• 제목/요약/키워드: Seismic source spectrum

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후쿠오카 지진('05. 3. 20, $M_{JMA}=7.0$)에 대한 일본 인근 지진관측소와 국내 지진관측소의 주파수응답특성 비교 (Site responses of Japanese stations near the epicenter and Korean stations for the Fukuoka earthquake)

  • 연관희;박동희;장천중;최원학;이대수
    • 한국지구물리탐사학회:학술대회논문집
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    • 한국지구물리탐사학회 2005년도 공동학술대회 논문집
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    • pp.79-86
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    • 2005
  • 2004년까지 국내에 축적된 지진파 스펙트럼 D/B를 기반으로 비교적 상세하게 추정된 국내 지진특성으로부터, 190km${\omega}^2$ 지진원모델에 개략적으로 근사되었으나, 2-corner 지진원모델의 특성을 보다 뚜렷하게 보여주었다. 또한 지진원 인근 지역 (R<100km) 일본 지진관측망(F-net, KiK-net 지중, Hi-net, K-net)별로 개략적인 지진원 스펙트럼을 추정하였으며, 국내 지진관측자료부터 추정된 지진원스펙트럼과 비교하였다. 비교 결과 KiK-net 지중 및 Hi-net 등의 심부시추공 관측자료로부터 추정된 지진원스펙트럼이 국내 지진파기저면 지진원스펙트럼과 $1Hz^{\sim}30Hz$에서 유사한 수준을 나타내었다. 이러한 결과로부터 한반도 주변 해상 지진에 대해 국내 지진관측자료만으로 추정한 지진원스펙트럼의 적합성 및 추정에 사용된 국내 지진파전달, 관측소응답 특성 등의 신뢰성을 입증할 수 있었다. 또한 지진원 인근 지역의 KiK-net 지중 및 Hi-net 관측소의 응답특성과 국내 지진파기저면 관측소응답특성이 유사함을 확인하였다.

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Conditional mean spectrum for Bucharest

  • Vacareanu, Radu;Iancovici, Mihail;Pavel, Florin
    • Earthquakes and Structures
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    • 제7권2호
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    • pp.141-157
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    • 2014
  • The Conditional Mean Spectrum represents a powerful link between the seismic hazard information and the selection of strong ground motion records at a particular site. The scope of the paper is to apply for the city of Bucharest for the first time the method to obtain the Conditional Mean Spectrum (CMS) presented by Baker (2011) and to select, on the basis of the CMS, a suite of strong ground motions for performing elastic and inelastic dynamic analyses of buildings and structures with fundamental periods of vibration in the vicinity of 1.0 s. The major seismic hazard for Bucharest and for most of Southern and Eastern Romania is dominated by the Vrancea subcrustal seismic source. The ground motion prediction equation developed for subduction-type earthquakes and soil conditions by Youngs et al. (1997) is used for the computation of the Uniform Hazard Spectrum (UHS) and the CMS. The disaggregation of seismic hazard is then performed in order to determine the mean causal values of magnitude and source-to-site distance for a particular spectral ordinate (for a spectral period T = 1.0 s in this study). The spectral period of 1.0 s is considered to be representative for the new stock of residential and office reinforced concrete (RC) buildings in Bucharest. The differences between the Uniform Hazard Spectrum (UHS) and the Conditional Mean Spectrum (CMS) are discussed taking into account the scarcity of ground motions recorded in the region of Bucharest and the frequency content characteristics of the recorded data. Moreover, a record selection based on the criteria proposed by Baker and Cornell (2006) and Baker (2011) is performed using a dataset consisting of strong ground motions recorded during seven Vrancea seismic events.

Micro-seismic monitoring in mines based on cross wavelet transform

  • Huang, Linqi;Hao, Hong;Li, Xibing;Li, Jun
    • Earthquakes and Structures
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    • 제11권6호
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    • pp.1143-1164
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    • 2016
  • Time Delay of Arrival (TDOA) estimation methods based on correlation function analysis play an important role in the micro-seismic event monitoring. It makes full use of the similarity in the recorded signals that are from the same source. However, those methods are subjected to the noise effect, particularly when the global similarity of the signals is low. This paper proposes a new approach for micro-seismic monitoring based on cross wavelet transform. The cross wavelet transform is utilized to analyse the measured signals under micro-seismic events, and the cross wavelet power spectrum is used to measure the similarity of two signals in a multi-scale dimension and subsequently identify TDOA. The offset time instant associated with the maximum cross wavelet transform spectrum power is identified as TDOA, and then the location of micro-seismic event can be identified. Individual and statistical identification tests are performed with measurement data from an in-field mine. Experimental studies demonstrate that the proposed approach significantly improves the robustness and accuracy of micro-seismic source locating in mines compared to several existing methods, such as the cross-correlation, multi-correlation, STA/LTA and Kurtosis methods.

