Cellular responses to human cytomegalovirus infection

이찬희 忠北大學校 遺傳工學硏究所 1988 遺傳工學硏究 Vol.2 No.1

공동주택에서의 실내조경 도입을 위한 거주자 의식 조사 연구

이찬희,조성우,오세규,Lee, Chan-Hui,Cho, Sung-Woo,Oh, Se-Gyu 한국주거학회 2006 한국주거학회 논문집 Vol.17 No.5

This study begins to make inquires about user's opinion of introducing Interior Landscape into Apartment Housing to grip the problems of contemporary Interior Landscape and suggest the fundamental data to improve it. The city-ward drifting of population drawn from industrial development and aggravation of living condition bring about exclusion of nature and lack of green space. Furthermore, it increases the length of stay of urban liver in indoor space. Thus, dwellers' desire to Interior Landscape increase but housing can't follow it. The purpose of this study is to understand characteristics of Interior Landscape, derive essential factors, study plans, establish radical data, and suggest better plans including Interior Landscape through making inquires about user's opinion.

北韓 '조선력사 '新敎科書의 內容分析

李讚熙 한국사회과교육연구회 1993 사회과교육 Vol.- No.26

대조사 석조 미륵보살 입상의 산출상태, 풍화 및 훼손과 보존처리

이찬희,최석원,서만철,최명윤 대한지질학회 2001 대한지질학회 학술대회 Vol.2001 No.

[인권 보호받지 못하는 외국인 노동자들] 우리시대 또 다른 약자 교회가 껴안아야

이찬희 새가정사 1993 새가정 Vol.- No.-

개선된 SOG 기반 고속 세선화 알고리즘($SOG^*$)

이찬희,정순호,Lee, Chan-Hui,Jeong, Sun-Ho 한국정보처리학회 2001 정보처리학회논문지B Vol.8 No.6

본 논문은 기존의 신경망을 이용한 세선화 방법 중에서 자기 구성 그래프(Self-Organized Graph:SOG) 세선화 기법의 우수한 세선화 결과를 유지하면서, 수행 속도를 향상시키기 위하여 Kohonen Features Map의 새로운 점증 기법을 변형된 SOG에 적용한 개선된 SOG(Improved SOG:$SOG^*$) 세선화 기법을 제안한다. 실험 결과로써 숫자와 문자 모두 기존의 SOG와 같은 우수한 세선화 결과를 나타내며, O((logM)3)의 시간 복잡도를 가지는 속도 향상을 이루었다. 따라서 본 논문에서 제안한 방법은 숫자 또는 문자 인식에 있어 특징 추출의 빠른 전처리 과정으로 사용할 수 있다. In this paper, we propose Improved Self-Organized Graph(Improved SOG:$SOG^*$)thinning method, which maintains the excellent thinning results of Self-organized graph(SOG) built from Self-Organizing features map and improves the performance of modified SOG using a new incremental learning method of Kohonen features map. In the experiments, this method shows the thinning results equal to those of SOG and the time complexity O((logM)3) superior to it. Therefore, the proposed method is useful for the feature extraction from digits and characters in the preprocessing step.

歷史意識의 槪念과 歷史敎育

李讚熙 한국사회과교육연구회 1989 사회과교육 Vol.- No.22

Authigenic Phillipsite in Deep-sea Manganese Nodules from the Clarion-Clipperton Fracture Zones, NE Equatorial Pacific

이찬희,이성록,Lee, Chan Hee,Lee, Sung-Rock The Korean Society of Economic and Environmental G 1996 자원환경지질 Vol.29 No.4

