• Transactions of the Korean Society of Mechanical Engineers B
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• v.36 no.3
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• pp.351-361
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• 2012

The leading surgical method for correcting the misalignment of the varus and valgus in the knee joint is the high tibial osteotomy (HTO). In the opening wedge HTO (OWHTO), there is no concern about damaging the peroneal nerve on the lateral tibia of the proximal fibula. OWHTO has been the preferred choice, as the opening of the correction angle can be modulated during the operation. The correction of the varus and valgus on the coronal plane are performed adroitly. Nevertheless, there have been numerous reports of unintended changes in the medial tibial plateau and posterior slope angle (PSA). The authors have developed an HTO method using computer-assisted surgery with the aim of addressing the abovementioned problems from an engineer's perspective. CT images of the high tibia were reconstructed three-dimensionally, and a virtual osteotomy was performed on a computer. In addition, this study recommends a surgical method that does not cause changes in the PSA after OWHTO. The results of the study are expected to suggest a clear relationship between the anteromedial cortex oblique angle of each patient and the PSA, and an optimal PSA selection method for individuals.

• Economic and Environmental Geology
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• v.48 no.5
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• pp.379-390
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• 2015

Multibeam backscatter strength is dependent not only on seafloor sediment facies but also on changed incidence angle due to the actual bottom slope. Therefore, the correction for actual bottom slope should be considered before the analysis of backscatter strength. This paper demonstrates the backscatter correction technique for the actual incidence angle and ensonified area. The target area is a part of the eastern Yellow Sea with water depths of 46~55 m. The area is located between the sand ridges and covered by large dunes with various bottom slopes. The dunes usually have the gentle slopes of about $1{\sim}3^{\circ}$, but show some steep slopes of $5{\sim}15^{\circ}$ on the crest. The backscatter strength values on the crest range from -34 to -23 dB, assuming that the bottom is flat. However, this study shows that the backscatter strength range was somewhat reduced (-32~-25 dB) after correction for actual bottom slope. In addition, the backscatter imagery was significantly improved; high and low backscatter strength values on the crest due to the actual bottom slope were normalized. The results demonstrate that the correction technique in this study is an effective tool for processing backscatter strength.

• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.102-102
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• 2019

토양수분은 수문 및 기상 현상의 주요 요인으로 가뭄, 홍수 및 범람과 같은 자연 재해와 관련이 깊은 인자이다. 이러한 토양수분의 관측 기술 중 위성 데이터를 활용한 원격탐사 기술은 광범위한 지역의 관측이 용이하고 지점이 아닌 공간 데이터를 제공하는 장점을 지니고 있어 토양수분의 관측에 유리하다. 특히 높은 해상도의 위성기반 토양수분 데이터는 토양수분의 변동성이 큰 지역의 수문, 기상학적 현상을 보다 자세히 분석할 수 있게 해주며 가뭄 및 범람과 같은 수자원 관련 재해를 정확하게 분석하는데 요구된다. 이로 인해 최근 Sentinel-1 위성에서 운용중인 Synthetic Aperture Radar(SAR) 데이터를 이용한 매우 높은 공간해상도(10m~1km)를 지니고 있는 토양수분데이터 생산에 관한 연구가 세계적으로 활발히 진행되고 있다. 그러나 국내에서는 Sentinel-1 위성을 이용한 토양수분 데이터 복원에 관한 연구가 미비한 실정이다. 따라서 본 연구에서는 파주 감악산 설마천 유역에서의 Sentinel-1 위성의 SAR 데이터를 이용한 고해상도 토양수분 데이터를 복원하고자 한다. 파주 설마천 유역은 감악산 일대로 경사가 심하고 식생이 두터운 산악지형이다. SAR를 이용하여 산지에서 신뢰성 있는 토양수분 자료를 복원하기 위해서는 가장 큰 오차의 원인으로 작용하는 경사와 식생을 고려하여야 한다. 먼저 표면 경사의 영향의 경우 SAR 센서의 레이더 입사각과 수치 표고 모델을 이용하여 고려하고자 한다. 다음 과정으로 표면 경사가 고려된 Sentinel-1 데이터의 후방산란계수와 Landsat-8 데이터 및 지점 토양수분 데이터를 이용하여 식생에 따른 후방산란계수의 거동을 Water Cloud Model을 이용하여 분석하였다. Water Cloud Model은 토양위의 식생의 수분이 후방산란계수에 혼동을 주는 구름과 같이 작용한다고 가정하고 식생수분을 후방산란계수와 레이더 입사각 및 식생지수를 통해 계산하는 모델이며 이를 이용하여 토양수분 복원에 있어 식생의 영향을 제거하고자 하였다. 이를 통해 식생과 표면 경사를 고려하여 복원된 토양수분 데이터를 설마천 유역의 지점 데이터와 비교 분석하고 다른 위성기반 토양수분 데이터 및 강우 데이터를 이용하여 평가하였다. 본 연구결과를 통해 한반도 산지에서의 SAR 데이터를 이용한 토양수분 복원 기술의 기초가 마련될 것이며 이를 통해 산지가 대부분인 한반도의 토양수분 거동을 이해하는데 유용한 자료를 제공할 수 있을 것으로 기대된다. 본 연구 이후에는 연구결과분석을 통한 산지에서의 고해상도 토양수분 복원 알고리즘을 분석, 보완하고 한반도에서의 SAR 기반 토양수분 데이터의 정확도를 높이는 연구가 진행되어야 할 것이다.

