• Proceedings of the Korean Information Science Society Conference
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• 2004.04b
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• pp.826-828
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• 2004

홍채인식 시스템은 영상획득, 전처리, 특징 추출, 패턴 정합의 단계로 이루어져 있다. 이 중 특징 추출은 특징 차원의 감소뿐만 아니라 분류 정착도의 증가를 위한 필수적인 과정이다. 본 논문에서는 특징을 추출하는데 있어서, 홍채데이타에 웨이블렛 변환의 다해상도 분석 기법을 시도하여 일정 영역을 추출한 후, 그 영역에 유전자 알고리즘(Genetic Algorithm)을 적용하여 가장 분별력 있는 특징들만을 추출 및 사용하는 홍채인식 시스템을 제안한다. 유전자 알고리즘의 선택연산자로는 적응도 비례 방식과 전역 엘리트 방식을 사용하였으며, 적합도 함수로는 Gaussian Kernel을 사용하는 Support Vector Machine(SVM)을 사용하였다. 본 시스템을 통해 나온 최적의 특징집합을 이용한 SVM분류기로 인식률을 알아본 결과 웨이블렛만을 사용했을 때 보다 대략 1.5%정도 더 좋은 인식률을 얻을 수 있었다.

• Proceedings of the Korea Information Processing Society Conference
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• 2015.04a
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• pp.901-904
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• 2015

본 논문에서는 사진의 태그정보 및 통계정보, 사용자 평점을 이용하여 여행에 앞서 본인의 취향 등에 맞는 개인화 된 여행계획을 생성할 수 있도록 지원하는 연구를 진행하였다. 개인화 된 여행계획의 자동생성을 위하여, 나이, 성별, 직업, 소득, 학력에 따라 선호하는 여행의 태마를 통계자료를 통해 구분하였고, 사진의 태그정보를 이용하여 사용자가 가장 선호하는 테마를 분별하여 개인화 할 수 있도록 하였다. 이렇게 구분된 태마는 다양한 포털사이트에 등록된 사용자 평점 정보를 토대로 하여 여행계획을 생성하여 사용자에게 제공할 수 있도록 하였다.

• Proceedings of the Korea Information Processing Society Conference
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• 2000.04a
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• pp.288-292
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• 2000

본 논문은 컴퓨터 그래픽 이미지의 데이터를 디지털화 하는 과정에서 Aliasing으로 인하여 손실된 Pixel 정보에 대해 동적 블럭으로 분할 연산하고 벡터 양자화, Gaussian 함수를 이용하여 손실된 정보들을 보간하여 해상도가 높아진 영상을 얻을 수 있는 새로운 Anti-Aliasing 알고리즘을 제시한다. Anti-Aliasing의 효과를 더욱 시각적으로 분별 할 수 있도록 하기 위해 Gray 레벨의 이미지로 실험을 하였고, 현재 Graphic을 지원하는 하드웨어 구조의 PC 기반에 변화 없이 적용할 수 있고, 이미지의 질감을 더욱 부드럽게 향상 시킬수가 있다.

• Nuclear Engineering and Technology
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• v.15 no.2
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• pp.149-153
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• 1983

The removal of zinc (II) from aqueous solutions has been studied by the adsorptive bubble separation processes such as solvent sublation and foam fractionation processes using capric acid as collector. The efficiency of the remoal process has been studied by changing the ionic strength and pH and the bubble separation method has been compared with the solvent extraction process using the capric acid dissolved in benzene as extractant.

• The Journal of the Petrological Society of Korea
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• v.23 no.3
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• pp.221-227
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• 2014

With the advent of multi collector-inductively coupled plasma mass spectrometry, stable isotopic variations of non-traditional metal elements have provided important constraints on the sources of geologic materials. This review introduces the principles of magnesium isotopic fractionation and analytical methods. Recent case studies are also reviewed for the use of magnesium isotope signatures to decipher the source materials of I-, S-, and A-type granitoids in western North America, Australia, and China.

