• 한국신재생에너지학회:학술대회논문집
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• 한국신재생에너지학회 2007년도 추계학술대회 논문집
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• pp.564-568
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• 2007

Gas hydrate has been attractive topic for two dedicates because it may cause the global warming, ocean hazards associated with the instability of marine slope due to the gas hydrate release as well as high potential of future energy resources. The study on gas hydrate in Ulleung basin has been performed since 1999 to explore the potential and distribution of gas hydrate offshore Korea. The numerous multi channel seismic data have been acquired and processed by Korea Institute of Geosciences and Mineral Resources (KIGAM). The results showed clearly the gas hydrate indicators such as pull up structure, bottom simulating reflector (BSR), seismic blanking zone. The prestack depth migration has been considered as fast and accurate technique to image the subsurface. In this paper, we will present both the conventional seismic data processing and apply Kirchhoff prestack depth migration for gas hydrate data set. The results will be applied for core sample collections and for proposal more detail 2D with long offset or 3D seismic exploration.

• Nuclear Engineering and Technology
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• 제30권3호
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• pp.245-261
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• 1998

In order to validate the variable aperture channel model that can deal with the non-uniform How rate in flow domain, migration experiments of conservative tracer were performed in two artificial fractures, a parallel and a wedge-shaped fracture. These different fracture shapes were designed to give different flow pattern. The fractures were made from a transparent acrylic plastic plate and a granite slab with dimensions of 10 $\times$ 61 $\times$ 61 cm. Uranine (Fluorescein sodium salt) was used as a conservative tracer. The volumetric flow rates of uranine feed solution were 30 mL/ hr, giving a mean residence time in the fracture of approximately 24 hours for the parallel fracture and 34 hours for the wedge-shaped fracture. The migration plumes of uranine were photographed to obtain profiles in space and time for movement of a tracer in fractures. The photographed migration plume was greatly affected by the geometric shape of fractures. The variable aperture channel model could have predicted the experimental results for the parallel fracture with a large accuracy. It is expected that the variable aperture channel model would be effective to predict the transport of the contaminant, especially, with the flow rate variation in a fracture.

• 한국세라믹학회지
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• 제37권1호
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• pp.102-109
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• 2000

When PbZrO3 (PZ) and PbTiO3 (PT) particles were scattered on polished surfaces of sintered Pb(Zr0.52Ti0.48)O3 (PZT; Zr/Ti=1.08) and then annealed, the PZT grain boundaries migrated. Near the scattered particles, grain boundaries were corrugated and thus the grain shape changed from a normal one to irregular ones. Especially, near the scattered PZ particles, fast grain growth occurred. In the regions swept by moving grain boundaries, the Zr/Tiratio was measured to be about 1.35 for of PZ scattering and about 0.8 for PT scattering, respectively. This result indicates that the grain boundary migration was induced by alloying of Zr and Ti ions in PZT grains, as in usual diffusion induced grain boundary migration(DIGM). A calculation showed that higher coherency strain energy was induced for PT scattering because of higher alloying of Ti than of Zr.

• 자원환경지질
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• 제43권4호
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• pp.349-358
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• 2010

탄성파 심도영역 중합전 역시간 구조보정은 음원영역 파동외삽과 수진기영역 파동외삽의 상호상관으로 지층구조를 영상화하는 방법으로 암염돔 하부, 단층, 습곡, 심한 경사층 등 복잡한 층서구조를 영상화하는데 주로 이용된다. 여기에서는 한국지질자원연구원에서 개발된 중합전 심도영역 역시간 구조보정 기술을 국내 대륙붕 제주분지 제 5광구 탄성파 현장자료에 적용하여 음원번호 1280번 하부에 존재하는 향사 층서구조 영상을 향상시키고자 하였다. 음원모음 신호음을 향상시키기 위해 기본 자료처리를 실시하였고, 반복적으로 속도스펙트럼을 계산하는 방법으로 중합속도를 결정하여 속도모델을 구축하였다. 중합단면도상에 나타나는 향사구조는 산란파 영향으로 지층경계면의 연속성이 떨어져 보이지만 구조보정 적용 결과 탄성파 반사 에너지가 집중된 곳에서 향사구조 영상이 향상된 심도영역 지층단면도를 구할 수 있었다.

• Korean Chemical Engineering Research
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• 제54권5호
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• pp.659-664
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• 2016

In order to resolve the AAEM species migration routes and the interaction relationship between biochar structure and AAEM species during biomass pyrolysis, experiments were performed in an entrained flow reactor with $N_2$ at $500{\sim}900^{\circ}C$. ICP-AES, XPS and SEM-EDX were used to examine content and distribution of AAEM species and the physicochemical structures of biochar. The results show that at $500{\sim}700^{\circ}C$, the precipitation rate of AAEM species is relatively high. At high temperature (>$700^{\circ}C$), the AAEM species continue to migrate from interior to exterior, but little precipitation from biochar surface. And the migration of AAEM species is mainly realized by the C-O bond as the carrier medium. The AAEM species on biochar surface are mainly Na, Mg and Ca (<$700^{\circ}C$), while changing to K, Mg and Ca (${\geq}700^{\circ}C$). From $500^{\circ}C$ to $900^{\circ}C$, the biochar particle morphology gradually changes from fibers to porous structures, finally to molten particles. At $700{\sim}900^{\circ}C$, Ca element is obviously enriched on the molten edge of the biochar porous structures.

• ETRI Journal
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• 제36권6호
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• pp.988-998
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• 2014

For memory-based big data storage, using hybrid memories consisting of both dynamic random-access memory (DRAM) and non-volatile random-access memories (NVRAMs) is a promising approach. DRAM supports low access time but consumes much energy, whereas NVRAMs have high access time but do not need energy to retain data. In this paper, we propose a new data migration method that can dynamically move data pages into the most appropriate memories to exploit their strengths and alleviate their weaknesses. We predict the access frequency values of the data pages and then measure comprehensively the gains and costs of each placement choice based on these predicted values. Next, we compute the potential benefits of all choices for each candidate page to make page migration decisions. Extensive experiments show that our method improves over the existing ones the access response time by as much as a factor of four, with similar rates of energy consumption.

• Nuclear Engineering and Technology
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• 제22권1호
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• pp.20-28
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• 1990

처분 안전성 평가를 위해서는 지하매질을 통한 방사성핵종의 이동특성 규명과 신뢰성 있는 지하 핵종이동 모델의 확보가 무엇보다 중요하다. 본 연구에서는 지하핵종이동 모델 개발을 위한 기초연구로서 충전층 실험을 수행하고, 실험결과를 제안된 핵종이동모델과 비교ㆍ검토하였다. 실험에서는 분쇄응회암으로 충전된 칼럼에서의 핵종이동 현상을 규명하고, 모델 시뮬레이션을 통해서는 세공확산을 모델에 고려하여 핵종이동에서 세공확산의 역할을 검토하였다. 충전층 실험에서 수력학적 분산계수는 비흡착성의 iodine을 사용하여 측정하였으며, 이 때 측정한 분산계수는 공극율 $\varepsilon$=0.483, 평균유속 (equation omitted)=0.915$\times$$10^{-2}$ cm/min에서 D$_{L}$=0.11$\times$$10^{-2}$ $\textrm{cm}^2$/min이었다. 그리고 중ㆍ저준위 방사성폐기물의 대표 핵종으로 사용한 Cs-137은 응회암에 대해 높은 지연특성을 보였으며, 파과곡선은 비대칭 형태로서 단말현상이 길게 나타났다. 모델 시뮬레이션 결과, 매질 세공내 확산과정은 다공성의 지하매질을 통한 핵종이동에서 중요한 율속단계 역할을 하였다.다.

• 한국방사성폐기물학회:학술대회논문집
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• 한국방사성폐기물학회 2011년도 춘계학술논문요약집
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• pp.303-304
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• 2011

• 한국진공학회:학술대회논문집
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• 한국진공학회 2012년도 제42회 동계 정기 학술대회 초록집
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• pp.279-279
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• 2012

In order to estimate the average migration lengths of $H_3O^+$ ions in amorphous ice, we conducted experiments of reactive ion scattering (RIS), low energy sputtering (LES), and reflection absorption IR spectroscopy (RAIRS) with an ultra-high vacuum (UHV) chamber. Dopped water-ice films were grown on the clean surface of Ru single crystal and analyzed with RIS, LES and RAIRS methods. The population changes of probe molecules, which were buried at a controlled distance from the surface, were monitored by those methods so that we can mesure the migration efficiencies. From the measured efficiencies, we evaluated the average migration lengths. This result is expected to give the information about the dynamics of proton in water-ice film.

• 한국화재소방학회논문지
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• 제33권6호
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• pp.114-119
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• 2019

우리는 LED등기구의 Printed circuit board (PCB)에서 화재의 원인으로 특정할 수 있는 금속 마이그레이션(Metallic migration) 현상을 발견하고, 본 연구를 진행하였다. 금속 마이그레이션 현상 가속화 실험인 물방울 시험을 소량의 물과 저전압(3 V)로 진행하고 절연되어있는 양극에서 직접적으로 금속 마이그레이션의 성장과 회로의 단락을 확인하였다. 그리고 전자주사현미경(SEM)을 통해 형태를 관찰하고 에너지 분산형 분광기(EDS)를 이용하여 성분을 분석한 결과, 절연된 부분에서 전극을 이루고 있는 구리의 성분을 검출하였다.