망간단괴내에 자생하는 필립사이트는 단괴의 핵을 이루는 풍화된 화산암편과 고화된 해저퇴적물 또는 단괴를 이루는 망간광물들의 층간에서 산출된다. 이 광물은 주로 화산성 유리질 석기들의 가상조직을 보이고 있으며, 연한 노란색을 갖는 등립질의 판상으로 산출된다. 필립사이트 입자들은 자형의 삼각능, 사각기둥 또는 도변상을 가지며 크기는 길이 $2{\sim}20{\mu}m$, 두께 $2{\sim}5{\mu}m$정도이다. 이 광물의 화학조성은 $({Ca_{0.1}Mg_{0.3}Na_{1.1}K_{1.5}})_3{(Fe_{0.3}Al_{4.2}Si_{11.8})O_{32}{\cdot}10H_2O}$이며, $Si/(Al+Fe^{+3})=2.37-2.78$, Na/K=0.59-0.81 로서 Si와 알카리의 함량이 아주 높다. 결정구조는 단사정계($P2_l/m$) 속하며 $a=10.005{\AA}$, $b=14.129{\AA}$, $c=8.686{\AA}$, ${\beta}=124.35^{\circ}$ 이고 $V=1013.6{\AA}^3$ 이다. 심해저 환경으로 보아 망간단괴에서 산출되는 필립사이트는 보통 $10^{\circ}C$ 이하의 온도, 0.7 kb 정도의 압력, pH 8 정도의 조건에서 자생하는 것으로 추정된다. The occurrence, optical property, chemical composition, crystal structure and formation environments of the phillipsite within deep-sea manganese nodules were systematically investigated in this study. Phillipsite in manganese nodules occurs in nucleus of nodules along with consolidated bottom sediments, weathered volcanic debris, and interstitial grains in the each layer of manganese encrusts. Phillipsite is predominantly pseudomorphs of volcanic shards, and occurs as white to pale yellow in color lath-shaped and equant crystals. These show aggregations of prismatic, blocky, and bladed of 2 to $20{\mu}m$ long, and 2 to $5{\mu}m$ thick. The simplified average chemical formula of phillipsite is $({Ca_{0.1}Mg_{0.3}Na_{1.1}K_{1.5}})_3{(Fe_{0.3}Al_{4.2}Si_{11.8})O_{32}{\cdot}10H_2O}$ with a very siliceous and alkalic. The $Si/(Al+Fe^{+3})$ ratio is 2.37 to 2.78 and alkalis greatly exceed the divalent exchangeable cations, and Na/K ratio is 0.59 to 0.81. The phillipsite is monoclinic ($P2_l/m$) with the unit-cell parameters, $a=10.005{\AA}$, $b=14.129{\AA}$, $c=8.686{\AA}$, ${\beta}=124.35^{\circ}$, and $V=1013.6{\AA}^3$. Phillipsites in manganese nodules formed apparently authigenically at a temperature less than $10^{\circ}C$, and they crystallized at a pressure of less than 0.7 kb, and pH of about 8 in deep-sea environments.

불국사 다보탑의 암석학적 특징, 훼손도 및 보존과학적 진단

이찬희,이명성,최석원,서만철,김만갑 대한지질공학회 2002 대한지질공학회 학술발표회논문집 Vol.2002 No.1

공주제일광산 수계에 분포하는 지하수, 지표수, 토양 및 퇴적물의 환경지구화학적 특성과 중금속 오염

이찬희 대한자원환경지질학회 1999 자원환경지질 Vol.32 No.6

Enviromental geochemisty and heary metal contamination at the Kongjueil mine creek were underaken on the basis of physicohemical properties and mineralogy for various kinds of water (surface, mine and ground water),soil, precipitate and sediment collected of April and December in 1998. Hydrgeochemical composition of the water samples are characterized by relatively significant enricant of Ca+Na, alkiali ions $NO_3$ and Cl inground and surfore water, wheras the mine waters are relatively eneripheral water of the mining creek have the characteristics of the (Ca+Mg)-$(HCO_3+SO_4)$type. The pH of the mine water is high acidity (3.24)and high EC (613$\mu$S/cm)compared with those of surface and ground water. The range of $\delta$D and $\delta^{18}O$ values (relative to SMOW) in the waters are shpwn in -50.2 to -61.6% and -7.0 to -8.6$\textperthousand$(d value=5.8 to 8.7). Using computer program, saturation index of albite, calcite, dolomite in mine water are nearly saturated. The gibbiste, kaolinite and smectite are superaturated in the surface and ground water, respectively. Calculated water-mineral reaction and stabilities suggest that weathing of silicate minerals may be stable kaolinite owing to the continuous water-rock reaction. Geochemical modeling showed that mostly toxic heavy metals may exist larfely in the from of metal-sulfate $(MSO_4\;^2)$and free metal $(M^{2+})$ in nmine water. These metals in the ground and surface water could be formed of $CO_3$ and OH complex ions. The average enrichment indices of water samples are 2.72 of the groundwater, 2.26 of the surface water and 14.15 of the acid mine water, normalizing by surface water composition at the non-mining creek, repectively. Characteristics of some major, minor and rate earth elements (Al/Na, K/Na, V/Ni, Cr/V, Ni/Co, La/Ce, Th/Yb, $La_N/Yb_N$, Co/Th, La/Sc and Sc/Th) in soil and sediment are revealed a narrow range and homogeneous compositions may be explained by acidic to intermediate igneous rocks. And these suggested that sediment source of host granitic gneiss colud be due to rocks of high grade metamorphism originated by sedimentary rocks. Maximum concentrations of environmentally toxic elements in sediment and soil are Fe=53.80 wt.% As=660, Cd=4, Cr=175, Cu=158, Mn=1010, Pb=2933, Sb=4 and Zn=3740 ppm, and extremely high concentrations are found are found in the subsurface soil near the ore dump and precipitates. Normalizing by composition of host granitic gneiss, the average enerichment indices are 3.72 of the sediments, 3.48 of the soils, 10.40 of the precipitates of acid mine drainage and 6.25 of the soils near the main adit. The level of enerichment was very severe in mining drainage sediments, while it was not so great in the soils. mineral composition of soil and sediment near the mining area were partly variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. reddish variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. Reddish brown precipitation mineral in the acid mine drainage identifies by schwertmanite. From the separated mineralgy, soil and sediment are composed of some pyrite, arsenopyite, chalcopyrite, sphalerite, galena, malachite, goethite and various kinds of hydroxied minerals.