• Korean Journal of Optics and Photonics
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• v.9 no.2
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• pp.86-91
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• 1998

Multimode planar waveguides have been fabricated by an electric-field assisted ion exchange in soda-lime glass substrates. Measurements of the mode indices have been made and the index profiles modeled on modified Fermi function are explained by a comparative analysis with the concentration profiles obtained using an electron probe X-ray micro analyzer. The analytical measurements showed that no more than 95% of sodium ions were replaced by the cesium ions. We established formulas for guide depth, mobility, and refractive index change, given the applied electric field, the diffusion temperature, and the time. We have verified the linear relations in the formulas not only between guide and root of diffusion time but also between guide depth and the applied electric filed experimentally.

• Proceedings of the Korea Society of Environmental Biology Conference
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• 2002.11a
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• pp.61-71
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• 2002

광양만내 해양바이러스양은 2.0$\times$$10^{8}$ particles/ml로 매우 풍부했다. 각 계절별 바이러스의 밀도는 여름에 최대 9.0$\times$$10^{8}$ particles/ml에서 겨울에는 최소값인 0.7$\times$$10^{8}$ particles/ml을 기록했다. 광양만 내의 바이러스, 박테리아, 식물플랑크톤 생물량의 공간적 분포는 open ocean system에 해당하는 정점 28, 38, 42, 46, 51에서 보다 closed estuarine system에 해당하는 정점 2, 5, 10 ,12, 16, 20에서 많은 것으로 나타났다. 그리고, 다른 closed estuarine system에 해당하는 정점 22, 26, 32, 34는 높은 바이러스 밀도를 보였지만 상대적으로 open ocean system에 비해서 낮은 박테리아와 식물플랑크톤의 생물량을 나타냈다. 몇몇 정점의 수심 깊이에서는 박테리아의 밀도가 바이러스의 밀도를 100배정도 초과했다. 해양 바이러스와 그들의 host system의 계절별 밀도는 역동적으로 번화했으며, 그들의 계절별 변화는 밀집한 상호연관성을 가졌다. 여름에 바이러스와 박레리아의 밀도는 증가된 반면 식물플랑크톤의 엽록소-a 농도는 평균값을 유지하였다. 겨울에는 바이러스와 박테리아의 밀도가 급속하게 줄어들었고, 마찬가지로 엽록소-a 농도 역시 감소하다가, 곧 다시 증가했다. 바이러스의 밀도는 2001년 8월에 최고점에 도달했으며, 박테리아의 밀도는 2001년 8월과 2002년 6월에 최고값을 가졌다. 반면에 엽록소-a의 농도는 2002년 4월에 최대치에 도달했다. 전체 host와 바이러스 밀도로 볼 때, 그들의 pool은 바이러스에 의한 mortality에 의해서 steady-state 상태로 유지되고, 바이러스의 밀도 또한 steady-state를 유지하는 것으로 보였다. 이러한 시도는 우리 나라 광양만 내에 존재하는 해양 바이러스의 생태적 분포 연구를 다루는 첫 번째 실험으로 사료된다.

• Journal of the Korean Institute of Telematics and Electronics D
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• v.36D no.3
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• pp.27-33
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• 1999

We have investigated the ultra-low energy B, P, and As ion implantation using upgraded MDRANGE code to study formation of nanometer junction depths. Even at the ultra-low energies simulated in this paper, it was revealed that ion channeling should be carefully considered. It was estimated that ion channelings have much effect on dopant profiles when B ion implant energies were more than 500 eV, P more than 2 keV and As approximately more than 4 keV. When we compared 2-dimensional dopant profiles of 1 keV B with that of tilted one, 2 keV P with tilt, and 5 keV As with tilt, we could find that most channeling cases occurred not lateral directions but depth directions.

• Journal of the Korean GEO-environmental Society
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• v.11 no.10
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• pp.41-48
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• 2010

In this study, grain size distribution of dredged soil and suspended solid distribution of supernatant in containment area were measured and compared with design prediction for suitability evaluation on prediction of suspended solid concentration of supernatant in conventional design of containment area. In addition to that, relationship were also analyzed between current velocity and suspended solid concentration of supernatant. Evaluation results show a relatively good agreement between field measurement and design prediction. On contrast, field measurement and design prediction show a quite different value each other in the early stage of dredging or at a point that current velocity increases. It is believed that this is due to that conventional design method of containment area does not account for ponding depth and current velocity which change sensitively with dredging period. Since current velocity and distribution of suspended solid concentration measured simultaneously show a similar trend, it is observed that there exists a close relationship between current velocity and distribution of suspended solid concentration. Therefore, a new design method for containment area, which can consider sedimentation of suspended solid that changes with interface height of dredged soil, ponding depth, current speed of supernatant, is necessary in order to predict the situation change of containment area more precisely.

• Journal of the Korean Vacuum Society
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• v.12 no.3
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• pp.162-167
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• 2003

To find the concentration according to the depth-direction of ions implanted in the sample, with sputtering of the sample surface, one needs the depth profiling of ion implanted in the sample. On measuring of depth profiling, the sputtering rate to affect depth direction, is calculated by SRIM simulation. When ion is implanted in the sample, the atomic density of the sample rises up a little, and it alters sputtering yield. This alteration then causes differences of sputtering rate to affect depth-direction, on measuring of depth profiling. With the usage of SRIM Monte Carlo simulation code, one calculates sputtering rate, with sputtering yield by the alteration of atomic density of the sample through ion implantation. As a result, it goes to prove that its difference affects depth distribution, on measuring of depth profiling.

• Proceedings of the Korean Vacuum Society Conference
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• 2011.02a
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• pp.41-41
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• 2011

Flash memory에서 tunnel oxide film은 electron tunnelling 현상을 이용하여 gate에 전하를 전달하는 통로로 사용되고 있다. 특히, tunnel oxide film 내부의 charge trap 현상과 불순물이 소자 특성에 직접적인 영향을 주고 있어, 후속 N2O/NO 열처리 공정에서 SiO2/Si 계면에 nitrogen을 주입하여 tunnel oxide film 특성을 개선하고 있다. 따라서 N2O/NO 열처리 공정 최적화를 위해서는 tunnel oxide film 내 N 농도와 분포에 대한 정확한 평가가 필수적이다[1]. 본 실험에서는 low energy magnetic SIMS를 이용하여 N2O로 열처리된 tunnel oxide film 내의 N농도를 보다 정확하게 평가하고자 하였다. 사용된 시료는 Si substrate에 oxidation 이후 N2O 열처리를 진행하여 tunnel oxide를 형성시켰으며, 분석 impact energy는 surface effect최소화와 최상의 depth resolution 확보를 위해 250eV를 사용하였으며, matrix effect와 mass interference를 방지하기 위해 MCs+ cluster mode[2]로 CsN signal를 검출하였다. 실험 결과, 특정 primary beam 입사각도에서 nitrogen depth resolution 저하 현상이 발생하였고, SIMS crater 표면이 매우 거칠게 나타났다. 이에, Depth resolution 저하 현상을 개선하기 위해 극한의 glancing 입사각 조건으로 secondary extraction voltage 변화를 통해 depth resolution이 개선되는 최적의 impact energy와 primary beam 입사각 조건을 확보하였다. 그 결과 nitrogen의 depth resolution은 1.6nm의 depth resolution을 확보하였으며, 보다 정확한 N 농도와 분포를 평가할 수 있게 되었다.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2008.11a
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• pp.47-49
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• 2008

기상장 수치모의 결과 Case NGSST와 Case Default의 해수면 온도가 다르게 표현 되어 대상지역의 온도장을 변화 시켰고, 이에 따른 바다와 육지간의 온도경도 변화는 해풍 및 육풍의 침투 깊이를 변화 시켰을 뿐만 아니라 풍속의 변화에도 영향을 미쳤다. 이러한 기상장의 차이는 대기질 모의결과에도 영향을 미쳐 오존농도 분포의 차이로 나타났다.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.271-272
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• 2002

현재 우리나라에서는 PM10이 분진 측정 항목으로 대변되고 있으나 미세 영역에 해당하는 PM2.5나 PM1.0의 범위의 측정에 관심이 집중되고 있다. 미세 영역의 분진은 많은 양이 호흡기에 침착되거나 시정의 감쇄를 야기 시킨다 (Eldering and Cass, 1996 : Anderson et al., 1992). 미국 National Ambient Air Quality Standard (NAAQS)는 1997년 PM2.5 항목의 추가를 공표하였다. (중략)

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.7 no.3
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• pp.277-288
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• 1995

Prediction of turbidity due to fine-grained bed material load under wave action is critical to any assessment of anthropogenic impart on the coastal or lacustrine environment Waves tend to loosen mud deposits and generate steep suspension concentration gradients, such that the sediment load near the bottom is typically orders of magnitude higher than that near the surface. In a physically realistic but simplified manner, a simple mass conservation principle has been used to simulate the evolution of fine sediment concentration profiles and corresponding erodible bed depths under progressive, nonbreaking wave action over mud deposits. Prior field observations support the simulated trends. which reveal the genesis of a near-bed. high concentration fluidized mud layer coupled with very low surficial sediment concentrations. It is concluded that estimation of the depth of bottom erosion requires an understanding of mud dynamics and competent in situ sediment concentration profiling. Measurement of sediment concentration at the surface alone, without regard to the near-bed zone, can lead to gross underestimation of the erodible bed depth.

• Economic and Environmental Geology
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• v.29 no.6
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• pp.713-724
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• 1996

The time-series resident solute concentrations, monitored at two field plots using the automated 144-channel TDR system by Kim (this issue), are used to investigate the dominant transport mechanism at field scale. Two models, based on contradictory assumptions for describing the solute transport in the vadose zone, are fitted to the measured mean breakthrough curves (BTCs): the deterministic one-dimensional convection-dispersion model (CDE) and the stochastic-convective lognormal transfer function model (CLT). In addition, moment analysis has been performed using the probability density functions (pdfs) of the travel time of resident concentration. Results of moment analysis have shown that the first and second time moments of resident pdf are larger than those of flux pdf. Based on the time moments, expressed in function of model parameters, variance and dispersion of resident solute travel times are derived. The relationship between variance or dispersion of solute travel time and depth has been found to be identical for both the time-series flux and resident concentrations. Based on these relationships, the two models have been tested. However, due to the significant variations of transport properties across depth, the test has led to unreliable results. Consequently, the model performance has been evaluated based on predictability of the time-series resident BTCs at other depths after calibration at the first depth. The evaluation of model predictability has resulted in a clear conclusion that for both experimental sites the CLT model gives more accurate prediction than the CDE model. This suggests that solute transport at natural field soils is more likely governed by a stream tube model concept with correlated flow than a complete mixing model. Poor prediction of CDE model is attributed to the underestimation of solute spreading and thus resulting in an overprediction of peak concentration.