Emergent phenomena in transition-metal-oxide heterostructures such as interface superconductivity and magnetism have been attributed to electronic reconstruction, which, however, is difficult to detect and characterise. Here we overcome the associated difficulties to simultaneously address the electronic degrees of freedom and distinguish interface from bulk effects by implementing a novel approach to resonant X-ray reflectivity (RXR). Our RXR study of the chemical and valance profiles along the polar (001) direction of a LaCoO3 film on NdGaO3 reveals a pronounced valence-state reconstruction from Co3+ in the bulk to Co2+ at the surface, with an areal density close to 0.5 Co2+ ions per unit cell. An identical film capped with polar (001) LaAlO3 maintains the Co3+ valence over its entire thickness. We interpret this as evidence for electronic reconstruction in the uncapped film, involving the transfer of 0.5e− per unit cell to the subsurface CoO2 layer at its LaO-terminated polar surface.
Heterostructures comprising transition-metal oxides (TMOs) exhibit a particularly rich variety of phenomena, including, for instance, superconductivity at interfaces of non-superconducting copper oxides,1 the coexistence of superconductivity and ferromagnetism2,3 or orbital reconstruction.4 This is largely due to their structural, electronic and magnetic degrees of freedom, tuned by heteroepitaxial exposure and strain.5 A prominent example is the formation of a two-dimensional electron gas at the (001) interface between the two band insulators SrTiO3 (STO) and LaAlO3 (LAO).6 Various ideas have been put forward to explain this,6,
This charge can be provided by various reconstruction mechanisms,6,7,10,
Recent research has focused on the LAO/STO system, in which the conjectured electronic reconstruction would entail the transfer of 0.5e− per two-dimensional unit cell (u.c.) from the LAO surface to the interface, where it would lead to a Ti valence reduction and to the observed two-dimensional electron gas in the intrinsically non-polar STO. LAO/STO and related TMO systems have been extensively studied both theoretically7,10 and by various experimental techniques,19,
Therefore, the origin of the two-dimensional electron gas in LAO/STO remains highly debated, and microscopic evidence is required, which supports the whole concept of electronic reconstruction in polar TMO films in general. Here we present such evidence, which we have collected in a judiciously chosen sample system devoid of several of the complications encountered in LAO/STO, namely LaCoO3 (LCO) on a polar substrate, and by using resonant X-ray reflectivity (RXR), an experimental technique with sub-nanometre resolution and interface sensitivity.
Choice of the experimental technique
Various experimental techniques are being routinely used to explore the electronic properties of TMO heterostructures and interfaces, among them transport and Hall measurements, X-ray absorption (XAS),19,31 hard X-ray photoemission spectroscopy,20 resonant inelastic X-ray scattering,22 standing-wave excited PES23 or electron energy loss spectroscopy in scanning transmission-electron geometry.21 These techniques exhibit different depth resolutions, mostly lacking interface sensitivity, and they probe different quantities such as the total charge density versus the mobile charge density; this contributes to the uncertainty regarding the interfacial properties.
There are several experimental complications associated with the vacuum/LAO/STO system: first, there is typically some degree of cation intermixing at the interface. Second, it contains two polar–non-polar (P/NP) interfaces. Finally, the polar LAO comprises elements with a rather stable, single valence, making electronic reconstruction within the LAO film itself prohibitively expensive. Therefore, we have chosen to study a LaCoO3 film39,
The two samples—LCO//NGO and LAO/LCO//NGO—were grown using pulsed laser epitaxy and characterised as described in the Materials and Methods section. The total film thickness is about 15 nm, including the 2 u.c. LAO capping in the LAO/LCO sample.
