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4D seismic data acquisition method during coal mining

机译:煤矿开采中的4D地震数据采集方法

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In order to observe overburden media changes caused by mining processing, we take the fully-mechanized working face of the BLT coal mine in Shendong mine district as an example to develop a 4D seismic data acquisition methodology during coal mining. The 4D seismic data acquisition is implemented to collect 3D seismic data four times in different periods, such as before mining, during the mining process and after mining to observe the changes of the overburden layer during coal mining. The seismic data in the research area demonstrates that seismic waves are stronger in energy, higher in frequency and have better continuous reflectors before coal mining. However, all this is reversed after coal mining because the overburden layer has been mined, the seismic energy and frequency decrease, and reflections have more discontinuities. Comparing the records collected in the survey with those from newly mined areas and other records acquired in the same survey with the same geometry and with a long time for settling after mining, it clearly shows that the seismic reflections have stronger amplitudes and are more continuous because the media have recovered by overburden layer compaction after a long time of settling after mining. By 4D seismic acquisition, the original background investigation of the coal layers can be derived from the first records, then the layer structure changes can be monitored through the records of mining action and compaction action after mining. This method has laid the foundation for further research into the variation principles of the overburden layer under modern coal-mining conditions.
机译:为了观察采掘过程中覆盖层介质的变化,我们以神东矿区BLT煤矿的综采工作面为例,开发了采煤过程中的4D地震数据采集方法。实施4D地震数据采集是为了在不同时期采集4D 3D地震数据,例如在采矿之前,采矿过程中以及采矿之后,以观察煤矿开采过程中覆盖层的变化。该研究区的地震数据表明,在煤矿开采之前,地震波的能量更强,频率更高并且具有更好的连续反射器。但是,由于开采了覆盖层,地震能量和频率降低,并且反射具有更多的不连续性,因此在采煤后,所有这些情况都可以逆转。将调查中收集的记录与新近开采的记录以及在同一调查中获得的其他记录(具有相同的几何形状,并且开采后需要较长的沉降时间)进行比较,可以清楚地表明,地震反射的振幅更大并且更连续,因为开采后经过长时间的沉降后,通过覆盖层压实已恢复了介质。通过4D地震采集,可以从最初的记录中得出煤层的原始背景调查,然后可以通过采矿作用和采矿后的压实作用的记录来监视层结构的变化。该方法为进一步研究现代采煤条件下覆土层的变化规律奠定了基础。

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