A New Anelasticity Model for Wave Propagation in Partially Saturated Rocks
Elastic wave propagation in partially saturated reservoir rocks induces fluid flow in multi-scale pore spaces, leading to wave anelasticity (velocity dispersion and attenuation). The propagation characteristics cannot be described by a single-scale flow-induced dissipation mechanism. To overcome thi...
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2021
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oai:doaj.org-article:d3477075289a46a194696714e85557262021-11-25T17:27:19ZA New Anelasticity Model for Wave Propagation in Partially Saturated Rocks10.3390/en142276191996-1073https://doaj.org/article/d3477075289a46a194696714e85557262021-11-01T00:00:00Zhttps://www.mdpi.com/1996-1073/14/22/7619https://doaj.org/toc/1996-1073Elastic wave propagation in partially saturated reservoir rocks induces fluid flow in multi-scale pore spaces, leading to wave anelasticity (velocity dispersion and attenuation). The propagation characteristics cannot be described by a single-scale flow-induced dissipation mechanism. To overcome this problem, we combine the White patchy-saturation theory and the squirt flow model to obtain a new anelasticity theory for wave propagation. We consider a tight sandstone Qingyang area, Ordos Basin, and perform ultrasonic measurements at partial saturation and different confining pressures, where the rock properties are obtained at full-gas saturation. The comparison between the experimental data and the theoretical results yields a fairly good agreement, indicating the efficacy of the new theory.Chunfang WuJing BaXiaoqin ZhongJosé M. CarcioneLin ZhangChuantong RuanMDPI AGarticlepartial saturationpatchy saturationsquirt flowP-wave velocity dispersion and attenuationanelasticityultrasonic measurementsTechnologyTENEnergies, Vol 14, Iss 7619, p 7619 (2021) |
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partial saturation patchy saturation squirt flow P-wave velocity dispersion and attenuation anelasticity ultrasonic measurements Technology T |
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partial saturation patchy saturation squirt flow P-wave velocity dispersion and attenuation anelasticity ultrasonic measurements Technology T Chunfang Wu Jing Ba Xiaoqin Zhong José M. Carcione Lin Zhang Chuantong Ruan A New Anelasticity Model for Wave Propagation in Partially Saturated Rocks |
description |
Elastic wave propagation in partially saturated reservoir rocks induces fluid flow in multi-scale pore spaces, leading to wave anelasticity (velocity dispersion and attenuation). The propagation characteristics cannot be described by a single-scale flow-induced dissipation mechanism. To overcome this problem, we combine the White patchy-saturation theory and the squirt flow model to obtain a new anelasticity theory for wave propagation. We consider a tight sandstone Qingyang area, Ordos Basin, and perform ultrasonic measurements at partial saturation and different confining pressures, where the rock properties are obtained at full-gas saturation. The comparison between the experimental data and the theoretical results yields a fairly good agreement, indicating the efficacy of the new theory. |
format |
article |
author |
Chunfang Wu Jing Ba Xiaoqin Zhong José M. Carcione Lin Zhang Chuantong Ruan |
author_facet |
Chunfang Wu Jing Ba Xiaoqin Zhong José M. Carcione Lin Zhang Chuantong Ruan |
author_sort |
Chunfang Wu |
title |
A New Anelasticity Model for Wave Propagation in Partially Saturated Rocks |
title_short |
A New Anelasticity Model for Wave Propagation in Partially Saturated Rocks |
title_full |
A New Anelasticity Model for Wave Propagation in Partially Saturated Rocks |
title_fullStr |
A New Anelasticity Model for Wave Propagation in Partially Saturated Rocks |
title_full_unstemmed |
A New Anelasticity Model for Wave Propagation in Partially Saturated Rocks |
title_sort |
new anelasticity model for wave propagation in partially saturated rocks |
publisher |
MDPI AG |
publishDate |
2021 |
url |
https://doaj.org/article/d3477075289a46a194696714e8555726 |
work_keys_str_mv |
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