H
Hong-Shuo Li
Researcher at University of New South Wales
Publications - 91
Citations - 2351
Hong-Shuo Li is an academic researcher from University of New South Wales. The author has contributed to research in topics: Magnetization & Magnetic anisotropy. The author has an hindex of 25, co-authored 91 publications receiving 2260 citations. Previous affiliations of Hong-Shuo Li include Trinity College, Dublin & Commonwealth Scientific and Industrial Research Organisation.
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Evidence in rare‐earth (R)–transition metal (M) intermetallics for a systematic dependence of R‐M exchange interactions on the nature of the R atom
TL;DR: In this paper, the molecular field coefficient nRM has been obtained for a number of series of rare earth-transition metal compounds, and the analysis reveals that nRM is not a constant going across a given serie.
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Intrinsic magnetic properties of the iron-rich ThMn12-structure alloys R(Fe11Ti); R=Y, Nd, Sm, Gd, Tb, Dy, Ho, Er, Tm and Lu
TL;DR: In this paper, the spin reorientation transitions for rare earths with a negative second-order Stevens coefficient alpha J(Nd, Tb, Dy) were derived to account for the transitions in a consistent way.
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Structural properties of a novel magnetic ternary phase: Nd3(Fe1−xTix)29 (0.04 ≤ x≤ 0.06)
TL;DR: In this paper, a structural determination of the new magnetic ternary rare-earth iron-rich intermetallic Nd3(Fe1−xTix)29 phase was carried out by means of powder X-ray diffraction on a Nd0.955Ti0.045) sample.
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New rare‐earth intermetallic phases R3(Fe,M)29Xn: (R=Ce, Pr, Nd, Sm, Gd; M=Ti, V, Cr, Mn; and X=H, N, C) (invited)
TL;DR: In this article, the authors reviewed the work carried out to date on the 3:29 compounds and showed improved magnetic properties after interstitial modification with H or N; in particular, room temperature coercivity has been reported in Sm3(Fe,Ti)29N5, making this compound a candidate for possible permanent magnet applications.
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Magnetization of a Dy(Fe11Ti) single crystal.
TL;DR: Spin reorientation observed in the other members of the {ital R}(Fe{sub 11}Ti) ({ital R]==rare earth) series, except those in Tb( Fe{sub 12}Ti), are explained by the same crystal-field coefficients.