• 한국해안해양공학회지
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• 제14권3호
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• pp.222-231
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• 2002

ADP는 음향의 Doppler효과를 이용하여 층별 유속과 유향을 측정하는 장비이며, 최근에는 반사음향의 강도로부터 부유 퇴적물의 농도측정이 가능하다고 제기되고 있다. 본 연구에서는 염산 인근의 한 정점에 ADP 기기를 설치하고 자료를 수집하였다. 부유사 농도를 분석하기 위하여 해수 분석을 통한 음향계수를 정한 후 보정된 음향강도를 이용하여 부유사 농도를 구하였다. 관측된 부유사 농도분포 식은 해석해와 비교하였으며, 농도변화의 경향에 대해서는 비교적 양호한 결과를 나타냈다. 또한, 관측기간 동안의 부유물질의 이동량에 대한 정량적 결과를 얻었으며 ADP를 활용한 연직방향의 부유입자 농도변화를 관측할 수 있음을 보였다.

• 한국해양학회지
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• 제28권4호
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• pp.313-322
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• 1993

한국남서해역은 음향학적 특징에 따라 4개의 음향학적 퇴적상 (acoustic facies) 으로 구분된다. 고해상도 (3.5kHz) 물리탐사기록에 나타난 대표적인 음향학적 특징은 확산된 형(prolonged type), 내부 반사형(internal reflected type), 비투과 형 (non-penetrated type)과 투명한 형(transparent type)이다. 이러한 형(type)들은 해 저면 상황(bottom condition)과 퇴적물의 입도, 굳기(compaction)에 따라 변화한다. 음향학적 퇴적상 I은 확산된 형이 대표적으로 나타난다. 이 형은 불규칙 또는 규칙적 인 해저면 상황과 자갈, 패각편을 함유한 조립질퇴적물에 의해 음파신호가 하부로 흡 수되어 나타난다. 음향학적 퇴적상 II는 내부반사형이 나타난다. 내부반사구조는 퇴적 물의 굳기변화에 의해 발생하는 것으로 추측된다. 음향학적 퇴적상 III은 비투과 형이 나타난다. 이는 분급이 양호한 세립사와 극세립사가 퇴적된 곳에서 음파신호가 투과 하지 못하고 해저면에서 산란되어 나타난다. 음향학적 퇴적상 IV는 일정한 층후에 내 부반사 구조가 없는 투명한 형이 나타난다. 고해상도 물리탐사 기록상에 나타난 음향 학적 형들은 퇴적층서 뿐만 아니라 천해저의 퇴적기작에 대한 중요한 정보를 나타낸 다.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2003년도 춘계학술대회
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• pp.1603-1608
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• 2003

The Present Study reported on the experimental and numerical results of heat transfer in the acoustic fields induced by ultrasonic waves. The strong upwards flow called as acoustic streaming was visualized by a particle image velocimetry (P.I.V). in addition, the augmentation of heat transfer was experimentally investigated in the presence of acoustic streaming and was compared with the profiles of acoustic pressure calculated by the numerical analysis. Experimental and numerical studies clearly show that acoustic pressure variations are closely related to the augmentation of heat transfer.

• 한국가시화정보학회:학술대회논문집
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• 한국가시화정보학회 2004년도 추계학술대회 논문집
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• pp.22-25
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• 2004

The present paper investigated the correlation between acoustic pressure and heat transfer augmentation in acoustic fields. The acoustic pressure predicted by numerical work and compared with the augmentation ratio of heat transfer coefficient was experimentally measured. Also, particle image velocimetry(PIV) was used for the visualization of velocity vectors and kinetic energy distribution inside liquid region. For the numerical work, SVS programed with Fortran language and based on a coupled FE-BEM was used. Results of the present study, the acoustic pressure is increased by $60\%$ and the largest augmentation of heat transfer about $28\%$ was measured. Finally, the profiles of acoustic pressure is consistent with that of augmentation of heat transfer. It is concluded that a correlation exists between the acoustic pressure and the heat transfer augmentation.

• 지구물리와물리탐사
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• 제7권1호
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• pp.62-69
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• 2004

The objective of this study is to estimate the distribution of a zone disturbed by excavation (EDZ) around tunnels that have been excavated at about 500 m depth in pre-Tertiary hard sedimentary rock. One of the most important tasks is to evaluate changes in the dynamic stability and permeability of the rock around the tunnels, by investigating the properties of the rock after the excavation. We performed resistivity and acoustic tomography using two boreholes, 5 m in length, drilled horizontally from the wall of a tunnel in pre-Tertiary hard conglomerate. By these methods, we detected a low-resistivity and low-velocity zone 1 m in thickness around the wall of the tunnel. The resulting profiles were verified by permeability and evaporation tests performed at the same boreholes. This anomalous zone matched a high-permeability zone caused by open fractures. Next, we performed resistivity monitoring along annular survey lines in a tunnel excavated in pre-Tertiary hard shale by a tunnel-boring machine (TBM). We detected anomalous zones in 2D resistivity profiles surrounding the tunnel. A low-resistivity zone 1 m in thickness was detected around the tunnel when one year had passed after the excavation. However, two years later, the resistivity around the tunnel had increased in a portion, about 30 cm in thickness, of this zone. To investigate this change, we studied the relationship between groundwater flow from the surroundings and evaporation from the wall around the tunnel. These features were verified by the relationship between the resistivity and porosity of rocks obtained by laboratory tests on core samples. Furthermore, the profiles matched well with highly permeable zones detected by permeability and evaporation tests at a horizontal borehole drilled near the survey line. We conclude that the anomalous zones in these profiles indicate the EDZ around the tunnel.

