Sundaram Chandrasekarana,
Seung Hyun Hur*a,
Eui Jung Kima,
Balasubramaniyan Rajagopalana,
Kadumudi Firoz Babua,
Velusamy Senthilkumarb,
Jin Suk Chunga,
Won Mook Choia and
Yong Soo Kimb
aSchool of Chemical Engineering, University of Ulsan, Daehak-ro, 102, Nam-gu, Ulsan 680-749, South Korea. E-mail: shhur@ulsan.ac.kr; Fax: +82 52 259 1689; Tel: +82 52 259 1028
bDepartment of Physics and Energy Harvest-Storage Research Center, University of Ulsan, Ulsan 680-749, South Korea
First published on 19th March 2015
Highly ordered γ-Fe2O3/reduced graphene oxide (RGO) was synthesized via a facile solution technique combined with calcination at various temperatures. The maghemite iron oxide structure was obtained on the GO surface and improved crystallinity of γ-Fe2O3 was observed as the calcination temperature increased. The prepared highly ordered maghemite structure on RGO exhibited an excellent water splitting performance under UV light (∼360 nm) illumination. The photocurrent density of RGO/γ-Fe2O3 calcined at 500 °C was 6.74 mA cm−2 vs. RHE and a high incident photon to current conversion efficiency (IPCE) of 4.7%, was achieved. This photocurrent density and the IPCE values are 3.7 times and 4 times higher than that of pristine iron oxide, respectively.
(1) |
The rate of water splitting by photoelectrochemical cell (PEC) can be increased significantly when artificial UV light sources are used.5
Recently, various metal oxides (such as TiO2, ZnO, WO3, and CoO) and graphene based metal oxide composites have been investigated for PEC water splitting.6–12 Among them, iron oxides (Fe3O4, α-Fe2O3 and γ-Fe2O3 etc.) have received much attention due to their favourable optical band gap, excellent chemical stability, natural abundance, and low material cost.13–16 The maximum theoretical efficiency of solar-to-hydrogen (STH) conversion is 16.8% so far, however, the reported value of STH for iron oxide is much lower than the expected value due to its very short lifetime of photo generated charge carriers (<10 ps) and short hole diffusion length (∼2–4 nm).17
Lately, graphene and graphene based hybrid materials have drawn great attention due to their unique microstructures and properties, which promote their extensive potential application in many fields.18,19 Moreover, the properties of graphene oxide (GO) and mildly reduced graphene oxide (RGO) prepared by the chemical method can be easily tailored compared with the graphene grown by the chemical vapour deposition (CVD) due to the formation of various functional groups such as the hydroxyl, carbonyl, and carboxyl groups on the graphene surface, which enables GO and RGO more easily modified by other materials.20–24 Therefore, semiconductor nanoparticles assembled on the surface of GO are believed to provide a new way to design high-performance energy harvesting electrode materials. Even though iron oxide/graphene composites have been extensively studied for use as an anode material for Li-ion batteries,25 super capacitors,26,27 sensors28 and catalysts,29,30 to the best of our knowledge, no PEC study of RGO/γ-Fe2O3 has been reported in the literature so far. There are few reports available on the electrochemical behaviour of RGO-maghemite (γ-Fe2O3) nanocomposites,25,31,32 while many literatures are available for magnetite and hematite based composites.13–16 Moreover, due to a lack of studies on maghemite/graphene composites, the actual nature of iron oxide is still unrevealed and most of the previous reports on iron oxide/graphene composites have assumed that iron oxide has magnetite phase.
Although nano-sized iron oxide and iron oxide composites made by atmospheric pressure chemical vapor deposition (APCVD)15,33 and atomic layer deposition (ALD)34 have shown excellent PEC performance, these techniques require special instruments such as atomizers or CVD or ALD. Moreover, ALD systems need toxic and flammable metal–organic precursors. In this paper, we report highly efficient photocatalytic materials that exhibit high energy conversion efficiency and excellent operational stability. We fabricated crumpled RGO/iron oxide (maghemite) nanocomposites by a facile solution technique. In addition, the structure of iron oxide anchored on GO was accurately identified in this work. After calcination at 300, 400 and 500 °C for 4 h (for sample identification the as-prepared, 300, 400 and 500 °C calcined samples are denoted as RGO-M1, RGO-M2, RGO-M3 and RGO-M4, respectively), the PEC performances were highly improved. The overall water splitting photocurrent density of 6.74 mA cm−2 with high incident photon to current conversion efficiency (IPCE) of 4.7% was achieved for the RGO-M4 (under UV light ∼360 nm), which is the highest IPCE for RGO based iron oxide photocatalysts under UV light.
