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应用地球物理  2020, Vol. 17 Issue (2): 243-252    DOI: 10.1007/s11770-019-0798-6
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TI 介质Love 型槽波频散曲线特性*
姬广忠1, 2,3, 张平松1, 2, 3,郭立全1, 2, 3,杨思通4,丁仁伟4
1.安徽理工大学深部煤矿采动响应与灾害防控国家重点实验室,安徽淮南 232001;
2.安徽理工大学矿山地质灾害防治与环境保护安徽普通高校重点实验室,安徽淮南 232001;
3.安徽理工大学地球与环境学院,安徽淮南232001;
4.山东科技大学地球科学与工程学院,山东青岛 266590
Characteristics of dispersion curves for Love channel waves in transversely isotropic media*
Ji Guang-Zhong 1,2,3, Zhang Ping-Song?1,2,3, Guo Li-Quan 1,2,3, Yang Si-Tong 4, and Ding Ren-Wei 4
1.State Key Laboratory of Mining Response and Disaster Prevention and Control in Deep Coal Mines, Anhui University of Science and Technology, Huainan 232001, China
2.Key Laboratory of Mine Geological Disaster Prevention and Environment Protection of Anhui Higher Education Institutes,Anhui University of Science and Technology, Huainan 232001, China
3.School of Earth and Environment, Anhui University of Science and Technology, Huainan 232001, China
4.College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
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摘要 煤层层理结构显著,裂隙较为发育,具有明显的各向异性,但目前对各向异性煤层的槽波频散性质研究很少。本文以VTI 介质和HTI 介质为模型,采用广义反射-透射系数法求解Love 槽波频散曲线数值解,分析了TI 介质中几种典型模型的Love 槽波频散特征。结果表明:各向同性介质和VTI 介质频散曲线差异较大,VTI 介质相速度和Airy 相速度均大于各向同性介质,在实际槽波探测中忽略此差异会造成较大探测误差;各向同性介质和HTI 介质频散曲线差异相对较小,各阶Airy 相速度接近;含夹矸煤层模型群速度曲线极不规则,基阶Airy 相不明显,一阶Airy 相凸显,适合选用一阶槽波探测夹矸。
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关键词煤层   TI 介质   Love 槽波   频散曲线   广义反射-透射系数     
Abstract: Coal seams have a pronounced bedding structure with developed cracks and exhibit significant anisotropy. However, few studies have examined the frequency dispersion properties of channel waves in anisotropic coal seams. In this study, numerical solutions are calculated using the generalized reflection–transmission coefficient method for the dispersion curves of Love channel waves in vertical transversely isotropic (VTI) and horizontal transversely isotropic (HTI) medium models. Moreover, the frequency dispersion characteristics of Love channel waves in several typical transversely isotropic models are analyzed. We find that the dispersion curves for isotropic and VTI media diff er significantly. In addition, the phase and Airy-phase velocities in VTI media are higher than those in isotropic media. Thus, neglecting this difference in practical channel wave detection will result in large detection errors. The dispersion curves for the isotropic and HTI media do not differ significantly, and the Airy-phase velocities of various modes are similar. The group-velocity curve for a coal seam model containing a dirt band is found to be extremely irregular. The fundamental-mode Airy phase is not pronounced, but the first-mode Airy phase can be clearly observed. Hence, first-mode channel waves are suitable for detecting dirt bands.
Key wordsCoal seam   transverse isotropy   Love channel wave   dispersion curve   generalized reflection–transmission coefficient   
收稿日期: 2018-08-20;
基金资助:

本研究由国家重点研发计划(编号:2018YFC0807804-3)、安徽省重点研发计划(编号:1804a0802213)和安徽理工大学引进人才科研启动基金联合资助。

通讯作者: 张平松(E-mail: pszhang1971@163.com)     E-mail: pszhang1971@163.com
作者简介: 姬广忠,安徽理工大学讲师,2010 年硕士毕业于中国地质大学(武汉),2017 年博士毕业于煤炭科学研究总院,目前主要从事槽波地震勘探与地震波理论研究. Email:jj-gg-zz@163.com。
引用本文:   
. TI 介质Love 型槽波频散曲线特性*[J]. 应用地球物理, 2020, 17(2): 243-252.
. Characteristics of dispersion curves for Love channel waves in transversely isotropic media*[J]. APPLIED GEOPHYSICS, 2020, 17(2): 243-252.
 
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