Obtaining the optical constants from XAS
XAS and RXR measurements were performed at 300 K with σ-polarised light, using the four-circle ultra-high vacuum diffractometer at the REIXS 10ID-2 beamline of the Canadian Light Source in Saskatoon, Canada (see Materials and Methods and ref. 45). The XAS data of the two samples around the Co L3 and L2 absorption edges, measured in total electron yield (TEY) mode, which has a shallow probing depth of a few nanometres, are compared in Figure 2a. The spectrum of the capped sample, XAScap, represents stoichiometric LaCo3+O3 (high-spin- to low-spin-state ratio ~1/2, see refs 39,44). The contribution from Co2+, which is observed in non-stoichiometric films, and which would result in a shoulder around 777.5 eV and a prepeak around 776 eV, is negligible. In contrast, the spectrum of the uncapped sample, XASuncap, clearly shows non-Co3+ contributions with features indicative of Co2+. The fact that a capping of 2 u.c. is sufficient to suppress them, suggests that this Co with non-3+valence is localised near the surface. A further indication for that comes from a comparison with XAS measured in the bulk-averaging fluorescence yield mode in Figure 2b: here the spectra of the capped and uncapped films are nearly indistinguishable and very much resemble the Co3+ spectrum shown in Figure 2a.
In order to assess the precise nature of the non-Co3+ contribution, we have subtracted the LAO/LCO//NGO spectrum from the LCO//NGO spectrum, scaling the spectra with respect to each other as described in the Materials and Methods section. In Figure 2c, we compare the difference spectrum XASdiff with published experimental data of Co2+ in octahedral coordination.46 The agreement is excellent, strongly supporting the hypothesis of a structurally intact LCO surface containing Co2+.
RXR measurements and fits
In order to substantiate our findings we will next precisely determine the distribution of Co2+ by analysing RXR data, which were measured at and around the relevant absorption edges and which are shown in Figure 3. The novel analysis scheme we have developed to determine valence-state profiles is based on our approach in ref. 38, and is described in the Materials and Methods section.
Here the properties to scrutinise are the surfacial and interfacial roughnesses, and the Co2+ concentration in a surface layer of variable thickness. Therefore, the initial layer sequence is (O, organic contamination)/LaAlO3/LaCo3+O3/NdGaO3 for the LAO/LCO//NGO sample and (O, organic contamination)/LaCo1−x2+Cox3+O3/LaCo3+O3/NdGaO3 for the LCO//NGO sample (Figure 4). We have included the first layer to account for oxygen adsorption to the surface47 and inevitable contaminations due to air exposure of the sample before the measurement.38
Details about how the implementation of the fitting procedure influences the quality of the fits are discussed in ref. 38 and references therein. In particular, the initial choice of a suitable layer sequence, and therefore of a reasonable number of parameters is crucial. If there are too many parameters, the convergence in a finite time is not guaranteed, and the fitting procedure might get trapped in local minima. For this reason, the substrate and the bulk of the films have been kept stoichiometric, a restriction that was not enforced at the surface to be able to track the individual cation profiles in detail. Also, all the elements have been allowed to converge towards individual roughnesses at the interfaces.
Starting with the initial layer sequence, we apply the fitting procedure described in the Materials and Methods and in ref. 38. For both samples, we use constant-energy θ−2θ scans measured up to qz-values of at least 0.58 Å−1 and at various energies around the La and Co edges (Figure 3a,c), as well as constant-qz scans (Figure 3b,d) at the marked qz-positions. Panels a and b also contain the final fits for the LAO/LCO//NGO sample, while panels c and d contain those for the LCO//NGO sample. The corresponding final elemental and valence depth profiles are shown in Figure 4.
We will now elaborate on important details of the fit. An important property of the LAO/LCO//NGO RXR data, which our fit correctly reproduces, is the absence of Co2+-related structures around 777.5 eV at any wave number qz. This confirms that there is no Co2+ in this sample in appreciable amounts. In contrast, the RXR data of the uncapped LCO//NGO sample exhibit prominent features around 777.5 eV at high qz, a qualitative indication of a Co2+ accumulation localised in depth. Indeed, the quantitative fit reveals a narrow Co2+ distribution at the film surface with a full width at half maximum of 8.6 Å (~2 u.c.), concomitant with a decline in Co3+ concentration (Figure 4a). Importantly, the total amount of Co2+, if it was confined to one monolayer, would correspond to an areal density of 0.55±0.15 ions per u.c., close to half coverage.
