• Journal of the Korean Physical Society
• /
• 제73권9호
• /
• pp.1295-1302
• /
• 2018

In the present investigation, we have studied the magnetohydrodynamic (MHD) heat transfer of peristaltic flow in a tube. The analysis is made without imposing any assumption to obtain the streamline and isothermal line directly. Galerkin's finite element method has been used on the governing Navier-Stoke's equation in the form of ${\psi}-{\omega}$. The graphs of the computed longitudinal velocity, temperature and pressure are plotted against different value of the emerging parameter by using the stream function and vorticity. The results are valid beyond the long wavelength and the low Reynolds number limits. We conclude that higher values of the parameters are not independent of the time mean flow rate.

• 한국산학기술학회논문지
• /
• 제14권11호
• /
• pp.5417-5422
• /
• 2013

본 논문은 MODIS 위성 영상을 이용하여 논벼 생산량을 추정하는 모형의 적합도 개선 및 추정모형내 적절한 설명변수를 탐색하고자 수행되었다. 또한 이 연구는 한국에서 논벼 생산량 조사를 위해 위성 영상을 사용하는 방안을 검토하기 위해 수행되었다. 미국, 호주, 일본 등 많은 선진국들은 재배면적 및 생산량 조사와 같은 농업통계를 산출하기 위해 위성 영상을 이용하고 있다. 그러나 위성 영상을 이용한 작물 생산량 조사의 정확성은 아직 충분치 않은 수준이다. 본 연구는 위성 영상을 이용한 논벼 생산량 조사의 정확도를 증대시키기 위한 몇 가지 방법을 검토하고 있다. 많은 작물 중 논벼를 연구대상으로 선정한 이유는 논벼가 다른 작물 보다 재배면적과 작황의 영상 분석이 용이하였기 때문이고, 다양한 위성 영상 중 MODIS 영상을 이용한 것은 한국 논벼 생산량 조사 연구를 위해 보다 적절한 영상을 다수 포함하고 있었기 때문이다. 이 연구에서 등온선에 의해 구분된 논벼로부터 도출된 NDVI지수, 논벼 등숙기의 일조시간, 강우량, 온도 등 기상변수를 이용하여 단수함수가 추정되었다. 단수함수 추정결과, 모형의 적합도(R-squared)는 0.768-0.891를 보였다. 이 연구는 연평균 등온선에 의해 구분된 NDVI지수와 (등숙기) 기상변수가 단수함수 추정에 매우 유용하게 이용될 수 있음을 보이고 있다.

• 청정기술
• /
• 제26권3호
• /
• pp.186-195
• /
• 2020

활성탄에 의한 Acid black(AB)과 Quinoline yellow(QY)의 등온흡착과 속도실험을 염료의 초기농도, 접촉 시간, 온도 및 pH를 흡착변수로 수행하여 등온흡착과 동력학적, 열역학적 파라미터에 대해 조사하였다. 흡착평형자료는 Freundlich 등온흡착식에 잘 맞았으며, 계산된 Freundlich 분리계수 값으로부터 활성탄이 AB와 QY를 효과적으로 제거할 수 있다는 것을 알았다. 속도실험 데이터는 흡착공정은 유사 이차 반응속도식이 오차율 10% 이내로 잘 맞았다. 입자 내 확산식에 대한 결과는 두단계의 직선으로 구분되었다. 입자내 확산을 나타내는 두 번째 직선의 기울기가 경계층 확산의 기울기보다 작아서 입자 내 확산이 속도지배단계인 것을 확인하였다. 열역학 실험으로부터 AB와 QY의 활성화 에너지는 각각 19.87 kJ mol^-1, 14.17 kJ mol^-1였고 물리흡착공정(5 ~ 40 kJ mol^-1)에 해당하였다. 활성탄에 의한 AB와 QY의 흡착반응의 자유에너지 변화는 298 ~ 318 K 범위에서 모두 음의 수치를 나타냈기 때문에 흡착반응이 자발적이었으며 온도가 증가할수록 자유에너지 값이 감소하였기 때문에 자발성이 더 높아졌다. pH 변화실험 결과, 활성탄에 의한 AB와 QY는 해리하여 발생한 음이온의 영향으로 pH 3에서 가장 높은 흡착제거율을 나타냈으며, 흡착메카니즘은 정전기적 인력이었다.

