2018
DOI: 10.1007/s11600-018-0192-4
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Dispersion features of transmitted channel waves and inversion of coal seam thickness

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Cited by 14 publications
(3 citation statements)
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“…Therefore, the coal seam can be regarded as a typical lowspeed interlayer, comparable to a beam wave guide [11]. Once a longitudinal/transverse wave is excited in the coal seam, part of the excited energy undergoes repeated total reflections in the said interface as the wave propagates through the coal seam [12].…”
Section: Formation Mechanismmentioning
confidence: 99%
“…Therefore, the coal seam can be regarded as a typical lowspeed interlayer, comparable to a beam wave guide [11]. Once a longitudinal/transverse wave is excited in the coal seam, part of the excited energy undergoes repeated total reflections in the said interface as the wave propagates through the coal seam [12].…”
Section: Formation Mechanismmentioning
confidence: 99%
“…As a dispersion parameter, we obtain frequency‐dependent group velocity, which is the velocity of wave transport. Measurement of group velocity from guided wave signals and inversion of the data deliver seam structure, which is crucial for the safety of underground mining (Dresen & Ruter, 1994; Liu et al., 1994; Hu et al., 2018; Zhu et al., 2019). The measurement of observed group velocity is generally performed through multiple filtering and time–frequency analysis (Bhattacharya, 1983; Cox & Mason, 1988).…”
Section: Introductionmentioning
confidence: 99%
“…Hence, precise prediction of coal thickness and of hidden geological anomalies in the working face is fundamental to realization of intelligent and unmanned mining. This is also directly related to the transformation of the whole process, and to the safety of underground workers [3].…”
Section: Introductionmentioning
confidence: 99%