Fuchs Florian, Schneider Felix M, Kolínský Petr, Serafin Stefano, Bokelmann Götz
University of Vienna, Department of Meteorology and Geophysics, Vienna, 1090, Austria.
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, 14473, Germany.
Sci Rep. 2019 Sep 10;9(1):13027. doi: 10.1038/s41598-019-49494-2.
On September 1st, 2018 a devastating explosion occurred on the facility of an oil refinery near Ingolstadt, Germany. We analyzed data of 400 permanent and temporary seismic stations and find strong seismo-acoustic signals on more than 80 seismic stations. The infrasound signal is detectable on seismic stations within 10-350 km from the source, with 40 km spatial resolution. We confirm the explosion site both by the seismic and seismo-acoustic arrivals. Apart from seismic P- and S-waves, we identified three separate acoustic phases with celerities of 332, 292, and 250 m/s, respectively, each of which has a particular spatial pattern of positive detections at the ground. Seismo-acoustic amplitudes are strongly affected by the type of seismic installation but still allow insight into regional infrasound attenuation. Our observations likely represent tropospheric, stratospheric, and thermospheric phases. We performed 3D acoustic ray tracing to validate our findings. Tropospheric and thermospheric arrivals are to some extent reproduced by the atmospheric model. However, ray tracing does not predict the observed acoustic stratospheric ducts. Our findings suggest that small-scale variations had considerable impact on the propagation of infrasound generated by the explosion.
2018年9月1日,德国因戈尔施塔特附近的一家炼油厂设施发生了毁灭性爆炸。我们分析了400个永久和临时地震台站的数据,在80多个地震台站上发现了强烈的地震声学信号。次声信号在距离震源10 - 350公里范围内的地震台站上可检测到,空间分辨率为40公里。我们通过地震波和地震声波的到达时间确定了爆炸地点。除了地震P波和S波外,我们还识别出三个单独的声学相位,其波速分别为332、292和250米/秒,每个相位在地面都有特定的正检测空间模式。地震声学振幅受地震装置类型的影响很大,但仍能让我们了解区域次声衰减情况。我们的观测结果可能代表了对流层、平流层和热层相位。我们进行了三维声线追踪以验证我们的发现。大气模型在一定程度上再现了对流层和热层的波至。然而,声线追踪并未预测到观测到的平流层声导管。我们的发现表明,小规模变化对爆炸产生的次声传播有相当大的影响。