• 한국수자원학회논문집
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• 제56권2호
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• pp.103-113
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• 2023

하천 합류부는 서로 다른 지형학적 특성과 수리학적 특성을 가지는 두 개의 하천이 하나로 합쳐지는 구간으로 급격한 흐름의 변화 및 퇴적물의 유입과 수리학적 지형변화가 발생하는 구간이다. 합류부 구간에서는 물질의 종류 또는 온도 차로 유체의 흐름이 밀도 차이로 발생하게 되는데 이것을 밀도류라고 한다. 밀도 차이에 의해 성층이 생긴 수체혼합거동을 파악하기 위해서는 본류 및 지류의 일정 구간을 포함하는 합류부 구간에 대한 정밀한 계측 및 관찰이 필요하다. 이러한 수체 혼합에 대한 종합적인 분석은 유속장 및 유량 정보를 취득하여 파악할 수 있지만, 성층류가 흐르는 하천의 서로 상이한 물리적 특성과 수질특성을 가지는 수체의 혼합양상 및 그에 따른 물질혼합양상을 파악하는데 한계가 있다. 따라서 본 연구에서는 합류부 구간에서의 수온 분포를 통하여 밀도류를 파악하고자 한다. 하천의 광범위한 데이터 중 연직 자료와 수표면 자료를 취득하였고, 이를 통해 합류부의 성층현상을 확인하고자 하였다. ADCP를 보트 측면에 설치하여 저속운행으로 수리량을 측정하는 방식과 YSI를 이용해 측선설치 없이 측선 선정 후 보트를 이용하여 흐름에 직각인 방향으로 이동하며 실시간 농도를 측정하는 방식으로 얻은 연직자료 중 수온, 전도도(Conductivity) 등의 직독식 센서 데이터 값을 사용하여 수온 차에 따른 수체혼합 패턴을 분석하여 합류부의 혼합양상을 분석하고자 하였다. 본 연구는 기존 수질 측정의 한계였던 1차원적인 측정결과가 나타내는 분석결과를 2차원적으로 보완이 가능하며, 비교 분석한 결과를 토대로 밀도류에 따른 혼합양상 결과가 지니는 혼합패턴을 분석한다면 향후 하천 하류구간의 취수 시스템에 많은 도움을 줄 뿐만 아니라 합류부 구간의 혼합패턴에 따라 수층 내 성층구간의 현황조사와 하천 합류부의 혼합특성 파악하여 합류구간의 수질 관리방안이나 수체 흐름특성을 제시할 수 있을 것으로 사료된다.

• 대기
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• 제27권2호
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• pp.133-150
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• 2017

This study evaluates CMIP5 model performance on rainy season evolution in the East Asian summer monsoon. Historical (1986~2005) simulation is analyzed using ensemble mean of CMIP5 19 models. Simulated rainfall amount is underestimated than the observed and onset and termination of rainy season are earlier in the simulation. Compared with evolution timing, duration of the rainy season is uncertain with large model spread. This area-averaged analysis results mix relative differences among the models. All model show similarity in the underestimated rainfall, but there are quite large difference in dynamic and thermodynamic processes. The model difference is shown in horizontal distribution analysis. BEST and WORST group is selected based on skill score. BEST shows better performance in northward movement of the rain band, summer monsoon domain. Especially, meridional gradient of equivalent potential temperature and low-level circulation for evolving frontal system is quite well captured in BEST. According to RCP8.5, CMIP5 projects earlier onset, delayed termination and longer duration of the rainy season with increasing rainfall amount at the end of 21st century. BEST and WORST shows similar projection for the rainy season evolution timing, meanwhile there are large discrepancy in thermodynamic structure. BEST and WORST in future projection are different in moisture flux, vertical structure of equivalent potential temperature and the subsequent unstable changes in the conditional instability.

• 설비공학논문집
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• 제6권3호
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• pp.302-314
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• 1994

The effects of the inclination of enclosure and partition on natural convective flow and heat transfer were investigated numerically. The enclosure was composed of the lower hot and the upper cold horizontal walls and the adiabatic vertical walls, and a partition was positioned perpendicularly at the mid-height of one vertical insulated wall. The governing equations are solved by using the finite element method with Galerkin method. The computations were performed with the variations of the partition length and Rayleigh number based on the temperature difference between two horizontal walls and the enclosure height with water(Pr=4.95). The effects of the inclination angle of enclosure and partition on the heat transfer within an enclosure were also studied. As the results, the increase of the inclination angle of enclosure rapidly raised the heat transfer rate, while the inclination angle for the maximum Nusselt number was retarded with the increase of the partition length and the decrease of the heat transfer rate became larger in proportion to the increase of the partition length. The Nusselt number obtained by the inclination of partition was smaller than that of the inclination of enclosure. However, the difference of the heat transfer rates was considerably decreased at the longer partition lengths and the trends for the variation of the average Nusselt number were more similar with that of the inclination of enclosure. The upward oriented partition increases the convective heat transfer distinctly in contrast to that of the inclination of enclosure as the partition length increases.

