O-013 Communicating malapposition and its impact on aneurysm healing

Autor: John Wainwright, Robert M. King, T Tamaura, Erin T. Langan, Frédéric Clarençon, Matthew J. Gounis, Ajit S. Puri, Miklos G. Marosfoi, Olivia W. Brooks

Publikováno v: Oral Abstracts.

Introduction/Purpose Malapposition has a negative correlation to aneurysm healing 1 . We examine the influence of malapposition communicating into the aneurysm, and the effect of malapposition incidence at any position along the parent artery on heal

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::bbea3e5834104c96d0b0352910a64b5e
https://doi.org/10.1136/neurintsurg-2017-snis.13

The CALET, CALorimetric Electron Telescope, mission for the International Space Station

Autor: K. Mizutani, T. Tamaura, Y. Uchihori, H. Murakami, Hisashi Kitamura, Kenji Yoshida, Katsuaki Kasahara, M. Shibata, T. Yuda, Masahiro Takayanagi, K. Hibino, N. Tateyama, Yoshitaka Saito, Jun Nishimura, Tadashi Kobayashi, Takamasa Yamagami, Yoshiko Komori, T. Yamashita, K. Anraku, Y. Katayose, Shoji Torii, F. Makino, T. Kashiwagi

Publikováno v: Nuclear Physics B - Proceedings Supplements. 113:103-110

The CALorimetric Electron Telescope, CALET, mission is proposed for the Japanese Experiment Module Exposure Facility of the International Space Station. Major goals of the mission are precise measurements of the electrons in a few GeV - 10 TeV and th

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ee085fe324adeb739ee5d8eb0c872c2f
https://doi.org/10.1016/s0920-5632(02)01828-5

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The solar-driven coal/Fe3O4 redox system

Autor: Masamichi Tsuji, K. Ehrensberger, Aldo Steinfeld, T. Tamaura

Publikováno v: Scopus-Elsevier
Journal de Physique IV Proceedings
Journal de Physique IV Proceedings, EDP Sciences, 1997, 07 (C1), pp.C1-685-C1-686. ⟨10.1051/jp4:19971281⟩

The solar-driven endothermic reaction of coal and magnetite was studied for mixing solar and fossil energies. The overall reaction can be represented by CH x + Fe 3 O 4 = CO + 3FeO+1/2xH 2 where x depends on the coal(x= 0.2 in our study). Laboratory

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http://www.scopus.com/inward/record.url?eid=2-s2.0-0031096912&partnerID=MN8TOARS

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