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Matsuo, Kiyomi,Murata, Tomoyuki,Koga, Takanori,Kubo, Atsuko,Yoshida, Yuichi,Karakawa, Yosuke,Kawaguchi, Hiroshi,Tanaka, Toru,Masaki, Jun,Taketomi, Toshikatsu,Kitajima, Takeo Rehabilitation Engineering And Assistive Technolog 2008 재활복지공학회논문지 Vol.2 No.1
In this paper, I will report the cases of children who are able to study at kindergarten or elementary school because they learned how to move by themselves using a moving aid before school age, and I will also discuss the development of a mobility device which allows severely disabled preschoolers to practice moving around by themselves safely and easily at home and institutions.
Kiyomi Matsuo,Tomoyuki Murata,Takanori Koga,Atsuko Kubo,Yuichi Yoshida,Yosuke Karakawa,Hiroshi Kawaguchi,Toru Tanaka,Jun Masaki,Toshikatsu Taketomi,Takeo Kitajima 한국재활복지공학회 2008 재활복지공학회논문지 Vol.2 No.1
In this paper,I will report the cases of children who are able to study at kindergarten or elementary school because they learned how to move by themselves using a moving aid before school age, and I will also discuss the development of a mobility device which allows severely disabled preschoolers to practice moving around by themselves safely and easily at home and institutions.
Effects of Mechanical Rotation and Vibration on Spin Currents
Mamoru Matsuo,Jun’ichi Ieda,Sadamichi Maekawa,Eiji Saitoh 한국물리학회 2013 THE JOURNAL OF THE KOREAN PHYSICAL SOCIETY Vol.62 No.10
We discuss theoretically the generation of spin currents in both rotationally and linearly accelerated systems. The spin-orbit interaction modified by inertial effects is derived from the low energy limit of the generally covariant Dirac equation. It is shown that the spin-orbit interaction is responsible for the generation of spin currents by mechanical rotation and vibration. We also study effects of impurity scattering on the mechanically induced spin current, and calculate the spin accumulation by solving the spin diffusion equation with the spin-source term originating from the inertial effects.
Kiyomi Matsuo,Tomoyuki Murata,Takanori Koga,Atsuko Kubo,Yuichi Yoshida,Yosuke Karakawa,Hiroshi Kawaguchi,Tom Tanaka,Jun Masaki,Toshikatsu Taketorni,Takeo Kitajima 한국재활복지공학회 2008 한국재활복지공학회 학술대회논문집 Vol.2008 No.11
In this paper, I will report the cases of children who are able to study at kindergarten or elementary school because they learned how to move by themselves using a moving aid before school age, and I will also discuss the development of a mobility device which allows severely disabled preschoolers to practice moving around by themselves safely and easily at home and institutions.
Isezaski, Nobuhiro,Matsuo, Jun Korean Society of Earth and Exploration Geophysici 2009 지구물리와 물리탐사 Vol.12 No.1
On Aogashima Island, a volcanic island located in the southernmost part of the Izu Seven Islands Chain, vector magnetic anomalies were obtained in a helicopter-borne magnetic survey. The purpose of this study was to understand the volcanic structure of Aogashima Island in order to mitigate future disasters. Commonly, to obtain the magnetic structure of a volcanic island, total intensity anomalies (TIA) have been used, even though they have intrinsic errors that have not been evaluated correctly. Because the total intensity magnetic anomaly (TIA) is not a physical value, it does not satisfy Maxwell's Equations, Laplace's Equation, etc., and so TIA is not suitable for any physical analyses. In addition, it has been conventionally assumed that TIA is the same as the projected total intensity anomaly vector (PTA) for analyses of TIA. However, the effect of the intrinsic error ($\varepsilon_T$ = TIA.PTA) on the analysis results has not been taken into account. To avoid such an effect, vector magnetic anomalies were measured so that a reliable analysis of Aogashima Island magnetization could be carried out. In this study, we evaluated the error in TIA and used vector anomalies to avoid this erroneous effect, in the process obtaining reliable analysis results for 3D, vector magnetization distributions. An area of less than 1 A/m magnetization was found in the south-west part of Aogashima Island at the depth of 1.2 km. Taking the location of fumarolic activity into consideration, the lower-magnetization area was expected to be the source of that fumarolic activity of Aogashima Island.