulsive interaction between the adsorbed As(V) species and unabsorbed As(V) species in solution. When the content of Fe3O4 NP is comparatively low in the sample composite, such electrostatic repulsion is the key effect promoting a dominant monolayer adsorption. In contrast, when the electrostatic repulsive effect is weakened by the increased content of Fe3O4 NP in the sample composite, there is competition between the monolayer adsorption process and the multilayer adsorption process. Furthermore, in the case of FHGC-1, the maximum adsorption capacity (qm, Table S2†) of 4.42 mg g−1 was calculated using the Langmuir model, while the Freundlich parameter (n, Table S2†) value of 7.06 indicated that the designed FHGC-1 is a potentially fair arsenate adsorbent. Normally, when the content of Fe3O4 is decreased in the sample composite, FHGC-2 or FHGC-3 shows the lowest qm value (Table S2†). This result is still remarkably higher than that of commercial Fe3O4 (1.35 mg g−1),49 which therefore implies that because of the strong affinities of the FHGC series developed in our work for arsenate, especially sample FHGC-1, they might serve as efficient adsorbents for the removal of arsenic ions in water treatment.49,50 In order to detect the stability of FHGC-n (n = 1, 2, or 3) in the adsorption process, the concentrations of Fe, Al, and Si in simulated As(V) polluted water were also investigated by ICP MS. As shown in Fig. S9,† it is clear that the concentrations of such ions were almost unchanged during the adsorption process, indicating that no secondary pollution is produced by FHGC-n (n = 1, 2, or 3) adsorbent.
Additionally, the adsorption data for arsenate ions by the FHGC series is illustrated in the pattern of Fig. 4c at different time intervals, which indicates the importance of adsorption kinetics. As shown in Fig. 4c, in each of the FHGC series, the adsorption process of As(V) is rapid at first, which is ascribed to the process of arsenic adsorption on the exterior surface of the Fe3O4 particles without any repulsion. When the diffusion resistance and the electrostatic repulsive interactions gradually played their roles, the adsorption process slowed down and at last reached equilibrium. In each case of the FHGC series, equilibrium was obtained in less than 30 min, which is almost the best example in literature.9,48,50–53 As shown in Fig. 4d, the above adsorption kinetic experimental data were best fitted by the pseudo-second-order rate kinetic model in each of the three FHGC cases, which is presented as follows:
t/qt = 1/(k2qe2) + 1/qt |
V0 = k2qe2 |
Footnote |
† Electronic supplementary information (ESI) available: Synthesis of graphene oxide, TEM images, FTIR and XRD results, VSM isotherms, nitrogen adsorption desorption isotherms, and tables. See DOI: 10.1039/c6ra01279e |
This journal is © The Royal Society of Chemistry 2016 |