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Seismic attenuation model using artificial neural networks

机译:基于人工神经网络的地震衰减模型

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This research aims at deriving a simple yet powerful ground motion prediction model for the Himalayas and Indo-Gangetic plains, which has a high probability of damage due to moderate or great earthquake, utilizing an entirely data-driven methodology known as an artificial neural network (ANN) from the earthquake recordings of program for excellence in strong motion studies (PESMOS) and central Indo-Gangetic plains network (CIGN) database. Apart from the widely used independent input parameters, magnitude and distance, we have introduced two new variables, focal depth and average seismic shear-wave velocity from the surface to a depth of 30 m (V-s(30)) to improve model predictability. Peak ground acceleration (PGA) and pseudo-spectral acceleration (PSA) at twenty-five periods are chosen as response variables.The network architecture consisting of 9 hidden nodes were found optimal for the selected database and input-output mapping. The performance of the model is ascertained based on the standard deviation of the error, and the ground motion predictability is tested using real recordings at eight stations and the corresponding widely used ground motion prediction equations (GMPEs) for the Himalayas and Indo-Gangetic Plains. The GMPEs considered for comparison are National Disaster Management Authority (2011), Raghukanth and Kavitha (2014), Anbazhagan et al. (2013), Muthuganeisan and Raghukanth 2016, and Singh et al. (2017). The total standard deviation of response variables in log10 units varies between 0.267-0.343 with period and model predictability plots shows that the current ANN model is competent to predict the response spectrum with good accuracy in both the seismically critical regions of India. Finally, the model is scripted into MATLAB and Excel and supplemented with this article for further use.
机译:这项研究旨在通过使用完全数据驱动的方法(称为人工神经网络)为喜马拉雅山和印度恒河平原推导出一个简单而强大的地面运动预测模型,该模型由于中度或强烈地震而具有很高的破坏可能性( (ANN)来自强力运动研究(PESMOS)和印度中央恒河平原中央网络(CIGN)数据库卓越计划的地震记录。除了广泛使用的独立输入参数,幅度和距离外,我们还引入了两个新变量,即震源深度和从地表到深度为30 m(V-s(30))的平均地震剪切波速度,以提高模型的可预测性。选择25个周期的峰值地面加速度(PGA)和伪谱加速度(PSA)作为响应变量。发现由9个隐藏节点组成的网络体系结构最适合所选的数据库和输入输出映射。根据误差的标准偏差确定模型的性能,并使用八个站点的实际记录以及喜马拉雅山和印度恒河平原相应的广泛使用的地面运动预测方程(GMPE)测试地面运动的可预测性。被考虑进行比较的GMPE是国家灾难管理局(2011),Raghukanth和Kavitha(2014),Anbazhagan等。 (2013),Muthuganeisan和Raghukanth 2016,以及Singh等。 (2017)。 log10单位的响应变量的总标准偏差随周期变化在0.267-0.343之间,模型可预测性图表明,当前的ANN模型能够胜任印度两个地震关键地区的响应谱,且精度很高。最后,将模型编写脚本到MATLAB和Excel中,并在本文中进行补充以供进一步使用。

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