• 인터넷정보학회논문지
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• 제19권1호
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• pp.77-86
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• 2018

지난 수년간 KISTI는 EDISON이라는 온라인 시뮬레이션 실행 플랫폼을 통해 사용자들이 다양한 계산과학공학 분야에서 제공된 사이언스 애플리케이션에 대한 시뮬레이션을 수행할 수 있는 서비스를 제공하고 있다. 일반적으로 이러한 시뮬레이션은 대규모 계산을 수반하므로 대용량의 출력 데이터를 생산해 낸다. 온라인 플랫폼에서 이러한 시뮬레이션을 수행 할 때 발생하는 중요한 문제 중 하나는 많은 사용자가 동일한 (또는 거의 변하지 않는) 입력 매개 변수 또는 파일을 사용하여 시뮬레이션 요청 (또는 작업)을 플랫폼에 동시에 제출함으로써 플랫폼에 상당한 부담을 준다는 점이다. 다시 말해, 동일한 컴퓨팅 작업으로 인해 중복 컴퓨팅 및 스토리지 리소스가 빠른 속도로 소모된다는 점이다. 이와 같은 동일한 시뮬레이션 요청으로 인한 과도한 자원 사용 문제를 극복하기 위해, 본 논문은 실행 메타 데이터, 즉 프로비넌스를 기반으로 시뮬레이션 데이터를 효율적으로 관리하기 위한 IceSheet라는 새로운 프레임 워크를 제안한다. IceSheet 프레임워크는 시뮬레이션 실행과 관련된 프로비넌스를 수집하여 저장한다. 수집된 프로비넌스 정보는 중복 시뮬레이션 요청을 제외할 뿐만 아니라 오픈소스 검색 엔진인 ElasticSearch를 통해 기존 시뮬레이션 결과를 검색하는 데도 사용된다. 특히 본 논문은 IceSheet 프레임워크에서 저장된 시뮬레이션 결과를 검색하고 재사용할 수 있는 핵심 구성 요소에 대해 자세히 설명한다. 우리는 온라인 시뮬레이션 실행 플랫폼과 함께 연동하는 검색 엔진을 기반으로 제안된 프레임워크의 프로토타입을 구현하였다. 플랫폼에서 수집된 실제 시뮬레이션 실행 프로비넌스를 기반으로 제안된 프레임워크의 성능 평가를 수행하였다. 플랫폼과 완벽히 연동된 IceSheet 프레임워크는 사용자로 하여금 선택된 시뮬레이션 소프트웨어에 대해 과거에 입력된 매개 변수 값을 빠르게 검색하고 동일한 입력 매개 변수 값이 존재하는 경우 기존의 결과를 곧바로 반환할 수 있도록 할 것으로 기대된다. 따라서 제안된 프레임워크를 통해 이전에 실행된 시뮬레이션과 동일한 요청에 대해 중복 자원 소모를 없애고 실행 시간을 크게 단축시키는 데 도움이 될 것으로 기대한다.

• 대한치과기공학회지
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• 제32권4호
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• pp.341-350
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• 2010

Purpose: This study focused on achieving desired shades by combining zirconia core with different thickness porcelain in order to make dental prostheses effectively. Methods: White and colored $LAVA^{TM}$ All Ceramic (3M-ESPE, Seefeld, Germany), and Zirkonzahn (Bruneck, Italy) Trans and prettau were used to have Zirconia. LAVATM Ceram (3M-ESPE, Germany) and ICE (Zirkonzahn, Italy) powder were used to have the porcelain. We made quadrilateral specimen of thickness 0.3mm, 0.5mm, 0.7mm and diameter 10 to use zirconia ceramics system of 2 kinds that color tone reappearance way is different and produced total 120 specimens to 4 experimental groups. We used Spectrophotometer to analyze color tone. Data's value getting by dispersal colorimetry period found L*, a*, b* value using Excel program. We used one-way ANOVA to use SPSS WIN 12.0 program. Results: All L*, a*, b* indexes of zirconia core and porcelain veneer in LAVA group and Zirkonzahn group were different. When you combine the white zirconia core of LAVA group with a porcelain veneer, the thickness of the porcelain must be more than 0.5mm to meet the standard target. When all the colored zirconia cores of LAVA group were combined with porcelain veneers, there was no significant difference from the standard target. When the zirconia cores of Zirkonzahn group are combined with porcelain veneers, the thinner thicknesses were closer to the standard tab than thicker thicknesses; however, there was a significant difference in all combinations, with Delta E* value indicating more than 3. Conclusion: When it comes to colored zirconia, which is the most popular, the thicknesses of both a core and a dentin veneer must be more than 0.3mm to get an appropriate shade. There is more possibility to get desirable shades when the thicknesses of a white core are thinner; however, they would be vulnerable to the environment and lose their color. When combine a zirconia core with a dentin veneer, using Zirkonzahn group needs more considerations in order to meet the standard target.

