• 한국지반공학회논문집
• /
• 제21권4호
• /
• pp.71-81
• /
• 2005

지반의 표면에서 비파괴적으로 지반의 구조나 하부강성을 구하는 표면파 기법의 초기형태는 2차원 평면파의 측정과 해석에 기반을 두었으나, 이후 3차원 입체파에 기반을 두는 형태로 발전하였다. 그러나 체적파의 간섭, 근접장 효과, 표면파 측정해상도의 한계 등으로 인하여 3차원 입체파의 활용은 제한적이었고, 측정 지반을 대표하는 1차원 평가에 국한되었다. 본 연구에서는 SASW 시험의 수치모델링을 통하여 수직 레일레이파, 수평 레일레이파, 러브파 등의 표면파 전파 특성을 3차원 영역에서 심도있게 고찰하였으며, 표면파의 근접장 효과를 최소화하기 위한 새로운 필터조건을 정립하였고, 결과적으로 CAP(common-array-profiling)-SASW라는 기법이라고 하는 개선된 표면파 기법을 제안하게 되었다. CAP-SASW 기법의 적용으로 인하여 좁은 폭의 지반단면에 대한 전단파 속도 주상도 평가가 가능하게 되었고, 지반 단면에 대한 2차원 지반강성 평가도 가능하게 되었다. 본 연구에서 제안한 기법의 검증을 위하여 자연 지반을 대상으로 하여 CAP-SASW 시험, 기존 SASW 시험, 다운홀 시험 등을 수행하여 획득된 전단파 주상도를 비교하였다.

• Geomechanics and Engineering
• /
• 제31권6호
• /
• pp.615-622
• /
• 2022

In this paper, considering the temperature dependence of material physical parameters as well as the effects of thermal effect and shear deformation, we have conducted an in-depth study on the wave propagation of functionally graded (FG) materials circular plate in thermal environment based on the physical neutral surface concept. The dynamic governing equations of functionally graded plates are established, and the dispersion relation of wave propagation is derived. The influence of different temperature fields on the propagation characteristics of flexural waves in FG circular plates is discussed in detail. It can be found that the phase velocity and group velocity of wave propagation in the plate decrease with the increase of temperature.

• 한국환경과학회지
• /
• 제13권8호
• /
• pp.721-731
• /
• 2004

The dispersion of suspended particulates in the coastal complex terrain of mountain-inland basin (city)-sea, considering their recycling was investigated using three-dimensional non-hydrostatic numerical model and lagrangian particle model (or random walk model). Convective boundary layer under synoptic scale westerly wind is developed with a thickness of about I km over the ground in the west of the mountain, while a thickness of thermal internal boundary layer (TIBL) is only confined to less than 200m along the eastern slope of the mountain, below an easterly sea breeze circulation. At the mid of the eastern slop of the mountain, westerly wind confronts easterly sea breeze, which goes to the height of 1700 m above sea level and is finally eastward return flow toward the sea. At this time, particulates floated from the ground surface of the city to the top of TIBL go along the eastern slope of the mountain in the passage of sea breeze, being away the TIBL and reach near the top of the mountain. Then those particulates disperse eastward below the height of sea-breeze circulation and widely spread out over the coastal sea. Total suspended particulate concentration near the ground surface of the city is very low. On the other hand, nighttime radiative cooling produces a shallow nocturnal surface inversion layer (NSIL) of 200 m thickness over the inland surface, but relatively thin thickness less than 100m is found near the mountain surface. As synoptic scale westerly wind should be intensified under the association of mountain wind along the eastern slope of mountain to inland plain and further combine with land-breeze from inland plain toward sea, resulting in strong wind as internal gravity waves with a hydraulic jump motion bounding up to about 1km upper level in the atmosphere in the west of the city and becoming a eastward return flow. Simultaneously, wind near the eastern coastal side of the city was moderate. Since the downward strong wind penetrated into the city, the particulate matters floated near the top of the mountain in the day also moved down along the eastern slope of the mountain, reaching the. downtown and merging in the ground surface inside the NSIL with a maximum ground level concentration of total suspended particulates (TSP) at 0300 LST. Some of them were bounded up from the ground surface to the 1km upper level and the others were forward to the coastal sea surface, showing their dispersions from the coastal NSIL toward the propagation area of internal gravity waves. On the next day at 0600 LST and 0900 LST, the dispersed particulates into the coastal sea could return to the coastal inland area under the influence of sea breeze and the recycled particulates combine with emitted ones from the ground surface, resulting in relatively high TSP concentration. Later, they float again up to the thermal internal boundary layer, following sea breeze circulation.

• 지구물리와물리탐사
• /
• 제14권1호
• /
• pp.42-49
• /
• 2011

대룡 흙댐익 누수경로를 포함한 이상대 탐지를 위하여, 댐 정상부의 250 m 측선을 따라 P 파와 레일리파를 기록하였다. 5 kg 해머를 이용하여 인공적으로 소규모 지진파를 발생시켰으며, 3m 간격으로 설치한 4.5 Hz 수직지오폰 24개로 탐지하였다. 이 저수지댐과 하부 기반암의 P파 속도와 S파 겉보기속도를 초동주시와 레일리파 분산곡선 역산으로 각각 구하였다. 겉보기 동포아송비가 0.46에 달하는 높은 값들이 복통이 위치한 북서쪽 끝부분의 댐 기저와 누수저지를 위해 과거 여러 차례 그라우팅 작업을 실시한 측선 남서쪽 끝 부분의 점토코아 내에서 탐지되었다. 상부 점토코아의 높은 포아송비를 갖는 이 이상대는, 조사 후 실시한 그라우팅 작업 시 그라우트 물질이 유출된 부분에 해당한다. P파 토모그래피와 레일리파 분산곡선 역산을 함께 사용하면 흙댐의 잠재적 누수경로 및 기존 그라우팅 위치를 매우 효과적으로 탐지할 수 있다.

• 지구물리와물리탐사
• /
• 제16권3호
• /
• pp.109-118
• /
• 2013

높이 23 m인 보령시 청천댐 상부와 인근에서 5 kg 해머를 이용하여 소규모 굴절법 및 표면파 탐사를 실시하였다. 인공 지진파의 수직 및 수평성분을 초동주시 토모그래피 및 레일리파 분산곡선 역산을 통하여 천부 P파속도(${\nu}_p$)와 S파속도(${\nu}_s$) 구조를 파악하였다. 중생대 퇴적암질 기반암의 평균 ${\nu}_p$와 ${\nu}_s$는 댐마루 30 m 깊이에서 각각 1650 m/s와 950 m/s, 하류쪽 댐체 끝 지점 10 m 깊이에서 각각 1650 m/s와 940 m/s로 분석된다. 이 층들의 동포아송비는 0.24 ~ 0.25의 범위로, 고화된 퇴적층의 값과 일치한다. 댐체로부터 152 m 하류지점의 깊이 45 m 시추공 부근에서의 SH파 굴절법 토모그램은 10 ~ 12 m 깊이에 평균 vs가 870 m/s인 임계굴절면이 존재함을 보여준다. 이 지역에서는 덮개층의 ${\nu}_p$와 ${\nu}_s$가 각각 500 m/s와 200 m/s인 상부층과 깊이에 따라 속도가 거의 선형으로 증가하는 하부층으로 구성되어 있다.

• 비파괴검사학회지
• /
• 제26권6호
• /
• pp.390-402
• /
• 2006

The elastic properties and thickness of mullite environmental barrier coatings grown through chemical vapor deposition (CVD) on silicon carbide substrates were measured using frequency domain photoacoustic microscopy. In this technique, extremely narrow bandwidth surface acoustic waves are generated with an amplitude modulated laser source. A photorefractive crystal based interferometer is used to detect the resulting surface displacement. The complex displacement field is mapped as a function of source-to-receiver distance in order to extract the wavelength of the surface acoustic wave at a given excitation frequency, and the phase velocity is determined. The coatings tested exhibited spatial variations in thickness and mechanical properties. The measured surface wave dispersion curves were used to extract an effective value for the elastic modulus and the coating thickness. Nanoindentation was used to validate the measurements of the effective elastic modulus. The average elastic modulus measured through the coating thickness using nanoindentation is compared to the effective modulus found using the photoacoustic system. Optical microscopy is used to validate the thickness measurements. The results indicate that the photoacoustic microscopy technique can be used to estimate the effective elastic properties in coatings exhibiting spatial inhomogeneities, potentially providing valuable feedback for the optimization of the CVD growth process.

• 한국지반공학회논문집
• /
• 제28권8호
• /
• pp.55-63
• /
• 2012

깊이에 따른 지반의 전단파 속도(또는 전단탄성계수) 분포는 일반적인 지반 해석 설계 또는 지진해석과 같은 다양한 지반공학분야에서 사용되는 중요한 물성치이다. 이러한 지반의 전단파속도 주상도는 탄성파 탐사를 통해 결정할 수 있으며, 이를 위한 다양한 탄성파 탐사 방법이 연구개발 되어 있다. 표면파 탐사법은 모든 실험이 지표면에서 이루어지는 탄성파 탐사법들 중의 하나로서 현장 실험, 파장(또는 주파수)에 따른 표면 계측파의 위상속도 곡선인 분산곡선의 결정, 역산을 통한 대상 지반의 전단파 속도 주상도의 결정으로 동일하게 구성되어 있다. 본 논문에서는 표면파 실험을 위한 자동화된 역산 방법을 개발하였으며, 제안된 방법을 가장 최근에 개발된 표면파 탐사법들 중 하나인 HWAW(Harmonic Wavelet Analysis of Waves) 방법에 적용하였다. 제안된 방법에서는 새로운 오차함수를 제안하고 이를 이용한 유전자 알고리즘을 역산에 사용하였다. 제안된 방법의 타당성을 검토하고자 수치모의 실험과 현장 실험을 수행하였으며, 이를 통해 제안된 방법의 현장 적용성 및 타당성을 확인할 수 있었다.

• 비파괴검사학회지
• /
• 제33권3호
• /
• pp.264-269
• /
• 2013

Since MFC(macro-fiber composite) transducer has been developed, many researchers have tried to apply this transducer on SHM(structural health monitoring), because it is so flexible and durable that it can be easily embedded to various kinds of structures. The objective of this paper is to figure out the benefits and feasibility of applying MFC transducers to guided wave technique. For this, we have experimentally tested the performance of MFC patches as transmitter and sensors for excitation and reception of guided waves on the thin aluminum alloy plate. In order to enhance the signal accuracy, we applied the FIR filter for noise reduction as well as used STFT(short-time Fourier transform) algorithm to image the guided wave characteristics clearly. From the results, the guided wave generated based on MFC showed good agreement with its theoretical dispersion curves. Moreover, the ultrasonic Lamb wave techniques based on MFC patches in pitch-catch manner was tested for detection of surface notch defects of which depths are 10%, 20%, 30% and 40% of the aluminum plate thickness. Results showed that the notch was detectable well when the notch depth was 10% of the thickness or greater.

• Smart Structures and Systems
• /
• 제3권4호
• /
• pp.439-454
• /
• 2007

In this paper a damage imaging technique using pre-stack migration is developed using Lamb (guided) wave propagation in composite structures for imaging multi damages by both numerical simulations and experimental studies. In particular, the paper focuses on the experimental study using a finite number of sensors for future practical applications. A composite laminate with a surface-mounted linear piezoelectric ceramic (PZT) disk array is illustrated as an example. Two types of damages, one straight-crack damage and two simulated circular-shaped delamination damage, have been studied. First, Mindlin plate theory is used to model Lamb waves propagating in laminates. The group velocities of flexural waves in the composite laminate are also derived from dispersion relations and validated by experiments. Then the pre-stack migration technique is performed by using a two-dimensional explicit finite difference algorithm to back-propagate the scattered energy to the damages and damages are imaged together with the excitation-time imaging conditions. Stacking these images together deduces the resulting image of damages. Both simulations and experimental results show that the pre-stack migration method is a promising method for damage identification in composite structures.

• Geomechanics and Engineering
• /
• 제16권2호
• /
• pp.169-176
• /
• 2018

An attempt has been made here to study the propagation of SH-type surface waves in an elastic medium, which is initially stressed and heterogeneous and has a point source inside the medium. The upper portion of the composite medium is a sandy layer. It is situated on an initially stressed heterogeneous half-space, whose density, rigidity and internal friction are function of depth. The analysis has been carried out by using Fourier transform and Green's function approach. The phase velocity has been investigated for several particular situations. It has been shown that the results of the study agree with those the case of Love wave propagation in a homogeneous medium in the absence of the sandy layer, when the initial stress is absent. In order to illustrate the validity of the analysis presented here, the derived analytical expression has been computed numerically, by considering an illustrative example and the variances of the concerned physical variables have been presented graphically. It is observed that the velocity of shear wave is amply influenced by the initial stress and heterogeneity parameters and the presence of the sandy layer. The study has an important bearing on investigations of different problems in the earth's interior and also in seismological studies.