Electronic structure, chemical bonding and X-ray photoelectron spectra of heavy rare-earth oxides

1985 ◽  
Vol 59 (1) ◽  
pp. 7-14 ◽  
Author(s):  
M. V. Ryzhkov ◽  
V. A. Gubanov ◽  
Yu. A. Teterin ◽  
A. S. Baev
Keyword(s):  
Electronic Structure ◽  
Rare Earth ◽  
Chemical Bonding ◽  
Rare Earth Oxides ◽  
Photoelectron Spectra ◽  
Heavy Rare Earth ◽  
X Ray

Electronic structure, chemical bonding and X-ray photoelectron spectra of light rare-earth oxides

1985 ◽  
Vol 59 (1) ◽  
pp. 1-6 ◽  
Author(s):  
M. V. Ryzhkov ◽  
V. A. Gubanov ◽  
Yu. A. Teterin ◽  
A. S. Baev
Keyword(s):  
Electronic Structure ◽  
Rare Earth ◽  
Chemical Bonding ◽  
Rare Earth Oxides ◽  
Photoelectron Spectra ◽  
Light Rare Earth ◽  
X Ray

Equiatomic indides REIrIn (RE=La, Pr, Nd, Er–Yb) – Crystal and electronic structure

2017 ◽  
Vol 72 (9) ◽  
pp. 631-638 ◽  
Author(s):  
Nazar Zaremba ◽  
Ihor Muts ◽  
Viktor Hlukhyy ◽  
Sebastian Stein ◽  
Ute Ch. Rodewald ◽  
...  
Keyword(s):  
Electronic Structure ◽  
Rare Earth ◽  
Solid Solutions ◽  
Chemical Bonding ◽  
Electronic Structure Calculations ◽  
Ionic Interactions ◽  
X Ray ◽  
Metallic Bonding ◽  
Structure Calculations ◽  
Crystal And Electronic Structure

AbstractThe equiatomic rare earth iridium indidesREIrIn (RE=La, Pr, Nd, Er–Yb) were synthesized by reaction of the elements in induction or muffle furnaces and were characterized through X-ray powder patterns. The structures of LaIr0.86In1.14, PrIr0.89In1.11, NdIr0.94In1.06, ErIrIn (all ZrNiAl type,P6̅2m), and YbIrIn (TiNiSi type,Pnma) were refined from single crystal X-ray diffractometer data. Refinements of the occupancy parameters revealed small degrees of solid solutions with indium substitution on the iridium sites. Chemical bonding analyses and electronic structure calculations indicate the dominance of metallic bonding in addition to partial ionic interactions between the cations and polyanions, as well as covalent contributions between the indium and iridium atoms.

Extended X-Ray Absorption Fine Structures and Chemical Shifts for the Heavy Rare-Earth Oxides

1977 ◽  
Vol 82 (2) ◽  
pp. 603-609 ◽  
Author(s):  
S. N. Gupta ◽  
V. P. Vijayavargiya ◽  
B. D. Padalia ◽  
B. C. Tripathi ◽  
M. N. Ghatikar
Keyword(s):  
Rare Earth ◽  
Chemical Shifts ◽  
Rare Earth Oxides ◽  
Heavy Rare Earth ◽  
X Ray ◽  
Absorption Fine ◽  
Fine Structures ◽  
X Ray Absorption

X-ray photoelectron spectra and electronic structure of rare-earth orthovanadates

1981 ◽  
Vol 39 (1) ◽  
pp. 7-14 ◽  
Author(s):  
M.V. Ryzhkov ◽  
S.P. Kostikov ◽  
I.K. Ivanov ◽  
V.A. Gubanov
Keyword(s):  
Electronic Structure ◽  
Rare Earth ◽  
Photoelectron Spectra ◽  
X Ray ◽  
Rare Earth Orthovanadates

Rare-earth crystal chemistry of thalénite-(Y) from different environments

2018 ◽  
Vol 82 (2) ◽  
pp. 313-327
Author(s):  
Markus B. Raschke ◽  
Evan J. D. Anderson ◽  
Jason Van Fosson ◽  
Julien M. Allaz ◽  
Joseph R. Smyth ◽  
...  
Keyword(s):  
Rare Earth ◽  
Rare Earth Element ◽  
Earth Element ◽  
Spatial Scales ◽  
Structure Refinement ◽  
X Ray Diffraction ◽  
Heavy Rare Earth ◽  
Heavy Rare Earth Element ◽  
X Ray ◽  
Golden Horn