• 청정기술
• /
• 제26권2호
• /
• pp.122-130
• /
• 2020

입상 활성탄에 대한 reactive blue 4 (RB 4) 의 등온흡착과 동력학적, 열역학적 파라미터에 대해 활성탄의 양, pH, 초기농도, 접촉시간, 온도를 흡착변수로 하여 조사하였다. 활성탄에 의한 RB 4 염료의 흡착은 pH 7을 기점으로 양쪽으로 흡착 백분율이 증가하는 concave 모양을 나타내었다. 등온흡착자료는 Langmuir, Freundlich, Temkin 등온흡착식에 적용하였다. Freundlich과 Langmuir 등온흡착식이 모두 잘 맞았다. 계산된 Freundlich 분리계수(1/n = 0.125 ~ 0.232)과 Langmuir 분리계수(R_L = 1.53 ~ 1.59) 으로부터 활성탄이 RB 4를 효과적으로 처리할 수 있다는 것을 알 수 있었다. Temkin의 흡착열관련상수(B_T = 17.611 ~ 29.010 J mol^-1)는 이 공정이 물리흡착임을 나타냈다. 동력학적 실험으로부터 흡착공정은 유사 이차 반응속도식에 잘 맞았다. 입자 내 확산식에 대한 결과는 표면확산을 나타내는 두 번째 직선의 기울기보다 입자내 세공확산을 나타내는 첫 번째 직선의 기울기가 작게 나타나서 입자내 세공확산이 속도지배단계인 것을 확인하였다. Gibbs 자유에너지 변화(ΔG = -3.262 ~ -7.581 kJ mol^-1)와 엔탈피 변화(ΔH = 61.08 kJ mol^-1)은 각각 흡착공정이 자발적 공정 및 흡열과정임을 나타내었다.

• Bulletin of the Korean Chemical Society
• /
• 제31권2호
• /
• pp.435-441
• /
• 2010

We report the preparation and characterization of a new and water soluble complex of palladium(II) with 1,10- phenanthroline and butyldithiocarbamate ligands. This compound has been studied through spectroscopic techniques, $^1H$ NMR, IR, electronic spectra and elemental analysis and conductivity measurements. The complex shows 50% cytotoxic concentration ($Ic_{50}$) value against chronic myelogenous leukemia cell line, K562, much lower than that of cisplatin. Thus the mode of binding of this complex to calf thymus DNA have been extensively investigated by isothermal titration UV-visible spectrophotometry, fluorescence, gel filteration and other methods. UV-visible studies show that the complex exhibits cooperative binding with DNA and remarkably denatures the DNA at extremely low concentration ($~13\;{\mu}M$). Fluorescence studies indicate that the complex intercalate into DNA. Gel filtration studies suggest that the binding of Pd(II) complex with DNA is strong enough that it does not readily break. In these interaction studies, several thermodynamic and binding parameters are also determined which may reflect the mechanism of action of this type of compound with DNA.

• 대한기계학회논문집
• /
• 제15권1호
• /
• pp.262-273
• /
• 1991

본 연구에서는 벽면에서의 압력은 압력측정 정치를 제작하여 측정하였으며 평 균유동 및 난류량들은 열선 유속계(hot wire system)을 사용하여 측정하였다.

• 대한원격탐사학회:학술대회논문집
• /
• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
• /
• pp.251-253
• /
• 2003

Landsat images were globally used to monitoring the Earth's. But it is not positively applied to a field of environment such as coastal environment, heat island effect and drought condition and so on. Until recently, Information about a ecology natural environment came to do by direct investigation. But Information about a ecology·natural environment of wide area were quickly getting possible with the progress of remote sensing technique. Specially, the up-to-date characteristic information about an ecology·natural environment as the basic intelligence for a country development activity are very important. So, it applies the satellite images that the periodic observation of data is possible. In this study, We planned the function which is possible helping the renewal of an ecology·natural environmental information using Landsat imagery. Also planned the DB suitable for these purpose. For application of thermal infrared band images we developed the function that extracts an isothermal line. It used the thermal infrared band images and it grasped a temperature distribution. The result is useful in analysis of the city heat island effectiveness.

