Core–hole spectroscopies such as x-ray photoelectron spectroscopy (XPS) and high-resolution electron energy loss spectroscopy (HR-EELS) in combination with multiplet calculation are important tools to elucidate the electronic structure of transition metal compounds. This work presents a comparison between the electronic structure obtained by XPS and HR-EELS for polycrystalline perovskite-type Ba0.9Ca0.1Ti0.9Zr0.1O3. Raman analysis suggests that Ca2+ cations could partly occupy the Ti4+ cations in the B-site of a perovskite structure with the tetragonal phase. A multiplet structure was determined by XPS for Ti 2p and by HR-EELS for Ca L2,3 and Ti L2,3 edges. Octahedral (Oh) symmetry in the crystal field (CF) effects reproduces the local distortion of TiO6 octahedra. The charge transfer (CT) effects were also considered to reproduce L3-edge EELS shoulders and the satellite in the Ti 2p XPS region. CF and CT parameters, 10 Dq, (charge transfer energy) Δ, and (Coulomb repulsion energy) Udd, are reported for future reference. The broadening of the Ti L2-edge suggests the presence of the Coster–Kronig electron decay process. Multiplet calculation in Oh symmetry for the Ca L2,3-edge could support the Raman interpretation.
The synergetic role of the phase transitions taking place between long-range, polar ordered, ferroelectric phases in lead-free ceramics with Ba 0.85 Ca 0.15 Ti 0.90 Zr 0.10 O 3 composition on their electromechanical behavior has been analyzed. Synchrotron X-ray diffraction (XRD) and Rietveld analysis revealed a room temperature coexistence of rhombohedral (R), tetragonal (T), and orthorhombic (O) phases. The proportions of these phases in the investigated samples vary from the order of 42R-45T-13O in the nonpolarized condition to an estimated 65R-26T-9O in the polarized, significantly textured sample. These characteristics are related to the complex ferroelectric domain distribution that electron scanning microscopy exposes, which favors domain wall mobility and provides a large extrinsic contribution to the electromechanical response of the material. A confocal Raman spectroscopy and imaging study was carried out on both unpoled and poled samples and reveals that, under the action of the electric field, the E(LO 3 ) + A 1 (LO 2 ) + E(TO 4 ) mode of the Raman spectra shifts from 517.8 to 516.4 cm −1 , indicating the lengthening of the distance between B 5+ type ions and their coordinated oxygens for the poled samples. Besides, the mentioned spatially resolved model of the Raman spectra shows a narrower distribution in the poled sample, compatible with the strong texture revealed by XRD. Photoacoustic signal evolution with the temperature, in agreement with the dielectric permittivity curve, reveals the diffusive character of the phase transition taking place at 40 °C between the long-range polar ordered phase at low temperature and the high temperature one, which influences the phase coexistence at room temperature. Moreover, an evaluation of the resultant complex piezoelectric, dielectric, and elastic coefficients at resonance, including all losses, is presented. The obtained results indicate the remarkable electromechanical activity, its anisotropy, and the soft character of this ferro-piezo-electric type ceramic.
Calcium sulfate (CaSO4) is one of the most common evaporites found in the earth’s crust. It can be found as four main variations: gypsum (CaSO4∙2H2O), bassanite (CaSO4∙0.5H2O), soluble anhydrite, and insoluble anhydrite (CaSO4), being the key difference the hydration state of the sulfate mineral. Naica giant crystals’ growth starts from a supersaturated solution in a delicate thermodynamic balance close to equilibrium, where gypsum can form nanocrystals able to grow up to 11–12 m long. The growth rates are reported to be as slow as (1.4 ± 0.2) × 10−5 nm/s, taking thousands of years to form crystals with a unique smoothness and diaphaneity, which may or may not include solid or liquid inclusions. Conservation efforts can be traced back to other gypsum structures found prior to Naica’s. Furthermore, in the last two decades, several authors have explored the unique requirements in which these crystals grow, the characterization of their environment and microclimatic conditions, and the prediction of deterioration scenarios. We present a state-of-the-art review on the mentioned topics. Beyond the findings on the origin, in this work we present the current state and the foreseeable future of these astounding crystals.
The Material Properties Open Database (MPOD, http://mpod.cimav.edu.mx) is a functional element of the web-based open databases system linked with crystallography. MPOD delivers single-crystal tensor properties in several representations, ranging from numerical matrices to 3D printing. Longitudinal moduli surfaces can be displayed in computers as well as in smart cell phones. Properties are stored as '.mpod' files. IUCr formatting standards (CIF) are followed. The original published paper containing the data is cited. Structural and experimental information is also registered and linked. 'Coupling properties', say piezo-effects and magnetoelectricity, represent interactions linking different subsystems in a material. Currently, piezoelectricity occupies a significant fraction of cases in MPOD. The implications of crystal symmetry in piezoelectricity are systematically taken into account. Matrices' elements and longitudinal moduli surfaces are checked for consistency with the Neumann principle. The inclusion of magnetoelectric axial tensors introduces exciting features into MPOD.
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