Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Fu, Lin"'
Autor:
Vitali B. Prakapenka, Mingqiang Hou, Youjun Zhang, Yingwei Fei, Eran Greenberg, Jung-Fu Lin, Guangtao Liu, Chengwei Zhang, Ronald E. Cohen
Publikováno v:
Physical review letters, vol 125, iss 7
The amount of heat transport from the core, which constrains the dynamics and thermal evolution of the region, depends on the transport properties of iron. Ohta et al.(2016) and Konopkova et al.(2016) measured electrical resistivity and thermal condu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ea6ffb5872558f09e7511721e539e5fd
https://escholarship.org/uc/item/9g09d36c
https://escholarship.org/uc/item/9g09d36c
Publikováno v:
American Mineralogist. 100:2590-2601
Single-crystal elasticity of candidate minerals in the Earth’s mantle, such as that of ferropericlase and bridgmanite, etc., is very important for understanding the seismic observations, geodynamic flow patterns, and testing geochemical and mineral
Autor:
Ji-Jung Kai, Tao Yang, W.H. Liu, King-Fu Lin, C.T. Liu, Can Wang, Huan-Yu Lin, Yilu Zhao, C.H. Hsueh, Tianlong Zhang
Publikováno v:
Materials Science and Engineering: A. 786:139371
Diffusionless martensitic transformation (MT) exerts one of the most significant influences on the mechanical properties of alloys. However, the application of martensitic transformation to improve mechanical performance was seldom involved in the ma
Publikováno v:
Journal of Magnetism and Magnetic Materials. 361:7-11
Co49Pt51 alloy films with strong perpendicular magnetic anisotropy (PMA) have been most often grown on either single crystal or glass substrates with deposition temperature of about 350 °C using Pt/Ru as an underlayer. In contrast, in this study, 5-
Autor:
Russell J. Hemley, Viktor V. Struzhkin, A. A. Mironovich, Stanislav V. Sinogeikin, Pavel G. Naumov, Paul Chow, Yuming Xiao, Alexander G. Gavriliuk, Jung-Fu Lin, Igor S. Lyubutin, Sergey Ovchinnikov
Publikováno v:
Proceedings of the National Academy of Sciences. 110:7142-7147
Ferropericlase [(Mg,Fe)O] is one of the most abundant minerals of the earth’s lower mantle. The high-spin (HS) to low-spin (LS) transition in the Fe 2+ ions may dramatically alter the physical and chemical properties of (Mg,Fe)O in the deep mantle.
Publikováno v:
Transactions of Nonferrous Metals Society of China. 22:2098-2105
The recrystallization kinetics and microstructural evolution of a Ni 3 Al-based single crystal superalloy were presented, especially the different recrystallization behaviors between the dendrite arm and the interdendritic region. The single crystal
Publikováno v:
Scientific Reports
Knowing the elasticity of ferropericlase across the spin transition can help explain seismic and mineralogical models of the lower-mantle including the origin of seismic heterogeneities in the middle to lowermost parts of the lower mantle1,2,3,4. How
Autor:
Andrea Wheat, Jung-Fu Lin
Publikováno v:
Hyperfine Interactions. 207:81-88
Silicate perovskite and ferropericlase are thought to be the primary constituents of the lower mantle, whereas silicate post-perovskite is more likely found in the lowermost mantle. Because these minerals contain certain amounts of iron, their proper
Publikováno v:
Materials Science and Engineering: A. 528:8244-8248
The (Zr 48 Cu 36 Al 8 Ag 8 ) 99.25 Si 0.75 -based bulk metallic glass composite (BMGC) rods ex situ dispersed with Ta particles (with a diameter of 2–4 mm) have been successfully fabricated by suction casting and characterized. These Ta-added BMGCs
Publikováno v:
Mechanics Research Communications. 37:384-388