• 한국결정성장학회지
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• 제33권4호
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• pp.145-152
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• 2023

2.31 × 10⁴ ≤ Gr_t ≤ 4.68 × 10⁴의 범위에서 온도 Grashof 수(Gr_t)의 변화에 대하여, 소스와 결정영역에서의 평균 Nusselt수를 나타내고 있다. 결정영역에서의 평균 Nusselt 수가 소스영역에서의 평균 Nusselt 수 보다 2배 이상 큰 것으로 나타나고 있다. 소스영역에서의 평균 Nusselt 수는 온도 Grashof 수(Gr_t)에 대하여, 증가하는 경향을 보여주고 있으며, 반면에 결정영역에서의 평균 Nusselt 수는 온도 Grashof 수(Gr_t)에 대하여, 감소하는 경향을 나타나고 있다. 3.28 × 10⁵ ≤ Gr_s ≤ 4.43 × 10⁵의 범위에서 농도 Grashof 수(Gr_s)의 변화에 대하여, 소스와 결정영역에서의 평균 Sherwood 수를 나타내고 있다. 소스영역과 결정영역에서의 평균 Sherwood 수는 농도 Grashof 수(Gr_s)가 증가함에 따라, 감소하는 경향을 보이고 있다. 결정영역에서의 평균 Sherwood 수는 소스영역에서의 평균 Sherwood 수보다 약 4배 정도 크다.

• Journal of Astronomy and Space Sciences
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• 제38권2호
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• pp.135-143
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• 2021

We report, for the first time, the afternoon (i.e., from noon to sunset time) observations of the northern mid-latitude E-region field-aligned irregularities (FAIs) made by the very high frequency (VHF) coherent backscatter radar operated continuously since 29 December 2009 at Daejeon (36.18°N, 127.14°E, 26.7°N dip latitude) in South Korea. We present the statistical characteristics of the mid-latitude afternoon E-region FAIs based on the continuous radar observations. Echo signal-to-noise ratio (SNR) of the afternoon E-region FAIs is found to be as high as 35 dB, mostly occurring around 100-135 km altitudes. Most spectral widths of the afternoon echoes are close to zero, indicating that the irregularities during the afternoon time are not related to turbulent plasma motions. The occurrence of afternoon E-regional FAI is observed with significant seasonal variation, with a maximum in summer and a minimum in winter. Furthermore, to investigate the afternoon E-region FAIs-Sporadic E (E_s) relationship, the FAIs have also been compared with E_s parameters based on observations made from an ionosonde located at Icheon (37.14°N, 127.54°E, 27.7°N dip latitude), which is 100 km north of Daejeon. The virtual height of E_s (h'E_s) is mainly in the height range of 105 km to 110 km, which is 5 km to 10 km greater than the bottom of the FAI. There is no relationship between the FAI SNR and the highest frequencies (f_tE_s) (or blanket frequencies (f_bE_s)). SNR of FAIs, however, is found to be related well with (f_tE_s-f_bE_s).

• Structural Engineering and Mechanics
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• 제57권4호
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• pp.587-602
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• 2016

In structural reliability analysis, the response surface method is widely adopted because of its numerical efficiency. It should be understood that the response function must approximate the actual limit state function accurately in the main region influencing failure probability where it is evaluated. However, the size of main region influencing failure probability was not defined clearly in current response surface methods. In this study, the concept of sub-region of interest is constructed, and an improved response surface method is proposed based on the sub-region of interest. The sub-region of interest can clearly define the size of main region influencing failure probability, so that the accuracy of the evaluation of failure probability is increased. Some examples are introduced to demonstrate the efficiency and the accuracy of the proposed method for both numerical and implicit limit state functions.

• Asian Journal of Business Environment
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• 제1권1호
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• pp.21-25
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• 2011

Sub-region cooperation is necessary based on the condition that China-Japan-Korea free trade area has not been established. Shandong has common interests with Koreain economic and trade cooperation and it has been equipped with prominent external environment and industrial advantages in sub-region cooperation. The article discusses the advantages, the specific patterns, the cooperation contents and the matched government measures of sub-region cooperation between Shandong and Korea, with the purpose of modifying the relevant policies launched by government.

• 한국지형학회지
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• 제17권3호
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• pp.49-57
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• 2010

본 연구는 GIS를 이용하여 경상북도를 대상으로 10가지 지질 지역별 지형 기복의 분포 특성을 분석하였다. PEs, PEgrgn, Pp₂, Kav·Kiv, Khgr 지역은 급경사-고고도 지형과 급경사-중고도 지형 기복이 60% 이상을 차지하는 지역으로, 풍화와 침식에 대한 저항력이 강한 경암 지역으로 판단되고, 사면에서의 풍화·침식 작용이 아직 덜 진행된 곳으로 경상북도에서 높은 산지를 형성하고 있다. 한편, Ke_1-9, Te_1-2 지역은 저고도 지형 기복이 70% 이상을 차지하는 지역으로, 상대적으로 풍화와 침식에 대한 저항력이 약한 연암 지질 지역으로 판단되고, 사면에서의 풍화·침식 작용도 활발한 지역이다. Ke_1-9 지역은 낙동강 본류와 그 지류 하천에 인접한 지역으로 경상북도에서 내륙의 평지와 구릉성 산지를 형성하고 있으며, Te_1-2 지역은 동해안에 인접한 지역으로 경상북도에서 해안 저지대를 형성하고 있다. 또한, Jgr 지역은 중고도 지형이 70% 이상을 차지하며, 경상북도에서 낮은 산지 또는 평지를 형성하고 있다. 마지막으로, Ols₁ 지역은 급경사 지역이 50% 이상을 차지하며 사면에서의 풍화·침식 작용이 활발한 지역으로 경상북도에서 내륙의 산지를 형성하고 있다.

