Gradient Structure Formation in the Subsurface Layers of a ZrO2(Y)-Al2O3Ceramic Material Under Low-Energy, High-Current Electron Beams; Russian Physics Journal; Vol. 57, iss. 6

Bibliographic Details
Parent link:Russian Physics Journal.— , 1965-
Vol. 57, iss. 6.— 2014.— [P. 738-741]
Main Author: Surzhikov A. P. Anatoly Petrovich
Corporate Author: Национальный исследовательский Томский политехнический университет Институт неразрушающего контроля Проблемная научно-исследовательская лаборатория электроники, диэлектриков и полупроводников
Other Authors: Frangulyan (Franguljyan) Т. S. Tamara Semenovna, Gyngazov (Ghyngazov) S. A. Sergey Anatolievich
Summary:Title screen
The role of a low-energy, high-current electron beam on the microstructural state of subsurface layers of a composite ZrO2(Y)-Al2O3 ceramic material is investigated. It is found out that irrespective of the initial porosity of the ceramic material an electron beam treatment gives rise to formation of a characteristic microstructure in the subsurface layers of the specimens. Grains are observed to orient towards the specimen surface. The layers immediately below the surface are characterized by finer grains than those in the bulk.
Режим доступа: по договору с организацией-держателем ресурса
Language:English
Published: 2014
Subjects:
Online Access:http://dx.doi.org/10.1007/s11182-014-0298-3
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=647206

MARC

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200 1 |a Gradient Structure Formation in the Subsurface Layers of a ZrO2(Y)-Al2O3Ceramic Material Under Low-Energy, High-Current Electron Beams  |f A. P. Surzhikov, Т. S. Frangulyan (Franguljyan), S. A. Gyngazov (Ghyngazov) 
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330 |a The role of a low-energy, high-current electron beam on the microstructural state of subsurface layers of a composite ZrO2(Y)-Al2O3 ceramic material is investigated. It is found out that irrespective of the initial porosity of the ceramic material an electron beam treatment gives rise to formation of a characteristic microstructure in the subsurface layers of the specimens. Grains are observed to orient towards the specimen surface. The layers immediately below the surface are characterized by finer grains than those in the bulk. 
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463 |t Vol. 57, iss. 6  |v [P. 738-741]  |d 2014 
610 1 |a электронный ресурс 
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