• Transactions of the Korean Society of Mechanical Engineers A
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• v.38 no.12
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• pp.1335-1343
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• 2014

Piezoelectric paint can be used to monitor vibrations or impacts occurring in large engineering structures such as ships and airplanes. This study investigated the impact detection characteristics of a piezoelectric paint sensor and possible errors in detecting impacts according to boundary conditions. The piezoelectric paint sensor used in this study was coated on an aluminum plate with four different electrode areas. After the occurrence of the poling process, the output voltages from the paint sensors were obtained when impact occurred in a certain sensor region. The experimental results revealed a large difference in magnitudes between the sensor signal in the impact region and those in the other regions, and this relation was maintained regardless of the changes in the boundary conditions.

• Journal of Korean Society for Geospatial Information Science
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• v.12 no.3 s.30
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• pp.23-31
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• 2004

Cadastral surveying is related to demarcating legal boundaries and areas for the sake of registering a properly on cadastral records or restoring registered boundaries on the ground. It is composed of control surveying (cadastral triangulation and supplementary control surveying) and detail surveying. Detail surveying is classified into plane table surveying by graphical cadastral map and numerical surveying by boundary point coordinates. In this study we compared the accuracy of plane table surveying with numerical surveying using Parcel Based Land Information System(PBLIS) data constructed by the cadastral map digitalization business. In conclusion the result by numerical surveying was analyzed as more accurate than the result of plane table surveying, as Root Mean Square Errors(RMSE) of graphical cadastral surveying is 0.766m and that of numerical cadastral surveying using Total Station(T/S) is 0.683m. Therefore, PBLIS data is expected to be used for surveying legal boundaries and areas in the near future.

• Journal of KIISE:Software and Applications
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• v.32 no.1
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• pp.41-49
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• 2005

In this Paper, we Propose an automatic lung registration technique using local distance propagation for correcting the difference between two temporal images by a patient's movement in abdomen CT image obtained from the same patient to be taken at different time. The proposed method is composed of three steps. First, lung boundaries of two temporal volumes are extracted, and optimal bounding volumes including a lung are initially registered. Second, 3D distance map is generated from lung boundaries in the initially taken volume data by local distance propagation. Third, two images are registered where the distance between two surfaces is minimized by selective distance measure. In the experiment, we evaluate a speed and robustness using three patients' data by comparing chamfer-matching registration. Our proposed method shows that two volumes can be registered at optimal location rapidly. and robustly using selective distance measure on locally propagated 3D distance map.

• Proceedings of the Korea Water Resources Association Conference
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• 2020.06a
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• pp.394-394
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• 2020

최근 빈번히 발생하고 있는 슈퍼 태풍과 집중호우로 인해 크고 작은 침수피해가 발생하고 있다. 우리나라는 4대강 사업을 통해 주요 국가하천에 대한 정비를 마친 바 있으나 이후 지속적으로 변화하는 하천 환경에 대한 홍수예측 모형의 반영은 미비한 실정이었다. 따라서 본 연구에서는 낙동강 본류 및 지류의 최신 단면자료를 수집하여 수리학적 홍수예측모형에 반영하고자 하였다. 또한, 기존의 모형에 비해 정확도를 개선할 수 있는 방안을 모색하여 적용성을 검증하고 이를 반영한 수리학적 홍수예측 모형을 제시하고자 한다. 본 연구에서는 낙동강 본류 및 주요 지류에 대한 최신 횡단면 측량자료를 활용하여 1차원 수리학적 홍수예측 모형을 구축하고 2012년 태풍 산바 사상에 대한 검보정을 실시하였다. 대상구간은 안동조정지댐으로부터 낙동강 하구둑 하류 8km지점이며, 상류단 경계조건은 안동조정지댐 방류량을 입력하고 하류단 경계조건은 가덕도 조위관측소의 조위를 활용하였다. 또한, 반변천, 내성천, 위천, 감천, 금호강, 황강, 남강 등 7개 지류에 대한 하도를 하도추적이 가능한 네트워크 모형으로 구축함으로써 지류에 대한 홍수예보에 활용할 수 있도록 하였다. 낙동강 본류의 하도 길이는 340km, 824개의 단면으로 구성하였으며, 지류를 포함한 전체 하도 길이는 572km, 1,570개의 단면으로 구성하였다. 또한, 낙동강 본류에 위치한 8개의 다기능보와 지류에 위치한 횡단구조물의 반영을 위해 다기능보의 제원 및 하천기본계획을 참고하여 내부경계조건으로 활용하였다. 본 연구에서 구축된 낙동강 본류 및 지류의 수리학적 홍수예측 모형을 낙동강 유역에 대한 홍수주의보 및 홍수경보 등 홍수특보 발령 업무에 활용함으로써 정확한 홍수예보가 가능하도록 하였다.

