• Journal of Periodontal and Implant Science
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• 제36권1호
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• pp.69-84
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• 2006

Reports on the comparison of clinical effect between non-surgical and surgical therapy, and the change of the clinical parameters during maintenance phase have been rarely presented in Korea. This study was to observe the clinical changes during maintenance phase of 6 months in patients with chronic periodontitis treated by non-surgical or surgical therapy in Department of Periodontics, Chonnam National University Hospital. Among the systemically healthy and non-smoking patients with moderate to severe chronic periodontitis, twenty eight patients (mean age: 47.5 years) treated by non-surgical therapy (scaling and root planning) and nineteen patients (mean age: 47.3 years) treated by surgical therapy (flap surgery) were included in this study. The periodontal supportive therapy including recall check and oral hygiene reinforcement was started as maintenance phase since 1 month of healing after treatment. Probing depth, gingival recession. clinical attachment level and tooth mobility were recorded at initial, baseline and 1, 2, 3 and 6 month of maintenance phase. The clinical parameters were compared between the non-surgical and surgical therapies using Student t-test and repeated measure ANOVA by initial probing depth and surfaces. Surgical therapy resulted in greater change in clinical parameters than non-surgical therapy. During the maintenance phase of 6 months, the clinical effects after treatment had been changed in different pattern according to initial probing depth and tooth surface. During maintenance phase, probing depth increased more and gingival recession increased less after surgical therapy, compared to non-surgical therapy. The sites of initial probing depth less than 3 mm lost more clinical attachment level, and the sites of initial probing depth more than 7 mm gained clinical attachment level during maintenance phase after non-surgical therapy, compared to surgical therapy. Non-surgical therapy resulted in greater reduction of tooth mobility than surgical therapy during maintenance phase. These results indicate that the clinical effects of non-surgical or surgical therapy may be different and may change during the maintenance phase.

• Ocean Systems Engineering
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• 제5권4호
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• pp.245-259
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• 2015

The numerical simulation of wave slamming on a 3D platform deck was investigated using a coupled Level-Set and Volume-of-Fluid (CLSVOF) method for overset grid system incorporated into the Finite-Analytic Navier-Stokes (FANS) method. The predicted slamming impact forces were compared with the corresponding experimental data. The comparisons showed that the CLSVOF method is capable of accurately predicting the slamming impact and capturing the violent free surface flow including wave slamming, wave inundation and wave recession. Moreover, the capability of the present CLSVOF method for overset grid system is a prominent feature to handle the prediction of wave slamming on offshore structure.

• 한국지리정보학회지
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• 제17권3호
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• pp.160-174
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• 2014

본 연구의 목적은 광역의 일단위 수문순환을 모의할 수 있는 격자기반의 분포형 모델을 구축한 후, 이를 미래 기후변화에 따른 광역적 수문영향을 평가하는데 있다. 격자별로 지표 유출층, 지표하 불포화 및 포화 토양층의 3단으로 구성하여 일별 물수지를 계산하며, 증발산량은 Penman-Monteith방법을 사용하였고, 지표 및 지표하유출은 지체계수(lag coefficient)와 감수곡선 계수(recession curve slope)를 적용하였다. 모델의 검보정을 위하여 한강유역의 충주댐과 소양강댐을 대상으로 9개년(2001-2009)의 댐유입량 자료를 이용하여 모델의 6개 주요매개변수를 보정하였으며, Nash-Sutcliffe 모델효율 (NSE)은 각각 0.57, 0.71의 값을 보였으며, 결정계수($R^2$)는 각각 0.65, 0.72의 값을 보였다. 5개의 IPCC SRES A1B 기후변화 시나리오자료(CSIRO MK3, GFDL CM2_1, CONS ECHO-G, MRI CGCM2_3_2, UKMO HADGEMI)를 적용한 결과, 미래 유출량의 변화는 강수량과 비슷한 경향을 보이면서 전체적으로 7.0%~27.1% 증가하였고, 증발산량도 미래 기온의 증가경향으로 일부 경우를 제외하고 증가하는 경향을 나타내었으며, 이들의 공간적 변화를 제시하였다.

• Journal of Periodontal and Implant Science
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• 제29권2호
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• pp.401-415
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• 1999