ABSTRACTThalénite-(Y), ideally Y3Si3O10F, is a heavy-rare-earth-rich silicate phase occurring in granite pegmatites that may help to illustrate rare-earth element (REE) chemistry and behaviour in natural systems. The crystal structure and mineral chemistry of thalénite-(Y) were analysed by electron microprobe analysis, X-ray diffraction and micro-Raman spectroscopy from a new locality in the peralkaline granite of the Golden Horn batholith, Okanogan County, Washington State, USA, in comparison with new analyses from the White Cloud pegmatite in the Pikes Peak batholith, Colorado, USA. The Golden Horn thalénite-(Y) occurs as late-stage sub-millimetre euhedral bladed transparent crystals in small miarolitic cavities in an arfvedsonite-bearing biotite granite. It exhibits growth zoning with distinct heavy-rare-earth element (HREE) vs. light-rare-earth element (LREE) enriched zones. The White Cloud thalénite-(Y) occurs in two distinct anhedral and botryoidal crystal habits of mostly homogenous composition. In addition, minor secondary thalénite-(Y) is recognized by its distinct Yb-rich composition (up to 0.8 atoms per formula unit (apfu) Yb). Single-crystal X-ray diffraction analysis and structure refinement reveals Y-site ordering with preferential HREE occupation of Y2 vs. Y1 and Y3 REE sites. Chondrite normalization shows continuous enrichment of HREE in White Cloud thalénite-(Y), in contrast to Golden Horn thalénite-(Y) with a slight depletion of the heaviest REE (Tm, Yb and Lu). The results suggest a hydrothermal origin of the Golden Horn miarolitic thalénite-(Y), compared to a combination of both primary magmatic followed by hydrothermal processes responsible for the multiple generations over a range of spatial scales in White Cloud thalénite-(Y).

Crystal structure characterization and electronic structure of a rare-earth-containing Zintl phase in the Yb–Al–Sb family: Yb3AlSb3

2021 ◽  
Vol 77 (6) ◽  
Author(s):  
Rongqing Shang ◽  
An T. Nguyen ◽  
Allan He ◽  
Susan M. Kauzlarich
Keyword(s):  
Crystal Structure ◽  
Electronic Structure ◽  
Rare Earth ◽  
Electronic Structure Calculations ◽  
Structure Characterization ◽  
Charge Balance ◽  
X Ray Diffraction ◽  
Zintl Phase ◽  
X Ray ◽  
Structure Calculations

A rare-earth-containing compound, ytterbium aluminium antimonide, Yb3AlSb3 (Ca3AlAs3-type structure), has been successfully synthesized within the Yb–Al–Sb system through flux methods. According to the Zintl formalism, this structure is nominally made up of (Yb2+)3[(Al1−)(1b – Sb2−)2(2b – Sb1−)], where 1b and 2b indicate 1-bonded and 2-bonded, respectively, and Al is treated as part of the covalent anionic network. The crystal structure features infinite corner-sharing AlSb4 tetrahedra, [AlSb2Sb2/2]6−, with Yb2+ cations residing between the tetrahedra to provide charge balance. Herein, the synthetic conditions, the crystal structure determined from single-crystal X-ray diffraction data, and electronic structure calculations are reported.

scholarly journals Chemical Bonding and the Sulfur K X-Ray Spectrum

1965 ◽  
Vol 9 ◽  
pp. 354-364 ◽  
Author(s):  
D. W. Wilbur ◽  
J. W. Gofman
Keyword(s):  
Electronic Structure ◽  
Single Crystal ◽  
Organic Compounds ◽  
Sulfur Atom ◽  
Chemical Bonding ◽  
Proportional Counter ◽  
Pulse Height ◽  
X Ray ◽  
Pulse Height Analysis ◽  
Chemical States

AbstractAn investigation has been made of the relative Kβ intensities in different chemical states of the sulfur atom using the Kα lines, with appropriate corrections, to provide the intensity standards. Both inorganic and organic compounds were included in the study. The data for each compound appear to be reliable to about ± 0.5%, while the whole series of compounds shows a variation greater than 20% in the corrected Kβ/Kα ratios. Energies were also measured, particularly the Kα energies, and their shifts were studied relative to the Kβ, intensity shifts. The work was done with a plane, single-crystal, helium-path spectrometer with proportional counter and pulse-height analysis for detection. The results are indicative of the usefulness of the method both in clarifying an uncertain chemical state and in studying the electronic structure of the bonded atom.

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