• Journal of the Korean Society of Hazard Mitigation
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• v.10 no.5
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• pp.159-168
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• 2010

This study investigates the relationships between the maximum freshwater pumping discharge and hydraulic properties of coastal aquifer using a laboratory model. The experiment performed the fresh pumping test in various locations near the saltwedge induced by saltwater intrusion to freshwater over aquifer characteristics of hydraulic conductivity, salinity, and ground surface slope. Saltwater pumping also tested to protest saltwater intrusion to the excessively discharging freshwater well. The maximum freshwater discharges were achieved, and then the optimum saltwater discharges were measured. It is found that greater hydraulic conductivity and ground surface slope produced greater the maximum freshwater pumping discharge. Salinity gave less impact on the pumping discharge relatively. Higher freshwater discharge was found at higher hydraulic conductivity and steeper ground surface slope. The optimum saltwater discharge required 14% more pumping rate than the maximum freshwater discharge to keep saltwater intrusion to the freshwater pumping well. Pumping well located closer to salt-wedge profile promoted less freshwater pumping discharge. Therefore, pumping well location, hydraulic conductivity, ground surface slope, and salinity should be taken into account in freshwater pumping in coastal aquifer.

• 한국해양학회지
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• v.30 no.1
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• pp.57-63
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• 1995

Two-layered fluid with sloping bottom and top(${\beta}$-effect) in rigid cylinder is put on the rotating table. To drive the lower-layer motion in "the Sverdrup type" flow external fluid is pumped into the lower-layer. By introducing inlet-outlet system in the upper-layer, an analogy to the Tsushima Tsugaru, Soya of the East Sea has been tested. The position of the inlet-outlet system and the difference between the strength of inlet or outlet flow are changed to see the effects of the wind stress on the upper-layer. The northern part of inflow toward the outlet may be interpreted roughly as the position of the polar front in the East Sea. Experimental observations have revealed that the inflow flows along the western boundary before it separates into the interior and flows straight toward the outlet position. However, the wind effect is imposed upon the upper-layer, the western boundary flow branches into two parts of which one flows along the boundary and the other flows into the interior under the influence of negative wind stress curl, while southward western boundary flow seems to block the flow and deflect it to the interior. The changes in the position of inlet-outlet system produce more significant changes in flow pattern in that cyclonic flow in the north controls the northern extent of the polar front by deflecting the northward interior motion toward the west(outlet). Interface displacement which depends strongly on the velocity difference between two layers seems to play crucial role in terms of the path of upper-layer flow, particularity, the inflow.

• Transactions of the Korean Society of Mechanical Engineers B
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• v.39 no.10
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• pp.795-803
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• 2015

The boundary layer developing over the suction surface of a first-stage turbine blade for power generation has been investigated in this study. For three locations selected in the region where local thermal load changes dramatically, mean velocity, turbulence intensity, and one-dimensional energy spectrum are measured with a hot-wire anemometer. The results show that the suction-surface boundary layer suffers a transition from a laminar flow to a turbulent one. This transition is confirmed to be a "separated-flow transition", which usually occurs in the shear layer over a separation bubble. The local minimum thermal load on the suction surface is found at the initiation point of the transition, whereas the local maximum thermal load is observed at the location of very high near-wall turbulence intensity after the transition process. Frequency characteristics of turbulent kinetic energy before and after the transition are understood clearly from the energy spectrum data.

• Journal of the Korean Society for Aeronautical & Space Sciences
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• v.37 no.11
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• pp.1055-1065
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• 2009

In this study, stability analysis of boundary layers on airfoils is performed by using parabolized stability equations(PSE). Boundary layer edge conditions are obtained by compressible inviscid flow calculations. Mean velocity and temperature profiles of the laminar boundary layer are obtained by solving compressible boundary layer equations in generalized curvilinear coordinates with fourth order accuracy in the wall normal direction. Laminar mean flow profiles are used as input data for PSE to investigate growth rates of disturbances and stability characteristics. For the cases of boundary layer on NACA0012 and HSNLF(1)-0213 airfoils at Mach number 0.5, growth rates with respect to disturbance frequencies and profiles of disturbance amplitude are investigated. The effect of angle of attack on stability characteristics are examined at both upper and lower surfaces. The neutral stability curves, effect of Mach number and effect of airfoil section shapes are also analyzed.