Root surfaces affected by periodontal disease undergo various forms of changes. Cementum exposure from gingival recession may result in absorption of calcium, phosphorus, and fluoride and subsequent hypermineralization and increased radiodensity. Although some reports have suggested that inorganic content with root cementum might show various changes depending upon age or extent of periodontal disease, but no consensus can be reached regarding the the distribution of various elements. The present study examines the difference in mineral content between healthy and periodontal diseased roots by analyzing three areas per tooth along the root surface in cervico-apical direction using electron probe and scanning electron microscope. Healthy tooth that was extracted for orthodontic purpose was used as control. Experimental teeth include those with periodontal pocket depth exceeding 6mm and those with gingival recession and periodontal pocket depth of 2-4mm. Levels of Ca, P, Mg and Na were measured using wavelength dispersive x-ray spectrometer at three areas per tooth. The examined areas were located apical to cemento-enamel junction in control and periodontal ligament-depleted areas in experimental teeth. The corresponding areas were also examined with scanning electron microscope(x70) The results are as follows. 1. Minerals were detected in order of Ca, P, Mg and Na. In all root surfaces, levels of Ca and P were higher in dentin than in cementum. 2. Level of Mg was twice as high in dentin than in cementum. There was no significant difference in the level of Mg and Na between normal and periodontal diseased roots or between the various locations in the same root. 3. Level of Ca and P in the surface cementum showed no difference between normal and periodontal diseased root, although the areas in dentin with high level of either ion also showed high level of corresponding ion in cementum. 4. Difference in the Ca and P content between various locations within the same root was noted, although no coherent pattern existed. These results suggest that although the mineral content of the root cementum in periodontitis-affected tooth is affected by exogenous ions from saliva and food, but there was no difference in the mineral contents between normal and periodontally diseased root.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2011년도 학술발표회
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• pp.8-9
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• 2011

On 4 September 2010 an earthquake of magnitude 7.1 on the Richter scale occurred on the Canterbury Plains in the South Island of New Zealand. The Canterbury Plains are an area of extensive groundwater and spring fed surface water systems. Since the September earthquake there have been several thousand aftershocks (Fig. 1), the largest being a 6.3 magnitude quake which occurred close to the centre of Christchurch on 22February 2011. This second quake caused extensive damage to the city of Christchurch including the deaths of 189 people. Both of these quakes had marked hydrological impacts. Water is a vital natural resource for Canterburywith groundwater being extracted for potable supply and both ground and surface water being used extensively for agricultural and horticultural irrigation.The groundwater is of very high quality so that the city of Christchurch (population approx. 400,000) supplies untreated artesian water to the majority of households and businesses. Both earthquakes caused immediate hydrological effects, the most dramatic of which was the liquefaction of sediments and the release of shallow groundwater containing a fine grey silt-sand material. The liquefaction that occurred fitted within the empirical relationship between distance from epicentre and magnitude of quake described by Montgomery et al. (2003). . It appears that liquefaction resulted in development of discontinuities in confining layers. In some cases these appear to have been maintained by artesian pressure and continuing flow, and the springs are continuing to flow even now. In spring-fed streams there was an increase in flow that lasted for several days and in some cases flows remained high for several months afterwards although this could be linked to a very wet winter prior to the September earthquake. Analysis of the slope of baseflow recession for a spring-fed stream before and after the September earthquake shows no change, indicating no substantial change in the aquifer structure that feeds this stream.A complicating factor for consideration of river flows was that in some places the liquefaction of shallow sediments led to lateral spreading of river banks. The lateral spread lessened the channel cross section so water levels rose although the flow might not have risen accordingly. Groundwater level peaks moved both up and down, depending on the location of wells. Groundwater level changes for the two earthquakes were strongly related to the proximity to the epicentre. The February 2011 earthquake resulted in significantly larger groundwater level changes in eastern Christchurch than occurred in September 2010. In a well of similar distance from both epicentres the two events resulted in a similar sized increase in water level but the slightly slower rate of increase and the markedly slower recession recorded in the February event suggests that the well may have been partially blocked by sediment flowing into the well at depth. The effects of the February earthquake were more localised and in the area to the west of Christchurch it was the earlier earthquake that had greater impact. Many of the recorded responses have been compromised, or complicated, by damage or clogging and further inspections will need to be carried out to allow a more definitive interpretation. Nevertheless, it is reasonable to provisionally conclude that there is no clear evidence of significant change in aquifer pressures or properties. The different response of groundwater to earthquakes across the Canterbury Plains is the subject of a new research project about to start that uses the information to improve groundwater characterisation for the region. Montgomery D.R., Greenberg H.M., Smith D.T. (2003) Stream flow response to the Nisqually earthquake. Earth & Planetary Science Letters 209 19-28.

• 한국항공우주학회지
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• 제39권1호
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• pp.1-8
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• 2011

이차원 구조물의 열응력 및 기계적 삭마 과정 해석을 위하여 영역/경계 분할법에 근거한 유한요소법을 적용하여 열구조 연계 정식화를 수행하였다. 삭마 재료 거동의 온도 의존성과 열분해 반응으로 인한 재료 비선형성 및 열복사와 같은 비선형 경계 조건을 일부 부영역과 공유면에 한정할 수 있다. 문제를 단순화하기 위해 열화학적 삭마 효과는 고려하지 않았으며, 기계적 삭마에 따른 표면 후퇴 판정 기준으로 열응력 해석을 통한 최대 면내 전단 응력을 선택하였다. 간단한 수치 실험을 수행하여 제안된 기법의 신뢰성에 대한 분석과 기계적 삭마 과정의 기본적인 경향을 파악하였다.

