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饱和多孔介质多相流体系中孔隙压传播数值分析
杨多兴; 刘耀炜; 杨选辉; 张德良
Source Publication国际地震动态/RECENT DEVELOPMENTS IN WORLD SEISMOLOGY
2012-06-25
Issue6Pages:262-262
ISSN0253-4975
Abstract<正>孔隙压波传播与衰减对解释深部流体在地震孕育、触发和断裂活动过程中的作用机制,以及石油与天然成藏机理等方面具有重要的学术和应用价值。目前孔隙压波的理论与计算以孔隙弹性介质理论、BISQ理论为基础。Biot孔隙弹性理论仅考虑流体沿着波的传播方向发生流动,严重低估了Biot损失。
Keyword孔隙压:6153 饱和多孔介质:4573 弹性介质:2678 弹性理论:2659 传播与衰减:2523 地震孕育:2412 成藏机理:2098 深部流体:1960 作用机制:1925 应用价值:1679
Subject Area固体力学
URL查看原文
Language中文
DepartmentLHD激波与爆轰物理
Document Type期刊论文
Identifierhttp://dspace.imech.ac.cn/handle/311007/46527
Collection高温气体动力学国家重点实验室
Corresponding Author杨多兴
Recommended Citation
GB/T 7714
杨多兴,刘耀炜,杨选辉,等. 饱和多孔介质多相流体系中孔隙压传播数值分析[J]. 国际地震动态/RECENT DEVELOPMENTS IN WORLD SEISMOLOGY,2012(6):262-262.
APA 杨多兴,刘耀炜,杨选辉,&张德良.(2012).饱和多孔介质多相流体系中孔隙压传播数值分析.国际地震动态/RECENT DEVELOPMENTS IN WORLD SEISMOLOGY(6),262-262.
MLA 杨多兴,et al."饱和多孔介质多相流体系中孔隙压传播数值分析".国际地震动态/RECENT DEVELOPMENTS IN WORLD SEISMOLOGY .6(2012):262-262.
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