• 한국신재생에너지학회:학술대회논문집
• /
• 2009.06a
• /
• pp.33-36
• /
• 2009

고효율 양자점 태양전지를 위하여 $Si_{1-x}C_x$ 박막 내에 Si 양자점을 형성한 박막을 제작하고 그 특성을 분석하였다. $Si_{1-x}C_x$ 박막은 Si과 C target을 co-sputtering하여 증착하였다. C target의 RF power를 변화시켜 $Si_{1-x}C_x$ 박막의 조성비를 조절하였으며, 조성비는 auger electron spectroscopy로 정량적으로 측정하였다. 이 박막들을 질소 분위기에서 후 열처리하여 high resolution transmittance electron microscopy로 확인한 결과 박막 내에 2~10nm 크기의 양자점이 형성된 것을 관측할 수 있었다. 이 양자점은 transmittance electron diffraction과 grazing incident X-ray diffraction을 통해 Si 양자점과 SiC 양자점이 형성되었음을 알 수 있었다. Raman 측정 결과에서는 후 열처리한 $Si_{1-x}C_x$ 박막의 조성비가 증가할 수록 crystal Si peak의 shift가 증가함을 알 수 있었고, 이를 통해 양자점의 크기도 함께 계산할 수 있었다. Fourier transform infrared spectroscopy을 통해 후 열처리한 Si1-xCx 박막의 양자점의 형성 원인을 추정하였다.

• The Journal of Engineering Geology
• /
• v.12 no.2
• /
• pp.137-150
• /
• 2002

Recently, plane failure mode occurred frequently along the bedding plane having low angle dip about 20 degree when cutting slopes were constructed in sedimentary rock region of the Gyeongsang Basin. Landslide of the Whangryeong Mountain which was occurred at Busan Metropolitan City in 1999 belongs to the category mentioned above. Reconstruction for cutting slope of the Whangryeong Mountain has finished in 2000 and final grade of reconstructed cutting slope is 1:2.0. To analyze slope failure mode for landslide of the Whangryeong Mountain, various analyses were performed such as in-situ investigation and test, drilling, laboratory test, aerial photograph interpretation, X-ray diffraction analysis, and slope stability analysis using Stereographic Projection and Limit Equilibrium methods. As the result, it is identified that tension cracks had been developed one year before the landslide took place. The tension crack semis to be formed by merging several joint sets. It appears that failure blocks broke down along the sliding planes of different layers. Risk of plane failure is conformed as a result of stability analysis using Stereographic Projection and Limit Equilibrium methods in case that greenish gray tuffaceous shales, regared as sliding planes, are weathered. From now on, a detailed investigation is needed for the thin layers which is sensitive to weathering, and stability analysis for this layer is performed at cut slope construction site having similar geological condition.