• 한국환경과학회지
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• 제5권6호
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• pp.713-718
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• 1996

We identified two characteristic turbulent flow cases, weakening and strengthening, which appear at the downwind side. Observations were made two times, Dec. 2-3. 1995 and Feb. 13-14. 1996 at Pusan National University site located downwind side of Kumjeong mountain. Meteorological observation system, tethersonde, was adopted to present observation. In the case of the west wind which blows perpendicular to Sanghak mountain located westward from the site, the wind speed highly increased in exponential with height. Therefore, the low level wind speed was so weak just like Taylor(1988)'s review. While the wind speed was intensified at 200-400m layer when the northwest wind blows from the continental Siberian high. We suppose 기 is because of the strong vertical convergence of flow between the surface inversion layer and the upper one, and also the horizontal convergence along the saddle and valley between the two mountains, Kumjeong and Sanghak-because of Bernoulli's effect. The inversion layer existed at surface-l00m and 500-600m level and the strong wind existed at about 200-400m layer.

• 한국환경과학회지
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• 제14권6호
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• pp.577-582
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• 2005

Enormous apartment complexes in urban areas, temporary inversion state and heat island effect occur due to the strong sunshine and weak wind speeds which hinders the dispersion of air pollutants that are emitted from neighboring areas of apartment complexes. In this study, analysis were conducted by using the Fluent code based on the CFD(Computation Fluid Dynamics), including building layout, material, building height from the ground surface, the heat, analysis of flow field in the apartment complex. It was estimated that the temporal radiation inversion phenomenon during the daytime, which was caused by the weak wind speed and higher temperatures in the upper level, contributed to the stagnation of the air pollutants in the lower layer of the apartment complex.

• 한국환경과학회지
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• 제15권8호
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• pp.719-725
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• 2006

Since low-floor apartments ate vertically closer to patting lots and roadways, it is hypothesized that residents in low-floor apartments may be exposed to elevated ambient levels of motet vehicle emissions compared to residents in high-floor apartments. The present study examined this hypothesis by measuring two motor vehicle source-related pollutants(CO and PM10) in ambient air of high-rise apartment buildings within the boundary of industrial complexes according to atmospheric stability The ambient air concentrations of CO and PM10 were higher for low-floor apartments than for high-floor apartments, regardless of atmospheric stability, The median concentration ratio of the low-floor air to high-floor alt ranged from 1.3 to 2.0, depending upon atmospheric stabilities, seasons and compounds. Moreover, the CO and PM10 concentrations were significantly higher in the winter and in the summer, regardless of the Hoot height. Atmospheric stability also was suggested to be important for the residents' exposure of high-rise apartment buildings to both CO and PM10. The median ratios of surface inversion air to non-surface inversion air ranged from 1.2 to 1.7 and from 1.0 to 1.6 lot PM10 and CO, respectively, depending upon seasons. Conclusively, these parameters(apartment floor height, season, and atmospheric stability) should be considered when evaluating the exposure of residents, living in high-rise apartment buildings, to CO and PM10. Meanwhile, the median PMl0 outdoor concentrations were close to or higher than the Korean annual standards for PM10, and the maximum PM10 concentrations substantially exceeded the Korean PM10 standard, thus suggesting the need for a management strategy for ambient PM 10. Neither the median nor the maximum outdoor CO concentrations, however, were higher than the Korean CO standard.

• 한국운동역학회지
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• 제32권1호
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• pp.9-16
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• 2022

