Arto
Hiltunen
*a,
Tero-Petri
Ruoko
a,
Tomi
Iivonen
b,
Kimmo
Lahtonen
c,
Harri
Ali-Löytty
c,
Essi
Sarlin
d,
Mika
Valden
c,
Markku
Leskelä
b and
Nikolai
Tkachenko
a
aLaboratory of Chemistry and Bioengineering, Tampere University of Technology, P.O. Box 541, FI-33101 Tampere, Finland. E-mail: arto.j.hiltunen@tut.fi
bDepartment of Chemistry, University of Helsinki, P.O. Box 55, FI-00014 Helsinki, Finland
cSurface Science Group, Laboratory of Photonics, Tampere University of Technology, P.O. Box 692, FI-33101 Tampere, Finland
dLaboratory of Materials Science, Tampere University of Technology, P.O. Box 589, 33101 Tampere, Finland
First published on 31st July 2018
Iron and titanium oxides have attracted substantial attention in photoelectrochemical water splitting applications. However, both materials suffer from intrinsic limitations that constrain the final device performance. In order to overcome the limitations of the two materials alone, their combination has been proposed as a solution to the problems. Here we report on the fabrication of an atomic layer deposited (ALD) Fe2O3 coating on porous ALD-TiO2. Our results show that successful implementation requires complete mixing of the TiO2 and Fe2O3 layers via annealing resulting in the formation of a photoactive iron titanium oxide on the surface. Moreover, we found that incomplete mixing leads to crystallization of Fe2O3 to hematite that is detrimental to the photoelectrochemical performance. IPCE and transient photocurrent measurements performed using UV and visible light excitation confirmed that the iron titanium oxide extends the photocurrent generation to the visible range. These measurements were complemented by transient absorption spectroscopy (TAS), which revealed a new band absent in pristine hematite or anatase TiO2 that we assign to charge transfer within the structure. Taken together, these results provide design guidelines to be considered when aiming to combine TiO2 and Fe2O3 for photoelectrochemical applications.
One strategy to combine two materials is to divide the functions of light absorption and charge transport between an absorber and a high surface area scaffold similarly to dye-sensitized solar cells.4 The scaffolding approach (also known as the host-scaffold/guest-absorber approach) was first demonstrated in water splitting by Sivula et al. where a 60 nm thick hematite layer was deposited on nanostructured WO3.4 Later, demonstrations of a 25 nm thick hematite layer on TiS2 nanonets, a 5 nm thick layer on ZnO nanorods,5 and a few nanometer thick hematite coating on porous ZnO6 have been reported. The suitability of TiO2 as a scaffold for hematite has been studied previously despite the unfavorable band alignment for electron injection. Successful combining of the good electron transport properties of TiO2 and light absorption of iron oxide holds great promise for efficient solar water splitting with safe, abundant and stable materials.
Successful implementation of hematite on TiO2 has been reported to require an underlayer (Nb2O5),7 while at the same time successful realization without an underlayer has also been reported.8 Moreover, annealing the TiO2 with Fe2O3 to create a thin Fe2TiO5 layer on the surface has been proposed to be the mechanism to reach high photocurrents.9 Therefore, the varying experimental results implies that the question of how to combine TiO2 and Fe2O3 in the scaffold/absorber configuration requires further clarification. Furthermore, a recent review tells that the working principles of the Fe2O3–TiO2 heterojunction devices still remain unclear and suggests further investigation on this promising topic.10
The aim of this paper is to establish whether TiO2 is a suitable scaffold for Fe2O3 in the scaffold/absorber configuration. To answer this question, we applied 100, 200 and 400 atomic layer deposition (ALD) cycles of Fe2O3 on porous TiO2. The thicknesses correspond nominally to 5, 10 and 20 nanometers. The composite materials were characterized by scanning electron microscopy (SEM), transmission electron microscopy (TEM), X-ray photoelectron spectroscopy (XPS), Raman spectroscopy, X-ray diffraction (XRD), and they were tested as anodes in a photoelectrochemical (PEC) water splitting cell. The steady-state PEC experiments were complemented by transient absorption (TAS) and transient photocurrent (TPC) measurements to gain insight into the water oxidation dynamics.