Necessity and adequacy of near-source factors for seismically isolated buildings

  • Saifullah, Muhammad Khalid;Alhan, Cenk
    • Earthquakes and Structures
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    • 제12권1호
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    • pp.91-108
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    • 2017
  • Superstructures and isolation systems of seismically isolated buildings located close to active faults may observe increased seismic demands resulting from long-period and high-amplitude velocity and displacement pulses existent in near-fault ground motions as their fundamental periods may be close to or coincident with these near-fault pulse periods. In order to take these effects into account, the 1997 Uniform Building Code (UBC97) has specified near-source factors that scale up the design spectrum depending on the closest distance to the fault, the soil type at the site, and the properties of the seismic source. Although UBC97 has been superseded by the 2015 International Building Code in the U.S.A., UBC97 near-source factors are still frequently referred in the design of seismically isolated buildings around the world. Therefore it is deemed necessary and thus set as the aim of this study to assess the necessity and the adequacy of near-source factors for seismically isolated buildings. Benchmark buildings of different heights with isolation systems of different properties are used in comparing seismic responses obtained via time history analyses using a large number of historical earthquakes with those obtained from spectral analyses using the amplified spectrums established through UBC97 near-source factors. Results show that near-source factors are necessary but inadequate for superstructure responses and somewhat unconservative for base displacement response.

최근 백령도해역 발생지진의 지진원 및 응답스펙트럼 특성 분석 (Analysis of Characteristics of Seismic Source and Response Spectrum of Ground Motions from Recent Earthquake near the Backryoung Island)

  • 김준경
    • 지구물리와물리탐사
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    • 제14권4호
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    • pp.274-281
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    • 2011
  • 최근 백령도 해역에서 발생한 규모 4.3에 해당하는 중규모 지진(2011년 6월 17일)으로부터 관측된 지반진동 파형을 이용하여 지진원 기구 및 수평 응답스펙트럼을 분석하였다. 분석결과를 한반도의 응력방향과 비교하였고 또한 국내 원자력 관련 구조물의 내진설계 기준과 국내 일반 구조물 및 건축물 내진설계기준과 각각 비교하였다. 지진원 연구에 이용된 지반진동은 3개 관측소(각 관측소에서 3성분)에서 관측된 전파형에 대해 모멘트텐서 기본식을 이용한 격자탐색법을 적용하여 분석하였다. 지진원기구에서 제시하는 주압축응력 방향은 ENE-WSW 방향으로 기존 한반도 전체의 주 응력방향과 대체로 유사하였다. 원자력 관련 구조물의 내진설계 기준과 국내 일반 구조물 및 건축물 내진설계기준과 각각 비교하였다. 국내 원자력시설물의 내진기준으로 이용되고 있는 Reg. Guide 1.60과 비교한 결과 특히 약 3 Hz 이상의 높은 고유진동수 영역에서 Reg. Guide 1.60 기준보다 높은 값을 보여 주었다. 또한 국내 일반 구조물 및 건축물 내진설계기준인 표준 설계응답스펙트럼을 비교한 결과 약 0.8초 이하의 단주기 영역의 전체 대역(SD 지반조건)에서 자료처리 결과가 기준을 크게 초과하였다. 향후 국내 지진활동 실정에 적합한 내진설계 기준 마련을 위해 관측자료의 질적 향상 및 양적인 축적 등을 통하여 특히 높은 고유진동수 대역에서 수평응답스펙트럼 기준의 보수성을 재고할 필요가 있다.

한반도 지진특성을 고려하여 모사된 강진동에 대한 가속도 응답스펙트럼 (The Acceleration Response Spectrum for Simulated Strong Motions Considering the Earthquake Characteristics of the Korean Peninsula)

  • 김성균
    • 한국지구과학회지
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    • 제28권2호
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    • pp.179-186
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    • 2007
  • 응답스펙트럼은 내진설계에 있어서 중요한 기초자료의 하나이다. 응답스펙트럼을 얻기 위하여, 한반도에서 발생하는 지진들의 지진원 특성에 근거하여 다수의 강진동을 Boore(2005)에 의해 개발된 컴퓨터 프로그램 SMSIM을 사용하여 모사하였다. 여러 연구결과들에 대한 충분한 검토를 통하여, 모사에 필요한 입력자료들을 선정하였다. 모사된 강진동으로부터 얻은 응답스펙트럼은 가속도 1.0 g에 대하여 정규화하여 미국 원자력위원회(1973)의 표준응답스펙트럼과 비교하였다. 이 연구에서 얻어진 응답스펙트럼의 스펙트럼 진폭은 대략 10 Hz 이상의 고주파 대역에서 표준 응답스펙트럼 값에 비하여 큰 것으로 나타났다. 또한 응력강하량의 변화에 따른 응답스펙트럼의 변화를 평가하였다. 그 결과 큰 응력강하량에 대한 응답스펙트럼의 스펙트럼 진폭은 저주파 범위내에서 큰 값을 나타냄을 제시하였다.