Objective: The purpose of this study was to investigate how the chronic ankle instability affects postural control during forward jump landing. Method: 20 women with chronic ankle instability (age: 21.7 ± 1.6 yrs, height: 162.1 ± 3.7 cm, weight: 52.2 ± 5.8 kg) and 20 healthy adult women (age: 21.8 ± 1.6 yrs, height: 161.9 ± 4.4 cm, weight: 52.9 ± 7.2 kg) participated in this study. For the forward jump participants were instructed to stand on two legs at a distance of 40% of their body height from the center of force plate. Participants were jump forward over a 15 cm hurdle to the force plate and land on their non-dominant or affected leg. Kinetic and kinematic data were obtained using 8 motion capture cameras and 1 force plates and joint angle, vertical ground reaction force and center of pressure. All statistical analyses were using SPSS 25.0 program. The differences in variables between the two groups were compared through an independent sample t-test, and the significance level was to p < .05. Results: In the hip and knee joint angle, the CAI group showed a smaller flexion angle than the control group, and the knee joint valgus angle was significantly larger. In the case of ankle joint, the CAI group showed a large inversion angle at all events. In the kinetic variables, the vGRF was significantly greater in the CAI group than control group at IC and mGRF. In COP Y, the CAI group showed a lateral shifted center of pressure. Conclusion: Our results indicated that chronic ankle instability decreases the flexion angle of the hip and knee joint, increases the valgus angle of the knee joint, and increases the inversion angle of the ankle joint during landing. In addition, an increase in the maximum vertical ground reaction force and a lateral shifted center of pressure were observed. This suggests that chronic ankle instability increases the risk of non-contact knee injury as well as the risk of lateral ankle sprain during forward jump landing.

• 마이크로전자및패키징학회지
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• 제12권2호
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• pp.149-154
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• 2005

궁극적으로 게이트를 저저항 복합 실리사이드로 대체하는 가능성을 확인하기 위해 70 nm 두께의 폴리실리콘 위에 각 20nm의 Ni, Co를 열증착기로 적층순서를 달리하여 poly/Ni/Co, poly/Co/Ni구조를 만들었다. 쾌속열처리기를 이용하여 실리사이드화 열처리를 40초간 $700{\~}1100^{\circ}C$ 범위에서 실시하였다. 복합 실리사이드의 온도별 전기저항변화, 두께변화, 표면조도변화를 각각 사점전기저항측정기와 광발산주사전자현미경, 주사탐침현미경으로 확인하였다. 적층순서와 관계없이 폴리실리콘으로부터 제조된 복합실리사이드는 $800^{\circ}C$ 이상부터 급격한 고저항을 보이고, 두께도 급격히 얇아졌다. 두께의 감소는 기존의 단결정에서는 없던 현상으로 폴리실리콘의 두께가 한정된 경우 금속성분의 inversion 현상이 커서 폴리실리콘이 오히려 실리사이드 상부에 위치하여 제거되기 때문이라고 생각되었고 $1000^{\circ}C$ 이상에서는 실리사이드가 형성되지 못하였다. 이러한 결과는 나노급 두께의 게이트를 저저항 실리사이드로 만 들기 위해서는 inversion과 두께감소를 고려하여야 함을 의미하였다.

• 대기
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• 제31권4호
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• pp.395-404
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• 2021

In order to investigate downslope windstorm by using more detailed observation, we observed 6 cases at 3 sites - Inje, Yongpyeong, and Bukgangneung - during "3-D Meteorological Observation Project in Yeongdong region of Gangwon province, South Korea in 2020." The results from analysis of the project data were as follows. First, AWS data showed that a subsidence inversion layer appeared in 800~700 hPa on the windward side and 900~850 hPa on the leeward side. Second, before strong wind occurred, the inversion layer had descended to about 880~800 hPa. Third, with mountain wave breaking, downslope wind was intensified at the height of 2~3 km above sea level. After the downslope wind began to descend, the subsidence inversion layer developed. When the subsidence inversion layer got close to the ground, wind peak occurred. In general, UM (Unified Model) GDAPS (Global Data Assimilation Prediction System) have had negative bias in wind speed around peak area of Taebaek mountain range, and positive bias in that of East Sea coast area. The stronger wind blew, the larger the gap between observed and predicted wind speed by GDAPS became. GDAPS predicted strong p-velocity at 0600 LST 25 Apr 2020 (4^th case) and weak p-velocity at 2100 LST 01 Jun 2020 (6^th case) on the lee-side of Taebaek mountain range near Yangyang. As hydraulic jump theory was proved, which is known as a mechanism of downslope windstorm in Yeongdong region, it was confirmed that there is a relationship between p-velocity of lee-side and wind speed of eastern slope of Taebaek mountain range.