• 대한기계학회논문집B
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• 제23권11호
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• pp.1434-1443
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• 1999

The turbulent fluctuations of temperature and two components of velocity have been measured with hot- and cold-wires in the Thermally Stratified Wind Tunnel(TSWT). Using the fin-tube heat exchanger type heaters and the neural network control algorithm, both stable ($dT/dz=109.4^{\circ}C$) and unstable ($dT/dz=-49.1^{\circ}C$) stratifications were realized. An ambient air jet was issued normally into the cross flow($U_{\infty}=1.0 m/s$) from a round nozzle(d = 6 mm) flushed at the bottom waII of the wind tunnel with the velocity ratio of $5.8(U_{jet}/U_{\infty})$. The characteristics of turbulent dispersion in the cross flow jet are found to change drastically depending on the thermal stratification. Especially, in the unstable condition, the vertical velocity fluctuation increases very rapidly at downstream of jet. The fluctuation velocity spectra and velocity-temperature cospectra along the jet centerline were obtained and compared. In the case of stable stratification, the heat flux cospectra changes Its sign from a certain point at the far field because of the restratification phenomenon. It is inferred that the main reason in the difference between the vertical heat fluxes is caused by the different length scales of the large eddy motions. The turbulent kinetic energy and scalar dissipation rates were estimated using partially non-isotropic and isotropic turbulent approximation. In the unstable case, the turbulent energy dissipation decreases more rapidly with the downstream distance than in the stable case.

• 대한원격탐사학회지
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• 제22권6호
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• pp.507-518
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• 2006

지표면에서 방출된 $11{\mu}m$와 $12{\mu}m$의 복사량은 대기 입자에 의해 선택적으로 산란되고 흡수된다. 에어로솔이 대기 중에 존재할 경우 지표면에서 방출되는 $11{\mu}m$의 복사량이 $12{\mu}m$보다 흡수를 많이 하므로 밝기 온도가 낮게 나타나고, 반대로 구름에 대해서는 $12{\mu}m$가 흡수를 많이 하여 $11{\mu}m$의 밝기 온도가 높게 나타난다. 그러므로 $11{\mu}m$와 $12{\mu}m$의 밝기 온도 차이(BTD)를 통해 구름과 에어로솔의 존재 유무를 판별할 수 있고, 에어로솔의 광학 두께를 추정할 수 있다. 본 연구에서는 대기의 구성 물질과 연직 분포 상태, 지표면의 온도와 형태, 그리고 에어로솔의 구성성분에 따라 BTD 경계값과 민감도를 분석하였다. BTD 경계값은 이론적으로 $0^{\circ}K$라고 알려져 있으나 본 연구에서 US 표준 대기 상태일 때 $0.8^{\circ}K$의 경계값을 보인다. BTD 값은 태양 천정각, 에어로솔의 고도, 지표면 반사도, 그리고 대기의 연직적 온도 분포에 따라서는 영향을 적게 받았다. 그러나 위성 천정각, 지표면 온도와 방출율, 연직적 수증기 분포에 대해 영향이 크게 나타나며 에어로솔 탐지에 50%이상의 오차를 유발할 수도 있다. 그러므로 BTD 방법을 사용하는데 있어 주의가 요구되며, BTD값에 영향을 미치는 인자를 보정해 준다면 좀 더 정확한 에어로솔 탐지가 가능하리라 사료된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2010년도 추계 학술발표회
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• pp.800-807
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• 2010

In this study, a series of numerical analyses has been performed in order to evaluate the performance of a full-scale closed-loop vertical ground heat exchanger constructed in Wonju. The circulation pipe HDPE, borehole and surrounding ground were modeled using FLUENT, a finite-volume method (FVM) program, for analyzing the heat transfer process of the system. Two user-defined functions (UDFs) accounting for the difference in the temperatures of the circulating inflow and outflow water and the change of the surrounding ground temperature with depth were adopted in the FLUENT model. The thermal properties of materials estimated in laboratory were used in the numerical analyses to compare the thermal efficiency of the cement grout with that of the bentonite grout used in the construction. The results of the simulation provide a verification of the in situ thermal response test data. The numerical model with the ground thermal conductivity of 4W/mK yielded the simulation result closer to the in-situ thermal response test than with the ground thermal conductivity of 3W/mK. From the results of the numerical analyses, the effective thermal conductivities of the cement and bentonite grouts were obtained to be 3.32W/mK and 2.99 W/mK, respectively.

