• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2001년도 봄 학술발표회 논문집
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• pp.49-56
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• 2001

The techniques to make assessment of the structural integrity of underground structures include Infrared thermagraphy, GPR using the reflection of the electromagnetic wave, ultrasonic test, seismic methods using the propagation of elastic wave, and etc These methods have pros and cons in the assessment of the structural integrity in the complex environment of the underground structure, so that a single method alone is not enough to evaluate parameters required for the assessment. In this study, a new seismic method was proposed to improve the existing methods and to provide an additional information like stiffness of concrete. The proposed method combines the advantages of the modified impact-echo test and the SASW method. To verify the validity of the proposed method, a large scale model of a tunnel concrete liner was built and the proposed method was applied to the center of the model and also to the corner of the model which has several distinct reflection boundaries.

• Transactions on Electrical and Electronic Materials
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• 제10권2호
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• pp.53-57
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• 2009

In this paper we develop a method to observe faults in semiconductor devices and transmission lines by calculating the variation of the reflection function in a dielectric microstrip line that has an open-ended termination containing an optically induced plasma region. It is analyzed with the assumption that the plasma is distributed homogeneously in laser illumination. With the non linear material of degradation, the concentration of the carrier in the part of the material has changed. Since the input wave has produced the phenomenon of reflection, the input signal to the open-ended microstrip lines can be observed on reflection to identify the location of the fault. The characteristic impedances resulting from the presence of plasma are evaluated by the transmission line model. The variation of the reflection wave in the microwave system has been calculated by using an equivalent circuit model. The transient response has been also evaluated theoretically for changing the phase of the variation in the reflection. The variation of characteristic response in differentially localized has been also evaluated analytically.

• 기본간호학회지
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• 제16권4호
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• pp.438-448
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• 2009

Purpose: To examine the results of PBL classes for sophomore nursing students during one semester. Method: Self-reflection journals and class evaluation questionnaires were collected from 121 nursing students and analyzed. Results of class evaluation questionnaires were analyzed using mean scores, SD, frequencies and percentages. Significant statements were derived by repeated review of the self-reflection journals by the researchers. Results: The statements, 'Understanding of PBL' 'Improvement of human relationships' 'Expansion of nursing knowledge' 'Excellency in nursing class and application of nursing skills in nursing practices' and 'Improvement of learning ability and attitude during classes' were derived from the self-reflection journals. Analysis of class evaluation questionnaires showed the following scores: prerequisite of PBL (3.0/4), role of facilitator (3.48/4) and satisfaction with PBL learning (3.31/4). Also some complaints such as lack of adequate references in the library, and confusion in at the beginning of PBL were noted. Conclusion: PBL was effective. Using the results of the study for planning a more effective PBL class syllabus is recommended.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2004년도 춘계학술발표회
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• pp.807-814
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• 2004

Land seismic reflection survey has been increasingly demanded in various civil engineering works because of its own ability to delineate layers, water table, to detect cavities or fracture zones, to estimate seismic velocities of each layer. However, our shallow subsurface structures are very complex. The relatively thin layer(mostly soil) to the wavelength directly followed by a basic rock with high impedance used to generate complicated surface waves, kind of channel waves with high amplitude that is dominate in entire seismograms and hence the useful reflection events will be almost hopelessly immersed in the undesired surface waves. Thus, it would seem that the use of traditional seismic survey could not be likely to provide in itself a satisfactory information about our exploration targets. This paper hence introduces an efficient measuring strategy illustrating a properly controlled arrangement of the vertical single force sources commonly used, yielding a very sharply elongated form of P-energy with a minimum of S radiation energy, what we call, P-beam source. Abundant experiments of physical modeling showed that in that way the surface waves could be enormously reduced and the reflection events would be additive and thus reinforced. Examples of field data are also illustrated. The contribution of P-beam source will be great in civil engineering area as well as in general geological exploration area.

• 한국해안·해양공학회논문집
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• 제31권6호
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• pp.403-408
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• 2019

일반적으로 유공벽을 갖는 케이슨(유공케이슨)은 직립식 구조물 벽면에 유공부를 설치하여 반사파의 저감, 월파량의 저감 등의 목적으로 사용된다. 본 연구에서는 유공케이슨 유수실을 골재(사석)로 채운 형태의 구조물에 대한 수리특성(반사계수)을 수리모형실험을 통해 검토하였다. 유수실을 사석으로 채운 경우가 유수실이 비어있는 일반적인 형상보다는 반사계수가 크게 나타났으나, 속채움재를 유수실에 설치하여 중량을 확보함으로서 구조물의 안정성을 확보하고, 일정 수준에서 수리특성을 만족할 수 있는 것으로 검토되었다.