• 에너지공학
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• 제13권2호
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• pp.152-160
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• 2004

The present study investigates on the experimental and numerical results of heat transfer in the acoustic fields induced by ultrasonic waves. The strong upwards flow which moves from the bottom surface in a cavity to the free surface called as "acoustic streaming" was visualized by a particle image velocimetry (PIV). In addition, the augmentation ratio of heat transfer was experimentally investigated in the presence of acoustic streaming and was compared with the profiles of acoustic pressure calculated by the numerical analysis. A coupled finite element-boundary element method (FE-BEM) was applied for a numerical analysis. The results of experimental and numerical studies clearly show that acoustic pressure variations caused by ultrasonic waves in a medium are closely related to the augmentation of heat transfer.

• 대한설비공학회:학술대회논문집
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• 대한설비공학회 2005년도 동계학술발표대회 논문집
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• pp.591-596
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• 2005

The objectives in the present study are to investigate that the enhancement heat transfer was experimentally measured and was compared with the acoustic pressure obtained by numerical analysis. From the results of the present study, a strong Fluid motion initiated by ultrasonic vibrations can affect heat and mass transfer. This phenomenon. called acoustic streaming, clearly observed by PIV measurement leads to increase in velocity of a Fluid which is a crucial physical concept to explain the enhancement heat transfer. The heat transfer coefficient is increased with increase in the ultrasonic intensities. The largest enhancement heat transfer (about 26%) is measured at the ultrasonic intensity of 300W. Acoustic streaming results from sudden acoustic pressure variations in the liquid. The results of numerical analysis reveal that acoustic pressure is increased by 59.5% at the ultrasonic intensity of 300W. The higher acoustic pressure near four ultrasonic transducers develops more intensive flow destroying the flow instability. Also, the profiles of acoustic pressure variation are consistent with those of enhancement heat transfer.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2004년도 추계학술대회
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• pp.1069-1074
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• 2004

This study investigated the effect of pressure variations on augmentation of heat transfer when the ultrasonic waves were applied. The augmentation ratio of heat transfer was experimentally investigated and was compared with the profiles of pressure distributions calculated applying a coupled finite element-boundary element method (coupled FE-BEM). As the ultrasonic intensities increase from 70W to 340W, the velocity of the liquid paraffin is found to increase as well as kinetic energy, This physical behavior known as quasi-Eckart streaming results from acoustic pressure variations in the liquid. Especially, the higher acoustic pressure distribution near two ultrasonic transducers develops more intensive flow (quasi-Eckart streaming), destroying the flow instability. Also, the profile of acoustic pressure variation is consistent with that of augmentation of heat transfer. This mechanism is believed to increase the ratio of hear transfer coefficient.

• Journal of Advanced Marine Engineering and Technology
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• 제34권8호
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• pp.1222-1229
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• 2010

비선형 측심기를 이용한 초고해상 음향탐사는 기존의 고해상 음향탐사보다 투과력은 작지만 해상력이 뛰어나기 때문에 천해역에서의 해저환경조사에 유용하게 사용된다. 비선형 지층탐사 시스템은 정확한 수심측정 뿐 아니라 퇴적층과 하부구조에 대한 상세한 정보를 제공한다. 특히 상부 퇴적층의 정밀층후 및 퇴적구조 확인을 통해 해저에 파묻혀 있는 pipeline, 침몰선박, 인위적 물체 등에 대한 탐색에 이용된다. 이 연구에서는 초고해상 지층탐사기를 이용하여 얻어진 지층탐사 기록과 지질자료를 대비하여 오염퇴적층을 구분하였다. 그리고 지층 기록에 나타나는 음향이상을 해석하여 해저에 매설된 케이블의 매설 깊이를 검측하였다.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2008년도 공동학술대회
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• pp.79-84
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• 2008

초고해상 음향탐사는 기존의 고해상 음향탐사보다 투과력은 작지만 해상력이 뛰어나기 때문에 천해역에서의 해저환경조사에 유용하게 사용된다. 특히 상부 퇴적층의 정밀 층후 및 퇴적구조 확인을 통해 해저에 파묻혀 있는 pipeline, 침몰선박, 인위적 물체 등에 대한 탐색에 이용된다. 이 연구에서는 초고해상 지층탐사기를 이용하여 얻어진 지층탐사 기록과 지질자료를 대비하여 오염퇴적층을 구분하였다. 그리고 지층 기록에 나타나는 음향이상을 해석하여 해저에 매설된 케이블의 매설 깊이를 검측하였다.