http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
홍성민,이필홍,고경현,안재환,이순일,Hong, Seong-Min,Lee, Pil-Hong,Go, Gyeong-Hyeon,An, Jae-Hwan,Lee, Sun-Il 한국재료학회 1998 한국재료학회지 Vol.8 No.3
Phase transition kinetics of nonstoichiometric amorphous titanium oxide thin films deposited by reactive sputtering was investigated after cooling down with various rate followed by l0min.-3hrs. annealing at $500^{\circ}C$~$600^{\circ}C$ After short duration and fast cooling. Magneli was the only crystalline phase because the oxidation rates of $TiO_{2-x}$, could be relatively slower than that of crystallization. When the films were cooled slowly between $500^{\circ}C$~$300{\circ}C$, Magneli was transformed into an anatase and stabilized, but directly into a rutile under fast cooling. Because the rutile also prevailed after cooling from $600^{\circ}C$, it was concluded that the rutile phase could be formed directly from Magneli as well as converted from the anatase. Changes in volume and surface morphology were observed related to crystallization and oxidation processduring heat treatment. 비정량적 조성을 가진 비정질 산화타이타늄 박막을 반응성 스퍼터링으로 제조한후, $500^{\circ}C$~$600^{\circ}C$에서 10분-3시간 열처리후 냉각속도를 달리하였을 때의 상변태과정을 고찰하였다. 10분-30분정도의 단기간의 열처리후 급냉한 경우에는 Mageneli상이 관찰되어 비정상정 상($TiO_{2-x}$)이 산화되는 속도가 결정화속도보다 훨씬 느린 것으로 생각되었다. 그러나 열처리 유지시간이 증가하면 $500^{\circ}C$에서 부터의 느린 냉각과정에서는 Magneil가 anatase로 변화하며 변태한 anatase는 저온에서는 rutile로 변화하지 않았으나 $500^{\circ}C$~$300{\circ}C$의 온도 구간을 비교적 빠르게 냉각하면 Matneli상은 직접 rutile상으로 변화할 수 있는 것으로 고찰되었다. 또한 $600^{\circ}C$에서 냉각시에도 rutile상이 형성됨으로서 rutile상은 $500^{\circ}C$이상의 고온에서도 이 상ㅇ르 거치지 않고 변태할 수 있는 것으로 분석된다. 결정화 및 산화과정은 부피의 변화를 야기하여 박막의 표면 형상의 변화도 가져옴이 관찰되었다.
홍성민,정인균,박종윤,이미선,김성준,Hong, Seong-Min,Jung, In-Kyun,Park, Jong-Yoon,Lee, Mi-Seon,Kim, Seong-Joon 한국관개배수위원회 2011 한국관개배수논문집 Vol.18 No.2
This study is to delineate the watershed hydrological parameters such as area, slope, rain gauge weight, NRCS-CN and time of concentration (Tc) by using the Geographic Information Sytem (GIS) technique, and estimation of design flood for an ungauged watershed. Especially, we attempted to determine the Tc of ungauged watershed and develop simple program using the cell-based algorithm to calculates upstream or downstream flow time along a flow path for each cell. For a $19km^2$ watershed of tributary of Nakdong river (Seupmoon), the parameters including flow direction, flow accumulation, watershed boundary, stream network and Tc map were extracted from 30m Agreeburn DEM (Digital Elevation Model) and landcover map. And NRCS-CN was extracted from 30m landcover map and soil map. Design rainfall estimation for two rainfall gauge which are Sunsan and Jangcheon using FARD2006 that developed by National Institute for Disaster Prevention (NIDP). Using the parameters as input data of HEC-l model, the design flood was estimated by applying Clark unit hydrograph method. The results showed that the design flood of 50 year frequency of this study was $8m^3/sec$ less than that of the previous fundamental plan in 1994. The value difference came from the different application of watershed parameter, different rainfall distribution (Huff quartile vs. Mononobe) and critical durations. We could infer that the GIS-based parameter preparation is more reasonable than the previous hand-made extraction of watershed parameters.