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Yonggang G. Yu

Researcher at University of Minnesota

Publications -  20
Citations -  826

Yonggang G. Yu is an academic researcher from University of Minnesota. The author has contributed to research in topics: Phase transition & Ringwoodite. The author has an hindex of 14, co-authored 19 publications receiving 729 citations. Previous affiliations of Yonggang G. Yu include Virginia Tech & University of Colorado Boulder.

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Thermodynamic Properties and Phase Relations in Mantle Minerals Investigated by First Principles Quasiharmonic Theory

TL;DR: A review of the essential first-principles approach used to investigate solids at high temperatures and pressures, summarize their performance for mantle minerals, and point to critical results that have stirred us in the current research path as discussed by the authors.
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Design and discovery of a novel half-Heusler transparent hole conductor made of all-metallic heavy elements

TL;DR: The search theoretically for electronic structures that simultaneously lead to optical transparency while accommodating intrinsic defect structures that produce uncompensated free holes leads to the prediction of a stable, never before synthesized TaIrGe compound made of all-metal heavy atom compound.
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Spin transition in (Mg,Fe)SiO3 perovskite under pressure

TL;DR: In this article, a density functional study of the pressure-induced spin transition in ferrous iron (Fe 2+ ) at the A site in MgSiO3 perovskite was presented.
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First principles investigation of the postspinel transition in Mg2SiO4

TL;DR: In this paper, the authors investigated the dissociation of ringwoodite into MgO periclase and MgSiO3 perovskite using quasi-harmonic free energy computations within the local density approximation (LDA) and generalized gradient approximation (GGA).
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Spin crossover of iron in aluminous MgSiO3 perovskite and post-perovskite

TL;DR: In this article, the authors investigated how aluminum affects the spin crossover of iron in MgSiO3 perovskite (Pv) and post-perovskites (Ppv), the major mineral phases in the Earth's lower mantle.