Our results show that an annealing step which creates a thin FeTi-oxide layer on the surface is necessary for successful device operation. Importantly, we find that crystallization of ALD-Fe2O3 to hematite will lead to reduced photocurrent once hematite begins to dominate the surface. The growth of hematite can be avoided by using a low number of ALD cycles. For our device architecture, we discover that 100 ALD-cycles is sufficient to increase the absorption of the photoanode without significant hematite crystal growth.
The results presented herein provide new insight into the fabrication of porous TiO2/Fe2O3 photoanodes with the scaffold/absorber technique by clarifying the surface science of the material composition from the perspective of solar water splitting. While this study was carried out by the means of ALD the here presented phenomena and the design principles derived from them are applicable to other fabrication techniques as well.
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Fig. 1 (a–c) SEM images of a TiO2 scaffold coated with 100, 200, and 400 cycles of ALD-Fe2O3, respectively. Images (d–f) are TEM images of the corresponding samples. |
X-ray photoelectron spectroscopy was implemented to further characterize the surface of the structure. Table 1 shows the relative elemental concentrations of Ti, Fe and O for the TiO2 sample with 100 cycles of ALD-Fe2O3 coating. Upon annealing at 680 °C the Ti/Fe ratio increases from 1.16 to 2.03, which indicates diffusion of Ti towards the surface. Furthermore, annealing increases the Fe 2p and Ti 2p peak separation by 0.3 eV (Ti 2p peak shifts to lower binding energy), which can be assigned to the formation of a mixed FeTi-oxide. In the studied samples, titanium was found to have oxidation state Ti4+ and iron Fe3+ suggesting the formation of a Fe(III)Ti(IV) oxide. A similar peak shift has been previously observed and associated to the formation of amorphous FexTi1−xOy, where a thin TiO2 coating was deposited over Fe2O3 nanorods.12 The XPS spectra for Fe 2p and Ti 2p energy regions are given in the ESI (Fig. S2†). No Sn was detected on the surface, while the diffusion of tin originating from the underlying FTO has been reported to occur upon annealing at high temperatures.13
Sample | Concentration, at% (XPS peak position, eV) | ||||
---|---|---|---|---|---|
Fe 2p3/2 | Ti 2p3/2 | O 1s | Ti/Fe | Δ(Fe 2p3/2–Ti 2p3/2) | |
As-deposited | 11.69 (710.62) | 13.53 (458.84) | 74.78 (530.07) | 1.16 | (251.78) |
Annealed | 7.44 (710.53) | 15.07 (458.43) | 77.49 (529.78) | 2.03 | (252.10) |
X-ray diffraction (XRD) was used to identify the crystal structures. As XRD is a bulk characterization method, all samples indicated crystalline SnO2 from the substrate and anatase TiO2. In the as-deposited condition, the existence of hematite was visible for the sample with 400 ALD cycles, as indicated by its highest intensity {104} peak at 33.3° (see Fig. S3† for the diffractogram). The hematite signal was not detected for the 100 or 200 cycle samples suggesting an amorphous structure. Even though ALD metal oxide films obtained at high temperatures are usually crystalline as-deposited, ultra-thin films (<5 nm) regularly remain amorphous until a critical film thickness value is reached.14 Upon annealing, the high intensity peak of hematite at 33.3° is intensified for the 400 cycles sample which suggests increased degree of crystallinity in the hematite layers compared to the non-annealed ones. Hematite was found in the annealed 100 and 200 cycle samples only in trace amounts.