To synthesize RGO/γ-Fe2O3 nanocomposites, 20 mg of GO was first dispersed in deionized water (40 mL) with vigorous stirring at 70 °C to obtain a homogeneous dispersion. Then, the GO solution was added to 0.5 mol L−1 of iron(III) chloride aqueous solution (80 mL) and the mixture was stirred for 1 h. An ammonia–ethanol solution with a 1:1 (v/v) ratio (4 mL) was added to the above solution. Finally, RGO/γ-Fe2O3 precipitates were collected, washed with distilled water, and dried at 70 °C for 15 h. Then, the dried sample was further calcined at 300 °C, 400 °C and 500 °C for 4 h. Pure iron oxide was prepared by the same procedure without RGO.
ERHE = EAg/AgCl + 0.241 V + 0.0591 × pH at 25 °C |
The PEC water splitting performance of the photoanodes was evaluated using 1.0 M NaOH buffer solution (pH = 13.6) in a three electrode chemical cell under 360 nm UV light illumination.
The presence of iron nanoparticles reduces the aggregation of graphene sheets, which results in less stacking of GO sheets. As a result, a weak GO related peak was observed in the XRD patterns. Maghemite (γ-Fe2O3) and magnetite (Fe3O4), two main forms of iron oxide, have cubic inverse spinel structure and they are very similar in structure to each other. The distinct feature of maghemite is the presence of iron vacancies in the sub lattice. The cation or vacancy distribution in octahedral positions can give rise to several crystal symmetries in maghemite with the corresponding differences in the XRD patterns (Fig. 1b). Usually, disordered maghemite particles belong to the space group Fd3m.25 The spinel structure of γ-Fe2O3 contains cation vacancies that can be ordered (tetragonal superstructure), partially ordered (cubic superstructure), or completely disordered with a high probability of the aggregated vacancies.35 The precise nature of the ordering in γ-Fe2O3 particles with GO is still unclear.35,36 The observed and standard d-values for the iron oxide in the RGO/γ-Fe2O3 nanocomposites fabricated in this study agree well with JCPDS card no. 39-1346, confirming the cubic symmetry of maghemite (γ-Fe2O3), i.e. Fe3+ in octahedral sites and O in close-packed cubic arrangement (the maghemite structure was further confirmed by SAED patterns, which will be discussed in TEM analysis). It is well known that during the heat treatment of GO/γ-Fe2O3 iron atoms can interact with the oxygen related functional groups of GO and form Fe–O–C bonds, which results in the formation of maghemite structure of iron oxide on the GO sheets. Further, the functional groups on the surface of GO disappear when GO is thermally reduced and more π electrons on C atoms are regenerated by the restoration of sp2 networks. Thus, the unpaired π electrons are attracted to free Fe atoms, which results in the preferred growth of γ-Fe2O3 on the surface of RGO. From the Debye–Scherer formulae,31 the broad diffraction peaks are indicative of small-sized iron oxide nanoparticles (20–24 nm) in the RGO/γ-Fe2O3 nanocomposites. The functional groups of the crumpled RGO/γ-Fe2O3 were identified from FTIR spectra in Fig. 2a. Absorption peaks at 586.94, 632.06, and 793.60 cm−1 can be ascribed to the maghemite structure of iron oxide.37 The peak around ∼586 cm−1 is attributed to Fe–O bonds, and the enhanced intensity of Fe–O peak is due to iron oxide loaded to RGO.38 Serna et al.39 reported that a less-ordered maghemite (γ-Fe2O3) structure is evidenced by multiple lattice absorption bands within 800 cm−1. The broad peaks at around 800 and 580 cm−1 is the characteristic of well-ordered γ-Fe2O3.35 No peaks appeared at 3438 and 3150 cm−1, which strongly implies that α-FeOOH is absent in the prepared iron oxides. The peaks at 1638.39 cm−1 and 2357 cm−1 were due to the OH bending of water and the presence of atmospheric CO2, respectively. The stretching vibrations of epoxy C–O (1226.92 cm−1), weak aromatic CC (1578 cm−1), and carboxyl O–CO (1386.11 cm−1) bonds were observed in RGO/iron oxide samples, which can be ascribed to the functional groups of GO and RGO.40 As the calcination temperature increased, some functional groups present in the RGO-M1 disappeared due to the thermal reduction of functional groups in GO.
