Shallow S-wave Velocity Profile Estimation using Surface Velocity and Microtremor HVSR with a Linear Velocity Increase Approach

IF 0.5 Q4 MULTIDISCIPLINARY SCIENCES Journal of Mathematical and Fundamental Sciences Pub Date : 2023-07-26 DOI:10.5614/j.math.fund.sci.2023.54.3.4
Andi Muhamad Pramatadie, H. Yamanaka, A. Afnimar
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Abstract

We propose a simple method for 1D S-wave velocity (Vs) profile estimation using a measured surface S-wave velocity (V1) and peak frequency of the observed microtremor horizontal-to-vertical spectral ratio (HVSR). In this method, the S-wave velocity profile is presented as linear velocity increase with depth in sediments over a bedrock layer that has a given constant S-wave velocity. Thus, the profile can be parameterized with the measured surface S-wave velocity and the velocity gradient. The gradient can be estimated based on the agreement of the peak frequencies of the observed microtremor HVSR and the theoretical ellipticity of the fundamental mode of the Rayleigh wave. We examined the applicability of the proposed method using numerical tests as well as application to actual data at five sites in the Bandung Basin, Indonesia, where observed Rayleigh wave phase velocities from microtremor array surveys were available. The applicability was confirmed in numerical tests using sample models of soil profiles in the basin. Actual application indicated the appropriateness of the estimated S-wave velocity profiles due to the similarity of their theoretical Rayleigh wave phase velocities with the observed Rayleigh wave phase velocities. Since the proposed method needs prior confirmation of the linear increase of the S-wave velocity, it is suitable for use in spatial interpolation of shallow S-wave velocity profiles with simple data acquisition.
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基于地表速度和微震HVSR的横波速度剖面估计
我们提出了一种简单的利用测量到的表面s波速度(V1)和观测到的微震水平-垂直谱比(HVSR)的峰值频率估计一维s波速度(Vs)剖面的方法。在这种方法中,横波速度曲线呈现为基岩层上沉积物的线速度随深度的增加而增加,基岩层具有给定的恒定横波速度。因此,剖面可以用测量到的表面横波速度和速度梯度参数化。根据观测到的微震动HVSR的峰值频率与瑞利波基模的理论椭圆度的一致性,可以估计出梯度。我们通过数值试验以及应用于印度尼西亚万隆盆地五个站点的实际数据来检验所提出方法的适用性,在这些站点中可以获得微震阵列调查观测到的瑞利波相速度。在流域土壤剖面样品模型的数值试验中证实了该方法的适用性。实际应用表明,由于理论瑞利波相速度与观测瑞利波相速度的相似性,估计的横波速度剖面是适当的。由于该方法需要事先确认横波速度的线性增长,因此适用于数据采集简单的浅层横波速度剖面的空间插值。
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来源期刊
CiteScore
1.30
自引率
0.00%
发文量
0
审稿时长
24 weeks
期刊介绍: Journal of Mathematical and Fundamental Sciences welcomes full research articles in the area of Mathematics and Natural Sciences from the following subject areas: Astronomy, Chemistry, Earth Sciences (Geodesy, Geology, Geophysics, Oceanography, Meteorology), Life Sciences (Agriculture, Biochemistry, Biology, Health Sciences, Medical Sciences, Pharmacy), Mathematics, Physics, and Statistics. New submissions of mathematics articles starting in January 2020 are required to focus on applied mathematics with real relevance to the field of natural sciences. Authors are invited to submit articles that have not been published previously and are not under consideration elsewhere.
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