research papers
Truly bulk-sensitive spectroscopic measurements of valence in heavy †
materialsaINFM - Dipartimento di Fisica, Politecnico di Milano, I-20133 Milano, Italy, bEcole Polytechnique Fédérale (EPFL), CH-1015 Lausanne, Switzerland, cEuropean Synchrotron Radiation Facility, BP 220, Grenoble, France, and dLos Alamos National Laboratory, Los Alamos, NM 87545, USA
*Correspondence e-mail: claudia.dallera@fisi.polimi.it
Intermediate valence is one of the typical phenomena of systems with strong electronic correlation. The Anderson impurity model predicts a scaling of the valence with the reduced temperature T/TK, which is difficult to observe by traditional surface-sensitive electronic spectroscopies. This paper presents results obtained by resonant inelastic X-ray scattering (RIXS), a bulk-sensitive configuration- and chemical-specific technique. The temperature dependence of the valence of YbInCu4 and YbAgCu4 was measured by tuning the incident energy to the resonance of the Yb2+ spectral component. In the case of YbInCu4 a sharp as known from thermodynamical measurements, has been found. The valence of YbAgCu4 reveals a smooth dependence consistent with a Kondo temperature TK = 70 K. These findings establish RIXS as a powerful tool for measuring bulk electronic properties of solids.
Keywords: mixed valence; RIXS; heavy fermions; Kondo behaviour; ytterbium; rare earths; Anderson impurity model.
1. Introduction
Mixed valence arises in strongly correlated solids from the conflict between the natural tendency of electrons to form extended bands and the opposite tendency to occupy atomic-like localized states. This leads to spectacular physical properties including Kondo and heavy et al., 1986).
behaviour as well as unconventional magnetism and superconductivity (LeeValence fluctuations can be revealed by various transport, thermodynamic and spectroscopic measurements. The latter probe, in the most direct way, the nature of the electronic ground state but typically only sample a thin layer (∼10–20 Å) below the surface. Recent experiments at higher photon energy (Sekiyama et al., 1997; Braicovich et al., 1997) with larger probing ranges (∼20–50 Å) highlight the limitations of conventional measurements. This disadvantage is overcome by photon in–photon out spectroscopies like resonant inelastic X-ray scattering (RIXS), which probes the electronic states of a much thicker (∼10 µm in our experiment) bulk-like layer. RIXS is also element-specific and can distinguish between different electronic configurations. These characteristics make RIXS an ideal tool to obtain bulk information about intermediate-valence systems, as we prove in the present study of valence in the two Yb-based Kondo systems YbInCu4 and YbAgCu4. The valence is predicted by the Anderson impurity model (AIM) to scale with the reduced temperature T/TK, where TK is the Kondo temperature (Bickers et al., 1987). YbInCu4, a moderately heavy was chosen as a model compound. It exhibits a first-order transition at TV = 42 K, where the valence suddenly decreases from 2.96 to 2.83, and TK changes from ∼20 K to ∼400 K. Such a small valence difference gives rise to large changes in all the physical properties. For YbAgCu4, a with temperature is expected, consistent with TK ≃ 60–100 K. The mentioned valence changes have been hinted at by a wealth of non-spectroscopic measurements. Spectroscopic results in these and in related Kondo systems are controversial, due to possible contributions from perturbed surface layers (Malterre et al., 1997). The present findings unambiguously demonstrate the validity of the AIM predictions providing results that are related to truly bulk states.
2. Experimental
The experiment was performed on the ESRF beamline ID16. The incident radiation was monochromated by an Si(111) monochromator. X-rays scattered at 90° by the sample were energy-analyzed with a Rowland circle-based spectrometer equipped with a silicon crystal cut along the (620) direction. We measured Lα1 (3d–2p) RIXS spectra of ytterbium at selected excitation energies across the L3 (2p3/2) threshold, and L3 absorption spectra (XAS) by recording the intensity of the Lα1 fluorescence while scanning the incident photon energy. These partial (PFY) spectra are free from the lifetime broadening of the deep core-hole (Hämäläinen et al., 1991). The overall resolution was 1.3 eV. The samples were polished single crystals mounted on an He closed-cycle refrigerator allowing accurate temperature control between 15 K and 300 K.
3. Results and discussion
The ground state of ytterbium in YbInCu4 and YbAgCu4 is a coherent superposition of Yb2+ (4f14) and Yb3+(4f13) states. Fig. 1 shows the of ytterbium in the ground state and in the intermediate and final states of the RIXS process, together with the main transitions connecting the different configurations. The fingerprints of both Yb2+ (4f14) and Yb3+(4f13) are visible in the Yb L3 PFY spectra of YbInCu4, recorded below and above the transition temperature (Fig. 2). The intensity of the Yb2+ component drops at TV, reflecting the sudden change of valence. For comparison we show the same absorption spectra measured in the traditional total mode. These results are consistent with previous data (Cornelius et al., 1997) but the use of the PFY detection results in superior resolution and much better defined spectral features.
The quantitative determination of the Yb2+ weight in the ground state is necessary to evaluate the deviation from the integer 3+ valence. The corresponding signal is small. However, the sensitivity to the divalent configuration can be greatly enhanced by tuning the to the peak of the Yb2+ signal and recording the corresponding RIXS spectrum. This is clearly illustrated by Fig. 3, showing RIXS spectra collected at various energies around the Yb2+ resonance. At the peak of the resonance the Yb2+ signal dominates the spectrum for T = 15 K (below the transition). Above the transition temperature ytterbium is closer to trivalent, and the divalent contribution is less intense.