• Proceedings of the Korean Society of Precision Engineering Conference
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• 2009.06a
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• pp.987-988
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• 2009

• The korean journal of orthodontics
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• v.33 no.4 s.99
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• pp.259-277
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• 2003

This study was designed to investigate the position of anteroposterior center of resistance for genuine intrusion and the mode of change of the minimum distal force for simultanous intrusion and retraction of the upper and lower incisors according to the increase of labial inclination. For this purpose, we used the three-piece intrusion arch appliance and three-dimensional finite element models of upper and lower incisors. 1. Positions of the center of resistance in upper incisors according to the increase of the labial inclination were as follows; 1) In normal inclination situation, the center of resistance was located in 6m behind the distal surface of the lateral incisor bracket. 2) In $10^{\circ}$ increase of the labial inclination situation, the center of resistance was located in 9mm behind the distal surface of the lateral incisor bracket. 3) In $20^{\circ}$ increase of the labial inclination situation, the center of resistance was located in 12m behind the distal surface of the lateral incisor bracket. 4) In $30^{\circ}$ increase of the labial inclination situation, the center of resistance was located in 16m behind the distal surface of the lateral incisor bracket. 2. Positions of the center of resistance in lower incisors according to the increase of the labial inclination were as follows; 1) In normal inclination situation, the center of resistance was located in 10mm behind the distal surface of the lateral incisor bracket. 2) In $10^{\circ}$ increase of the labial inclination situation, the center of resistance was located in 13m behind the distal surface of the lateral incisor bracket. 3) In $20^{\circ}$ increase of the labial inclination situation, the center of resistance was located in 15m behind the distal surface of the lateral incisor bracket. 4) In $30^{\circ}$ increase of the labial inclination situation, the center of resistance was located in 18m behind the distal surface of the lateral incisor bracket. 3. The patterns of stress distribution were as follows; 1) There were even compressive stresses In and periodontal ligament when intrusion force was applied through determined center of resistance. 2) There were gradual increase of complexity in compressive stress distribution pattern with Increase of the labial inclination when intrusion and retraction force were applied simultaneously. 4. With increase of the labial inclination of the upper and lower incisors, the position of the center of resistance moved posteriorly. And the distal force for pure intrusion was increased until $20^{\circ}$increase of the labial inclination.

• Proceedings of the Korean Society of Precision Engineering Conference
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• 2009.06a
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• pp.955-956
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• 2009

• Proceedings of the Korean Society of Precision Engineering Conference
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• 2008.06a
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• pp.263-264
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• 2008

• Economic and Environmental Geology
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• v.49 no.2
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• pp.121-134
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• 2016

We characterize the spatial distribution of Cobalt-rich ferromanganese crusts covering the summit and slopes of a seamount in the western Pacific, using acoustic backscatter from multibeam echo sounders (MBES) and seafloor video observation. Based on multibeam bathymetric data, we identify that ~70% of the summit area of this flattopped seamount has slope gradients less than $5^{\circ}$. The histogram of the backscatter intensity data shows a bi-modal distribution, indicating significant variations in seabed hardness. On the one hand, visual inspection of the seafloor using deep-sea camera data exhibits that the steep slope areas with high backscatter are mainly covered by manganese crusts. On the other hand, the visual analyses for the summit reveal that the summit areas with relatively low backscatter are covered by sediments. The other summit areas, however, exhibit high acoustic reflectivity due to coexistence of manganese crusts and sediments. Comparison between seafloor video images and acoustic backscatter intensity suggests that the central summit has relatively flat topography and low backscatter intensity resulting from unconsolidated sediments. In addition, the rim of the summit and the slopes are of high acoustic reflectivity because of manganese crusts and/or bedrock outcrops with little sediments. Therefore, we find a strong correlation between the acoustic backscatter data acquired from sea-surface multibeam survey and the spatial distribution of sediments and manganese crusts. We propose that analyzing acoustic backscatter can be one of practical methods to select optimal minable areas of the ferromanganese crusts from seamounts for future mining.

• The korean journal of orthodontics
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• v.28 no.5 s.70
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• pp.791-802
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• 1998

The purpose of this study was to obtain the angulation and inclination of FACC of all teeth to FH plane. Study models of 31 persons with normal occlusion were selected and mounted on the semiadjustable articulator for this study. Using T.A.R.G. with a little modified method, the angulation and inclination of FACC of all teeth to FH plane were measured and then the measurements were analyzed statistically. The obtained results were as follows. Mean, standard deviation, maximum value, and minimum value of the angulation and inclination of FACC of upper and lower teeth were obtained. $\cdot$The FACC in both upper and lower arch was progressively lingually-inclined from anterior teeth to posterior teeth. $\cdot$In the angulations of FACC of upper teeth, central and lateral incisor showed similar value. Yet, the FACC of the rest was progressively distally-angulated from the canine to posterior teeth. The FACC in lower arch was progressively mesially-angulated from anterior teeth to posterior teeth. $\cdot$The angulation and inclination of FACC of any tooth in both upper and lower teeth correlated strongly and positively with the angulation and inclination of FACC of adjacent tooth.

• Journal of the Korean Society of Marine Environment & Safety
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• v.20 no.2
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• pp.241-246
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• 2014

The purpose of this study is to investigate the flow characteristics around underwater triangular structure with various inclination and Reynolds number. A flow fields around the triangular structure model were measured by visualization method and PIV in the circulating water channel. The result of the experiment is where the triangular structure that has a inclination of $45^{\circ}$ and the reynolds number at $Re=2.9{\times}10^3$ showed rising velocity component to 2.7 times of the structure height. When the reynolds number is steady and when the inclination is greater the descending velocity component of the structure's rears current form is greatly shown and for the areas where it's more than y/hs=1.75 has a change in the angle of inclination but it doesn't give a great effect to it.