Raman spectroscopy was used as a complementary experiment to study the annealed samples in more detail. The TiO2 scaffold shows typical anatase signal peaks at 144, 197, 395, 515 and 636 cm−1.15 The hematite peaks16 at 244, 291, 297, 410, 499, 610 cm−1 become clearly visible only after the coating thickness increases up to 400 cycles (Fig. 2). For the 100 and 200 cycle coatings the hematite signal is weak indicating that only a minor amount of ALD-Fe2O3 crystallized to hematite being in line with the XRD results. The LO (longitudinal optical mode) peak at 660 cm−1, which was observed only for the 400 cycle coated sample, has been assigned to disorder within the hematite lattice.17 The appearance of this peak has been also previously observed to appear for high temperature (650 °C) annealed Fe2O3–TiO2 systems and assigned to a reaction between hematite and TiO2.12 This peak is not detected for the 100 and 200 cycle samples as the hematite signal itself is barely visible.
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Fig. 2 Raman spectra of TiO2 scaffold with varying thickness of ALD-Fe2O3 coating. H: hematite, A: anatase, LO: longitudinal optical mode. |
Fig. 3 shows IV-curves for TiO2 scaffold coated with ALD-Fe2O3 along with the bare weblike TiO2 scaffold for comparison. The IV-curves are measured after annealing at 680 °C, which was found to be prerequisite for obtaining reasonable photocurrent from the ALD-Fe2O3 coated samples (see Fig S4† for the IV-curves of as-deposited samples). The TiO2-web shows an IV-curve with photocurrent in the same order of magnitude that has been previously reported for cellulose templated porous ALD-TiO2.18 This allows us to conclude that the web worked as expected and provided a suitable platform for the ALD-Fe2O3 coatings.
For the ALD-Fe2O3 samples we found out that the 100 and 200 cycle coatings gave significantly higher photocurrent than the thicker 400 cycle coating. Based on the results obtained by Raman spectroscopy and XRD we can see that the drop of the photocurrent is caused by the crystallization of ALD-Fe2O3 into hematite (see Fig. 2 & 3). This is in accordance with the observation noted previously by Sivula et al.4 and Stefik et al.7 that hematite overlayers on titania results in no photocurrent. This indeed is expected as hematite has a conduction band edge below that of titania, creating an injection barrier for the electrons photogenerated in the hematite layer.7,19 The photoelectrochemical performance of our materials closely matches those published earlier for Fex–TiO2 photoanodes prepared via sol–gel.20
The XPS analysis indicated the formation of an FeTi-oxide layer on the surface upon annealing. When the ALD-Fe2O3 cycle number is kept low, in our case 200 or below, the mixing of ALD-Fe2O3 with Ti during annealing is complete resulting in FeTi-oxide on the surface. This explains why the 100 & 200 cycle coated samples overperform the 400 cycle coated sample, where part of the ALD-Fe2O3 film crystallizes as hematite. Previously, a Fe2TiO5 (pseudobrookite) layer has been synthesized on TiO2 nanotubes by high temperature annealing of electrodeposited Fe2O3.9 More frequently, however, the Fe2TiO5 has been designed to inject electrons to hematite12,21–23 in contrast to what we report here.
Han et al.24 noted on the importance of not covering the whole TiO2 substrate with hematite in their system where the photoactive material was the TiO2. Our system is significantly different as the photoactive material is the mixed FeTi-oxide. To prove that the improved efficiency stems from the increased spectral response, originating from the mixed oxide, incident photon-to-current-efficiency (IPCE) was measured. As expected, the bare TiO2 gives rise to photocurrent only with UV excitation, and no signal with visible light excitation due to the large band gap of the material. However, upon coating of the TiO2 electrode with ALD-Fe2O3 followed by annealing, the spectral response is observed to extend into the visible range up to 600 nm. The IPCE of the hematite containing sample (400 cycles) is reduced compared to the 100 & 200 cycle samples, because hematite cannot contribute to the photocurrent due to the conduction band misalignment. The IPCE spectra are given in the ESI† along with UV-Vis absorption spectra of the materials Fig. S5a and b.†
Transient photocurrent (TPC) decays, measured with UV (355 nm) and visible light (410 nm) laser excitation, complement the steady-state IPCE measurements. The TPC experiment measures the decay of the photocurrent signal created by the laser excitation. The signal is a sum of two decay pathways: the electron–hole recombination and the electron extraction by the external circuit.25,26Fig. 4 shows TPC decays for bare TiO2 and FeTi-oxide normalized relative to the TiO2 355 nm signal. All the presented decays have similar kinetics, which imply that the aforementioned processes are not significantly altered by the coating within the resolution of the experiment. This similarity of the decay curves is evidence that the FeTi-oxide layer is able to inject electrons to the TiO2 network through which the charges diffuse to the FTO contact.
