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Dipole Oscillations along Principal Coordinates in a Frozen Channel in the Context of Symmetric Linear Thickness of Porous Ice Научная публикация

Журнал Journal of Marine Science and Engineering
ISSN: 2077-1312
Вых. Данные Год: 2024, Том: 12, Номер: 1, Номер статьи : 198, Страниц : 23 DOI: 10.3390/jmse12010198
Ключевые слова dipole; oscillations; channel; ice plate; porous ice; ice deflections; hydroelastic waves; strains
Авторы Shishmarev Konstantin 1 , Sibiryakova Tatyana 2 , Naydenova Kristina 2 , Khabakhpasheva Tatyana 3,4
Организации
1 College of Shipbuilding Engineering, Harbin Engineering University, Harbin 150001, China
2 Department of Differential Equations, Altai State University, 656049 Barnaul, Russia
3 Lavrentyev Institute of Hydrodynamics, Siberian Branch of the Russian Academy of Sciences (SB RAS), 630090 Novosibirsk, Russia
4 School of Mathematics, University of East Anglia, Norwich NR4 7TJ, UK

Информация о финансировании (1)

1 Министерство науки и высшего образования Российской Федерации FWGG-2021-0011

Реферат: The problem of periodic oscillations of a dipole, specifically its strength, along the principal axes in a three-dimensional frozen channel is considered. The key points of the problem are taking into account the linear thickness of ice across the channel and ice porosity within Darcy’s law. The fluid in the channel is inviscid and incompressible; the flow is potential. It is expected that the oscillations of a small radius dipole well approximate the oscillations of a small radius sphere at a sufficient depth of immersion of the dipole. It was found that during oscillations along the channel and vertical oscillations, waves are generated in the channel, propagating along the channel with a frequency equal to the frequency of dipole oscillations. These waves decay far from the dipole, and the rate of decay depends on the porosity coefficient.
Библиографическая ссылка: Shishmarev K. , Sibiryakova T. , Naydenova K. , Khabakhpasheva T.
Dipole Oscillations along Principal Coordinates in a Frozen Channel in the Context of Symmetric Linear Thickness of Porous Ice
Journal of Marine Science and Engineering. 2024. V.12. N1. 198 :1-23. DOI: 10.3390/jmse12010198 WOS Scopus РИНЦ OpenAlex
Даты:
Поступила в редакцию: 23 дек. 2023 г.
Принята к публикации: 17 янв. 2024 г.
Опубликована в печати: 22 янв. 2024 г.
Идентификаторы БД:
Web of science: WOS:001151456200001
Scopus: 2-s2.0-85183340120
РИНЦ: 65659968
OpenAlex: W4391099648
Цитирование в БД:
БД Цитирований
OpenAlex 1
РИНЦ 2
Scopus 1
Web of science 1
Альметрики: