• 제목/요약/키워드: Shear Wave Velocity

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댐체 물성 평가를 위한 S파 반사법에 관한 연구 (A Study on S-wave Reflection method for the assessment of physical property of dam body)

  • 김형수;김중열;하익수;김유성
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2005년도 춘계 학술발표회 논문집
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    • pp.392-399
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    • 2005
  • Shear modulus (or rigidity) of dam material is an important parameter which can be directly associated with the deformation of dam. Seepage or leakage of water can cause the defects or cracks of dam body. The existence of cracks and rigidity of dam body are decisive information for the estimation of dam safety. Rigidity of material is mainly determined from S-wave velocity and the defects of dam body can be detected by seismic reflection survey. Therefore, seismic reflection survey will be a desirable method which can give a solution about dam safety problem. Among various physical properties of dam body, S-wave velocity is the most important information but it is not easy to get the information. In this study, diverse measuring techniques of S-wave reflection survey were attempted to get the information about S-wave velocity of dam body. Ultimately, S-wave velocity could be estimated by the analysis of SH reflection events which can be easily observed in shot gather data obtained from SH measuring technique. Meanwhile, P-wave reflection survey was also performed at the same profile. P-beam radiation technique which can reduce the surface waves and reinforce the P-wave reflection events was applied for giving a help to analyse P-wave velocity. In the end, P-and S-wave velocity, Vs/Vp, Poisson's ratio distribution of the vertical section under the profile could be acquired.

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포화 및 부분 포화 사질토의 Vp와 Vs 속도 및 과잉간극수압 측정을 위한 비틂전단 시험기의 개발 (Development of Torsional Shear Testing System to Measure P-wave Velocity, S-wave Velocity and Pore Water Pressure Buildup on Fully and Partially Saturated Sands)

  • 김동수;이세현;추연욱
    • 한국지반환경공학회 논문집
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    • 제7권1호
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    • pp.55-66
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    • 2006
  • 사질토의 액상화에 대한 저항 강도는 포화도에 상당히 의존한다. 압축파 속도는 현장에서 쉽게 측정이 가능하고 포화도의 영향을 크게 받기 때문에 현장 지반의 포화도를 예측하고자 할 때 효율적으로 사용될 수 있다. 본 논문에서는 시료의 포화가 가능하고 전단파, 압축파 속도 측정 및 비배수 상태에서 비틂전단 시험을 수행시 유발되는 과잉간극수압을 측정할 수 있는 비틂전단 시험기를 개발하였다. 토요라 모래에 대해 전단파, 압축파 속도 측정이 수행되고, 비배수 비틂전단 시험을 실시하였다. 포화도(B값)에 따른 시료의 전단파 속도 및 압축파 속도를 이론식과 비교하여 개발된 시험기를 검증하였으며, 여러 B값에서 비배수 TS 시험동안 유발되는 과잉 간극수압의 변화를 측정 분석하였다.

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지반 구조의 불확실성이 고려된 1차원 확률론적 지반응답해석 (1D Probabilistic Ground Response Analysis)

  • 황혜진;박형춘
    • 한국지진공학회논문집
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    • 제18권2호
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    • pp.73-78
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    • 2014
  • In this paper, the stochastic 1D site response analysis method using Monte Carlo simulation and considering thespatial variation of shear wave velocity profile isproposed. To consider thespatial variation of shear wave velocity profile for 1D site response analysis, the proposed method generates random shear wave velocity profiles representing the target site, and Monte Carlo simulation is used to calculate theprobability distribution of the site response analysis results such as thepeak ground acceleration. Through the field application, The applicability of the proposed method is verified through field application.

An Extended Numerical Calibration Method for an Electrochemical Probe in Thin Wavy Flow with Large Amplitude Waves

  • Park, Ki-Yong;No, Hee-Cheon
    • 한국원자력학회:학술대회논문집
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    • 한국원자력학회 1998년도 춘계학술발표회논문집(1)
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    • pp.553-558
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    • 1998
  • The calibrating method for an electrochemical Probe, neglecting the effect of the normal velocity on the mass transport, can cause large errors when applied to the measurement of wall shear rates in thin wavy flow with large amplitude waves. An extended calibrating method is developed to consider the contributions of the normal velocity. The inclusion of the turbulence-induced normal velocity term is found to have a negligible effect on the mass transfer coefficient. The contribution wave-induced normal velocity can be classified on the dimensionless parameter V. If V above a critical value of V, $V_{crit}$, the effects of the wave-induced normal velocity become larger with an increase in V. IF V its effects negligible for V < $V_{crit}$. The unknown shear rate is numerically determined by solving the 2-D mass transport equation inversely. The president inverse method can predict the unknown shear rate more accurately in thin wavy flow with large amplitude waves than the previous method.

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굵은 골재 최대치수 및 시멘트 종류에 따른 압축강도와 전단파 속도의 상관관계에 대한 실험적 연구 (An Experimental Study on Relation between compressive strength and Shear Wave velocity for characteristics of coarse aggregate size and type of cement)

  • 안지환;전성일;남정희;권수안
    • 한국도로학회논문집
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    • 제13권1호
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    • pp.169-175
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    • 2011
  • 콘크리트에서 강도는 콘크리트의 물리적 특성을 평가할 수 있는 중요한 인자 중 하나이며 콘크리트에 가장 많은 부피를 차지하는 것이 골재이다. 또한 시멘트는 콘크리트 만드는 결합재로서 이 역시 강도와 매우 밀접한 관계가 있다. 이러한 골재와 시멘트의 특성이 콘크리트 압축강도와 전단파 속도의 상관관계에 미치는 영향을 파악하고자 굵은 골재 최대치수와 시멘트 종류별로 실험을 실시하였다. 시멘트는 1종 시멘트와 초속경 시멘트를 사용했고, 골재는 서로 다른 지역의 3가지 골재를 사용하였다. 골재의 입도는 굵은 골재 최대치수 19mm와 13mm의 단입도 골재를 사용하여 동일 배합시 압축강도와 전단파 속도의 상관관계를 살펴보았다. 또한 골재의 특성을 정량화 하고자 LA마모시험을 실시하였다. 그 결과 압축강도와 전단파 속도의 상관관계는 시멘트 종류에 따라 달랐으나, 골재의 종류, 입도 및 마모감량에 관계없이 일정한 상관성을 보이는 것으로 나타났다.

MASW 조사를 통한 사력댐 코어존 동적물성의 평가 (Estimation of Dynamic Characteristics of Core Zone of Rockfill Dam by Multi-channel Analysis of Surface Waves)

  • 이종욱;하익수;오병현
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2008년도 추계 학술발표회
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    • pp.860-868
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    • 2008
  • Seismic safety analysis of rockfill dams are consist of the stability analysis as an simplifed method and the dynamic analysis as an detailed method. When high risk dams such as Multi-purpose dams were often applied detailed method by dynamic analysis, dynamic properties of dam materials such as shear modulus are considered as most important factor. Dynamic material properties such as shear modulus had to be investigated by cyclic triaxial test et al. during design and construction stage but these were not conducted because of the condition of domestic seismic design technique. MASW and SASW methods had been applied as a non destructive method to investigate dynamic material properties of existing rockfill dam, has no problems in dam safety at present. These methods were usually performed under the assumptions that the subsurface can be described horizontally homogeneous and isotropic layers. Recent studies(Marwin, 1993, Kim, 2001) showed that surface waves generated through inclined structures have different characteristics from those through a horizontally homogeneous layered model. further Kim et al(2005) and Min and Kim(2006) showed that central core type rockfill dam overestimated the shear wave velocities as increasing the depth through the 3D numerical modelling dut to the effect of outer rockfill and geometrical reasons In this study the results of shear wave velocities of seven rockfill dams form comprehensive facility review, was carried out from 2003 to 2007, were collected and analysed to establish the shear wave velocity distribution characteristics in increasing confining stress in rockfill dams and surface wave velocity ranges in rockfill dam through MASW and the limitation in application are discussed to be utilized as an reference value for dynamic analysis.

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HWAW방법을 이용한 지반의 전단파 속도 3-D 영상화 (3-Dimensional Imaging of Shear Wave Velocity in the Soil Site using HWAW Method)

  • 박형춘;황혜진;조성은
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2010년도 춘계 학술발표회
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    • pp.176-181
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    • 2010
  • The evaluation of shear modulus (or shear wave velocity) profile of the site is very important in various fields of geotechnical engineering. In the field, there exist spatial variations of shear modulus that case uncertainty in the geotechnical analysis or design. So it is necessary to evaluate the spatial variation of shear wave velocities of the soil site. In this study, the HWAW method is applied to the determination of a 3-D Vs map of soil site. The HWAW method, which is based on harmonic wavelet transforms, has been developed to determine phase and group velocities of waves. The HWAW method uses only the signal portion of the maximum local signal/noise ratio to evaluate the phase velocity in order to minimize the effect of the noise. The field testing of this method is relatively simple and fast because only one experimental setup, which consists of one pair of receivers on the surface, is needed using a short receiver spacing setup (1~3m). These characteristics make it possible to determine detailed local Vs profile in the site with lateral Vs variation and to evaluate 3-D Vs map by performing a series of tests on the grid. To estimate the applicability of the proposed method, field tests were performed. Through field applications validity and applicability of the proposed method were verified.

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개선된 직접전단시험을 이용한 전단영역의 거동 (Behavior of Shear Zone by Improved Direct Shear Test)

  • 변용훈;쭝꽝훙;짠밍콰;이종섭
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2010년도 춘계 학술발표회
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    • pp.607-614
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    • 2010
  • Shear behavior of granular soils largely affects the safety and stability of underground and earth structures. This study presents the characteristics of shear zone in a direct shear test using shear wave and electrical resistivity measurements. An innovative direct shear box made of transparent acrylic material has been developed to prevent direct electric current. Bender elements and electrical resistivity probe are embedded in the wall of direct shear box to estimate the shear wave velocities and the electrical resistivity at the shear and non-shear zones. Experimental results show that the void ratio and shear wave velocity at shear zone increase during shearing while the values remain constant at non-shear zone. The results demonstrate correlation among the contact force, small strain shear modulus, and void ratio at shear zone. This study suggests that the application of the modified direct shear box including shear wave and electrical resistivity measurements may become an effective tool for analyzing soil behavior at shear zone.

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상시미동 측정을 통한 천부 횡파속도 연구 (Shallow Shear-wave Velocities Using the Microtremor Survey Method)

  • 황윤구;김기영
    • 지질공학
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    • 제16권4호
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    • pp.381-392
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    • 2006
  • 상시미동을 이용하는 수동적 표면파 탐사를 결정질암 기반암 지역에서 실시하여, 내진설계 지반분류 기준인 30 m 깊이까지의 평균 횡파속도(Vs30)를 구하고자 연구를 수행하였다. 시험자료는 조사지 A와 B에서 삼각형 배열과 'L' 자형 직각 배열로 2 ms 간격으로 4초 동안 기록하였다. 조사지 A에서 기록한 자료를 공간 자기상관 방법으로 분석하여 위상속도 스펙트럼을 작성하고, 수신기 배열의 길이 및 형태, 기록 횟수, 수신기 수 등의 주요인자들의 영향을 고찰하였다. 조사지 B에서 상시미동 기록자료의 역산을 통해서 구한 횡파속도와 근처 시추공에서 수직탄성파 방법으로 구한 결과가 대체로 일치함을 보여 상시미동을 이용한 표면파 탐사법이 Vs30을 구하는데 효율적인 방법으로 판단된다.