Fig. 2b represents the Raman spectra of RGO/γ-Fe2O3 nanocomposites. The spectral values are in good agreement with the standard Raman spectrum of maghemite.41,42
For maghemite structure,43 the net structure is spinel symmetry with randomly distributed vacancies in its structure. The projected vibrational modes of the first Brillouin zone center of a spinel structure is given as,
Γvib = A1g + E1g + T1g + 3T2g + 2A2u + 2Eu + 4T1u + 2T2u |
In the above equation, excluding T1g, A2u, Eu, T1u and T2u modes (Raman inactive modes), all modes of vibrations are easily observable for maghemite spinel structure in the Raman spectra. The enduring symmetrical modes like A1g, Eg, and T2g are Raman active modes. As shown in Fig. 2b, three active modes were observed for maghemite phase, i.e. ∼263 cm−1 (Eg: Fe–O symmetric bending), ∼345 cm−1 (Eg: Fe–O symmetric stretching), ∼395 cm−1 (T2g: Fe–O asymmetric bending) and ∼665 cm−1 (A1g: symmetric stretching). The active modes of the Raman signal varies with materials preparation conditions and the vacancies in the maghemite crystal unit cell.37 The weak Raman signal is the result of poor scattering properties of maghemite.42 Compared with other samples, the RGO-M4 samples exhibited a red-shifted peak frequency for the main A1g peak, indicating a greater degree of maghemite crystallinity. The RGO in the RGO/γ-Fe2O3 nanocomposites are more amorphous than GO and the broadened and shifted band is due to the destruction of conjugated system in graphite. Compared with other samples, a smaller ID/IG ratio for the RGO-M4 (1.02) implies a larger sp2 domain size at higher calcination temperature.31 The optical band gap of pristine iron oxide (∼2.13 eV) and RGO/γ-Fe2O3 nanocomposites was evaluated from the UV-vis absorption spectra using Tauc relation ((αhν)1/2 vs. the photon energy where α is the absorption coefficient) as shown in Fig. 2c and S1.† Similar to previous results acquired for RGO–metal oxide nanocomposites, the RGO/γ-Fe2O3 composites exhibited a narrower band gap after the modification of γ-Fe2O3 with RGO and subsequent calcination. This phenomenon can be attributed to the formation of metal–O–C chemical bonds in the RGO/γ-Fe2O3 composites.44,45
Fig. 3(a–c) represents the FE-SEM and TEM images of the pure iron oxide sample. It clearly shows that the sample consists of agglomerated spherical particles of diameter ranging from 15 to 25 nm. Fig. 3d displays the electron diffraction (SAED) pattern indexed with the cubic symmetry of the magnetite phase, which is in good agreement with JCPDS file (no. 89-0951) and the above XRD results. Fig. 4 illustrates the TEM images and SAED patterns of RGO/γ-Fe2O3 nanocomposites. As shown in Fig. 4, large amounts of iron oxide nanoparticles are uniformly decorated on RGO46 and the intensity of SAED pattern evidently displays the graphene (002 plane reflection). It should be noted that the increased crystallinity of γ-Fe2O3 compared with pure iron oxide denotes that GO affects the formation of maghemite crystalline structure.