The fits demonstrate that both samples exhibit a sharp substrate–film interface and thus grow with very good quality (Figure 3). Our analysis also suggests that the La profile extends about half a u.c. further than the Co profile, which is consistent with a predominant LaO termination and is expected from the NdO termination of the substrate. This, and the fact that we achieve our fits using Co2+ and Co3+ spectra typical for bulk cobaltates, strongly indicate that both samples maintain their crystallinity up to the LCO surface, and are not subject to chemical decomposition.
We have confirmed the quality and robustness of our fits in several ways. First, the successful determination of chemical and valence-state profiles crucially depends on how different the optical constants of the involved species are. From Figure 2 it is clear that Co3+ and Co2+ have distinctly different resonant absorption edges. Co2+ can be particularly well identified by the prepeak at 777.5 eV, and we have exploited this to distinguish the profiles of the two Co valences. The fact that the signatures of Co2+ are stronger at the Kiessig fringe minima (Figure 3b, right column) than at the maxima (left column), and that the fits at the maxima are superior to those at the minima fully support our conclusion, namely that Co2+ is limited to the surface: the maxima reflect the superposition of surface and interface signal, and are therefore dominated by Co3+. The minima, on the other hand, reflect the difference between surface (Co2+ and Co3+) and substrate interface signal (Co3+ only), and are therefore particularly sensitive to Co2+. In addition, the minima are much sharper than the maxima and thus more prone to even small deviations in the elemental profiles.
Second, altering the Co2+ concentration from the 0.55 ions per u.c. quickly deteriorates the fit quality (χ2) and distorts the signatures of Co2+ both at minima and maxima. We use this sensitivity to estimate an error bar of 0.15 ions per u.c., which indicates the range of Co2+ concentrations within which the χ2 of the fit deviates by <15% from the best fit. Also, it is qualitatively observed that for concentrations outside this range the Co2+ features in the RXR simulations strongly under- or overestimate the corresponding features in the measured RXR data. This also demonstrates that the total Co2+ concentration, which characterises the electronic system, is a sensitive fitting parameter, as can be also expected on theoretical grounds (cf. references in ref. 38).
Third, further simulations showed that there is no accumulation of Co2+ near the LCO//NGO interface in either of the two samples. This indicates that LCO and NGO are of comparable polarity and the interface is not involved in the reconstruction.
Finally, we have tried to use Co optical constants based on XAS data from the LCO//NGO sample only, without subtracting the LAO/LCO//NGO spectrum. Fitting the Co profile in LCO//NGO reflectivity data with these optical constants did not result in a satisfactory fit, confirming that the film does not consist of a homogeneous mixture of Co2+ and Co3+.
How can we interpret the valence-state reconstruction we observe in LCO? Electrostatic considerations dictate that a polar sample of the given thickness must reconstruct in some manner.13,
The reconstruction scenario, applied to the LCO surface, is outlined in Figures 5 and 6. Beginning from the surface, the atomic layer sequence is LaO/CoO2/LaO/CoO2/..., which nominally corresponds to a charge concentration sequence of +e/−e/+e/−e/... per u.c. over the sample thickness, including the entire substrate (Figure 5). The compensation of the associated internal potential occurs successively during epitaxial growth: the NdO-terminated, polar substrate has undergone a reconstruction by an unidentified mechanism, resulting in effective charges of −e/2 and e/2 per u.c. at its surface and backside, respectively (Figure 6a). Upon successively depositing LCO monolayers, the surface reconstruction heals and the effective negative charge is established at the new film surface (Figure 6b,c), thereby keeping the internal potential in the now thicker sample compensated.
