Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean

Submarine permafrost is widely distributed in polar ocean, which has an important impact on polar engineering and subsea energy exploitation. According to the frozen porous medium theory, an analytical solution of the one-dimensional vertically dynamic response of the submarine permafrost is derived...

Full description

Bibliographic Details
Published in:Energies
Main Authors: Yunyu Chen, Qiang Li, Minjie Wen, Yifei Wang, Weiwei Duan
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/en15165941
id ftmdpi:oai:mdpi.com:/1996-1073/15/16/5941/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/1996-1073/15/16/5941/ 2023-08-20T04:09:08+02:00 Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean Yunyu Chen Qiang Li Minjie Wen Yifei Wang Weiwei Duan 2022-08-16 application/pdf https://doi.org/10.3390/en15165941 EN eng Multidisciplinary Digital Publishing Institute H: Geo-Energy https://dx.doi.org/10.3390/en15165941 https://creativecommons.org/licenses/by/4.0/ Energies; Volume 15; Issue 16; Pages: 5941 energy geotechnics submarine permafrost frozen porous medium dynamic response resonance analytical solution COMSOL Text 2022 ftmdpi https://doi.org/10.3390/en15165941 2023-08-01T06:06:14Z Submarine permafrost is widely distributed in polar ocean, which has an important impact on polar engineering and subsea energy exploitation. According to the frozen porous medium theory, an analytical solution of the one-dimensional vertically dynamic response of the submarine permafrost is derived by using the Laplace transform and the separation variable method. Using the general forms of partial differential equations and the pressure acoustics module in COMSOL software, a finite element model of submarine permafrost overlying a seawater layer is established. The results show that the degraded solution agrees well with the existing results of the vertically dynamic response of the saturated soil layer in the seabed, and the analytical and numerical solutions are in good agreement. The water depth, saturation and temperature have important effects on the dynamic responses of submarine permafrost. When the soil layer is fully saturated, the water depth has a weak effect on resonance frequency. However, if not fully saturated, even a small amount of air bubbles will have a significant impact on the resonance frequency of the soil layer, and this effect increases with the increase of water depth. The effect of temperature on the nearly saturated permafrost layer is also significantly higher than that on the saturated permafrost layer. Text permafrost MDPI Open Access Publishing Laplace ENVELOPE(141.467,141.467,-66.782,-66.782) Energies 15 16 5941
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic energy geotechnics
submarine permafrost
frozen porous medium
dynamic response
resonance
analytical solution
COMSOL
spellingShingle energy geotechnics
submarine permafrost
frozen porous medium
dynamic response
resonance
analytical solution
COMSOL
Yunyu Chen
Qiang Li
Minjie Wen
Yifei Wang
Weiwei Duan
Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean
topic_facet energy geotechnics
submarine permafrost
frozen porous medium
dynamic response
resonance
analytical solution
COMSOL
description Submarine permafrost is widely distributed in polar ocean, which has an important impact on polar engineering and subsea energy exploitation. According to the frozen porous medium theory, an analytical solution of the one-dimensional vertically dynamic response of the submarine permafrost is derived by using the Laplace transform and the separation variable method. Using the general forms of partial differential equations and the pressure acoustics module in COMSOL software, a finite element model of submarine permafrost overlying a seawater layer is established. The results show that the degraded solution agrees well with the existing results of the vertically dynamic response of the saturated soil layer in the seabed, and the analytical and numerical solutions are in good agreement. The water depth, saturation and temperature have important effects on the dynamic responses of submarine permafrost. When the soil layer is fully saturated, the water depth has a weak effect on resonance frequency. However, if not fully saturated, even a small amount of air bubbles will have a significant impact on the resonance frequency of the soil layer, and this effect increases with the increase of water depth. The effect of temperature on the nearly saturated permafrost layer is also significantly higher than that on the saturated permafrost layer.
format Text
author Yunyu Chen
Qiang Li
Minjie Wen
Yifei Wang
Weiwei Duan
author_facet Yunyu Chen
Qiang Li
Minjie Wen
Yifei Wang
Weiwei Duan
author_sort Yunyu Chen
title Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean
title_short Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean
title_full Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean
title_fullStr Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean
title_full_unstemmed Analytical and Numerical Analyses on Vertical Site Responses of Submarine Permafrost in Polar Ocean
title_sort analytical and numerical analyses on vertical site responses of submarine permafrost in polar ocean
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/en15165941
long_lat ENVELOPE(141.467,141.467,-66.782,-66.782)
geographic Laplace
geographic_facet Laplace
genre permafrost
genre_facet permafrost
op_source Energies; Volume 15; Issue 16; Pages: 5941
op_relation H: Geo-Energy
https://dx.doi.org/10.3390/en15165941
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/en15165941
container_title Energies
container_volume 15
container_issue 16
container_start_page 5941
_version_ 1774721876760723456