• Ocean and Polar Research
• /
• 제27권2호
• /
• pp.115-123
• /
• 2005

Recently, it has been observed in the East Sea that temperature increases below the thermocline, and dissolved oxygen increase in the intermediate layer but decrease below it. The layer of minimum dissolved oxygen deepens and the bottom homogeneous layer in oxygen becomes thinner. It emerges very probably that these changes are induced by the mode change of deep water formation associated with global warming. To further support this hypothesis, a one-dimensional model experiment is performed. First, a thermal profile is obtained by injecting a cold and high oxygen deep water into the bottom layer, say the bottom mode. Then, two thermal profiles are obtained from the bottom mode profile by assuming that either all the deep water introduce into the intermediate layer has been initiated, say the intermediate mode, or that only a part of the deep water has been initiated into the intermediate layer, say the intermediate-bottom mode. The results, from the intermediate-bottom mode experiment are closest to the observed results. They show quite well the tendency for oxygen to increase in the intermediate layer and the simultaneous thinning of the bottom homogeneous layer in oxygen. Therefore, it can be said that the recently observed slow variation of the thermal structure might be associated with changes in the deep water formation from the bottom mode to the intermediate-bottom mode.

• 반도체디스플레이기술학회지
• /
• 제21권1호
• /
• pp.67-70
• /
• 2022

In order to prevent water vapor and oxygen permeation in the organic light emitting diodes (OLED), Al₂O₃ thin-film encapsulation (TFE) technology were investigated. Atomic layer deposition (ALD) method was used for making the Al₂O₃ TFE layer because it has superior barrier performance with advantages of excellent uniformity over large scales at relatively low deposition temperatures. In this study, the thickness of the Al₂O₃ layer was varied by controlling the numbers of the unit pulse cycle including Tri Methyl Aluminum(Al(CH₃)₃) injection, Ar purge, and H₂O injection. In this case, several process parameters such as injection pulse times, Ar flow rate, precursor temperature, and substrate temperatures were fixed for analysis of the effect only on the thickness of the Al₂O₃ layer. As results, at least the thickness of 39 nm was required in order to obtain the minimum WVTR of 9.04 mg/m²day per one Al₂O₃ layer and a good transmittance of 90.94 % at 550 nm wavelength.

• 한국초전도ㆍ저온공학회논문지
• /
• 제5권3호
• /
• pp.52-56
• /
• 2003

This paper describes the results of a basic study (on a model samples) for the development of 22.9 kV high temperature superconducting (HTS) cable. The authors have established that the factors that decide the performance of HTS cables are butt gaps in tape insulation and carbon particles from semiconductive layer. The insulation performance of HTS cables is determined by size and quality of these elements. In the model tests of HTS cables, the minimum PD inception stress of the tape insulation impregnated with liquid nitrogen was found and insulation thickness was calculated from this result.

• 열처리공학회지
• /
• 제17권5호
• /
• pp.278-282
• /
• 2004

Effect of pre-treatment on the gas nitriding process of austenitic stainless steels has been investigated and the following results were obtained. Minimum pre-treatment time was decreased to 5min with increasing treatment temperature from $200^{\circ}C$ to $600^{\circ}C$. Surface activation effect by the pre-treatment was maintained in the air up to holding time of 64hr, judging from the analysis result of gas nitrided specimens. The Depth of nitrided layer of STS 304 and 316 stainless steels were ranged from $5{\mu}m$ to $90{\mu}m$ at $440^{\circ}C{\sim}600^{\circ}C$. The X-ray diffraction intensity for austenitic stainless steels were increases as nitriding temperature from $440^{\circ}C$ to $600^{\circ}C$.

