Of some peculiarities of generalized rheological body. 2

Peculiarities of high-rank rheological bodies (RB) formation through unification of two RBs with lesser number of elements were analyzed. The necessary and sufficient conditions for the nonsingularity of complex RB are formulated, which lie in the equality of difference between the quantity of paral...

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Datum:2014
1. Verfasser: Bytzan, Ye.
Format: Artikel
Sprache:Ukrainisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116054
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Geofizicheskiy Zhurnal
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author Bytzan, Ye.
author_facet Bytzan, Ye.
author_sort Bytzan, Ye.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:57:19Z
description Peculiarities of high-rank rheological bodies (RB) formation through unification of two RBs with lesser number of elements were analyzed. The necessary and sufficient conditions for the nonsingularity of complex RB are formulated, which lie in the equality of difference between the quantity of parallel and consecutive connections in the formed RB to one, and the RB relaxation times that are composed in case of parallel connections and aftereffect times in case of consecutive connection were different. The function of relaxation creeping were built, with the help of which the cores are built, as well as resolutions of integral equations of the 2nd kind, which describe nonelastic processes in media with aftereffects.
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spelling journalsuranua-geofizicheskiy-article-1160542020-10-07T11:57:19Z Of some peculiarities of generalized rheological body. 2 Bytzan, Ye. rheological body rheological equation deformation tension relaxation rank non-elasticity non-degeneracy wave field rheological medium Peculiarities of high-rank rheological bodies (RB) formation through unification of two RBs with lesser number of elements were analyzed. The necessary and sufficient conditions for the nonsingularity of complex RB are formulated, which lie in the equality of difference between the quantity of parallel and consecutive connections in the formed RB to one, and the RB relaxation times that are composed in case of parallel connections and aftereffect times in case of consecutive connection were different. The function of relaxation creeping were built, with the help of which the cores are built, as well as resolutions of integral equations of the 2nd kind, which describe nonelastic processes in media with aftereffects. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116054 10.24028/gzh.0203-3100.v36i3.2014.116054 Geofizicheskiy Zhurnal; Vol. 36 No. 3 (2014); 72-85 Геофизический журнал; Том 36 № 3 (2014); 72-85 Геофізичний журнал; Том 36 № 3 (2014); 72-85 2524-1052 0203-3100 uk https://journals.uran.ua/geofizicheskiy/article/view/116054/110157 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle rheological body
rheological equation
deformation
tension
relaxation
rank
non-elasticity
non-degeneracy
wave field
rheological medium
Bytzan, Ye.
Of some peculiarities of generalized rheological body. 2
title Of some peculiarities of generalized rheological body. 2
title_full Of some peculiarities of generalized rheological body. 2
title_fullStr Of some peculiarities of generalized rheological body. 2
title_full_unstemmed Of some peculiarities of generalized rheological body. 2
title_short Of some peculiarities of generalized rheological body. 2
title_sort of some peculiarities of generalized rheological body. 2
topic rheological body
rheological equation
deformation
tension
relaxation
rank
non-elasticity
non-degeneracy
wave field
rheological medium
topic_facet rheological body
rheological equation
deformation
tension
relaxation
rank
non-elasticity
non-degeneracy
wave field
rheological medium
url https://journals.uran.ua/geofizicheskiy/article/view/116054
work_keys_str_mv AT bytzanye ofsomepeculiaritiesofgeneralizedrheologicalbody2