• 한국항행학회논문지
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• 제20권1호
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• pp.29-36
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• 2016

위성항법시스템 (GPS; global positioning system)은 도심지의 빌딩이나 터널, 고가도로와 같은 지형적 환경에 의해 전파 수신이 어려워지면 가시 위성의 개수가 급격히 줄어들어 위치오차가 매우 커지거나 측위가 불가능하게 된다. 특히 수직 위치오차는 GPS의 기하학적 배치에 의한 한계로 인하여 수평오차보다 약 1.5 배 이상 크며 혹독한 신호 환경에서는 수평오차보다 더욱 크게 증가하게 된다. 본 논문에서는 GPS의 수직오차 개선을 위해 GPS와 저가형 기압 고도계의 결합 방법을 제안하였다. 제안된 방법은 기압 고도계에 의하여 제공된 기압 고도 측정치에 해면기압과 해면온도에 의한 보상치와 지오이드고를 적용시킨 후 칼만필터에 의하여 GPS 고도와 기압 고도를 융합하는 특징을 가진다. 정적 실험과 차량 실험을 통하여 제안된 기압 고도계와 GPS의 융합 방식의 정확도를 평가하였다. 그 결과 제안된 방법이 고도 정보의 정확도를 크게 향상시킬 수 있음을 확인하였다.

• 한국환경과학회지
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• 제20권9호
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• pp.1191-1203
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• 2011

In case of Typhoon Dianmu, the temperature, wind speed, wind direction and the rainfall per hour changed dramatically when the center of the typhoon passed through Gimhae. Such a change was commonly found in the regions where the center of the typhoon passed through but almost not in the regions far away from it. For example, in the case of Typhoon Malou where the center of the typhoon was far away from the observation site, such a phenomenon was not observed. The analysis of the vertical observation data showed that there was a little change in the wind speed and wind direction in the vertical direction in the case of Typhoon Dianmu of which center passed through Gimhae. There was a great change in the wind speed according to the height in the lower atmosphere just before the center of the typhoon approached the region. When the center of the typhoon was passing through the region, the vertical wind speed was decreased. However, the wind speed was rapidly increased again after the center of the typhoon had passed through the region. Unlike the Dianmu, the difference in the wind speed and wind direction between the upper layer and lower layer of the atmosphere was relatively great in the case of Malou.

• 한국안전학회지
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• 제30권6호
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• pp.18-25
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• 2015

Computational study of a gravity current prior to the backdraft was conducted using fire dynamic simulator (FDS). Various initial conditions of mixture compositions and compartment temperature as well as four opening geometries (Horizontal, Door, Vertical, and Full opening) were considered to figure out their effects on the gravity current. The density difference ratio (${\beta}$) between inside and outside of compartment, the gravity current time ($t_{grav}$) and velocity ($v_{grav}$), and non-dimensional velocity ($v^*$) were introduced to quantify the flow characteristics of the gravity current. Overall fluid structure of the gravity current at the fixed opening geometry showed similar development process for different ${\beta}$ conditions. However, $t_{grav}$ for entering air to reach the opposed wall to the opening geometry increased with ${\beta}$. Door, Vertical, and Horizontal openings where openings are attached on the ground showed similar development process of the gravity current except for Horizontal opening, which located on the middle of the opening wall. The magnitude of $v_{grav}$ at fixed ${\beta}$ was, from largest to smallest, Full > Vertical > Door > Horizontal, but it depended on both the size and location of the opening. On the other hand, $v^*$ was found to be independent to ${\beta}$, and only depended on the geometry of the opening.

• 오토저널
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• 제2권1호
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• pp.21-31
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• 1980

Two phase boundary layer equations of laminar filmwise condensation are solved by an approximate integral method under the following condition; saturated vapour flows vertically downward over a cooled surface of uniform temperature, the condensate film is so thin that the inertia and convection terms are neglected. The following conclusions are drawn under the above assumptions. 1. free convection In case of the linear temperature profile in a liquid film, numerical results for the average coefficients of heat transfer may be expressed as N $u_{m}$=4/3,(G $r_{l}$ /4.H)$^{1}$4/ and in case of the quadratic profile, numerical results may be expressed as N $u_{m}$=2/1.682,(G $r_{l}$ /H)$^{1}$4/. 2. Forced convection When the temperature profile is assumed to be linear in a liquid film, numerical results fir the average heat transfer coefficients may be expressed as N $u_{m}$=(A, R $e_{l}$ /H)$^{1}$2/. This expression is compared with the experimental results hitherto reported; For theoretical Nusselt number (N $u_{m}$)$_{th}$<2*10$^{4}$, the experimental Nusselt number (N $u_{m}$)$_{exp}$ is on the average larger than theoretical Nusselt number (N $u_{m}$)$_{th}$ by 30%. For (N $u_{m}$)$_{th}$>2*10$^{4}$, experimental Nusselt number (N $u_{m}$)$_{exp}$ is about 1.6 times as large as theoretical Nusselt number (N $u_{m}$)$_{th}$. These large deviation may be caused by the presence of turbulence in the liquid film. In case of the quadratic temperature profile in a liquid film, numerical results for the average coefficients of heat transfer may be expressed as N $u_{m}$'=(2,A,Re/H)$^{1}$2/. This formular shows that theoretical Nusselt number (N $u_{m}$)$_{th}$ is larger than experimental Nusselt number (N $u_{m}$)$_{exp}$ by 60%. It is speculated that when the temperature difference between cooled surface and saturated vapour is small, temperature profile in a liquid film is quadratic.quadratic.. quadratic.quadratic..atic..