La and O have a rather stable single valence and do not exhibit bands near the chemical potential, whereas calculations, for instance within the framework of LDA+U, have established that the first electron affinity state is within a Co d-band.48 Therefore, it is energetically favourable to leave the potential uncompensated over the topmost half u.c. and accommodate the compensating charge in the buried CoO2 layer, leading to the reconstructed surface configuration LaO (+1)/CoO2 (−1.5). This changes the Co valence to 2.5+, which we spectroscopically observe as a superposition of Co3+ and Co2+ (Figure 2). This electronic reconstruction scenario involving the subsurface layer is very different from the scenarios discussed for LAO/STO and related materials.
We will next consider different reconstruction scenarios. On the one hand, whereas chemical reconstruction or the surface deposition of anions such as OH− could hypothetically prevent the polar catastrophe, these mechanisms do not involve the creation of Co2+. On the other hand, the deposition of electropositive elements, e.g., in an additional LaO layer, or the creation of oxygen vacancies could explain the presence of Co2+, but would not prevent the polar catastrophe—therefore, the energy costs associated with such disruptions are not justified. These arguments, the close proximity of the observed Co2+ concentration to 0.5 per u.c. and the fact that it is energetically favourable to change the Co valence in a purely electronical way48 leave electronic reconstruction as the explanation by far most consistent with our data.
Importantly, based on XAS alone only very qualitative information can be obtained about the elemental and valence depth distribution by taking advantage of the different probing depth of the TEY and fluorescence yield mode extraction (see above). Our investigations indicate that even bulk properties should be better studied by RXR: surface reconstructions, stoichiometry variations and contaminations are ubiquitous effects. Using TEY, which typically has a probing depth of a few nanometres, will grossly overemphasise surface effects. As a case in point consider our TEY results: if interpreted as being representative of bulk properties, they would falsely indicate a bulk Co2+/Co3+ ratio of 1/4, whereas the actual bulk Co2+ content is negligible.
Using the more bulk sensitive fluorescence yield mode is not a viable alternative either, as it does not strictly represent absorption.49,50 The best option whether RXR is not available is to terminate the sample with a protective layer. However, in many cases it will be difficult to find a material that does not itself change the film properties: it has to be lattice matched, of the same polarity, of comparable oxygen affinity and so on.
In summary, we have demonstrated that RXR is an excellent tool to study reconstruction phenomena in heterostructures comprising complex materials. We have shown direct microscopic evidence for electronic reconstruction on the polar (001) surface of LaCoO3. Whereas a RXR analysis of the magnetic structure of LCO has to await future studies, our results indicate that LCO films are dominated by Co3+ and that Co2+ is limited to the surface: this sets stringent boundary conditions for the interpretation of ferromagnetism in LCO thin films42,44 and powders.18 It suggests that Co3+ spin-state transitions in the bulk drive the ferromagnetism and excludes schemes involving the presence of Co4+ at the surface.18
Our results stress the necessity to further develop RXR into a tool to routinely extract optical constants of the bulk and of buried interfaces. This is not only important in the presence of surface reconstruction but also when the detection of TEY drain current is technically difficult or not possible, such as in insulators, in the presence of strong magnetic fields and in femtosecond-resolved pump–probe experiments. Corresponding experimental endeavours are underway and our approach is ideally suited to analyse the resulting data.
Materials and Methods
We used pulsed laser epitaxy to grow LCO thin films with (001) orientation on NdO-terminated single-crystal NGO substrates with (001) orientation (pseudocubic notation). A KrF excimer laser (λ=248 nm) with a laser fluence of ~1 J/cm2 was used for ablating sintered LCO and single-crystal LAO targets. The samples were fabricated at 700 °C in 100 mTorr of oxygen partial pressure. We note that the growth at high oxygen partial pressure was necessary for high-quality, phase-pure LCO thin films. Lower oxygen partial pressure resulted in cobalt oxide impurity phases as evidenced by X-ray diffraction.
