Application of the Discrete Fréchet Distance in Site Classifications at Strong Motion Stations
-
摘要: 当强震台站场地资料不完整时,所收集到的强震数据因缺乏准确的场地类别信息而难以有效利用。为解决这一问题,本文提出一种基于离散Fréchet距离的强震台站场地分类方法。将获取到的664个KiK-net台站场地按照《建筑抗震设计规范(GB 50011—2010)》进行分类,并构建2个数据集。利用数据集1得到Ⅰ、Ⅱ、Ⅲ类场地标准谱比曲线,并结合离散Fréchet距离对数据集2中的台站进行场地分类,统计分类成功率与误判率。统计结果表明,本文方法能较准确地对场地进行分类,且误判率在可接受范围内。将本文方法分类统计结果与斯皮尔曼秩相关系数法分类的成功率与误判率进行对比,结合本文方法分类后得到的平均谱比曲线,均可表明应用本文方法进行强震台站场地分类具有合理性。
-
关键词:
- 强震台站 /
- 场地分类 /
- 离散Fréchet距离 /
- 标准谱比曲线 /
- 数据集
Abstract: Without complete site information of strong motion stations, the collected data cannot be effectively used due to lack of accurate site category information. In order to overcome this problem, this study proposed a site classification method for strong motion stations based on discrete Fréchet distance, which is a measurement of the similarity between curves. The site conditions at 664 strong motion stations from KiK-net were firstly classified according to the Chinese Code for Seismic Design of Buildings (GB 50011-2010), and then divided into two sets. Standard spectra-ratio curves for site class Ⅰ, Ⅱ and Ⅲ were derived for the sites in dataset1 and there were obvious differences between those three curves. At the same time, the distribution of the natural logarithmic deviation on response spectra periods of those standard curves was also calculated in order to examine the divergence of the dataset. The sites in dataset2 were reclassified based on the method proposed in this paper, and the corresponding success rates and error rates of classifications were calculated. The result shows that not only could the proposed method classify sites with accuracy but also the error rates would be acceptable. The proposed method shows reasonability, by the comparison of the results derived from the proposed method with those from the method of Spearman's rank correlation coefficient, combined with the average spectra ratio curves derived from the proposed method. -
表 1 KiK-net台站场地分类结果
Table 1. Classification result of KiK-net stations
场地类别 数量 比例/% 描述 I 94 14.16 包括I0跟I1 Ⅱ 481 72.44 - Ⅲ 36 5.42 - Ⅳ 4 0.60 - 5(剔除) 43 6.48 含有推测剪切波速 6(剔除) 6 0.90 含有软夹层 表 2 地震动记录选取信息
Table 2. Details on ground motion record selection
场地类别 数据集1 数据集2 场地数量 记录数量/组 记录占比/% 场地数量 记录数量/组 记录占比/% I 61 4153 26.06 25 1418 31.99 Ⅱ 367 8624 54.11 33 2294 51.76 Ⅲ 24 3160 19.83 4 720 16.25 表 3 KGWH03场地钻孔及场地分类
Table 3. Boring Information and Site Classification of KGWH03
层序 厚度/m 剪切波速/(m·s-1) 1 5.00 600.00 2 19.00 1820.00 3 26.00 2400.00 4 — 2950.00 等效剪切波速/(m·s-1) 600.00 覆盖层厚度/m 5.00 场地类别 I -
蒋其峰, 魏玮, 王红卫等, 2017.山东省场地类别分布及地震动峰值加速度区划调整.震灾防御技术, 12(3):501-510. http://zzfy.eq-j.cn/zzfyjs/ch/reader/view_abstract.aspx?flag=1&file_no=20170306&journal_id=zzfyjs 王珊, 张郁山, 尤贺, 2014.场地划分标准对基岩地震动参数衰减关系的影响.震灾防御技术, 9(4):759-769. http://zzfy.eq-j.cn/zzfyjs/ch/reader/view_abstract.aspx?flag=1&file_no=20140403&journal_id=zzfyjs 温瑞智, 冀昆, 任叶飞等, 2015.基于谱比法的我国强震台站场地分类.岩石力学与工程学报, 34(6):1236-1241. http://www.cnki.com.cn/Article/CJFDTotal-YSLX201506018.htm 赵万松, 2017.抗震设计规范中反应谱特征参数研究.合肥: 合肥工业大学. 中华人民共和国住房和城乡建设部, 中华人民共和国国家质量监督检验检疫总局, 2010.GB 50011-2010建筑抗震设计规范.北京: 中国建筑工业出版社. Alt H., Godau M., 1995. Computing the Fréchet distance between two polygonal curves. International Journal of Computational Geometry and Applications, 5(1-2):75-91. http://d.old.wanfangdata.com.cn/OAPaper/oai_arXiv.org_1307.2097 Borcherdt R. D., 1970. Effects of local geology on ground motion near San Francisco Bay. Bulletin of the Seismological Society of America, 60(1):29-61. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=0618ea10d16c1df048a3229894caa84b Building Seismic Safety Council (BSSC), 2003. The 2003 NEHRP recommended provisions for new buildings and other structures, part Ⅰ (provisions) and part Ⅱ (commentary). Washington, D. C.: FEMA. Eiter T., Mannila H., 1994. Computing discrete Fréchet distance. Vienna: Information System department, Technical University of Vienna. Fukushima Y., Bonilla L. F., Scotti O., et al., 2007. Site classification using horizontal-to-vertical response spectral ratios and its impact when deriving empirical ground-motion prediction equations. Journal of Earthquake Engineering, 11(5):712-724. doi: 10.1080/13632460701457116 Ghasemi H., Zare M., Fukushima Y., et al., 2009. Applying empirical methods in site classification, using response spectral ratio (H/V):A case study on Iranian strong motion network (ISMN). Soil Dynamics and Earthquake Engineering, 29(1):121-132. Lermo J., Chávez-García F. J., 1993. Site effect evaluation using spectral ratios with only one station. Bulletin of the Seismological Society of America, 83(5):1574-1594. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=fbe8db440669882caac22472a98d6f26 Ministry of Land, Infrastructure, Transport and Tourism (MLIT), 2007. Building standard law of Japan. Tokyo: Building Center of Japan. Nakamura Y., 1989. A method for dynamic characteristics estimation of subsurface using microtremor on the ground surface. Railway Technical Research Institute, 30(1):25-33. http://www.researchgate.net/publication/308073825_A_method_for_dynamic_characteristics_estimation_of_subsurface_using_microtremor_on_the_ground_surface Okada Y., Kasahara K., Hori S., et al., 2004. Recent progress of seismic observation networks in Japan -Hi-net, F-net, K-NET and KiK-net. Earth Planets & Space, 56(8):xv-xxviii. Wen R. Z., Ren Y. F., Shi D. C., 2011. Improved HVSR site classification method for free-field strong motion stations validated with Wenchuan aftershock recordings. Journal of Earthquake Engineering and Engineering Vibration, 10(3):325-337. doi: 10.1007/s11803-011-0069-x Yamazaki F., Ansary M. A., 1997. Horizontal-to-vertical spectrum ratio of earthquake ground motion for site characterization. Earthquake Engineering and Structural Dynamics, 26(7):671-689. doi: 10.1002/(SICI)1096-9845(199707)26:7<671::AID-EQE669>3.0.CO;2-S Zhao J. X., Irikura K., Zhang J., et al., 2006. An empirical site-classification method for strong-motion stations in Japan using H/V response spectral ratio. Bulletin of the Seismological Society of America, 96(3):914-925. doi: 10.1785/0120050124