Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions

<p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, real...
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Autor*in:	S. Lissa [verfasserIn] N. D. Barbosa [verfasserIn] J. G. Rubino [verfasserIn] B. Quintal [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Übergeordnetes Werk:	In: Solid Earth - Copernicus Publications, 2011, 10(2019), Seite 1321-1336
Übergeordnetes Werk:	volume:10 ; year:2019 ; pages:1321-1336

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.5194/se-10-1321-2019

Katalog-ID:	DOAJ03578640X

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allfields	10.5194/se-10-1321-2019 doi (DE-627)DOAJ03578640X (DE-599)DOAJ3cb5b6a5a58d4a818e43b721237aa7b7 DE-627 ger DE-627 rakwb eng QE1-996.5 QE640-699 S. Lissa verfasserin aut Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p< Geology Stratigraphy N. D. Barbosa verfasserin aut J. G. Rubino verfasserin aut B. Quintal verfasserin aut In Solid Earth Copernicus Publications, 2011 10(2019), Seite 1321-1336 (DE-627)62317720X (DE-600)2545676-3 18699529 nnns volume:10 year:2019 pages:1321-1336 https://doi.org/10.5194/se-10-1321-2019 kostenfrei https://doaj.org/article/3cb5b6a5a58d4a818e43b721237aa7b7 kostenfrei https://www.solid-earth.net/10/1321/2019/se-10-1321-2019.pdf kostenfrei https://doaj.org/toc/1869-9510 Journal toc kostenfrei https://doaj.org/toc/1869-9529 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 1321-1336
spelling	10.5194/se-10-1321-2019 doi (DE-627)DOAJ03578640X (DE-599)DOAJ3cb5b6a5a58d4a818e43b721237aa7b7 DE-627 ger DE-627 rakwb eng QE1-996.5 QE640-699 S. Lissa verfasserin aut Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p< Geology Stratigraphy N. D. Barbosa verfasserin aut J. G. Rubino verfasserin aut B. Quintal verfasserin aut In Solid Earth Copernicus Publications, 2011 10(2019), Seite 1321-1336 (DE-627)62317720X (DE-600)2545676-3 18699529 nnns volume:10 year:2019 pages:1321-1336 https://doi.org/10.5194/se-10-1321-2019 kostenfrei https://doaj.org/article/3cb5b6a5a58d4a818e43b721237aa7b7 kostenfrei https://www.solid-earth.net/10/1321/2019/se-10-1321-2019.pdf kostenfrei https://doaj.org/toc/1869-9510 Journal toc kostenfrei https://doaj.org/toc/1869-9529 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 1321-1336
allfields_unstemmed	10.5194/se-10-1321-2019 doi (DE-627)DOAJ03578640X (DE-599)DOAJ3cb5b6a5a58d4a818e43b721237aa7b7 DE-627 ger DE-627 rakwb eng QE1-996.5 QE640-699 S. Lissa verfasserin aut Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p< Geology Stratigraphy N. D. Barbosa verfasserin aut J. G. Rubino verfasserin aut B. Quintal verfasserin aut In Solid Earth Copernicus Publications, 2011 10(2019), Seite 1321-1336 (DE-627)62317720X (DE-600)2545676-3 18699529 nnns volume:10 year:2019 pages:1321-1336 https://doi.org/10.5194/se-10-1321-2019 kostenfrei https://doaj.org/article/3cb5b6a5a58d4a818e43b721237aa7b7 kostenfrei https://www.solid-earth.net/10/1321/2019/se-10-1321-2019.pdf kostenfrei https://doaj.org/toc/1869-9510 Journal toc kostenfrei https://doaj.org/toc/1869-9529 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 1321-1336
allfieldsGer	10.5194/se-10-1321-2019 doi (DE-627)DOAJ03578640X (DE-599)DOAJ3cb5b6a5a58d4a818e43b721237aa7b7 DE-627 ger DE-627 rakwb eng QE1-996.5 QE640-699 S. Lissa verfasserin aut Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p< Geology Stratigraphy N. D. Barbosa verfasserin aut J. G. Rubino verfasserin aut B. Quintal verfasserin aut In Solid Earth Copernicus Publications, 2011 10(2019), Seite 1321-1336 (DE-627)62317720X (DE-600)2545676-3 18699529 nnns volume:10 year:2019 pages:1321-1336 https://doi.org/10.5194/se-10-1321-2019 kostenfrei https://doaj.org/article/3cb5b6a5a58d4a818e43b721237aa7b7 kostenfrei https://www.solid-earth.net/10/1321/2019/se-10-1321-2019.pdf kostenfrei https://doaj.org/toc/1869-9510 Journal toc kostenfrei https://doaj.org/toc/1869-9529 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 1321-1336
allfieldsSound	10.5194/se-10-1321-2019 doi (DE-627)DOAJ03578640X (DE-599)DOAJ3cb5b6a5a58d4a818e43b721237aa7b7 DE-627 ger DE-627 rakwb eng QE1-996.5 QE640-699 S. Lissa verfasserin aut Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p< Geology Stratigraphy N. D. Barbosa verfasserin aut J. G. Rubino verfasserin aut B. Quintal verfasserin aut In Solid Earth Copernicus Publications, 2011 10(2019), Seite 1321-1336 (DE-627)62317720X (DE-600)2545676-3 18699529 nnns volume:10 year:2019 pages:1321-1336 https://doi.org/10.5194/se-10-1321-2019 kostenfrei https://doaj.org/article/3cb5b6a5a58d4a818e43b721237aa7b7 kostenfrei https://www.solid-earth.net/10/1321/2019/se-10-1321-2019.pdf kostenfrei https://doaj.org/toc/1869-9510 Journal toc kostenfrei https://doaj.org/toc/1869-9529 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 10 2019 1321-1336
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callnumber-first	Q - Science
author	S. Lissa
spellingShingle	S. Lissa misc QE1-996.5 misc QE640-699 misc Geology misc Stratigraphy Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
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topic_title	QE1-996.5 QE640-699 Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
topic	misc QE1-996.5 misc QE640-699 misc Geology misc Stratigraphy
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title	Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
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title_full	Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
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title_sort	seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
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title_auth	Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
abstract	<p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p<
abstractGer	<p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p<
abstract_unstemmed	<p<Considering poroelastic media containing periodically distributed parallel fractures, we numerically quantify the effects that fractures with variable aperture distributions have on seismic wave attenuation and velocity dispersion due to fluid pressure diffusion (FPD). To achieve this, realistic models of fractures are generated with a stratified percolation algorithm which provides statistical control over geometrical fracture properties such as density and distribution of contact areas. The results are sensitive to both geometrical properties, showing that an increase in the density of contact areas as well as a decrease in their correlation length reduce the effective seismic attenuation and the corresponding velocity dispersion. Moreover, we demonstrate that if equivalent physical properties accounting for the effects of contact areas are employed, simple planar fractures can be used to emulate the seismic response of fractures with realistic aperture distributions. The excellent agreement between their seismic responses was verified for all wave incidence angles and wave modes.</p<
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title_short	Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
url	https://doi.org/10.5194/se-10-1321-2019 https://doaj.org/article/3cb5b6a5a58d4a818e43b721237aa7b7 https://www.solid-earth.net/10/1321/2019/se-10-1321-2019.pdf https://doaj.org/toc/1869-9510 https://doaj.org/toc/1869-9529
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Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions

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