Crystal field studies in Eu3+ doped Bi12SiO20 and Bi12SiO20:V5+ single crystals

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Abstract

Site-selective laser spectroscopy investigations of Eu3+ in Bi12SiO20 (BSO) and Bi12SiO20:V5+ (BSO:V) single crystals have been carried out. The line narrowed fluorescence shows the existence of a single crystal field site for the rare earth in BSO whereas in BSO:V five different crystal field sites for Eu3+ may exist, which depend on the vanadium concentration. The number of Stark components observed in 5D07FJ transitions corresponds to a complete absence of degeneracy in 7FJ multiplets and indicates a symmetry C2v or lower for these optically active centres. Simulations of the sequence of Eu3+ energy levels for each of the five observed sites have been worked out by using the single-particle crystal-field theory. The nature of the new active optical sites has also been investigated by comparing the phenomenological crystal-field parameters with those calculated by a semi-empirical model which takes into account the distortions of the oxygen bonds produced by the presence of V5+.

Introduction

A growing interest is focused on Bi12SiO20 (BSO) due to its optical properties and technological applications, most of them derived from its photorefractive behaviour [1].

Bismuth oxide compounds of the Bi12SiO20 type have a body-centered cubic structure (sillenite structure) which is able to accommodate a variety of different M atoms (M=Si in this compound). This is due to the fact that the oxygen tetrahedron surrounding the M atom can change its size without a major effect on the remaining atomic arrangement [2]. This peculiarity has promoted an effort to establish the mechanisms of isomorphous replacement in sillenites. From a fundamental point of view the knowledge of the defects responsible for the photorefractive effect still remains as an unsolved question, in particular as regards to the absorption bands associated with those defects. Up to now most of the works adscribe the absorption shoulder, located at energies close to the absorption edge, to the photoconductive and photorefractive behaviour. However, no definite conclusions have been reached about which defects are responsible for these behaviours.

BSO crystals doped with several transition metal ions have been studied [3], [4], [5], [6] in order to ascertain their influence on the absorption shoulder appearing in pure BSO crystals. Among them, V5+ has shown very interesting features. In particular, it has been demonstrated [7] that at small concentrations V5+ gives an increase of the absorption coefficient in the shoulder region whereas at higher concentrations a bleaching of the BSO crystals occurs. Moreover, the presence of V5+ in the sillenite structure strongly affects the type of Bi–O bondings, and therefore, the Bi site symmetry [8], [9]. On the other hand, only a few studies are known on the optical properties of BSO doped with rare earths [10], [11], [12], [13], [14], [15], [16]. It is well established that spectroscopical studies of rare earths may give valuable information about lattice site, lattice distortion, degree of covalency to ligand ions, and many other related dopant-host properties.

In recent works [14], [15] some of the present authors reported, for the first time in pure and vanadium codoped BSO crystals, a preliminary identification of the spectroscopic active sites of Nd3+ and Eu3+ ions by using site-selective laser spectroscopy. Three different crystal-field sites for Nd3+ and five different crystal-field sites for Eu3+, which depend on vanadium concentration, were found and optically isolated. However, neither a clear explanation was found about the nature and characteristic features presented by the emission spectra corresponding to the optical active sites, nor a plausible argument permitting to relate the rare earth optical behaviour with the presence of vanadium in the BSO crystal structure.

The work reported here comprises the spectroscopic results on site-selective emission spectra and a detailed crystal-field (cf) simulation of the Eu3+ energy level scheme for the five different optical centres in the BSO host. Calculations of cf effects have been carried out by using the single-particle cf theory. The phenomenological simulation of each Eu3+ energy level scheme is conducted on the basis of the strongly reduced 7FJM set alone, i.e. only considering 49∣SLJMJ〉 levels. A descending symmetry method, from C2v to C2 symmetries, has been used in the fitting procedure. The appearance and relative intensity of these centres are discussed in terms of plausible crystallographic distortions of the EuO5 polyhedron when compared with the BiO5 in the non-substituted BSO host. Simulations of corresponding cf parameters for these changes in the Bi environment were performed through a semi-empirical model which considers the crystallographic positions of the oxygen atoms around Bi.

Section snippets

Experimental

Pure and doped BSO crystals were grown by the Czochralski method from grade A1 Johnson-Matthey powder. Several crystals were grown with rare earth concentrations up to 10 000 ppm in the melt. The absorption spectra of these samples revealed that a Eu3+ saturation is attained at concentrations greater than 5000 ppm. For this reason the codoped vanadium crystals (with vanadium contents of 100, 200, 500, and 999 ppm) were obtained while keeping 5000 ppm for rare earths.

The samples temperature was

Eu3+ spectroscopy

Time-resolved line-narrowed fluorescence spectra of the 5D07FJ transitions of Eu3+ in singly doped and vanadium codoped crystals were obtained at 4.2 K by using different resonant excitation wavelengths into the 7F05D0 transition. These spectra were obtained at different time delays after the laser pulse. As an example, Fig. 1a shows the 5D07F0,1,2 spectra at 4.2 K for a BSO crystal doped with 5000 ppm of Eu3+ obtained at 1 ms after the laser pulse by exciting at 579.1 nm. As can be observed

Structural considerations

The existence of several possible sites for rare earths in BSO can be understood on the basis of its structural framework. As shown in Fig. 2, the ideal sillenite structure is built up by Bi-polyhedra connected via common edges to form dimers that link translationally identical [MO(3)4] tetrahedra. Recent neutron diffraction studies [8], [9] have shown the existence of sillenites with M cations having an effective valence lower than four and with a structure being to a great extent O(3) atom

Crystal-field analysis and simulation of the energy level schemes

The phenomenological cf simulation of the Eu3+ energy level scheme can be conducted on the basis of the 7FJM set alone by using only 49 levels out of a total of 3003 of the 4f6 Eu3+ configuration. The use of this truncation is enabled by two facts: firstly, the cf operator mixes only the levels with the same multiplicity, and secondly, the ground 7FJ (J=0 – 6) term is well isolated from the rest of the configuration (about 12 000 cm−1 between 7F6 and 5D0), which renders the mixing of the

Discussion

The five energy level schemes for each of the optically active sites are characterized by strong splittings of the 7F1–6 levels under the cf effect, and in accordance very large cf parameters can be expected to be obtained. The close resemblance of these schemes from B, C, and D active sites in BSO is evidently due to the rather similar coordination of the Eu3+ in each case. From this point of view, differences observed in optical spectra corresponding to the two remaining A and E sites clearly

Conclusions

On the basis of the above arguments and account taken of the great flexibility of the BSO structure, the difficulty to assign particular sites to a rare earth in the BSO structure becomes clear. Nevertheless, regarding the spectroscopic results of Eu3+ ions in BSO it is worthwhile noticing the extreme sensitivity of the Bi polyhedra geometry to the presence of V5+ ions. Moreover, these geometrical changes are very sharply defined, and as the Eu3+ spectroscopy shows, they do not seem to present

Acknowledgements

This work has been financially supported by the Spanish Government CICYT (Ref. MAT97-1009) and Basque Country University (ref: G21/98).

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