Zobrazeno 1 - 10
of 90
pro vyhledávání: '"Wenli Bi"'
Publikováno v:
AIP Advances, Vol 14, Iss 6, Pp 065216-065216-7 (2024)
We report on a novel TaNbZrHfTi-based high entropy alloy (HEA) which demonstrates distinctive dual-phase superconductivity. The HEA was synthesized under high pressures and high temperatures starting from a ball milled mixture of elemental metals in
Externí odkaz:
https://doaj.org/article/2e5fdcc551304509a669b3d82fa15641
Publikováno v:
Catalysts, Vol 14, Iss 7, p 456 (2024)
Catalytic conversion of CO2 to CO via the reverse water gas shift (RWGS) reaction has been identified as a promising approach for CO2 utilization and mitigation of CO2 emissions. Bare Pt shows low activity for the RWGS reaction due to its low oxophil
Externí odkaz:
https://doaj.org/article/ca8bf2dbf83640b2b3fae98c6ffe769a
Autor:
Wenli Bi, Trenton Culverhouse, Zachary Nix, Weiwei Xie, Hung-Ju Tien, Tay-Rong Chang, Utpal Dutta, Jiyong Zhao, Barbara Lavina, Esen E. Alp, Dongzhou Zhang, Jingui Xu, Yuming Xiao, Yogesh K. Vohra
Publikováno v:
npj Quantum Materials, Vol 7, Iss 1, Pp 1-8 (2022)
Abstract High pressure is an effective tool to induce exotic quantum phenomena in magnetic topological insulators by controlling the interplay of magnetic order and topological state. This work presents a comprehensive high-pressure study of the crys
Externí odkaz:
https://doaj.org/article/604de6c3344c427a976d500ec6154f5b
Autor:
Jin Liu, Qingyang Hu, Wenli Bi, Liuxiang Yang, Yuming Xiao, Paul Chow, Yue Meng, Vitali B. Prakapenka, Ho-Kwang Mao, Wendy L. Mao
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-8 (2019)
Iron oxides prevail in the deep Earth, at extreme pressures and temperatures, with different stoichiometries than in ambient conditions. Here, high-pressure synchrotron X-ray spectroscopic measurements reveal the oxidation states of Fe and O in iron
Externí odkaz:
https://doaj.org/article/2e4fdc4ab4454d76ae993f43566079ae
Autor:
Jiachao Liu, Susannah M. Dorfman, Feng Zhu, Jie Li, Yonggang Wang, Dongzhou Zhang, Yuming Xiao, Wenli Bi, E. Ercan Alp
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
Bridgmanite is the most abundant mineral in the lower mantle and therefore is crucial to interpreting geophysical observations and models. Here, the authors show that ferric-iron-only bridgmanite Fe3+ undergoes a spin transition at 43–53 GPa at 300
Externí odkaz:
https://doaj.org/article/81f5966ea09645f1acd9ca8f6867a268
Autor:
Jin Liu, Nicolas Dauphas, Mathieu Roskosz, Michael Y. Hu, Hong Yang, Wenli Bi, Jiyong Zhao, Esen E. Alp, Justin Y. Hu, Jung-Fu Lin
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-6 (2017)
Terrestrial basalts have a unique iron isotopic signature taken as fingerprints of core formation. Here, high pressure studies show that force constants of iron bonds increase with pressure similarly for silicate and metals suggesting interplanetary
Externí odkaz:
https://doaj.org/article/2f4834cb57434e2698e38dcc342e26ce
Autor:
Shuyuan Huyan, Ryan, Dominic H., Slade, Tyler J., Lavina, Barbara, Jose, Greeshma, Haozhe Wang, Wilde, John M., Ribeiro, Raquel A., Jiyong Zhao, Weiwei Xie, Wenli Bi, Alp, Esen E., Bud'ko, Sergey L., Canfield, Paul C.
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America; 12/26/2023, Vol. 120 Issue 52, p1-8, 21p
Autor:
Byeongkwan Ko, Eran Greenberg, Vitali Prakapenka, E. Ercan Alp, Wenli Bi, Yue Meng, Dongzhou Zhang, Sang-Heon Shim
Publikováno v:
Nature. 611:88-92
Autor:
Mathieu Roskosz, Nicolas Dauphas, Justin Hu, Michael Y. Hu, Daniel R. Neuville, Dennis Brown, Wenli Bi, Nicole X. Nie, Jiyong Zhao, Esen E. Alp
Publikováno v:
Geochimica et Cosmochimica Acta. 321:184-205
Autor:
Zhe Zhang, Fang-Zhen Teng, Corliss Kin I Sio, Jiyong Zhao, S. M. Aarons, Jennika Greer, Michael J. Krawczynski, Frank S. Spear, Hao Zeng, Kelsey B. Prissel, Xi Chen, Nicolas Dauphas, J. Y. Hu, N. X. Nie, Anat Shahar, Wenli Bi, Da Wang, Heng-Ci Tian, M. Roskosz, Philipp R. Heck, Esen E. Alp, Michael Y. Hu
Publikováno v:
Geochimica et Cosmochimica Acta. 302:18-45
Interpreting isotopic signatures documented in natural rocks requires knowledge of equilibrium isotopic fractionation factors. Here, we determine equilibrium Fe isotope fractionation factors between several common rock-forming minerals using a compar