• 한국지구과학회지
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• 제26권7호
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• pp.691-697
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• 2005

최근에 수행되고 있는 중력 탐사는 고분해능의 중력계와 GPS(Global positioning system)를 통한 정밀한 측정과 측지가 이루어지고 있다. 중력탐사에서 모델링과 역산의 기술은 많은 발전이 있어왔지만, 중력자료처리는 거의 변화가 없었다. 통상적인 정밀한 중력 자료 보정을 통한 부우게이상은 측정점의 고도에서 기준면까지의 물질의 영향을 일정한 밀도를 이용해 제거해 버리기 때문에 측정점 바로 하부의 이상체에 의한 영향을 상당히 왜곡시키게 된다. 본 연구에서는 탐사 지역의 지형을 DEM(Digital Elevation Map) 자료와 Multiquadric equation을 이용하여 실제 지형과 유사한 Multiquadric surface를 자동적으로 구성하고, 이를 블록화 함으로써 보정의 대상이었던 기준면 상부에 대한 밀도를 탐사 지역의 지질 정보와 지형을 포함하는 역산을 통해 수치적으로 계산하였다. 이러한 지형을 포함한 역산 방법을 3차 원중력지형역산(3DGTI; 3-D Gravity Terrain Inversion)이라 한다. 이 연구의 효율성을 검증하기 위하여 주변암과 밀도차가 존재하는 관입지역에 대한 모델을 구성하고 적용한 결과 기존의 부게 보정 방법을 적용한 부게 이상도에 비해 자료의 왜곡이 감소하는 효과를 얻을 수 있었다. 이를 통하여 지형 역산을 통한 객관적인 부게 밀도의 결정과 부게 보정시 실제의 수평적인 밀도 변화를 반영함으로써 기존의 문제점을 보완하였다. 게다가, 3DGTI로부터 얻어진 밀도분포는 지형의 윤곽을 그대로 표현하고 있어서 보다 실질적인 지질을 보여준다고 하겠다. 이 방법을 화강암체가 관입하고 있는 마산$\cdot$창원 일대에서의 중력 탐사 자료에 적용해본 결과 기존 방법보다 관입 화강암체의 위치와 그 규모를 알아내는데 더 효과적이었다. 따라서, 수평적인 밀도 변화가 뚜렷하게 존재하는 지역의 경우, 새로운 중력 자료 처리 방법이 기존의 부게 보정에서 발생하였던 문제점을 해결함으로써 천부의 분해능을 높이고, 심부의 밀도 분포도 좀더 정확하게 계산할 수 있으리라 생각된다.

• Investigative Magnetic Resonance Imaging
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• 제18권1호
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• pp.34-42
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• 2014

