1987
DOI: 10.1007/bf00307991
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Investigation of copper minerals by NQR: Crystallochemistry, electronic structure, lattice dynamics

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Cited by 25 publications
(16 citation statements)
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“…The effect is related to the increased occupation of the 3d shell forced by the orbital potential, which makes the charge distribution of the 3d shell more spherical, when accommodating an increased number of electrons. The GGA calculations result in an EFG of about −5 ϫ 10 21 V / m 2 , which is only half of the experimental value of 10.6ϫ 10 21 V / m 2 ͑only the magnitude of the EFG can be measured͒ 34. However, with GGA+ U and a large U eff equal to 13.6 eV the calculated value ͑−10ϫ 10 21 V / m 2 ͒ comes close to the experimental EFG.Considering our results it is rather clear that the GGA + U method improves the electronic structure compared to calculations with GGA only.…”
mentioning
confidence: 85%
“…The effect is related to the increased occupation of the 3d shell forced by the orbital potential, which makes the charge distribution of the 3d shell more spherical, when accommodating an increased number of electrons. The GGA calculations result in an EFG of about −5 ϫ 10 21 V / m 2 , which is only half of the experimental value of 10.6ϫ 10 21 V / m 2 ͑only the magnitude of the EFG can be measured͒ 34. However, with GGA+ U and a large U eff equal to 13.6 eV the calculated value ͑−10ϫ 10 21 V / m 2 ͒ comes close to the experimental EFG.Considering our results it is rather clear that the GGA + U method improves the electronic structure compared to calculations with GGA only.…”
mentioning
confidence: 85%
“…Earlier studies of copper sulphides and oxides [6] have shown that the lattice contribution to the EFG is the dominant for monovalent copper. Taking Ÿ -13.8 [7], the calculated value of the lattice contribution to the 63Cu NQR frequency appeared to be equal to 2.3 MHz, about two times less than the observed one.…”
Section: Nqr Frequenciesmentioning
confidence: 99%
“…The 63,65 Сu NMR spectrum in a local field for samples of chalcopyrite (CuFeS 2 ) mineral was investigated in [3,4] at temperatures 77-300 K. It comprised six resonant lines and was formed by two widespread copper isotopes ( 63 Cu and 65 Cu) existing in the location of resonant nuclei in a local magnetic field of ~1.6 T. The spectrum of each copper isotope had three resonant lines (nuclear spins of both isotopes were I = 3/2) and consisted of the central line and two quadrupole satellites (Fig. 1a).…”
Section: Resultsmentioning
confidence: 99%