The temperature dependence of the divalent signal is most clearly observed at resonance. Fig. 4 shows the change of the spectral shape for both compounds. The small valence changes yield large changes in the weight of the divalent component, which is proportional to (1 − nh), where nh is the number of f-holes (nh = 0 for Yb2+, nh = 1 for Yb3+). The spectra of YbInCu4 exhibit a variation only across TV. For YbAgCu4 the line shape changes continuously between the two extreme cases of Fig. 4. The temperature dependence was followed continuously by monitoring the divalent peak intensity (shaded region in Fig. 4). The measured intensity was corrected to account for the overlapping tail of the trivalent signal, determined from the fluorescence spectrum excited 30 eV above the (dashed line).
The temperature evolution of the divalent component is presented in Fig. 5. The measured intensities have been converted into absolute (1 − nh) values by using the low-temperature nh values of Lawrence et al. (1994) (0.83 for YbInCu4 and 0.87 for YbAgCu4). A very different behaviour with temperature is identified: in YbInCu4 the edge located around TV = 42 K reveals the sudden valence change at the transition temperature. In YbAgCu4 the evolution is smooth and exhibits a concavity change around 70 K. The dashed curve is the prediction of the AIM, calculated within the non-crossing approximation (NCA), assuming a Kondo temperature TK = 70 K.
RIXS data at the L edges of rare earths contain a further independent indicator of valence. In fact, in addition to the dipolar 2p–5d transition, a 2p–4f quadrupolar excitation is also possible in the absorption step of the scattering process. The quadrupolar transition is much weaker than the dipolar one and is detected only for excitation energies well below the 2p–5d (Dallera et al., 2000). Nonetheless, this channel is very interesting because it directly involves the 4f states. This transition is therefore a very powerful indicator of rare-earth valence changes driven by external temperature and pressure conditions, especially in Yb, where the 4f shell is close to being filled. The quadrupolar transition cannot occur in divalent (4f14) metallic ytterbium. In compounds, following with the 5d orbitals, nh holes are available for the transition. The quadrupolar feature is indicated by the arrows in Fig. 6, displaying spectra excited at the resonance of the 2p–4f transition. It appears at a lower because the addition of an electron into the 4f states leaves the system in a less The peak is evident at high temperature when ytterbium is in an almost trivalent state. At low temperature it appears only as a shoulder. Both the dipolar and quadrupolar features carry in principle the same information on the Yb valence state. However, since the dipolar channel involves extended conduction states, a quantitative comparison of their relative intensities is not straightforward and should explicitly take into account the material-dependent 5d near EF, and subtle details of the resonance profile.
The present results confirm that the Anderson model provides a sound theoretical framework also for the spectral properties of Kondo systems. Previous inconsistencies are most likely due to the short probing depth of electron spectroscopies, and to perturbed surface layers. They demonstrate that RIXS is an extremely interesting bulk probe of intermediate valence thanks to the possibility of resonantly enhancing the contribution of a specific
of interest. Extensions to other strongly correlated systems like the transition metal oxides, and to experiments under pressure or in external fields, which are precluded to electron spectroscopies, are being considered.Footnotes
†Presented at the `International Workshop on High-Resolution Photoemission Spectroscopy of Correlated Electron Systems' held at Osaka, Japan, in January 2002.
Acknowledgements
We would like to thank M. H. Krisch and J. P. Rueff for assistance and discussion in the preliminary stage of the experiment. CD is indebted to R. Montegue for invaluable support.
References
Bickers, N. E., Cox, D. L. & Wilkins, J. W. (1987). Phys. Rev. B, 36, 2036–2079. CrossRef Web of Science Google Scholar
Braicovich, L., Brookes, N. B., Dallera, C., Salvietti, M. & Olcese, G. L. (1997). Phys. Rev. B, 56, 15047–15055. Web of Science CrossRef CAS Google Scholar
Cornelius, A. L., Lawrence, J. M., Sarrao, J. L., Fisk, Z., Hundley, M. F.,Kwei, G. H., Thompson, J. D., Booth, C. H. & Bridges, F. (1997). Phys. Rev. B, 56, 7993–8000. CrossRef CAS Web of Science Google Scholar
Dallera, C., Krisch, M. H., Rogalev, A., Gauthier, C., Goulon, J., Sette, F. & Sole, A. (2000). Phys. Rev. B, 62, 7093–7097. Web of Science CrossRef CAS Google Scholar
Hämäläinen, K., Siddons, D. P., Hastings, J. B. & Berman, L. E. (1991). Phys. Rev. Lett. 67, 2850–2853. CrossRef PubMed CAS Web of Science Google Scholar
Lawrence, J. M., Kwei, G. H., Canfield, P. C., DeWitt, J. G. & Lawson, A. C. (1994). Phys. Rev. B, 49, 1627–1631. CrossRef CAS Web of Science Google Scholar
Lee, P. A., Rice, T. M., Serene, J. W., Sham, L. J. & Wilkins, J. W. (1986). Comments Cond. Matt. Phys. 12, 99–161. CAS Google Scholar
Malterre, D., Grioni, M. & Baer, Y. (1997). Adv. Phys. 45, 299–348. CrossRef Web of Science Google Scholar
Sekiyama, A., Iwasaki, T., Matsuda, K., Saitoh, Y., Onuki, Y. & Suga, S. (2000). Nature (London), 403, 396–398. Web of Science CrossRef PubMed CAS Google Scholar
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