• 한국제4기학회지
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• 제19권2호
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• pp.55-58
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• 2005

A 120-cm core recovered from Lake Hovsgol, the northern Mongolia provides evidence for climate variability since the Marine Isotope Stage 3, representing a sharp lithological change. The lowermost part of the core consists of diatom-barren calcareous silty clay without coarse sands, framboidal pyrite, and biogenic components deposited during the MIS 3. Following the last glacial maximum, in-situ moss is included in the sediments, as lake-level was retreated by cold and dry environment with low precipitation. The AMS radiocarbon ages of the plant fragments match a marked lithologic boundary between 14,060 and 14,325 $^{14}C$ yr BP. The contents of coarse sands abruptly increase, indicating probably wind-derived sandy dust or coarse grains contributed from floating icebergs. And abundant framboidal pyrite grains were deposited in an anoxic environment, as reflected by high accumulation of organic matters at a low lake stand. During the deglaciation, quantities of coarse sands, ostracod, shell fragments, framboidal pyrite, and diatom markedly varies by regional and global scale climate regimes. Some allochthonous coarse sands were probably ice-rafted debris derived from floating icebergs. A rapid increase in diatom productivity probably marked the onset of Bolling-Allerod warming. Subsequent high concentration of framboidal pyrite probably represents a dry and cold condition, such as Younger Drays events. Consistent warm period with high precipitation at Holocene is documented by diatomaceous clayey ooze without framboidal pyrite, coarse sands, and ostracod.

• 한국제4기학회:학술대회논문집
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• 한국제4기학회 2005년도 추계학술대회
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• pp.34-39
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• 2005

A 120-cm core recovered from Lake Hovsgol, the northern Mongolia provides evidence for climate variability since the Marine Isotope Stage 3, representing a sharp lithological change. The lowermost part of the core consists of diatom-barren calcareous silty clay without coarse sands, framboidal pyrite, and biogenic components deposited during the MIS 3. Following the last glacial maximum, in-situ moss is included in the sediments, as lake-level was retreated by cold and dry environment with low precipitation. The AMS radiocarbon ages of the plant fragments match a marked lithologic boundary between 14,060 and 14,325 $^{14}C$ yr BP. The contents of coarse sands abruptly increase, indicating probably wind-derived sandy dust or coarse grains contributed from floating icebergs. And abundant framboidal pyrite grains were deposited in an anoxic environment, as reflected by high accumulation of organic matters at a low lake stand. During the deglaciation, quantities of coarse sands, ostracod, shell fragments, framboidal pyrite, and diatom markedly varies by regional and global scale climate regimes. Some allochthonous coarse sands were probably ice-rafted debris derived from floating icebergs. A rapid increase in diatom productivity probably marked the onset of Bolling-Allerodwarming. Subsequent high concentration of framboidal pyrite probably represents a dry and cold condition, such as Younger Drays events. Consistent warm period with high precipitation at Holocene is documented by diatomaceous clayey ooze without framboidal pyrite, coarse sands, and ostracod.

• Journal of Microbiology and Biotechnology
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• 제14권4호
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• pp.673-679
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• 2004