• Proceedings of the Korea Water Resources Association Conference
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• 2012.05a
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• pp.610-610
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• 2012

한강하구는 국가하천인 한강, 한강의 1지류인 임진강과 북한 황해도의 예성강이 만나 한강하류 수역을 형성하여 서해 중부해역과 합류하여 매우 복잡한 수리학적 특성을 지닌다. 또한 한강하구의 경우 교량, 수중보 등의 하천 구조물이 설치되어 있다. 수리학은 크게 수위와 관계되는 현상, 하상변화와 관계되는 현상, 외부 환경과 관계되는 현상으로 살펴 볼 수 있다(최계운, 2005). 하천구조물이 설치됨에 따라 구조물 주변에서 국부적으로 수위가 상승되거나 유속이 변화, 세굴현상 등의 하상 변화, 구조물 설치에 따른 생태계의 단절 현상 등 수리학적 현상에 영향을 미치게 된다. 한강하구는 이러한 복잡한 흐름현상에 더해 군사적으로 민감한 지역의 특성으로 현장의 접근성에 한계가 있어 이 지역의 연구조사는 더욱 어렵다. 그간 한강하구의 흐름 현상을 규명하기 위한 연구 방법으로 수치모의를 통한 다양한 연구가 진행되어 왔다. 수리학적 흐름 현상을 계산하기 위한 필수 조건인 하류경계조건 설정에도 어려움이 수반된다. 이 때문에 한강의 수리학적 수치모의 실험에 관한 연구들은 한강하구의 얕은 수심과 해석의 공간적 범위를 소홀히 하고, 공릉천 합류부를 기준으로 하류지점에 대해서는 인천 조위관측소의 조위자료를 사용하거나 하천정비기본계획상의 기점수위를 일괄적으로 적용하여 지점에 따른 수위의 차이를 적용하지 못하는 한계를 지닌다. 따라서 본 연구에서는 남북접경지역 접근의 어려움으로 인하여 발생되는 한강하구 흐름해석의 불확실성을 명확히 하기 위한 방안으로 한강하구지역에 해당 군부대와 군사정전위원회의 출입허가 승인을 얻어 현장조사를 실시하였다. 사전조사를 통하여 성동교, 대산교, 공릉천, 화도돈대, 철곶돈대 전방 수변, 애기봉전망대 전방 수변을 조사 지점으로 선정하였다. 기존 연구에서는 한강하구의 공릉천 합류부 지점을 하류경계조건으로 채택하고 있으나, 현장조사를 통하여 얻을 자료를 분석한 결과 공릉천 합류부 지점의 수위는 강우발생에 대한 하천의 영향을 받는 것으로 나타나 하류경계조건으로 적정하지 않은 것으로 판단되었으며, 공릉천보다 하류지역에 위치한 지역에 대하여 하류경계조건으로 적정한 지역을 찾을 수 있었다. 수치해석 시에는 공간적 범위와 연구의 목적을 고려하여 각 지점의 실제 관측 자료를 활용한 경계조건을 사용하는 것이 적합한 것으로 판단되며 보다 많은 현장조사와 특성분석을 통한 정확한 경계조건의 구축이 필요할 것으로 사료된다.

• Journal of the Korea Institute of Information and Communication Engineering
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• v.26 no.6
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• pp.865-871
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• 2022

In this paper, we propose a method of extracting prostate region using morphological characteristics of ultra-sonic image of prostate. In the first step of the proposed method, the edge area of the prostate image is extracted. The histogram of ultra-sonic image is used to extract base objects to detect the upper edge of prostate region by altering the contrast of the image, then, the lower edges of the extracted base objects are connected by using monotone cubic spline interpolation to extract the upper edge. Step 2, Otsu's binarization is applied to the region under the extracted upper edge of the prostate ultra-sonic image to extract the lower edge of prostate. In the last step, the upper and the lower edges are connected to extract prostate region and by comparing the extracted region of prostate with the one measured manually, the result showed that the morphological characteristics of prostate in ultrasonic image can be utilized to extract the prostate region.