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Koichiro Inomata

Researcher at Toshiba

Publications -  157
Citations -  3002

Koichiro Inomata is an academic researcher from Toshiba. The author has contributed to research in topics: Amorphous solid & Magnetoresistance. The author has an hindex of 30, co-authored 157 publications receiving 2922 citations. Previous affiliations of Koichiro Inomata include Tokyo Institute of Technology.

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Magnetoresistive element and magnetic memory device

TL;DR: In this paper, a magnetoresistive element has a double tunnel junction having a stacked structure of a first antiferromagnetic layer/a first ferromagnetic layers/a second dielectric layer, and a third antiferrous layer.
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New application of complex magnetic materials to the magnetic refrigerant in an Ericsson magnetic refrigerator

TL;DR: In this paper, a sintered layer structural complex has been prepared, composed of three kinds of RAl2.15 layers, where R's are rare earth atoms, from specific heat measurements made on this complex, its entropy and entropy change have been determined.
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Preferred crystal orientation of cobalt ferrite thin films induced by ion bombardment during deposition

TL;DR: In this article, strong crystallization enhancement and preferred crystallographic orientation were observed as the effects of ion bombardment. But the mechanism of crystal orientation is thought to have a close relationship with the preferential sputtering of oxygen by Ar+−ion impact.
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Magnetoresistance associated with antiferromagnetic interlayer coupling spaced by a semiconductor in Fe/Si multilayers.

TL;DR: In this article, a multilayer Fe/Si films with constant Fe thickness (2.6 nm) and variable Si thickness were investigated and negative magnetoresistance was observed and two different temperature dependences were found as a function of Si thickness.
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Two oscillatory behaviors as functions of ferromagnetic layer thickness in Fe/Cr(100) multilayers.

TL;DR: Oscillatory magnetoresistance as a function of the Fe layer thickness has been found in Fe/Cr(100) multilayers deposited on MgO(100), mainly attributed to an oscillatory interlayer exchange coupling between adjacent Fe layers as discussed by the authors.