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Fig. 4 Photocurrent decays of the ALD-Fe2O3 sensitized (100 cycles, annealed) TiO2 electrodes and the reference TiO2 scaffold. Decays are normalized relative to the TiO2 355 nm signal. |
The charge carrier recombination dynamics were studied in the ps–ns timescale using transient absorption spectroscopy of annealed planar 200 cycles ALD-Fe2O3 samples deposited on FTO and TiO2 coated FTO. The 200 cycle sample was selected for the study to achieve high enough absorbance on the planar samples. The excitation wavelength was set to 410 nm to selectively excite only the ALD-Fe2O3 overlayer. In this time-scale the transient absorption is composed of a superposition of the absorptions of both photoexcited holes and electrons.
The negative transient absorption band below 450 nm is due to the bleaching of the ground state absorption. The strong positive absorption band centered at 570–580 nm in the bare hematite sample has previously been assigned to the absorption of photoexcited electrons.27 However, recent investigations of hematite photoanodes under applied bias voltages have revealed a positive absorption at the same wavelength that is formed due to high valent iron-oxo species.28,29 We have previously observed that a bias dependent bleaching of this absorption occurs due to electron transfer into oxidised surface states.30 Thus, we conclude that this absorption band is most probably due to photoexcited holes in the hematite bulk. The decay of the photoexcited electrons is a multiexponential process dominated by recombination and electron trapping.30 The decay of the TAS signal was best fit with three exponential functions with lifetimes of 0.29, 17, and 320 ps (Fig. S6a–c & Table S2†).
The transient absorption spectrum of the ALD-Fe2O3 sample deposited on top of TiO2 and annealed at 680 °C shows the formation of a new broad positive absorption band between 450–680 nm (see Fig. 5b). Neither bare hematite or TiO2 (Fig. S6d†) show a positive transient absorption below 535 nm. Additionally, the globally fitted three exponential decay of the TAS signal now has lifetimes of 0.26, 4.7, and 320 ps. The fastest and slowest components of the decay match those for the bare hematite sample, whereas the middle component is now significantly faster. We determine this new positive absorption band to indicate that electrons have been transferred to the TiO2 layer. The transfer of electrons between the layers explains the faster decay component, and the positive transient absorption spanning from 450 to 680 nm is assigned to the free electrons transferred to the TiO2 layer.31 Interestingly, the ground state bleach observed for the bare hematite sample below 450 nm is not visible for the sample deposited on top of TiO2. This can be due to the transfer of conduction band electrons away from the FeTi-oxide layer leading to the ground state bleach disappearing, further supporting our determination of the electron transfer occurring through the mixed oxide layer, as indicated by the TPC results. Typically, electron transfer between unmixed layers should take place in the picoseconds to nanoseconds timescale. The fact that the change in the TAS spectrum occurs immediately after excitation suggests towards the proposed mixing of the two metal oxide layers.
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Fig. 5 Transient absorption spectra of (a) hematite and (b) FeTi-oxide. Timescale is linear until 1 ps and logarithmic for longer delay times. |
Planar samples for transient absorption measurements were prepared by coating FTO substrates with 30 nm of TiO2 using the same ALD procedure as for the cellulose substrates, and annealed at 450 °C. When used as a reference for the ALD-Fe2O3 coated samples, same post-annealings were applied to all.
Footnote |
† Electronic supplementary information (ESI) available: Additional SEM image, XPS data, XRD diffractograms, IV-curves, IPCE, and TAS spectra. See DOI: 10.1039/c8se00252e |
This journal is © The Royal Society of Chemistry 2018 |