Jul 2 – 6, 2018
Žofín Palace
Europe/Prague timezone

P1.2006 XFEL observation of shock-compressed highly oriented graphite

Jul 2, 2018, 2:00 PM
2h
Mánes

Mánes

Masarykovo nábřeží 1, 110 00 Praha 1

Speaker

Norimasa Ozaki

Description

See the full Abstract at http://ocs.ciemat.es/EPS2018ABS/pdf/P1.2006.pdf XFEL observation of shock-compressed highly oriented graphite Norimasa Ozaki1,2 , Kento Katagiri1 , Ryo Hazama1 , Takahiro Matsuoka3 , Takeshi Matsuoka4 , Kohei Miyanishi2 , Yuhei Umeda1 , Yusuke Seto5 , Yuichi Inubushi6 , Toshinori Yabuuchi6 , Tadashi Togashi6 , Makina Yabashi7 , and Ryosuke Kodama1,2 1 Graduate School of Engineering, Osaka University, Suita, Japan 2 Institute of Laser Engineering, Osaka University, Suita, Japan 3 Graduate School of Engineering, Gifu University, Gifu, Japan 4 Open and Transdisciplinary Research Initiative, Osaka Univeristy, Suita, Japan 5 Graduate School of Science, Kobe University, Kobe, Japan 6 JASRI/SPring-8, Sayo, Japan 7 RIKEN SPring-8 Center, Sayo, Japan High power laser-driven shock is widely used to investigate the states and behaviors of ma- terial in extreme conditions associated with warm dense matter (WDM) physics, planetary sci- ences, and inertial fusion energy research[1]. At the high pressure and extremely high strain rate conditions, it is known that mechanical properties and behaviors of material can change significantly more than expected. Such properties change is influenced by the micro-structure of material. We here present experimental results on X-ray free electron laser (XFEL) observa- tions of shock-compressed highly oriented materials at the SACLA-HEDS platform [2, 3, 4]. We shock compressed highly oriented pyrolytic graphite (HOPG) samples along the [002] ori- entation using a 3-4 ns optical laser pulse and observed the lattices under the shock compression using the XFEL pulse with changing the time delay between the optical and X-ray pulses. Once the HOPG interlayers were compressed uniaxially up to ∼20% or more, and then a high pressure form of carbon was created on picosecond time scale above ∼20 GPa pressures. This sequence might be different from reported very recently [5, 6]. This work was supported by a Grant-in-Aid for Scientific Research, KAKENHI (Grant No. 15K13609 and 16H02246), the Genesis Research Institute, Inc. (Konpon-ken, TOYOTA), and XFEL Priority Strategy Program at Osaka Univ. from the MEXT. References [1] N. Ozaki, W. J. Nellis, T. Mashimo et al., Sci. Rep. 6, 26000 (2016). [2] T. Pikuz, A. Faenov, T. Matsuoka et al., Sci. Rep. 5, 17713 (2015). [3] N. J. Hartley, N. Ozaki, T. Matsuoka et al., Appl. Phys. Lett. 110, 071905 (2017). [4] B. Albertazzi, N. Ozaki, V. Zhakhovsky et al., Sci. Adv. 3, e1602705 (2017). [5] D. Kraus, A. Ravasio, M. Gauthier et al., Nat. Comm. 3, e1602705 (2017). [6] S. J. Turneaure, S. M. Sharma, T. J. Volz et al., Sci. Adv. 3, eaao3561 (2017).

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