• Proceedings of the Korea Information Processing Society Conference
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• 2020.11a
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• pp.446-449
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• 2020

다크웹을 이용한 사이버 범죄율이 국내외에서 가파르게 상승 중이다. 그러나 다크웹의 특성상 숨겨져 있는 인터넷 영역에서 공유되는 악성코드들을 찾기란 어렵다. 특히 다크웹상 여러 서비스들은 크롤러 bot과 같은 정보 수집을 막고자 다양한 기법을 적용하고 있다. 따라서 우리는 기존의 연구 방법에 따라 다크웹 상의 URL을 수집한 후, 추가적으로 다운로더를 만들어 exe, zip과 같은 특정 형식의 파일을 수집하였다. 앞으로 해당 파일들은 통합 바이러스 스캔 엔진에서 검사하여 의심 파일들을 분별할 예정이다. 의심 파일들은 정적 / 동적 분석을 통해 상세한 보고서를 제출하여 향후 다크웹 내의 악성코드 분포 / 출처 분석에 유의미한 결과를 도출할 수 있다.

• Economic and Environmental Geology
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• v.46 no.5
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• pp.375-390
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• 2013

The Kenticha rare-element (Ta-Li-Nb-Be) mineralized zone is located in ophiolitic fold and thrust complex of southern Ethiopia and was firstly discovered by joint exploration program of Ethiopia-Soviet in 1980s. It includes Dermidama, Kilkele, Shuni Hill, Kenticha, and Bupo pegmatites from south to north. The Kenticha pegmatite intruded parallel to NS-striking serpentinite and talc-chlorite schist, and is exposed approximately 2 km length and 400-700 m width. The Kenticha pegmatite is internally zoned and subdivided into lower quartz-muscovite-albite granite, intermediate muscovite-quartz-albite-microcline pegmatite, and upper spodumene-quartz-albite pegmatite, based on their mineral assemblage. The major, trace elements (e.g., Rb, Li, Nb, Ta, and Ga), and element ratios (e.g., K/Rb, Nb/Ta, Mg/Li, and Al/Ga) suggest that the fractionation and solidification of pegmatite have progressed from the lower towards upper pegmatite. In contrast, unlike general magmatic fractionation, Mg/Li ratios of the Kenticha pegmatite tend to be increased towards the upper pegmatite. It may result from post-magmatic hydrothermal alteration and/or interaction with upper ultramafic rock. Rare-element mineralization in Kenticha pegmatite concentrates on the upper pegmatite, which contains up to 3.0 wt % $Li_2O$, 3,780 ppm Rb, 111 ppm Cs, 1,320 ppm Ta, and 332 ppm Nb. Ore minerals in Kenticha pegmatite mostly include tantalite, spodumene, and lepidolite, and tantalite has an association with coarser quartz-spodumene and relatively fine sacchroidal albite. The tantalite is classified into Mn-tantalite as a function of $Mn^*[Mn/(Mn+Fe)]$ and $Ta^*[Ta/(Ta+Nb)]$ values. Its compositions ($Mn^*$, $Ta^*$, and Nb/Ta) between coarse and fine tantalites are different and the former is strongly enriched in Ta and depleted in Nb compared to latter one. In conclusion, rare-element mineralization in the Kenticha pegmatite may has occurred in the latest stage of magmatic fractionation.

• Biomedical Science Letters
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• v.2 no.2
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• pp.187-198
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• 1996

The cut-off values and related factors for total cholesterol of serum in normal Korean adults were studied from March to October, 1995, based on the data of 1,818 healthy adults of human involved the male and female. The comparisons of the serum total cholesterol levels were analyzed by sex, age, systolic blood pressure, diastolic blood pressure, body weight, height, PIBW, BMI and other biochemical tests. 1. The serum total cholesterol level were 194.4 mg/dl in total group, 186.9 mg/dl for male, and 197.6 mg/dl for female. 2. There was no significant differences by sex among the 21 to 50 ages group, but significantly higher in women than in men over 51 years old. 3. In general, the levels of serum total cholesterol were increased with age, the highest level in men was 192.7 mg/ dl in 51 to 60 years old, and 210.5 mg/dl in more than 60 years old in women. 4. The cut-off values of serum total cholesterol for moderate risk were 191 mg/dl in 21 to 30 years group, 195 mg/dl in 31 to 40 years,214 mg/dl in 41 to 50 years, 227 mg/dl in 51 to 60 years, and 222 mg/dl in more than 61 years. The cut-off values of serum total cholesterol for high risk were 214 mg/dl dl in 21 to 30 years group, 214 mg/dll in 31 to 40 years, 239 mg/dl in 41 to 50 years, 213 mg/dl in 51 to 60 years, and 248 mg/dl in more than 61 years. 5. The mean values of serum total cholesterol were showed positive correlation with age, PIBW, BMI, systolic blood pressure and diastolic blood pressure. 6. Serum total cholesterol level of drinking group(188.9$\pm$34.85mg/dl) was showed love. than those of non-drinking group(196.0$\pm$36.0 mg/dl). 7. Serum total cholesterol levels of regular excercise group(192.1$\pm$33.3 mg/dl) was significantly lower than those of non regular excercise group(195.8$\pm$37.0 mg/dl).