Fig. 3 (a) FE-SEM, (b and c) TEM images at various scales and (d) SAED pattern of pristine iron oxide. |
Fig. 4 TEM images and SAED patterns of (a and b) RGO-M1, (c and d) RGO-M2, (e and f) RGO-M3 and (g and h) RGO-M4 samples. |
The electronic state and the chemical composition of the samples were investigated by XPS. The XPS survey spectra in Fig. S2† reveal the presence of Fe, C and O in the RGO/γ-Fe2O3. As shown in Fig. 5, several XPS peaks appeared for iron oxide. In the observed XPS spectra, the major peaks at ∼711.7 eV and ∼725.1 eV associated with Fe 2p3/2 and Fe 2p1/2 core-level binding energies of γ-Fe2O3 on RGO.25 The nature of the γ-Fe2O3 was clearly revealed by simulating the observed spectra. It shows that, ∼710.7 eV, 713.2 eV and 718.7 eV (satellite peak) is ascribed to Fe 2p3/2 state. The presence of satellite peak at ∼718.7 eV is characteristic for maghemite.47 The peaks at 725.1 eV and 732.7 eV well documented to Fe 2p1/2 state of iron oxide.26 The Fe0 (709 eV) peak was not observed and only Fe2+ and Fe3+ states were detected in the XPS spectra as the γ-Fe2O3 nanoparticles were oxidized. The O 1s core level XPS spectra of as prepared sample showed two peaks at 529.96 and 531.84 eV, corresponding to Fe–O and Fe–O–C bond formations, respectively. Further calcination, the binding energy values were found to be shifted slightly in positive are due to the formation of coordinated oxygen in the composites (Fig. S3 and Table S1†).48,49 The XPS data strongly support the XRD, FTIR and Raman results and confirm the high order of γ-Fe2O3 on the surface of GO in all prepared nanocomposites.
The linear sweep voltagrams of pure iron oxide, as-prepared and calcined samples are shown in Fig. 6a. In the absence of UV light illumination, no oxidation photocurrent was obtained, indicating that all the electrodes are inactive toward OER in the dark condition. When the UV light was illuminated, all the electrodes exhibited a considerable oxidation photocurrent. The maximum photocurrent density was 1.83, 3.04, 3.39, 4.65 and 6.74 mA cm−2 for pristine iron oxide, RGO-M1, RGO-M2, RGO-M3 and RGO-M4, respectively. This result indicates that photocatalytic performance of iron oxide can be significantly improved by its hybridization with GO and calcination process. As described in Fig. 6b, the RGO serves as an electron sink to facilitate the exciton separation and store the separated electron.47 The saturated photocurrent density of the RGO-M4 was ca. 6.74 mA cm−2, which is 3.7 times higher than that of the pristine iron oxide and 2.3 times higher than that of the RGO-M1. An increase in photocurrent with calcination temperature is believed to be the result of reduced defect density (i.e. highly ordered γ-Fe2O3) in RGO/γ-Fe2O3 samples.
Fig. 6 (a) Linear sweep voltamograms of pristine iron oxide and RGO/γ-Fe2O3 samples at a scan rate of 20 mV s−1 in 1.0 M NaOH electrolyte. (b) Schematic diagram of water splitting by RGO/γ-Fe2O. |
The photoconversion efficiency of the sample was calculated using the following equation:
η = I(1.23 − V)/Jlight | (2) |
To obtain a relationship between photo activity and light absorption of RGO/γ-Fe2O3, we have quantitatively investigated the photo activity of RGO/γ-Fe2O3 as a function of wavelength of incident light. In comparison to the photocurrent density, the photocurrent density, the photocurrent as a function of the wavelength and incident photon to current conversion efficiency (IPCE) is a more appropriate parameter to characterize the photoconversion efficiency of different photo anodes as it is independent of the light sources. IPCE can be calculated by the following equation:
IPCE(λ) = 1240J(λ)/λEλ(λ) | (3) |
Photocatalyst | Method | IPCE (%) value at 360 nm | Ref. |
---|---|---|---|
α-Fe2O3 | AACVD | 0.2 | 15 |
α-Fe2O3 | Deposition annealing | 3.2 | 50 |
Pt–α-Fe2O3 | Electro deposition | 4.0 | 52 |
n-Fe2O3 | Spray pyrolysis | 1.8 | 53 |
α-Fe2O3/graphene | Spray pyrolysis | 3.5 | 57 |
α-Fe2O3/CNT | Spray pyrolysis | 4.2 | 57 |
Fe3O4 | Solution method | 1.2 | Present work |
RGO-M4 (RGO/γ-Fe2O3 (500 °C calcined)) | Solution method | 4.7 | Present work |
The photo-induced electrons are spontaneously injected from the conduction band of iron oxide into that of graphene. Further, the applied positive potential that provides a driving force for the electrons to transfer to the RGO could increase the charge separation and suppress the charge recombination, which leaves long-lived holes in the γ-Fe2O3 to oxidize water increasing the photocatalytic water splitting rate.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c5ra02934a |
This journal is © The Royal Society of Chemistry 2015 |