论文标题
一种改善荷兰格罗宁根气田地震事件检测的神经网络方法
A Neural Network Approach for Improved Seismic Event Detection in the Groningen Gas Field, The Netherlands
论文作者
论文摘要
在过去的几十年中,Groningen气体(GGF)越来越受汽油产量引起的地震。格罗宁根的地震监测网络最近已致密,以提高地震网络性能,从而增加地震数据量。尽管传统的自动化事件检测技术通常成功地从连续数据中检测事件,但在信噪比较低的情况下,其检测成功受到挑战。来自这些网络的数据流对自动分类和解释引发了对神经网络的特定兴趣。在这里,我们探讨了神经网络在检测地震事件发生的可行性。为此,使用从荷兰皇家气象学研究所(KNMI)数据门户获得的GGF中的地震事件的公共数据培训了一个三层前馈神经网络。由KNMI确定了一个站数据子集确定的地震波形的第一个到达时间和持续时间,用于检测其他未解释的站点数据的到达时间和事件持续时间。随后,各种属性被用作神经网络的输入,这些属性基于不同的短期平均/长期平均(STA/LTA)和频率子频段设置。使用这些输入数据,对网络的参数进行了迭代改进,以最大程度地提高其成功区分噪声事件并确定事件持续时间的能力。结果表明,与参考方法相比,准确检测地震事件并确定其持续时间增加了65%。这为改善了格罗宁根地区的信号波形和自动地震事件分类的解释清除了道路。
Over the past decades, the Groningen Gas Field (GGF) has been increasingly faced by induced earthquakes resulting from gas production. The seismic monitoring network at Groningen has been recently densified to improve the seismic network performance, resulting in increasing amounts of seismic data. Although traditional automated event detection techniques generally are successful in detecting events from continuous data, its detection success is challenged in cases of lower signal-to-noise ratios. The data stream coming from these networks has initiated specific interest in neural networks for automated classification and interpretation. Here, we explore the feasibility of neural networks in detecting the occurrence of seismic events. For this purpose, a three-layered feedforward neural network was trained using public data of a seismic event in the GGF obtained from the Royal Netherlands Meteorological Institute (KNMI) data portal. The first arrival times and duration of earthquake waveforms determined by KNMI for a subset of the station data, were used to detect the arrival times and event duration for the other uninterpreted station data. Subsequently various attributes were used as input for the neural network, that were based on different short term averaging/long term averaging (STA/LTA) and frequency sub-band settings. Using these input data, the network's parameters were iteratively improved to maximize its capability in successfully discriminating seismic events from noise and determine the event duration. Results show an increase of 65 % in accurately detecting seismic events and determining their duration as compared to the reference method. This clears the way for improved interpretation of signal waveforms and automated seismic event classification in the Groningen area.