• Economic and Environmental Geology
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• v.50 no.5
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• pp.375-387
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• 2017

Amphibolite-hosted Fe-Ti mineralization at the Soyeonpyeong Island, located in central western part of the Korean Peninsula is a typical orthomagmatic Fe-Ti oxide deposit in South Korea. The amphibolite intruded into NW-SE trending Precambrian metasedimentary rocks. Lower amphibolite is characterized by igneous layering, consisting of feldspar-dominant and amphibole-Fe-Ti oxide-dominant layers. The igneous layering shows complicated and/or sharp contact. In contrast, upper amphibolite has a more complicated lithofacies (garnet-bearing, coarser, and schistose), and massive Fe-Ti oxide ore alternates with schistose amphibolite. NS- and EW-trending fault systems lead to redistribute upper amphibolite-hosted Fe-Ti orebody and igneous layering of lower amphibolite, respectively. The whole-rock compositions of amphibolite and Fe-Ti oxide ore reflect their constituent minerals. Amphibolite shows significantly positive Eu anomalies whereas Fe-Ti oxide ore has weak negative Eu anomalies. Plagioclase (Andesine to oligoclase) and Fe-Ti oxide minerals have constant composition regardless of their distribution. Amphibole has a compositionally variable but it doesn't reflect the chemical evolution. Mineral compositions within individual layers and successive layers are relatively constant not showing any stratigraphic evolution. This suggests that there are no successive injections of Fe-rich magma or assimilation with Fe-rich country rocks. Contrasting Eu anomalies between amphibolite and Fe-Ti oxide ore also suggest that extensive plagioclase fractionation during early crystallization stage cause increase in $Fe_2O_3/FeO$ ratio and overall Fe contents in the residual magma. Thus, Fe-rich residual liquids may migrate at the upper amphibolite by filter pressing mechanism and then produce sheeted massive Fe-Ti mineralization during late fractional crystallization.

• The korean journal of orthodontics
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• v.26 no.2 s.55
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• pp.205-218
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• 1996

A given facial type can be considered as a syndrome in which various features are aggregated, so a single parameter is not sufficient to accurately identify a given facial type. This study was designed to identify & characterize the skeletal types that blend under the headline-'Cl III,deepbite'. Cephalograms of thirty-four untreated mixed dentition patients, selected mainly on the basis of clinical impression of Cl III with reduced lower face heights were studied. The following conclusion can be drawn. 1. Cl III malocclusion with reduced lower face height could be classified into three types. 2. Subtype 1 was identified by the following features : strong ramus, more anteriorly positioned upper molars without alveolar hypoplasia, acutely reduced Mn. plane angle. 3. Subtype 2 was characterized by a short ramus, sharply reduced postrior alveolar height, and normal Mn. plane angle. In general, this type had hypoplasia tendency in the vertical dimension. 4. In subtype 3, the AUFH occupying more percentage than ALFH was a outstanding feature. Ramal height was in normal range, alveolar hypoplasia and slightly reduced Mn. plane angle was observed. 5. The features of the subtypes were reflected in certain indices, which can be regarded as discriminative index. LAFH: if reduced, regardless of subtypes, indicates reduced lower ant. face height consistently. FHR: when this ratio is increased, it indicates subtype 1. FHI: when this ratio is in normal range, it indicates subtype 2. FPI: if reduced greatly, it indicates subtype 3.