Post-earthquake warning for Vrancea seismic source based on code spectral acceleration exceedance

  • Balan, Stefan F.;Tiganescu, Alexandru;Apostol, Bogdan F.;Danet, Anton
    • Earthquakes and Structures
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    • 제17권4호
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    • pp.365-372
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    • 2019
  • Post-earthquake crisis management is a key capability for a country to be able to recover after a major seismic event. Instrumental seismic data transmitted and processed in a very short time can contribute to better management of the emergency and can give insights on the earthquake's impact on a specific area. Romania is a country with a high seismic hazard, mostly due to the Vrancea intermediate-depth earthquakes. The elastic acceleration response spectrum of a seismic motion provides important information on the level of maximum acceleration the buildings were subjected to. Based on new data analysis and knowledge advancements, the acceleration elastic response spectrum for horizontal ground components recommended by the Romanian seismic codes has been evolving over the last six decades. This study aims to propose a framework for post-earthquake warning based on code spectrum exceedances. A comprehensive background analysis was undertaken using strong motion data from previous earthquakes corroborated with observational damage, to prove the method's applicability. Moreover, a case-study for two densely populated Romanian cities (Focsani and Bucharest) is presented, using data from a $5.5M_W$ earthquake (October 28, 2018) and considering the evolution of the three generations of code-based spectral levels for the two cities. Data recorded in free-field and in buildings were analyzed and has confirmed that no structural damage occurred within the two cities. For future strong seismic events, this tool can provide useful information on the effect of the earthquake on structures in the most exposed areas.

한반도 발생 지진의 지진원 상수 (Source parameters of earthquakes occurred in the Korean Peninsula)

  • 김성균;김병철
    • 한국지진공학회:학술대회논문집
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    • 한국지진공학회 2002년도 춘계 학술발표회 논문집
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    • pp.3-11
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    • 2002
  • Source parameters for forty nine recent earthquakes occurred in and around Korean Peninsula are determined and the relations among them are studied. The corner frequency and seismic moment are estimated from three different methods. The spectral fitting of the source displacement spectrum with the $\omega$-square source model of Brune(1970) and Snoke(1987)'s method are applied to all events and empirical Green's function method for two events are adopted. The source parameters determined in this study show different values depending on the adopted method and on the stations of which seismograms are recorded. It is interpreted that the disagreements principally originate from insufficient consideration of source radiation pattern and attenuation and amplification according to path direction. The corner frequencies and seismic moments are averaged to exclude the directional effects and other source parameters are estimated from the mean corner frequency and seismic moment. The static stress drops estimated in this study tend to be independent of seismic moment or magnitude for events above a certain size. For earthquakes with the size less than about 3.0$\times$10$^{21}$dyne-cm(nearly same as M$_{L}$=3.7), the stress drop tends to decrease with the decreasing moment. This fact suggests a breakdown of scaling law of source parameters below the threshold magnitude. The moment magnitudes calculated from source parameters appear to be slightly larger than the Richter's local magnitudes in the range above M$_{L}$=3.5.3.5.

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내진설계를 위한 응답스펙트럼 연구 (Characteristics of Response Spectrum using Observed Ground Motion from the Recent Earthquakes)

  • 김준경
    • 대한자원환경지질학회:학술대회논문집
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    • 대한자원환경지질학회 1999년도 춘계 공동학술발표회
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    • pp.116-119
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    • 1999
  • Amplification factor spectrum, using the observed strong ground motions database in the Korean Peninsula, has been obtained and compared with Standard Response Spectrum, which was suggested by United States Nuclear Regulatory Committee. The observed und motions from the Yongwol and the Kyoungju, and the other recent Earthquakes, respectively, which ate supposed to represent domestic seismotectonic characteristics such as seismic source, attenuation of the propagation medium, and site specific effect, are used for the analysis of amplification factor spectrum. The database are slightly different from the those of the second study. Amplification factors hue been calculated by comparing the observed peak ground motions with results from responses to the observed horizontal na vertical ground motions. The comparison have shown that the amplification factors resultant from this study exceeds these of Standard Response Spectrum, The results suggest that the characteristics of seismic strong ground motion, which are supposed to represent the domestic seismotectonic characteristics, differs from those of Standard Response Spectrum, especially at higher frequencies. The results from the 2nd study are similar to those of 1st analysis.

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