A microbial cryoprotectant formulation using a W/O/W multiple emulsion system was developed. The psychrotolerant microorganism, B4, isolated from soil in South Korea, was observed by the drop freezing method, in which the microorganism sample inhibited ice nucleation activity. The antifreeze activity was eliminated when the microorganism sample was treated with protease, indicating that the antifreeze activity was due to the presence of antifreeze protein. The result of the l6S rDNA sequencing indicated the B4 strain was most closely related to a species of the genus Bacillus. Culture broth of B4 strain (Bacillus sp.) and rapeseed oil containing 1 % polyglycerine polyricinolate (PGPR) were used as core and wall material, respectively. The most stable W/O emulsion was prepared at a core/oil ratio of 1:2. The highest W/O/W emulsion stability was achieved when the primary emulsion to external aqueous phase containing 0.5% caster oil polyoxyethylene ether $(COG25^{TM})$ ratio was 1:1. Microcrystalline cellulose showed better W/O/W emulsion stability than other polymer types. The viability of cells in a W/O/W emulsion was higher than free cells during storage at $37^\circ{C}$. An acidic pH and UV exposure decreased the viability of free cells, but cells in W/O/W emulsion were more stable under these conditions.

• Ocean and Polar Research
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• 제33권3호
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• pp.211-221
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• 2011

Contents of biogenic components [opal, $CaCO_3$, TOC (total organic carbon)] were measured in Core LHB-3PC sediments collected off Lutzow-Holm Bay, in order to understand glacial-interglacial cyclic variation of the high-latitude surface-water paleoproductivity, in the Indian Sector of the Southern Ocean. An age model was established from the correlation of ARM/IRM ratios of Core LHB-3PC with LR04 stack benthic ${\delta}^{18}O$ records, in complement with radiocarbon isotope ages and biostratigraphic Last Appearance Datum (LAD). The core-bottom age was estimated to be about 700 ka. Although the $CaCO_3$ content is very low less than 1.0% throughout the core, the opal and TOC contents show clear glacial-interglacial cyclic variation such that they are high during the interglacial periods (7.2-50.3% and 0.05-1.00%, respectively) and low during the glacial periods (5.2-25.2% and 0.01-0.68%, respectively). According to the spectral analysis, the variation of opal content is controlled mainly by eccentricity forcing and subsequently by obliquity forcing during the last 700 kyrs. The opal contents of Core LHB-3PC also represent the apparent Mid-Pleistocene Transition (MPT)-related climatic variation in the glacial-interglacial cycles. In particular, the orbital variation of the opal contents shows increasing amplitudes since marine isotope stage (MIS) 11, which defines one of the important paleoclimatic events during the late Quaternary, called the "Mid-Brunhes Event". Based on the variation of the opal contents in Core LHB-3PC, we suggest that the surface-water paleoproductivity in the Indian Sector of the Southern Ocean followed the orbital (glacial-interglacial) cycles, and was controlled mainly by the extent of sea ice distribution during the last 700 kyrs.

• 한국광물학회지
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• 제24권1호
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• pp.19-29
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• 2011

베링해 알류샨 분지의 북부 사면지역에서 채취된 피스톤 코아 PC25A의 퇴적물에서 점토광물의 반정량적 함량 분석을 통해 지난 마지막 빙하기 동안 퇴적물의 기원지와 운송 경로의 변화를 살펴보았다. 코아 PC25A의 연대는 방산충 L. nipponica sakaii의 마지막 출현 시기($48.6{\pm}2\; ka$)와 인근 지역에서 채취한 연대가 잘 정립된 코아 PC23A의 퇴적물 색도($a^{\ast},\; b^{\ast}$) 및 퇴적 엽리층의 대비를 통해 설정되었다. 코아 PC25A의 최하단부가 약 57,600년 전으로 계산되었고, 코아 상부는 손실된 것으로 판단된다. 지난 마지막 빙하기 동안 스멕타이트, 일라이트, 캐올리나이트, 녹니석의 평균 함량은 각각 11% (5~24%), 47% (36~58%), 13% (9~19%), 29% (21~40%)이다. 코아 PC25A의 인근 지역에서 채취한 코아 MC24에서 분석된 홀로세의 점토광물 함량에 비하여 마지막 빙하기동안에 특징적으로 일라이트 함량이 증가하였고 스멕타이트 함량은 감소하였다. 따뜻한 기후의 홀로세 전기(Early Holocene) 동안 일라이트 함량이 높은 점토 퇴적물이 알라스카 대륙의 북부 지역(Province 1)으로부터 유입되는 융빙수에 의해 운반된 것으로 판단된다. MIS 2의 후빙기(B${\phi}$lling-All${\phi}$rod)동안에도 융빙수에 의해 점토광물이 운반되었으나, 일라이트 함량이 홀로 세 전기에 비해 낮기 때문에 북쪽의 Province 1보다는 남쪽에 위치한 Province 2와 Province 3에서 점토입자들이 기원된 것으로 해석된다. 마지막 최대 빙하기(Last Glacial Maximum)동안 나타나는 높은 스멕타이트 함량은 베링해 남동쪽 알라스카 반도 인근 지역(Province 4)에서 공급되는 점토 퇴적물의 양이 증가하였기 때문으로 보인다. MIS 3 초기에서 중기로 가면서 일라이트와 스멕타이트 함량이 감소하고, 녹니석의 함량은 증가하였다. MIS 3 동안 해수면이 낮아지면서 Province 2와 Province 3에서 점토 퇴적물의 공급이 증가한 것으로 보인다. 베링해 알류산 분지의 북부 사면지역에서 채취된 코아 PC25A에서 분석된 점토광물 조성의 변화는 마지막 빙하기동안 해수면의 하강으로 인하여 점토광물의 이동과 관련된 베링해의 표층 해류 순환이 현재와는 다른 양상으로 변화되었기 때문이다.

• Nuclear Engineering and Technology
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• 제37권2호
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• pp.127-138
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• 2005

Approaches to several recent issues in the operation of nuclear power plants using computational intelligence are discussed. These issues include 1) noise analysis techniques, 2) on-line monitoring and sensor validation, 3) regularization of ill-posed surveillance and diagnostic measurements, 4) transient identification, 5) artificial intelligence-based core monitoring and diagnostic system, 6) continuous efficiency improvement of nuclear power plants, and 7) autonomous anticipatory control and intelligent-agents. Several changes to the focus of Computational Intelligence in Nuclear Engineering have occurred in the past few years. With earlier activities focusing on the development of condition monitoring and diagnostic techniques for current nuclear power plants, recent activities have focused on the implementation of those methods and the development of methods for next generation plants and space reactors. These advanced techniques are expected to become increasingly important as current generation nuclear power plants have their licenses extended to 60 years and next generation reactors are being designed to operate for extended fuel cycles (up to 25 years), with less operator oversight, and especially for nuclear plants operating in severe environments such as space or ice-bound locations.

• 한국정보처리학회:학술대회논문집
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• 한국정보처리학회 2012년도 춘계학술발표대회
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• pp.1109-1112
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• 2012

해시 조인 알고리즘 성능 개선에 관한 연구는 이미 많은 연구자에 의해 수행된 바 있다. 새로운 알고리즘을 추가하는 연구에서부터 컴퓨팅 환경에 맞는 최적화 솔루션을 제시하는 연구에 이르기까지 해시 조인의 성능을 향상시키는 연구는 다양하게 찾아 볼 수 있었다. 이 논문에서는 2004년 ICDA에서 발표한 [1]의 연구를 최신의 컴퓨팅 환경에서도 똑같이 작동하는지 확인해 보고자 한다.

• 한국식생활문화학회지
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• 제16권2호
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• pp.109-117
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• 2001

Judging from the studies carried out by Dr. Jo, Yong Jin on the Koreans' faces, Koreans divided into two constitutions according to their facial features and heritages. The one population is the Northern lineage whose ancestor migrated from Siberia in ice age. In order to survive in cold climate, they have developed a high level of metabolic heat production. Cold adaptation for preventing heat loss results in a reduction in the facial surface area with small eyes, nose and lips. The other population is the Southern lineage who is the descent of native in Korean peninsular. They have big eyes with double edged eyelids, broad nose and thick lips. It is generally believed that both genetic and environmetal factors influence eating behaviors. Although we can't recognized their heritage that may contribute to the metabolism and eating behavior, we commonly recognize their physiological heritage acceding to their facial features. In order to investigate the relationship among the size and shape of facial feature, the eating behavior, anthropometric measurement in female college students, the eating behaviors was measured during an instant-noodle lunch eaten in a laboratory setting at the ambient temperature of $23^{\circ}C$. The anterior surface area of left eye and length of right eye were positively correlated with the difference between the peak postprandial and the meal-start core temperature. The surface area of lower lip also negatively correlated with the meal-start core temperature and meal duration. In addition, the total lips' area was positively correlated with the difference between the peak postprandial and the meal-start core temperature and negatively correlated with the meal duration. However anthropometric measurements were not related with the size of facial features.