• 한국해안해양공학회지
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• 제19권5호
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• pp.429-435
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• 2007

비선형 Boussinesq 파랑전파 모델에서 방파제, 호안 등의 반사 경계면에 스펀지층을 설치하여 반사율을 모의하는 방법을 제안하였다. 스펀지층의 반사특성을 도출하기 위하여 상대 스펀지폭(스펀지층 폭/입사파장)을 변화시키는 일차원 수치실험을 수행하였다. 실험결과, 상대 스펀지폭을 조정함으로써 무반사에서 완전반사까지 반사율을 효과적으로 구현할 수 있음을 보였으며, 실험결과에 근거하여 반사율과 관련 무차원 변수들간의 다중회귀분석식을 제시하였다. 마지막으로, 본 스펀지층을 이차원 방파제에 적용하였으며, 스펀지층이 반사경계로서 평면 이차원 조건에서도 충분히 효과적으로 사용될 수 있음을 예시하였다.

• Journal of Astronomy and Space Sciences
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• 제33권3호
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• pp.197-205
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• 2016

We investigated two flares in the solar atmosphere that occurred on June 3, 2012 and July 6, 2012 and caused propagation of Moreton and EIT waves. In the June 3 event, we noticed a filament winking which presumably was caused by the wave propagation from the flare. An interesting feature of this event is that there was a reflection of this wave by a coronal hole located alongside the wave propagation, but not all of this wave was transmitted by the coronal hole. Using the running difference method, we calculated the speed of Moreton and EIT waves and we found values of 926 km/s before the reflection and 276 km/s after the reflection (Moreton wave) and 1,127 km/s before the reflection and 46 km/s after the reflection (EIT wave). In the July 6 event, this phenomenon was accompanied by type II and type III solar radio bursts, and we also performed a running difference analysis to find the speed of the Moreton wave, obtaining a value of 988 km/s. The speed derived from the analysis of the solar radio burst was 1,200 km/s, and we assume that this difference was caused by the different nature of the motions in these phenomena, where the solar radio burst was caused by the propagating particles, not waves.

• 한국광학회지
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• 제22권4호
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• pp.170-178
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• 2011

기층의 후면에서 반사한 빛이 미치는 영향을 고려하여 반투명한 기층 위에 박막이 있는 시료의 분광타원상수를 모델링 분석하였다. 후면반사가 타원상수에 미치는 영향을 기층의 복소굴절률과 두께를 사용하여 나타내었고 이를 모델링 분석에 적용하였다. 유리 기층 위에 ITO 박막이 있는 시료에 대해 후면반사를 고려한 표현들을 사용하여 박막의 두께와 복소굴절률 등을 구한 결과가 후면에서 반사된 빛을 제거하여 측정, 분석하는 통상적인 타원법에 의한 결과와 일치함을 보였다.

• 정보저장시스템학회논문집
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• 제2권3호
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• pp.189-195
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• 2006

Bragg detuning effect if, one of the serious problems if the photopolymer is used for the recording material of holography memories. And the critical reasons of that are known as the bulk refractive index change and shrinkage of recording material. However, the trials for analyzing the effect are mainly on the K-sphere and biased on the transmission hologram. So, we approached Bragg detuning effect numerically and applied the method to the transmission holograms and the reflection holograms all together. We simulated it with MATLAB. As a result, the bulk refractive index change causes+Bragg detuning effect on the transmission holograms and the reflection holograms. But the shrinkage leads to+Bragg detuning effect on the transmission hologram and-Bragg detuning effect on the reflective hologram. Compared to experimental result, the bulk refractive index change(${\fallingdotseq}4{\times}10^{-4}$) and the ratio of shrinkage to the thickness of the material(${\fallingdotseq}1.67{\times}10^{-3}$) could be matched with Bragg detuning effect on the transmission hologram and the reflection hologram.

• 지구물리와물리탐사
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• 제11권2호
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• pp.109-115
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• 2008

공학적 목적의 지반조사에 양질의 자료를 제공하기 위해서는 여러 가지 조사들이 동시에 수행되어야 하고 또한 통합적인 해석이 필요하다. 본 연구에서는 천해저에서 지층 경계에 대한 분해능이 뛰어나며 지층 형태 파악이 용이한 2개의 부머와 단일채널 스트리머를 이용한 탄성파탐사 반사법과 지층의 물리적 특성 가운데 중요한 성질인 탄성파 속도를 구할 수 있도록 한 개의 에어건과 4 m 간격의 24채널 해저면 수신케이블을 제작하여 이용한 굴절법을 동시에 수행함으로써 보다 정확한 지질정보 획득을 시도하였다. 단일채널 반사법 탐사자료는 통상적인 전산처리과정을 통하여 해상도 및 품질이 향상된 2차원 고해상 탄성파 단면도를 얻었고, OBC (Ocean Bottom Cable) type의 수진기를 이용하여 얻은 굴절법 탐사자료는 토모그래피 방법을 통하여 속도 단면도를 구하였다. 두 가지 탐사 결과에 대한 통합적인 해석 단계로서 반사법 탄성파 단면도는 굴절법에서 얻은 속도정보를 이용하여 심도 전환된 단면도를 얻었고, 이로부터 3차원 기반암 심도 단면도와 퇴적층 두께 분포도 등에 대한 정보를 도출할 수 있었다. 천해저 지반조사 분야에 본 연구에서 제시한 방법을 이용하면 보다 정확하고 신뢰성 높은 지질정보가 파악될 것으로 사료된다.