• 한국해양학회지:바다
• /
• 제13권3호
• /
• pp.190-199
• /
• 2008

북동태평양 열대 해양의 해수특성과 해양구조를 파악하기 위하여 2005년 7-8월에 $131.5^{\circ}W$ 관측선에서 관측한 CTD 자료를 분석하였다. 또한 적도 부근 태평양의 해수특성을 전반적으로 이해하기 위하여 서태평양 $137^{\circ}-142^{\circ}E$에서의 CTD 자료도 분석하여 동태평양의 분석 결과와 비교하였다. 여름철 동태평양의 표층수온은 적도반류 해역에서 가장 높았다. 이것은 $28^{\circ}C$ 이상의 고온수가 봄과 여름철에 적도반류를 타고 서태평양으로부터 동태평양으로 이동하여 약 $4^{\circ}-15^{\circ}N$ 사이에서 동서로 연결되기 때문이다. 북적도해류의 표층에 나타나는 저염분 고용존산소의 해수는 동태평양의 파나마만으로부터 서태평양의 필리핀 부근까지 이동하는 저염분수 때문이다. 반면 남적도해류의 표층에 고염분과 저용존산소의 해수가 분포하는 것은 남태평양 아열대 기원의 고염분수가 적도를 넘어 남적도해류 표층의 열대해수(Tropical Water)와 심층의 고염분수를 형성하고 있기 때문이다. 수심 약 500-1500 m 사이의 중층에서는 염분최소층이 분포하는데, $5^{\circ}N$ 이남은 남극중층수(AAIW) 기원의 해수가, $5^{\circ}N$ 이북은 북태평양중층수(NPIW) 기원의 해수가 분포한다. $4^{\circ}-6^{\circ}N$ 해역에서는 직경 약 200 km이며 반시계 방향으로 회전하는 냉수성 소용돌이(cold eddy)가 관측되었다. 서태평양에 비해 동태평양에서 표층수온은 $1^{\circ}C$ 이상 낮았으며 표층염분은 높았다. 적도 부근의 표층 아래에 분포하는 고염분수는 동태평양에서 상대적으로 저염분(약 0.5 psu) 이었고, $14^{\circ}N$ 이남에서 염분최소층의 염분과 밀도는 동태평양에서 높았다.

• 한국정보통신학회논문지
• /
• 제19권5호
• /
• pp.1259-1268
• /
• 2015

음향층심도의 변화에 대한 이해는 해양상층에서 수중음향 통신, 음향 토모그레피 및 수중항체를 수색하거나 탐지하는 해군 작전에 많은 영향을 미친다. 일반적으로 음향층심도와 혼합층깊이의 정의는 다르게 내려져있으나 혼합층 깊이가 음향학적으로는 음향층심도와 같다고 할 수 있다. 본 연구에서는 동해에서 가용한 수온-염분 관측자료를 활용하여 연간 음향층심도와 혼합층깊이를 비교해 보았다. 비교를 위해 다양한 혼합층깊이 결정 기준과 방법으로부터 도출된 혼합층깊이 자료를 활용하였다. 분석결과 동해에서 음향층심도는 곡률변화를 이용한 혼합층깊이와 거의 유사하였으나 다른 혼합층깊이 기준을 적용하였을 시는 많은 차이를 보였다. 한편 음향층심도 계산의 정확도를 평가해 보기 위해 음파전달손실 모의 실험을 실시하였다. 이를 통해 음향층심도내에서 음파전달손실이 최소가 되는 최적주파수가 존재함을 확인하였다.

• 대기
• /
• 제23권4호
• /
• pp.413-424
• /
• 2013

Urban Heat Island (UHI) intensity is one of vital parameters in studying urban boundary layer meteorology as well as urban planning. Because the UHI intensity is defined as air temperature difference between urban and rural sites, an objective sites selection criterion is necessary for proper quantification of the spatial variations of the UHI intensity. This study quantified the UHI intensity and its spatial pattern, and then analyzed their connections with urban structure and metabolism in Seoul metropolitan area where many kinds of land use and land cover types coexist. In this study, screen-level temperature data in non-precipitation day conditions observed from 29 automatic weather stations (AWS) in Seoul were analyzed to delineate the characteristics of UHI. For quality control of the data, gap test, limit test, and step test based on guideline of World Meteorological Organization were conducted. After classifying all stations by their own local climatological properties, UHI intensity and diurnal temperature range (DTR) are calculated, and then their seasonal patterns are discussed. Maximum UHI intensity was $4.3^{\circ}C$ in autumn and minimum was $3.6^{\circ}C$ in spring. Maximum DTR appeared in autumn as $3.8^{\circ}C$, but minimum was $2.3^{\circ}C$ in summer. UHI intensity and DTR showed large variations with different local climate zones. Despite limited information on accuracy and exposure errors of the automatic weather stations, the observed data from AWS network represented theoretical UHI intensities with difference local climate zone in Seoul.

