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Periods of refracted P-waves in coal seams and their applications in coal thickness estimations

机译:煤层中的折射P波及其在煤厚度估计中的应用

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The direct and accurate estimations of coal thicknesses are prerequisites for intelligent mining practices. One of the most effective methods for detecting the distributions of coal thicknesses in coal mining panels is the in-seam seismic (ISS) method. In the present study, after examining the formation processes and propagation characteristics of refracted P-waves in ISS data, it was concluded that the refracted P-waves in coal seams are mainly formed by the multiple transmission and reflection of the P-waves between the coal and rock interfaces of roof and floor at critical angles. This results in the refracted P-waves having strong periodicity, and these periods are proportional to the coal thicknesses. This study adopted numerical simulation models with different coal thicknesses, and the aforementioned periodicity characteristics were examined. It was found that the coal seam thicknesses could be calculated using the periods of the refracted P-waves. However, in thin- or medium-thick coal seams, it was found that multiple transmitted P-waves overlapped and the periods could not be read directly. Therefore, in order to solve this problem, this study composed source wavelets with the main frequency of the source signals and then composite synthetic P-waves by convoluting the source wavelets with the sequences of various coal thicknesses. The suitable estimated coal thickness corresponded to the minimum value of the errors between the synthetic and actual refracted P-waves. An experiment was conducted in the No. 42224 panel of the Chaigou Coal Mine in order to validate the proposed method. The experimental results revealed that the estimated coal thicknesses from the refracted P-waves were consistent with the actual geologic conditions in the coal mine. Due to the fact that the refracted P-waves arrive earlier than other waves in seismic records, the refracted P-waves could be easily identified and processed. Overall, the proposed method was found to be a simple application process for accurate coal thickness estimations.
机译:煤厚度的直接和准确估计是智能采矿实践的先决条件。用于检测煤矿板中煤厚度分布的最有效方法之一是煤层中的地震(ISS)方法。在本研究中,在ISS数据中检查折射P波的形成过程和传播特性之后,得出结论,煤层中的折射P波主要由多个传输和反射之间的p波之间形成屋顶和地板的煤炭和岩石界面处以临界角度。这导致具有强周期性的折射的p波,并且这些时段与煤厚度成比例。本研究采用具有不同煤厚度的数值模拟模型,并检查了上述周期性特征。发现煤层厚度可以使用折射的p波的时段来计算。然而,在薄厚的煤层中,发现重叠的多个透射的p波并无法直接读取。因此,为了解决这个问题,本研究通过源信号的主频率组成了源小波,然后通过将源小波与各种煤厚度的序列卷积来复合合成的p波。合适的估计煤厚度对应于合成和实际折射P波之间的误差的最小值。在Chaigou煤矿的42224小组中进行了实验,以验证提出的方法。实验结果表明,折射波波的估计煤厚度与煤矿的实际地质条件一致。由于折射的P波在地震记录中的其他波提前到达,可以容易地识别和处理折射的P波。总的来说,发现该方法是一种简单的煤厚度估计的应用过程。

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