목적 : 유방암의 이중반전회복 자기공명영상 (double inversion recovery, DIR) 신호와 자기공명분광영상기법 (MR spectroscopy, MRS)에서 얻은 단일 화적소 콜린 양과 상관관계가 있는가를 알아보고자 하였다. 대상 및 방법 : 2008년 8월부터 2009년 12월까지 유방암으로 진단된 환자 중 이중반전회복 자기공명영상과 자기공명분광영상기법 모두를 시행한 28명의 환자를 대상으로 하였다. 이중반전회복영상과 조영증강 T1강조영상 (CE-T1WI)에서 종양에 해당하는 관심영역에서의 신호강도를 삼차원으로 얻었으며 병변 (L)과 동측 정상 섬유선 조직 (N)에 대한 용적을 같은 레벨에서 병변 대 정상조직의 신호강도 비 (LNR)를 구하였다. 자기공명분광영상 데이터는 단일복셀분광방법인 중점분해분광학을 이용하였다. 자기공명분광영상기법에서 총 콜린 공명의 높이, 폭, 면적과 조영증강 T1강조영상에서 병변 대 정상 조직의 신호강도 비 값, 그리고 이중반전회복 자기공명영상의 병변 대 정상조직의 신호강도비 값 간의 상관 관계에 대해 Pearson 상관분석을 시행하였고 유의수준은 p=0.05이었다. 결과 : 조영증강 T1강조영상의 병변 대 정상 조직의 신호강도 비 값과 자기공명분광영상기법에서 콜린의 높이 (r=-0.322, p= 0.094), 폭 (r=-0.233, p=0.232), 면적 (r=-0.309 p=0.109)값과, 또한 이중반전회복 자기공명영상의 병변 대정상 조직의 신호강도 비 값과 자기공명분광영상기법 콜린의 높이 (r=0.067, p=0.735), 폭 (r=-0.287, p=0.139), 면적 (r=0.012 p=0.953) 값 사이에 상관성은 통계적으로 유의하지 않았다. 조영증강 T1강조영상의 병변 대 정상조직의 신호강도 비 값과 이중반전회복 자기공명영상의 병변 대 정상조직의 신호강도 비 값 사이에서도 Pearson상관계수 0.186으로 두 군간에 관련성은 없었다 (p=0.344). 결론 : 이중반전회복 자기공명영상에서 유방암의 병변 대 정상조직간 신호강도 비와 자기공명분광영상에서의 콜린 공명의 상대적인 양은 서로 상관관계를 보이지 않았다.

• 한국진공학회:학술대회논문집
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• 한국진공학회 2015년도 제49회 하계 정기학술대회 초록집
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• pp.209.2-209.2
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• 2015

Two dimensional layered materials, such as transition metal dichalcogenides (TMDs) family have been attracted significant attention due to novel physical and chemical properties. Among them, molybdenum disulfide ($MoS_2$) has novel physical phenomena such as absence of dangling bonds, lack of inversion symmetry, valley degrees of freedom. Previous studies have shown that the interface of metal/$MoS_2$ contacts significantly affects device performance due to presence of a scalable Schottky barrier height at their interface, resulting voltage drops and restricting carrier injection. In this study, we report a new device structure by using few-layer graphene as the bottom interconnections, in order to offer Schottky barrier free contact to bi-layer $MoS_2$. The fabrication of process start with mechanically exfoliates bulk graphite that served as the source/drain electrodes. The semiconducting $MoS_2$ flake was deposited onto a $SiO_2$ (280 nm-thick)/Si substrate in which graphene electrodes were pre-deposited. To evaluate the barrier height of contact, we employed thermionic-emission theory to describe our experimental findings. We demonstrate that, the Schottky barrier height dramatically decreases from 300 to 0 meV as function of gate voltages, and further becomes negative values. Our findings suggested that, few-layer graphene could be able to realize ohmic contact and to provide new opportunities in ohmic formations.

• 한국환경과학회지
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• 제12권12호
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• pp.1245-1254
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• 2003

A numerical simulation for 11 February 1996 has been done to grasp main mechanisms of the occurrence of strong downslope winds near Gangnung area. The simulation performed by using ARPS (Advanced Regional Prediction System) showed that enhanced surface winds were not related with a reflection of vertically propagating gravity waves. Froude numbers were about 1.0, 0.4 and 0.6 for the atmosphere above Daekwanryoung and above a place located 220km upstream, and above another place located 230km downstream from the Taebak mountains, respectively. This suggested that as a subcritical flow ascended the upslope side of the Taebak mountains, Froude numbers would tend to increase according to the increase in wind speed, and near the crest the flow would become supercritical and continue to accelerate as it went down the downslope side until it was adapted back to the ambient subcritical conditions in a turbulent hydraulic jump. Simulated Froude numbers corroborated the hydraulic jump nature of the strong downslope wind. In addition, the inversion was found near the mountain top height upstream of the mountains, and it was favorable for the occurrence of strong downslope winds.