• Ocean and Polar Research
• /
• 제31권4호
• /
• pp.283-296
• /
• 2009

Oceanographic survey data were analyzed to understand the characteristics of a warm eddy observed in the Ulleung Basin in July 2005. The temperature distribution at 200 db and vertical sections provided evidence of the warm eddy in the Ulleung Basin (UWE05). Based on the 5$^{\circ}C$ isothermal line on 200 db temperature, the major axis was 160 km from southwest to northeast, and the minor axis was 80 km from southeast to northwest. The homogeneous layer in the thermocline of UWE05 had mean values of 10.40$^{\circ}C$ potential temperature, 34.35 psu salinity, and 26.37 kg/m$^3$ potential density (${\sigma}_{\theta}$) and provided evidence that UWE05 also existed during the winter of 2004-2005. A warm streamer initially flowed along the circumference of UWE05 and mixed with the upper central water. Two northward current cores were found on the western side of the measured current section at the central latitude of UWE05. One was the East Korean Warm Current (EKWC) and the other was the main stream of the western part of UWE05. Geostrophic transport of the upper layer (from the surface to the isopycnal surface of 26.9 ${\sigma}_{\theta}$) was approximately 2.5 Sv in the eastern side of UWE05. However, the measured transport was twice as large as the geostrophic transport. Mass conservation of geostrophic transport was well satisfied in the upper layer. The direct current measurements and geostrophic transport analysis showed that the EKWC meandered around UWE05.

• 설비공학논문집
• /
• 제7권4호
• /
• pp.577-588
• /
• 1995

A numerical study is made on the melting process of an unconstrained ice inside an isothermal ice-ball capsule. The unmelted ice core is continuously ascending on account of buoyancy forces. Such a buoyancy-assisted melting is commonly characterized by the existence of a thin liquid film above the ice core. The present study is motivated to present a full-equation-based analysis of the influences of the initial subcooling and the natural convection on the fluid flow associated with the buoyancy-assisted melting. In the light of the solution strategy, the present study is substantially distinguished from the existing works in that the complete set of governing equations in both the melted and unmelted regions are resolved in one domain. Numerical results are obtained by varying the wall temperature and initial temperature. The present results reported the transition of the flow pattern in a spherical capsule, as the wall temperature was increased over the density inversion point. In addition, time wise variation of the shapes for the liquid film and the lower ice surface, the time rate of change in the melt volume fraction and the melting distance at symmetric line is analyzed and is presented.

• 한국환경과학회지
• /
• 제2권1호
• /
• pp.27-42
• /
• 1993

Based on the Results of Marine Meteorological and Oceanographical Observations during 1966∼1987 and the Ten-day Marine Report during 1970∼1989 by Japan Meteorological Agency, the possible area where the Japan Sea Proper Water (JSPW) can be formed is investigated by analyzing the distribution of water types in the Japan Sea. The Japan Sea can be divided into three subareas of Northern Cold Water(NCW), Polar Front(PF) and Tsushima Warm Current (TWC) by the Polar Front identified by a 6℃ isothermal line at the sea surface in vinter. Mean position of the Polar Front is approximately parallel to the latitude 39∼40。N. The standard deviation of the Polar Front from the mean position of about 130km width is the smallest in the region between 136。E and 138。E where the Polar Front is very stable, because the branches of the Tsushima Current are converging in this region. However, standard deviations are about 180∼250km near the Korean peninsula and the Tsugaru Strait due to greater variability of warm currents. In the NCW area north of 40∼30。N and west of 138。E, the water types of the sea surface to the loom depth are similar to those of the JSPW. This fact indicates that the surface layer of the NCW area is the possible region of the JSPW formation in winter.