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Characteristics of transmitting channel wave in a coal seam

查看全文 作  者:YANG [1,2]Zhen;GE Mao-[1]chen;WANG Shu-[1]gang 高影响力作者 机构地区:[1]School of Mines, China University of Mining & Technology, Xuzhou, Jiangsu 221008, China;[2]College of Earth and Mineral Scienc, The Penn State University, PA 16802, USA高影响力机构 出  处:《Mining Science and Technology》索引2009年第19卷第3期,共6页高影响力期刊 基  金:Project B2532532 supported by the U.S. Mine Safety and Health Administration 摘  要:An embedded underground coal seam carries channel waves of low seismic velocity along a stratigraphic rock-coal-rock sequence.In a homogeneous and isotropic seam, seismic waves propagate as trapped waves within the seam, which leads to propagation of channel waves.We describe how to set up a field test for transmission in order to acquire channel waves in a coal seam.Because channel wave signals are non-stationary in their frequencies and amplitudes, a necessary velocity spectrum and wavelet transformation analysis are applied to interpret the characteristics of channel waves.The advantage of using a wavelet transformation is that different resolutions can be obtained at different times and different frequencies.According to analysis of the seismic signals acquired in the S7 sensor hole, it was clearly shown that the characteristics of channel waves are lower frequencies and attenuation which can guide an effective wave for detecting voids, boundaries and faults in coal seams with strong roofs and floors. 关 键 词:煤层 信道特性 传输 小波变换分析 传播渠道 地震信号 地震波传播 各向同性
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