结合使用 NGA-East 硬岩地面运动和场地放大模型的数据驱动调整

IF 3.1 2区 工程技术 Q2 ENGINEERING, CIVIL Earthquake Spectra Pub Date : 2024-03-18 DOI:10.1177/87552930241231825
María E Ramos-Sepúlveda, Jonathan P Stewart, Grace A Parker, Morgan P Moschetti, Eric M Thompson, Scott J Brandenberg, Youssef MA Hashash, Ellen M Rathje
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引用次数: 0

摘要

下一代衰减-东部(NGA-East)项目的模型开发包括两个同时独立开发的部分:(1)地震地动模型(GMMs),用于预测以震级和距离为条件的各种烈度测量值的中位数和随机变异性,这些测量值是以硬岩场地条件为参考得出的,场地上部 30 米(VS30)的平均剪切波速度 = 3000 米/秒;(2)场地放大模型,用于修改较软场地条件下的烈度测量值。我们使用扩大版的 NGA-East 数据库,其中包括从 2011 年 11 月(NGA-East 数据整理结束日期)到 2022 年 4 月的新事件,研究这些模型同时使用时是否与北美中部和东部(CENA)的地动记录兼容。扩充后的数据集有 187 个事件、2096 个站点和 16,272 个三分量记录,但震级范围仍然有限(4 至 5.8)。我们使用 17 个 NGA-East GMM 和三个数据选择标准计算残差,这些标准反映了中国国家地震中心内部地动属性的区域差异。残差的混合效应回归揭示了一种持续模式,即短周期(0.01-0.6 秒,包括峰值地面加速度 (PGA))地动预测过高,而长周期地动预测过低。这些误差随地区而变化,德克萨斯-奥克拉荷马-堪萨斯地区的绝对误差大于 CENA 的其他地区。可能影响这些误差的两个因素是:(1)NGA-East GMM 开发期间用于将数据调整为参考条件的场地放大模型与 2018 年国家地震危险性模型(NSHM)以来应用的 CENA 放大模型存在差异;(2)用于将地面运动从硬岩参考条件调整为 VS30 = 760 m/s 条件的基于模拟的因子可能存在偏差。我们提供了调整系数及其认识上的不确定性,并讨论了对应用的影响。
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Data-driven adjustments for combined use of NGA-East hard-rock ground motion and site amplification models
Model development in the Next Generation Attenuation-East (NGA-East) project included two components developed concurrently and independently: (1) earthquake ground-motion models (GMMs) that predict the median and aleatory variability of various intensity measures conditioned on magnitude and distance, derived for a reference hard-rock site condition with an average shear-wave velocity in the upper 30 m ( VS30) = 3000 m/s; and (2) a site amplification model that modifies intensity measures for softer site conditions. We investigate whether these models, when used in tandem, are compatible with ground-motion recordings in central and eastern North America (CENA) using an expanded version of the NGA-East database that includes new events from November 2011 (end date of NGA-East data curation) to April 2022. Following this expansion, the data set has 187 events, 2096 sites, and 16,272 three-component recordings, although the magnitude range remains limited (∼4 to 5.8). We compute residuals using 17 NGA-East GMMs and three data selection criteria that reflect within-CENA regional variations in ground-motion attributes. Mixed-effects regression of the residuals reveals a persistent pattern in which ground motions are overpredicted at short periods (0.01–0.6 s, including peak ground acceleration (PGA)) and underpredicted at longer periods. These misfits are regionally variable, with the Texas–Oklahoma–Kansas region having larger absolute misfits than other parts of CENA. Two factors potentially influencing these misfits are (1) differences in the site amplification models used to adjust the data to the reference condition during NGA-East GMM development relative to CENA amplification models applied since the 2018 National Seismic Hazard Model (NSHM), and (2) potential bias in simulation-based factors used to adjust ground motions from the hard-rock reference condition to a VS30 = 760 m/s condition. We provide adjustment factors and their epistemic uncertainties and discuss implications for applications.
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来源期刊
Earthquake Spectra
Earthquake Spectra 工程技术-工程:地质
CiteScore
8.40
自引率
12.00%
发文量
88
审稿时长
6-12 weeks
期刊介绍: Earthquake Spectra, the professional peer-reviewed journal of the Earthquake Engineering Research Institute (EERI), serves as the publication of record for the development of earthquake engineering practice, earthquake codes and regulations, earthquake public policy, and earthquake investigation reports. The journal is published quarterly in both printed and online editions in February, May, August, and November, with additional special edition issues. EERI established Earthquake Spectra with the purpose of improving the practice of earthquake hazards mitigation, preparedness, and recovery — serving the informational needs of the diverse professionals engaged in earthquake risk reduction: civil, geotechnical, mechanical, and structural engineers; geologists, seismologists, and other earth scientists; architects and city planners; public officials; social scientists; and researchers.
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