Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments
- Autores
- Santos, Juan E.; Gauzellino, Patricia Mercedes; Carcione, José M.; Ba, Jing
- Año de publicación
- 2021
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- We present a novel numerical upscaling technique for modeling the wave response of gas-hydrate bearing sediments composed of a rock frame, gas-hydrate and water, where the hydrate consists of ice-like lattice of water molecules with methane trapped inside. These sediments are highly heterogeneous at mesoscopic scales, much smaller than the wavelength but much larger than the pore size, inducing substantial seismic wave attenuation and dispersion due to mode conversions. The proposed numerical upscaling procedure simulates the wave-induced fluid-flow loss mechanism by computing an average effective viscoelastic medium having the same behavior of the original sediment. The method determines the complex stiffness coefficients associated with the viscoelastic medium by solving numerically boundary value problems formulated in the space-frequency domain, representing compressibility and shear experiments. The procedure is applied to composite media with regions of different amounts of hydrate with patchy or periodic-layer distributions, which define an anisotropic effective viscoelastic medium, respectively. The examples demonstrate that variations in hydrate content induce strong attenuation and dispersion effects on seismic waves due to the mesoscopic loss mechanism.
Facultad de Ciencias Astronómicas y Geofísicas - Materia
-
Geofísica
Gas-hydrate sediments
Finite elements
Wave-induced fluid flow attenuation
Seismic velocity - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/144140
Ver los metadatos del registro completo
id |
SEDICI_a89f484858d3644ca97a928540b3f2fa |
---|---|
oai_identifier_str |
oai:sedici.unlp.edu.ar:10915/144140 |
network_acronym_str |
SEDICI |
repository_id_str |
1329 |
network_name_str |
SEDICI (UNLP) |
spelling |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experimentsSantos, Juan E.Gauzellino, Patricia MercedesCarcione, José M.Ba, JingGeofísicaGas-hydrate sedimentsFinite elementsWave-induced fluid flow attenuationSeismic velocityWe present a novel numerical upscaling technique for modeling the wave response of gas-hydrate bearing sediments composed of a rock frame, gas-hydrate and water, where the hydrate consists of ice-like lattice of water molecules with methane trapped inside. These sediments are highly heterogeneous at mesoscopic scales, much smaller than the wavelength but much larger than the pore size, inducing substantial seismic wave attenuation and dispersion due to mode conversions. The proposed numerical upscaling procedure simulates the wave-induced fluid-flow loss mechanism by computing an average effective viscoelastic medium having the same behavior of the original sediment. The method determines the complex stiffness coefficients associated with the viscoelastic medium by solving numerically boundary value problems formulated in the space-frequency domain, representing compressibility and shear experiments. The procedure is applied to composite media with regions of different amounts of hydrate with patchy or periodic-layer distributions, which define an anisotropic effective viscoelastic medium, respectively. The examples demonstrate that variations in hydrate content induce strong attenuation and dispersion effects on seismic waves due to the mesoscopic loss mechanism.Facultad de Ciencias Astronómicas y Geofísicas2021info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/144140enginfo:eu-repo/semantics/altIdentifier/issn/1420-0597info:eu-repo/semantics/altIdentifier/issn/1573-1499info:eu-repo/semantics/altIdentifier/doi/10.1007/s10596-021-10077-8info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:32:26Zoai:sedici.unlp.edu.ar:10915/144140Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:32:27.055SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments |
title |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments |
spellingShingle |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments Santos, Juan E. Geofísica Gas-hydrate sediments Finite elements Wave-induced fluid flow attenuation Seismic velocity |
title_short |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments |
title_full |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments |
title_fullStr |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments |
title_full_unstemmed |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments |
title_sort |
Effective viscoelastic representation of gas-hydrate bearing sediments from finite-element harmonic experiments |
dc.creator.none.fl_str_mv |
Santos, Juan E. Gauzellino, Patricia Mercedes Carcione, José M. Ba, Jing |
author |
Santos, Juan E. |
author_facet |
Santos, Juan E. Gauzellino, Patricia Mercedes Carcione, José M. Ba, Jing |
author_role |
author |
author2 |
Gauzellino, Patricia Mercedes Carcione, José M. Ba, Jing |
author2_role |
author author author |
dc.subject.none.fl_str_mv |
Geofísica Gas-hydrate sediments Finite elements Wave-induced fluid flow attenuation Seismic velocity |
topic |
Geofísica Gas-hydrate sediments Finite elements Wave-induced fluid flow attenuation Seismic velocity |
dc.description.none.fl_txt_mv |
We present a novel numerical upscaling technique for modeling the wave response of gas-hydrate bearing sediments composed of a rock frame, gas-hydrate and water, where the hydrate consists of ice-like lattice of water molecules with methane trapped inside. These sediments are highly heterogeneous at mesoscopic scales, much smaller than the wavelength but much larger than the pore size, inducing substantial seismic wave attenuation and dispersion due to mode conversions. The proposed numerical upscaling procedure simulates the wave-induced fluid-flow loss mechanism by computing an average effective viscoelastic medium having the same behavior of the original sediment. The method determines the complex stiffness coefficients associated with the viscoelastic medium by solving numerically boundary value problems formulated in the space-frequency domain, representing compressibility and shear experiments. The procedure is applied to composite media with regions of different amounts of hydrate with patchy or periodic-layer distributions, which define an anisotropic effective viscoelastic medium, respectively. The examples demonstrate that variations in hydrate content induce strong attenuation and dispersion effects on seismic waves due to the mesoscopic loss mechanism. Facultad de Ciencias Astronómicas y Geofísicas |
description |
We present a novel numerical upscaling technique for modeling the wave response of gas-hydrate bearing sediments composed of a rock frame, gas-hydrate and water, where the hydrate consists of ice-like lattice of water molecules with methane trapped inside. These sediments are highly heterogeneous at mesoscopic scales, much smaller than the wavelength but much larger than the pore size, inducing substantial seismic wave attenuation and dispersion due to mode conversions. The proposed numerical upscaling procedure simulates the wave-induced fluid-flow loss mechanism by computing an average effective viscoelastic medium having the same behavior of the original sediment. The method determines the complex stiffness coefficients associated with the viscoelastic medium by solving numerically boundary value problems formulated in the space-frequency domain, representing compressibility and shear experiments. The procedure is applied to composite media with regions of different amounts of hydrate with patchy or periodic-layer distributions, which define an anisotropic effective viscoelastic medium, respectively. The examples demonstrate that variations in hydrate content induce strong attenuation and dispersion effects on seismic waves due to the mesoscopic loss mechanism. |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://sedici.unlp.edu.ar/handle/10915/144140 |
url |
http://sedici.unlp.edu.ar/handle/10915/144140 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/issn/1420-0597 info:eu-repo/semantics/altIdentifier/issn/1573-1499 info:eu-repo/semantics/altIdentifier/doi/10.1007/s10596-021-10077-8 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
dc.format.none.fl_str_mv |
application/pdf |
dc.source.none.fl_str_mv |
reponame:SEDICI (UNLP) instname:Universidad Nacional de La Plata instacron:UNLP |
reponame_str |
SEDICI (UNLP) |
collection |
SEDICI (UNLP) |
instname_str |
Universidad Nacional de La Plata |
instacron_str |
UNLP |
institution |
UNLP |
repository.name.fl_str_mv |
SEDICI (UNLP) - Universidad Nacional de La Plata |
repository.mail.fl_str_mv |
alira@sedici.unlp.edu.ar |
_version_ |
1844616203599872000 |
score |
13.070432 |