Registration of avalanches in the Khibiny Mountains by the geophysical methods

I. Fedorov, A. V. Fedorov, V. Asming
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引用次数: 0

Abstract

In the winter months of 2018-2020 the Kola Branch of the Unified Geophysical Service RAS conducted experiments on the joint registration of avalanches in the Khibiny mountain range using seismic and infrasonic sensors during work on the forced descent of the snow mass. The aim of the experiments is to assess the possibility of avalanche detection using the geophysical methods. The lack of representative statistics on the frequency and regularity of avalanches is the reason for the relevance of developing methods of their remote registration. The difficulty of registering avalanches is due to their occurrence often in hard-to-reach areas and in poor visibility conditions. To record signals generated by avalanches, different configurations of infrasound panels consisting of three spatially separated sensors (MPA 201 or Hyperion IFS-4000 microbarographs) and a portable seismic station Guralp CMG-6TD were used. As a result of the experiments, infrasound recordings were obtained at different distances from the avalanche source. The infrasound group recordings collected from the experiments were processed using an automatic detector implementing amplitude and cross-correlation signal detection methods. The spectral composition of the recordings and their characteristic appearance were analyzed. Avalanche-induced signals are characterized by long duration and changes in azimuth to the source. The dominant frequencies of the signal lie in the region of 1-10 Hz. Conclusions are made about the insufficient sensitivity of the seismic method when the seismometer is located at a distance of the first kilometers from the avalanche source, as well as the high applicability of the infrasound method for recording the facts of avalanches. The results obtained will make it possible to develop a methodology for automatic detection of signals generated by avalanches using the data of infrasound registration. This is the necessary basis for building a system for continuous monitoring of avalanche activity.
用地球物理方法记录希比尼山区的雪崩
在2018-2020年的冬季,统一地球物理服务局的科拉分部在雪团被迫下降的工作中,使用地震和次声传感器对基比尼山脉的雪崩进行了联合登记实验。实验的目的是评估使用地球物理方法探测雪崩的可能性。缺乏关于雪崩频率和规律性的有代表性的统计数据,是制定远程登记方法具有相关性的原因。雪崩的登记困难是因为它们经常发生在难以到达的地区和能见度低的条件下。为了记录雪崩产生的信号,使用了由三个空间分离的传感器(MPA 201或Hyperion IFS-4000微型arograph)和便携式地震台Guralp CMG-6TD组成的不同配置的次声面板。实验的结果是,在距离雪崩源不同距离处获得了次声记录。使用实现振幅和互相关信号检测方法的自动检测器来处理从实验中收集的次声组记录。分析了这些记录的光谱组成及其特征外观。雪崩诱发的信号具有持续时间长和震源方位角变化的特点。信号的主频率位于1-10Hz的范围内。得出的结论是,当地震仪位于距离雪崩源最初几公里的地方时,地震方法的灵敏度不够,次声方法在记录雪崩事实方面的适用性很高。所获得的结果将有可能开发一种利用次声配准数据自动检测雪崩产生的信号的方法。这是建立雪崩活动连续监测系统的必要基础。
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