• 한국항공우주학회지
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• 제41권2호
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• pp.91-97
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• 2013

고온에서 열분해 과정을 겪는 복합재료의 탄화 및 삭마 과정의 표면 침식은 주로 두께 방향으로 진행된다. 본 논문에서는 다공성 복합재료의 면내 및 두께 방향 거동을 효과적으로 기술하기 위하여 분리-혼합 기법을 적용하였다. 섬유와 기지로 구성된 복합재료의 횡방향 등방성 가정을 통해 분리-혼합 방정식을 삼차원으로 확장하였으며, 기공 압력, 열팽창, 열분해 과정의 수축 효과를 포함하였다. 다공성 복합재료의 대표 체적 요소를 유한요소법으로 해석하여 면내 및 두께 방향의 물성 값을 상호 비교함으로써, 확장된 분리-혼합 기법의 타당성을 확인하였다.

• 한국해양공학회지
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• 제29권6호
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• pp.411-417
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• 2015

The shipping and shipbuilding industries have had business difficulties since the implementation of regulations on the CO₂ emissions from ships by IMO and the occurrence of the global financial crisis in 2008. Under this global recession, most shipping firms have started to operate their fleets at slow steaming rates with the goal of improving the profit ratio per transported unit. This study analyzed the resistance performance of a 6,800 TEU container ship corresponding to its trim variation with slow steaming, compared with that at its original design speed. Two different grid systems were used for the numerical calculation, one that considered the free surface allowing the capture of the dynamic trim and one that did not. This made it possible to clearly classify each resistance component to provide useful information to hull-form designers. In addition, a form factor assumption method using CFD was used for a reasonable effective power prediction in compliance with the 1978 ITTC performance prediction method. It was found that the total resistance of a 6,800 TEU container ship was reduced by 2.6% in the case of a 1-m trim at the bow at 18 kn.

• 한국농림기상학회지
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• 제17권1호
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• pp.45-57
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• 2015

사면스케일에서 토양수분의 시공간적 분포를 이해하기 위해서는 사면의 단면선(Transect line)에 따른 토양수분 분포 및 변동에 대해 기본적인 해석과 이해가 선행되어야 한다. 이에 단면선에 따라 설계된 여러 토양수분 측정지점으로부터 토양수분 자료에 대해 토양수분 특성인자를 고려하여 토양수분의 특성변동에 대해 이해하고자 하였다. 또한 사면의 위치 및 지형 그리고 토성의 공간적 분포의 토양수분 특성에 대한 영향도 분석하였다. 연구 사면에서 깊은 토양 층에서 평균적 토양수분의 공간적 분포는 지표 층에서의 공간적 분포 경향과는 많이 달랐으며, 사면의 지형 및 위치 그리고 토성의 공간적 분포는 토양수분의 시공간적 분포특징에 큰 영향을 주는 것으로 나타났다. 특히 상부흐름의 기여가 상당한 측정지점에서는 토양수분 변동의 안정화가 진행이 되는 것으로 나타나, 수문학적 경계(hydrologic Threshold)에 대한 추가 연구가 진행되어야 할 것으로 보인다. 또한 토양수분의 불균질한 공간적 경향은 우선적 흐름의 영향과 관련이 있다고 보여진다.

• 한국산림과학회지
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• 제109권4호
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• pp.429-437
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• 2020

본 연구는 산림 소유역에서 강우량에 대한 계류유출량의 장기적인 변화추이를 정량화하고, 임목의 생장이 산림소유역의 유출변화에 어떠한 영향을 미치는지를 파악하기 위하여 실시했다. 연도별로 강우량과 유출량은 비례관계를 보였으며, 시간이 경과할수록 유출량은 점차 감소하는 것으로 나타났다. 월별 강우량과 유출량은 7월과 8월에 가장 높았으며, 유출률은 8월과 9월에 높은 값을 보여 강우량과 유출량, 유출률 변화가 반드시 일치하지는 않았다. 월별 변동계수(CV)는 강우량에 비해 유출량이 더 크게 나타났고, 강우량과 유출량 간의 편차는 점차 증가하였다. 강우량에 대한 총 유출량과 직접 유출량의 변화는 2011년~2017년의 추세선의 기울기가 더 낮아졌고, 기저유출량의 기울기는 증가하였다. 산림토양이 발달하면서 토양층의 수분보유력이 증가하였기 때문으로 보여지며, 기저유출량의 증가는 팔공산 산림소유역의 유출수량 증가와 함께 지하수위 상승에 영향을 줄 것으로 판단된다. 감수곡선의 기울기는 2003년~2010년에 비해 2011년~2017년이 더 낮은 것으로 나타났고, 시간이 경과함에 따라 유출량의 감소가 완화되고 유출량이 일정하게 유지되었다. 따라서 팔공산 산림소유역은 임목의 생장에 따라 지표류의 유출이 감소하고 기저유량이 증가하는 것으로 나타나, 산림의 수원함양기능이 점차 증가하는 것으로 나타났다.