КФУ. Карточка публикации. Eigen-oscillations of a transversely isotropic elastic layer attached to an isotropic half-space

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EIGEN-OSCILLATIONS OF A TRANSVERSELY ISOTROPIC ELASTIC LAYER ATTACHED TO AN ISOTROPIC HALF-SPACE

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2017

Язык

английский

Авторы, сотрудники КФУ

Данилова Анастасия Вадимовна, автор

Стехина Кристина Николаевна, автор

Авторы, студенты КФУ

Гибадуллина Эвелина Азатовна, автор

Библиографическое описание на языке оригинала

Anufrieva A.V., Stekhina K.N., Tumakov D.N., Gibadullina E.A. Eigen-oscillations of a transversely isotropic elastic layer attached to an isotropic half-space // J. Fundam. Appl. Sci., 2017, 9(1S), 1450-1461.

Аннотация

Layered media have waveguide properties - waves can propagate without sources in such structures. For the most part, such media are anisotropic ones. The simplest case of anisotropy is a transversely isotropic medium. The properties of such media are characterized by the fact that its elastic modules are the same in a plane perpendicular to the axis of symmetry, but they are different from the modules in the direction of the axis. As studies show, many sedimentary rocks are transversely isotropic. Besides, such structures are used in the production of composites. For example, if fibers parallel to each other are used as a reinforcing material, then the composite has a unidirectional structure and is transversely isotropic material in the planes perpendicular to the direction of reinforcement. Sheet metals are often non-isotropic ones, and have normal (transversal) anisotropy. Reinforced concrete is also considered as transversely isotropic after the appearance of cracks.

Ключевые слова

transversely isotropic layer, eigenvectors, elastic oscillations, dispersion equation

Название журнала

Journal of Fundamental and Applied Sciences

URL

http://www.jfas.info/index.php/jfas/article/view/2859

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https://repository.kpfu.ru/?p_id=164241

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Данилова Анастасия Вадимовна	ru_RU
dc.contributor.author	Стехина Кристина Николаевна	ru_RU
dc.contributor.author	Гибадуллина Эвелина Азатовна	ru_RU
dc.date.accessioned	2017-01-01T00:00:00Z	ru_RU
dc.date.available	2017-01-01T00:00:00Z	ru_RU
dc.date.issued	2017	ru_RU
dc.identifier.citation	Anufrieva A.V., Stekhina K.N., Tumakov D.N., Gibadullina E.A. Eigen-oscillations of a transversely isotropic elastic layer attached to an isotropic half-space // J. Fundam. Appl. Sci., 2017, 9(1S), 1450-1461.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=164241	ru_RU
dc.description.abstract	Journal of Fundamental and Applied Sciences	ru_RU
dc.description.abstract	Layered media have waveguide properties - waves can propagate without sources in such structures. For the most part, such media are anisotropic ones. The simplest case of anisotropy is a transversely isotropic medium. The properties of such media are characterized by the fact that its elastic modules are the same in a plane perpendicular to the axis of symmetry, but they are different from the modules in the direction of the axis. As studies show, many sedimentary rocks are transversely isotropic. Besides, such structures are used in the production of composites. For example, if fibers parallel to each other are used as a reinforcing material, then the composite has a unidirectional structure and is transversely isotropic material in the planes perpendicular to the direction of reinforcement. Sheet metals are often non-isotropic ones, and have normal (transversal) anisotropy. Reinforced concrete is also considered as transversely isotropic after the appearance of cracks.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	transversely isotropic layer	ru_RU
dc.subject	eigenvectors	ru_RU
dc.subject	elastic oscillations	ru_RU
dc.subject	dispersion equation	ru_RU
dc.title	Eigen-oscillations of a transversely isotropic elastic layer attached to an isotropic half-space	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU