• Journal of Korean Ophthalmic Optics Society
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• v.11 no.2
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• pp.77-83
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• 2006

We have studied the astigmatism according to the bevel position and the tilting(pantoscopic) angle of decentered spectacle lens for prism prescription. For prism prescription, generally we make a general spectacle lens into decentered spectacle lens. At this time the bevel position of decentered lens is a important matter, because the difference between optic axis and visual axis occur aberrations. Using the calculation we find that the case that the axis of bevel rotation band passes the front curvature center of (+) lens has a smaller astigmatism than the case that the axis of bevel rotation band passes the rear curvature center of (+) lens and that the case that the axis of bevel rotation band passes the rear curvature center of (-) lens has a smaller astigmatism than the case that the axis of bevel rotation band passes the front curvature center of (-) lens. We find the lens with higher refraction index has a smaller astigmatism.

• Annual Conference on Human and Language Technology
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• 1994.11a
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• pp.64-69
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• 1994

한국어 음성지각의 분절단위로서 음절의 역할을 알아보기 위하여, 음절탐지 과제를 사용하는 실험을 실시하였다. 실험1에서는 ${\ulcorner}$산악${\lrcorner}$ - ${\ulcorner}$산간${\lrcorner}$과 같은 단어쌍을 대비시켰다. 전자의 음절구조는 CV-CVC이며, 후자의 음절구조는 CVC-CVC이다. CV표적음절 /사/를 찾아내는데 걸리는 시간은 ${\ulcorner}$산악${\lrcorner}$ 에서보다 ${\ulcorner}$산간${\lrcorner}$에서 길었다. 그러나 CVC표적음절 /산/을 찾아내는데 걸리는 시간에서는 차이가 없었다. 실험2에서는 비단어쌍으로 ${\ulcorner}$산욱${\lrcorner}$ - ${\ulcorner}$산각${\lrcorner}$ 과 같은 것을 대비시켰다. 표적음절이 /사/인 경우는 ${\ulcorner}$산욱${\lrcorner}$에서 반응시간이 짧았고, 표적음절이 /산/인 경우에는 ${\ulcorner}$산각${\lrcorner}$ 에서 반응시간이 짧았다. 본 실험에서 얻어진 결과는 다른 언어에서 얻어진 결과와 몇 가지 차이가 있었다. 이것을 설명하기 위해, 한국어의 음절의 특징과 음성지각에서의 음절의 역할에 대해 논의하였다.

• Journal of Korean Society of Forest Science
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• v.108 no.4
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• pp.540-551
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• 2019

This study was conducted to provide basic data for classifying patterns of land creep in 37 areas in South Korea using geological and soil property analyses. Geological time, as it relates to land creep areas in South Korea, had been most impactful for the Gyeongsang Supergroup and its sedimentary bedrock during the Cretaceous period. In this area, perfect ridge cliffs in land creeping areas included 20 plots (approximately 54.0%), while tension cracking areas with ambiguous ridge cliff characteristics included 17 plots (approximately 46.0%). Hesitant slide slope types included 20 plots (approximately 54.0%) within theslide slope of an incident pattern (slide slope figure) in land creeping areas. Colluvial debris types among land creep patterns were the most frequent and included 25 plots (approximately 68.0%). The direct causes of land creep were cutting of foothills, quarrying, land-clearing in mountains, mining exploration, and the creation of burial grounds, all of which added to geological impacts. Among land creeping areas, 27 plots (approximately 73.0%) were the result of man-made activities, and 10 plots (approximately 27.0%) were derived via natural causes such as earthquakes, heavy rainfall, and caving.

• Journal of agriculture & life science
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• v.50 no.5
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• pp.111-120
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• 2016

The objective of this study was to provide basic information for selecting the right timing and the right place of erosion control of stream on Gyeongsangnam-do. In order to achieve this objective, a total of 526 erosion control dams and 230 mountains stream conservation facilities on the constructed places and construction planned places for the erosion control were investigated on site, forest physiognomy, and hydrologic conditions. The erosion control dams and mountain stream conservation facilities were mostly constructed in the area, which has the sedimentary rock, 200-400m of altitude, a slope of 21~30°, and II of landslide hazard map. Among the forest environmental factors, it was only similar to the construction frequency in the areas that have small diameter class, III age class. Also, we investigated the hydrological environmental factors that determine the size and numbers of erosion control dam. The places constructed to the highest frequency were below 50ha in the area, 2.1~4.0km/㎢ of drainage density, longitudinal water system, 61~90mm of maximum precipitation per hour, and 201~300mm of day maximum precipitation. As the results, the sites and floodgate conditions between the constructed places and stream conservation facilities for the erosion control showed to be very similar. Therefore, these results indicate that the erosion control of the stream of the areas, which have the disruption of mountain peaks and the high erosion risk areas, should be used on both the erosion control dam and stream conservation facilities.