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고주파 부분방전(HFPD)의 Pulse Analysis Map에 의한 GIS 결함 판별에 관한 연구
정현재(J.H. Jung),김지홍(J.H. Kim),김진기(J.G. Kim),고흥열(H.Y. Ko),구자윤(J.Y. Koo),김정태(J.T. Kim) 대한전기학회 2006 대한전기학회 학술대회 논문집 Vol.2006 No.10
Since one decade, the detection of High frequency Partial Discharge has been proposed as one of the effective method for the diagnosis of the power component under service in power grids. As a tool for this detection, UHF sensor based on the antenna technology has been commercialized for mainly GIS due to its advantages. However, regarding the recognition of the vital defects introducible into the GIS. different types of softwares have been proposed and employed without any convincing probability of identification. In this regards, our work leads us to suggest a novel method named "PA Map" to identify the defects inside the GIS based on the HFPD detection by use of HFCT sensor which is designed according to our patent.
정영상,류관식,임정남,Jung, Y.S.,Ryu, K.S.,Im, J.N. 한국토양비료학회 1980 한국토양비료학회지 Vol.13 No.1
강우강도가 100mm/hr인 인공강우기(人工降雨器)를 이용(利用)하여 밭토양의 강우침투성(降雨浸透性)을 조사(調査)하고, 침투수(浸透水)의 토양중재분포를 Youngs의 이론식(理論式)에 의(依)하여 추정(推定)한 것과 비교(比較)한 결과(結果)는 다음과 같았다. 1. 토양별 한계강우침투속도(限界降雨浸透速度)는 강우강도 100mm/hr 조건하(條件下)에서 식양토 내지(乃至) 식토(埴土)에서 10mm/hr 이하(以下), 양토에서 10~20mm/hr, 사양토에서 20~30mm/hr, 및 사토(砂土)에서 30mm/hr 이상(以上)으로 나타났으며, 한계강우침투속도(限界降雨浸透速度)에 도달(到達)하는 시간(時間)은 15~20분(分) 이었다. 2. 토양별 표토(表土)의 포화투수계수는 삼각사양토에서 0.47mm/min, 송정식양토에서 0.16mm/min, 그리고 전남미사질식양에서 0.14mm/min로 나타났다. 3. 강우후(降雨後) 토양수분의 재분포상양(再分布相樣)은 Youngs 이론식(理論式)에 의(依)하여 추정(推定)된 것과 거의 비슷한 경향이었다. The infiltration rates of the upland soils on hill side slope were investigated in situ using rainulator of which rainfall intensity was 100mm/hr. The soil moisture profile after the water infiltration was compared with that calculated from Youngs' equation. The results obtained are as follows: 1. Time required for infiltration rate to reach constant during rainfall was 15 to 25 min. The infiltration rate measured after 30 min was considered to be final infiltration rate. 2. The final infiltration rates of clay soils were lower than 10mm/hr., loamy soils 10 to 20., coarse loamy soils 20 to 30, and sandy soils higher than 30mm/hr., respectively. 3. The saturated hydraulic conductivity of the surface soil of Samgag sandy loam was 0.47mm/min., Songjeong clay loam0.16 mm/min., and Jeonnam silty clay loam 0.14mn/min., respectively. 4. The soil moisture profile calculated from Young's equation was in close agreement with measured in situ.
이중 크기분포를 가지는 자발형성 InAs 양자점의 광특성 평가
정순일,여현영,윤일구,한일기,이주인,Jung, S.I.,Yeo, H.Y.,Yun, I.,Han, I.K.,Lee, J.I. 한국진공학회 2006 Applied Science and Convergence Technology Vol.15 No.3
서로 다른 성장조건 하에서 자발형성 InAs 양자점 (quantum dot, QD)을 제작하고. 그 특성을 photoluminescence (PL) 로 분석하였다. 비교적 높은 기판온도에서 성장된 QD 시료들의 PL 스펙트럼에서 분명한 차이를 나타내는 double-peak이 관측되었다. 온도 및 여기광 출력의존성 (temperature- and excitation power dependence) PL을 이용하여 그 double-peak이 서로 다른 크기분포를 가지는 두개의 InAs QD집단에서의 기저발광 (Eo) 에 의한 peak 임을 알 수 있었다. 게다가 이중크기분포에서 InAs 두께변화는 서로 대립되는 두 QD집단에서 QD 수의 변화를 초래한다는 것 또한 증명하였다. We report a photoluminescence (PL) study on the growth process of self-assembled InAs quantum dots (QDs) under the various growth conditions. Distinctive double-peak feature was observed in the PL spectra of the QD samples grown at the relatively high substrate temperature. From the excitation power-dependent PL and the temperature-dependent PL measurements, the double-peak feature is associated with the ground state transitions from InAs QDs with two different size branches. In addition, the variation in the bimodal size distribution of the QD ensembles with different InAs coverage is demonstrated.