Optical constant determination by XAS
The off-resonant, imaginary parts of the atomic scattering factors of the involved elements, as well as those parts lying outside of the scrutinised XAS energy window of ~600–900 eV were retrieved from Chantler tables.51 The resonant parts of Co3+ and La were obtained from XAS measurements in TEY mode. The background was corrected and the data aligned with the tabulated values as previously described in ref. 4 to obtain the complete imaginary parts of the atomic scattering factors. The real parts were obtained by Kramers–Kronig transformation.
For the Co2+, intermediate steps were necessary: as described in the main text, a Co3+ spectrum was subtracted from the data of the uncapped LCO//NGO sample (Figure 2). The difference spectrum XASdiff depends on the scaling of the original spectra with respect to each other. However, the choice of the scaling underlies stringent restrictions: XASdiff may not become negative at any energy, it must reflect the edge jump51 and it should represent a meaningful Co valence. These restrictions lead to a close to perfect Co2+ spectrum (Figure 2) in octahedral high-spin configuration. Different scaling choices do not lead to either of the other possible Co valencies (3+ and 4+) in either of the known spin states, or mixtures thereof. To further improve the alignment of the cobalt spectra to the Chantler calculations, which is somewhat complicated by the vicinity of the La resonance, we have compared the areas below the Co3+ and the Co2+ resonances. For a purely ionic situation, the ratio is 4/3. We expect covalence effects, which are significantly stronger for Co3+ than for Co2+, to reduce this ratio to ~1.1. In the aligning process of the two spectra to the Chantler calculations, we have ensured that this ratio be kept.
Valence-state profiling based on RXR data
Our approach here is based on the chemical profiling scheme we describe in ref. 38. The sequence of steps to perform is as follows: first, we set up a model consisting of a sequence of layers k containing elements (in their respective valence) i, with the parameters being the thickness tk, atomic concentration ci,k and roughness of the respective upper interface σi,k. We then simulate the resulting RXR curves, compare them with the measured curves and optimise the parameters until convergence is achieved. The initial layer sequence depends on the complexity of the system and reflects preliminary information about surfactant layers, intermixing regions and so on. For the samples studied here, it is discussed in the main text.
From the parameters of the individual layers tk, ci,k and σi,k, we obtain the elemental depth concentration profiles ci(z) of the entire heterostructure, such as those shown in Figure 4. Their properties are described by atomic scattering factors fi(ω) with a unique photon frequency dependence, which we derive from the XAS spectra as described above.4,38 The entire heterostructure is then described by the depth-resolved susceptibility where k0 is the wave vector of the incoming beam, rel is the classical electron radius and NA is the Avogadro number. On the basis of χ(z,ω), RXR spectra can be simulated using the Parratt formalism.52 Finally, a least-squares algorithm is used to optimise χ2, the deviation between the measured data and the simulated spectra.38,53
At low qz-values (below about 0.05 Å−1) the measured intensity is suppressed due to geometrical shadowing effects and deviates from the expected intensity. We have applied a corresponding correction factor.54
We thank B Keimer and K Fürsich for helpful discussions. This work has been supported by the German Research Foundation DFG under grant number HA6470/1-2 and through SFB 1170 ‘ToCoTronics’ (project C04), as well as by the Canadian organisations NSERC, CFI and CRC. WSC was supported by the Basic Science Research Program through the National Research Foundation of Korea (NRF) funded by the Ministry of Science, ICT and future Planning (NRF-2014R1A2A2A01006478). Parts of the research were performed at the Max-Planck UBC Centre for Quantum Materials. Parts of the research were performed at the Canadian Light Source, which is funded by the Canada Foundation for Innovation, the Natural Sciences and Engineering Research Council of Canada, the National Research Council Canada, the Canadian Institutes of Health Research, the Government of Saskatchewan, Western Economic Diversification Canada and the University of Saskatchewan. The work at ORNL was supported by the U.S. Department of Energy, Office of Science, Basic Energy Sciences, Materials Sciences and Engineering Division.
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