• 대한기계학회논문집
• /
• 제14권2호
• /
• pp.453-462
• /
• 1990

The interaction of forced convection-conduction with thermal radiation in laminar boundary layer over a plate fin is studied numerically. The analysis is based on complete solution whereby the heat conduction equation for the fin is solved simultaneously with the conservation equations for mass, momentum and energy in the fluid boundary layer adjacent to the fin. The fluid is a gray medium and diffusion(Rosseland) approximation is used to describe the radiative heat flux in the energy equation. The resulting boundary value problem are convection-conduction parameter N$_{c}$ and radiation-conduction parameter m, Prandtl number Pr. Numerical results are presented for gases with the Prandtl numbers of 0.7 & 5 with values of N$_{c}$ and M ranging from 0 to 10 respectively. The object of this study is to provide the first results on forced convection-radiation interaction in boundary layer flow over a semi-infinite flay plate which can be used for comparisons with future studies that will consider a more accurate expression for the radiative heat flux. The agreement of the results from the complete solution presented by E. M. Sparrow and those from this paper for the special case of M=0 is good. The overall rate of heat transfer from the fin considering radiative effect is higher than that from the fin neglecting radiative effect. The local heat transfer coefficient with radiative effect is higher than that without radiative effect. In the direction from tip to base, those coefficients decrease at first, attain minimum, and then increase. The larger values of N$_{c}$ M, Pr give rise to larger fin temperature variations and the fin temperature without radiative effect is always higher than that with radiative effect.

• 센서학회지
• /
• 제16권6호
• /
• pp.457-461
• /
• 2007

This paper describes the characteristics of poly (polycrystalline) 3C-SiC grown on $SiO_{2}$ and AlN substrates, respectively. The crystallinity and the bonding structure of poly 3C-SiC grown on each substrate were investigated according to various growth temperatures. The crystalline quality of poly 3C-SiC was improved from resulting in decrease of FWHM (full width half maximum) of XRD and FT-IR by increasing the growth temperature. The minimum growth temperature of poly 3C-SiC was $1100^{\circ}C$. The surface chemical composition and the electron mobility of poly 3C-SiC grown on each substrate were investigated by XPS and Hall Effect, respectively. The chemical compositions of surface of poly 3C-SiC films grown on $SiO_{2}$ and AlN were not different. However, their electron mobilities were $7.65{\;}cm^{2}/V.s$ and $14.8{\;}cm^{2}/V.s$, respectively. Therefore, since the electron mobility of poly 3C-SiC films grown on AlN buffer layer was two times higher than that of 3C-SiC/$SiO_{2}$, a AlN film is a suitable material, as buffer layer, for the growth of poly 3C-SiC thin films with excellent properties for M/NEMS applications.

• 한국환경생태학회지
• /
• 제24권6호
• /
• pp.751-762
• /
• 2010

본 연구는 초고층 건축물 외부공간의 식물 피복 상태가 온도변화에 미치는 영향을 파악하고자 서울시에 위치한 초고층 건축물 12개소를 대상으로 연구를 수행하였다. 초고층 건축물 외부공간의 토지 피복 유형별 온도 차이 분석을 위해 6개 유형(외곽도로, 포장지, 관목/초지, 단층교목식재지, 다층식재지, 수경시설)으로 건축물외부공간의 피복유형을 구분하였으며 토지이용유형별 대표지점에서 온도를 실측하였다. 건축물 12개소의 주변 환경차이를 고려하기 위해 외곽도로의 중앙부에 대조구를 선정하여 온도를 측정한 후 일원배치 분산분석을 토대로 유사한 온도경향을 보이는 대상지를 4개 그룹으로 분류하였다. 분류된 그룹의 토지 피복 유형과 외부 공간 온도와의 일원배치 분산분석결과, 주로 단층교목식재지, 수경시설, 다층식재지는 저온역에 속하였으며, 관목/초지, 포장지, 외곽도로는 고온역에 속하였다. 저온역과 고온역의 온도차이는 약 $1.06{\sim}6.17^{\circ}C$의 차이를 보였다. 그러나 조성된 식재지와 수경시설 면적의 협소, 건축물로 인한 일사도달량의 저감과 반사량의 증가 등으로 초고층 건축물 외부공간 온도에 미치는 영향이 다양하게 나타났다. 이에 각 공간에 필요한 녹지량과 수공간의 면적을 조성 전 미리 산출하여, 효과를 발휘할 수 있는 최소한의 면적과 녹지량을 확보할 필요성이 있었다.