• 한국결정성장학회지
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• 제33권3호
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• pp.110-115
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• 2023

브로민화 수은(I)(Hg₂Br₂) 물리적 증착법 공정에서 구성요소 B의 분압, P_B를 40 Torr에서 200 Torr로 증가시켰을 때 1개의 셀(unicell)이 결정성장영역에서 기체상 공간의 중심으로 이동함을 보여주고 있다. P_B = 40 Torr에서는 경계층 흐름이 지배적이고, P_B = 200 Torr에서는 코어영역흐름(core region)을 보이고 있다. 고려되는 물리적 증착법 공정에서 P_B = 40 Torr와 P_B = 200 Torr에서 1개(single)의 셀(cell) 형태로 3차원의 유동의 흐름과 x, y 직교 중심축에 대하여 비대칭 유동흐름을 나타내고 있다. 소스와 결정 영역 사이의 임계 온도차는 약 30 K입니다. Hg₂Br₂의 총 몰 플럭스는 임계값에 도달할 때까지 온도차에 따라 증가한다. 임계 총 몰 플럭스에서 총 몰 플럭스는 갑자기 감소한다.

• 한국정보과학회:학술대회논문집
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• 한국정보과학회 2010년도 한국컴퓨터종합학술대회논문집 Vol.37 No.1(C)
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• pp.447-451
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• 2010

In this paper, we propose a simple but effective algorithm to increase the speed of Emphysema region classification. Emphysema region classification method based on CT image consumes a lot of time because of the large number of subregions due to the large size of CT image. Some of the sub-regions contain no Emphysema and the classification of these regions is worthless. To speed up the classification process, we create an algorithm to select Emphysema region candidates and only use these candidates in the Emphysema region classification instead of all of the sub-regions. First, the lung region is detected. Then we threshold the lung region and only select the dark pixels because Emphysema only appeared in the dark area of the CT image. Then the thresholded pixels are clustered into a region that called the Emphysema pre-detected region or Emphysema region candidate. This region is then divided into sub-region for the Emphysema region classification. The experimental result shows that Emphysema region classification using predetected Emphysema region decreases the size of lung region which will result in about 84.51% of time reduction in Emphysema region classification.

• Transactions on Electrical and Electronic Materials
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• 제17권2호
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• pp.104-108
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• 2016

To research the correlation between oxygen vacancy and the electrical characteristics of ZTO, which is made by using a target mixed ZnO:SnO₂=1:1, the ZnO, SnO₂ and ZTO were analyzed by PL, XPS, XRD patterns and electrical properties. It was compared with the electron orbital spectra of O 1s in accordance with the electrical characteristics of ZnO, SnO₂ and ZTO. The electrical characteristics of ZTO were improved by increasing the annealing temperatures, due to the high degree of crystal structures at a high temperature, and the physical properties of ZTO was similar to that of ZnO. The amorphous structure of SnO₂ was increased with increasing the temperature. The Schottky contact of oxide semiconductors was formed using the depletion region, which is increased by the electron-hole combination due to the annealing processes. ZnO showed the Ohmic contact in spite of a high annealing temperature, but SnO₂ and ZTO had Schottky contact. As such, it was confirmed that the electrical properties of ZTO are affected by the molecules of SnO₂.

• 전기학회논문지
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• 제65권10호
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• pp.1697-1701
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• 2016

The leakage conduction and critical voltage characteristic of ZnO ceramic were investigated as a function of $Sb_2O_3$ concentration. Leakage conduction in the ohmic region increased with increasing $Sb_2O_3$ concentration and was attributed to the potential barrier height. The nonlinear coefficient increased with an increasing amount of $Sb_2O_3$. It was found that increases in the apparent critical voltages were associated with the lowered donor concentration in the grain boundary of between two ZnO grains. And the decrease of donor concentration on doping with $Sb_2O_3$ additive was attributed to the lowered capacitance in the grain boundary layer.

• 충청수학회지
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• 제33권1호
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• pp.157-163
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• 2020

Conley introduced attracting sets and repelling sets for a flow on a topological space and showed that if f is a flow on a compact metric space, then 𝓡(f) = ⋂{A_U ∪ A*_U |U is a trapping region for f}. In this paper we introduce chain recurrent set, trapping region, attracting set and repelling set for a flow f on a TVS-cone metric space and prove that if f is a flow on a compact TVS-cone metric space, then 𝓡(f) = ⋂{A_U ∪ A*_U |U is a trapping region for f}.