Fractional dynamics and emissive activity of geosystems

Some particular problems and nonstandard ideas, reflecting up-to-date state of nonlinear-dynamic approach to the studies of geosystems are under consideration. Attention is concentrated on the mechanisms of generation of the wide-range, in general case, fractal spectrum of spontaneous seismoacoustic...

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Datum:2016
1. Verfasser: Shuman, V.N.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/107780
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Geofizicheskiy Zhurnal
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author Shuman, V.N.
author_facet Shuman, V.N.
author_sort Shuman, V.N.
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collection OJS
datestamp_date 2020-10-07T11:34:05Z
description Some particular problems and nonstandard ideas, reflecting up-to-date state of nonlinear-dynamic approach to the studies of geosystems are under consideration. Attention is concentrated on the mechanisms of generation of the wide-range, in general case, fractal spectrum of spontaneous seismoacoustic and electromagnetic emissions of lithosphere. The leading role of criticality fronts of different nature in their generation is mentioned. Fundamental characrer of fluctuation-dissipative theorem connecting spontaneous fluctuations of the system with its dissipative properties is accentuated. Well known definitions of the fields of spontaneous emissions of the time, more adequate from the viewpoint of their physical interpretation and possibilities of modeling are being generalized. In this case, seismoelectromagnetic activity is associated with uninterrupted in time transitional process, which is called transitional dispersion with non-stationary activity of geo-medium, its metastable state and sequence of such states. Necessary generalizations are reached by synthesis of fractal dynamics and fractal geometry that provides new possibilities of their self-consistent description. Fractal parabolic equation of spontaneous electromagnetic emission written down in generalized (fractal) derivatives by temporal and spatial variables is under consideration. An important class of localized oscillatory (fracton) excitation of the system is under discussion, which are coordinated with its (the system) fractal structure and which are analogous to ordinary in case of nd regular geometry, which can have neatly seismic, seismoelectromagnetic or electromagnetic nature.
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spelling journalsuranua-geofizicheskiy-article-1077802020-10-07T11:34:05Z Fractional dynamics and emissive activity of geosystems Shuman, V.N. spontaneous emission transitional processes fractal equation of generation fracton excitations fractal structure transitional dispersion Some particular problems and nonstandard ideas, reflecting up-to-date state of nonlinear-dynamic approach to the studies of geosystems are under consideration. Attention is concentrated on the mechanisms of generation of the wide-range, in general case, fractal spectrum of spontaneous seismoacoustic and electromagnetic emissions of lithosphere. The leading role of criticality fronts of different nature in their generation is mentioned. Fundamental characrer of fluctuation-dissipative theorem connecting spontaneous fluctuations of the system with its dissipative properties is accentuated. Well known definitions of the fields of spontaneous emissions of the time, more adequate from the viewpoint of their physical interpretation and possibilities of modeling are being generalized. In this case, seismoelectromagnetic activity is associated with uninterrupted in time transitional process, which is called transitional dispersion with non-stationary activity of geo-medium, its metastable state and sequence of such states. Necessary generalizations are reached by synthesis of fractal dynamics and fractal geometry that provides new possibilities of their self-consistent description. Fractal parabolic equation of spontaneous electromagnetic emission written down in generalized (fractal) derivatives by temporal and spatial variables is under consideration. An important class of localized oscillatory (fracton) excitation of the system is under discussion, which are coordinated with its (the system) fractal structure and which are analogous to ordinary in case of nd regular geometry, which can have neatly seismic, seismoelectromagnetic or electromagnetic nature. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016-07-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/107780 10.24028/gzh.0203-3100.v38i3.2016.107780 Geofizicheskiy Zhurnal; Vol. 38 No. 3 (2016); 72-83 Геофизический журнал; Том 38 № 3 (2016); 72-83 Геофізичний журнал; Том 38 № 3 (2016); 72-83 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/107780/102750 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle spontaneous emission
transitional processes
fractal equation of generation
fracton excitations
fractal structure
transitional dispersion
Shuman, V.N.
Fractional dynamics and emissive activity of geosystems
title Fractional dynamics and emissive activity of geosystems
title_full Fractional dynamics and emissive activity of geosystems
title_fullStr Fractional dynamics and emissive activity of geosystems
title_full_unstemmed Fractional dynamics and emissive activity of geosystems
title_short Fractional dynamics and emissive activity of geosystems
title_sort fractional dynamics and emissive activity of geosystems
topic spontaneous emission
transitional processes
fractal equation of generation
fracton excitations
fractal structure
transitional dispersion
topic_facet spontaneous emission
transitional processes
fractal equation of generation
fracton excitations
fractal structure
transitional dispersion
url https://journals.uran.ua/geofizicheskiy/article/view/107780
work_keys_str_mv AT shumanvn fractionaldynamicsandemissiveactivityofgeosystems