• 한국안전학회지
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• 제5권1호
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• pp.31-39
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• 1990

In this paper, the influence of the table speed, metal removal rate and grinding fluid on long wheel workpiece contact zone at high effect grinding was investigated by theoretical analyses and measuring the temperature, and discussed by the temperature distribution in grinding surface layer. Main results obtained are as follows, 1) Rega.dless of the table speed, the temperature gap of the workpiece(heat influx) is about 6-8 times as high in dry condition as in wet condition. 2) Good grinding condition can be obtained owing to the effect of grinding fluid without any burning defect under the condition of the metal removal rate(1.0mm$^3$/mm.s) in case of wet grinding. 3) When the depth from the surface layer is about 1.25-1.5mm under the condition of the slow table speed, surface temperature goes up higher as the table speed slows down, because long contact time is laked at the surface layer. 4) In case of the same metal removal rate, the lower the table speed becomes, the higher the surface temperature is, because grinding depth has a far more influence on wheel workpiece contact zone than the table speed.

• 한국환경과학회지
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• 제10권5호
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• pp.337-342
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• 2001

The Rondonia Boundary Layer Experiment (RBLE-II) was conceived to collect data the atmospheric boundary layer over two representative surface in the Amazon region of Brazil; tropical forest and a deforested, pasture area. The present study deals with the observations of atmospheric boundary layer growth and decay. Although the atmospheric boundary layer measurements made in RBLE-II were not made simultaneously over the two different surface types, some insights can be gained from analysing and comparing with their structure. The greater depth of the nocturnal boundary layer at the forest site may be due to influence of mechanical turbulence. The pasture site is aerodynamically smoother and so the downward turbulent diffusion will be much pasture than over the forest. The development of the convective boundary layer is stronger over the pasture than over the forest. The influence of the sensible heat flux is important but may be not enough to explain the difference completely. It seems that energy advection may occur from the wet and colder(forest) to the dry and warmer area(pasture), rapidly breaking up the nocturnal inversion. Such advection can explain the abrupt growth of the convective boundary layer at the pasture site during the early morning.

• Journal of Forest and Environmental Science
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• 제33권2호
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• pp.136-146
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• 2017

We selected 6 plots ($100m^2$) located 2.2-3.8 km from Minamidake Crater on the north flank of Sakurajima Volcano. We conducted a field study to investigate the effects of volcanic activity on vegetation succession and surface erosion rate. The results showed that trees growing in plots further from the crater had a greater diameter at breast height (DBH), total height, and age. In addition, these plots had a greater number of woody plants and species, as well as a greater total cross-sectional area at breast height. The Fisher-Williams index of diversity (${\alpha}$) and the proportion of evergreen broad-leaved trees were higher in plots located further from the crater. Vegetation succession in these plots was not at the level of a climax forest. From 1972 to 2015, the timing for active volcano, the depth of volcanic ash layer, the dry density, and the pH of ground surface were lower for plots located further from the crater. Furthermore, the average annual sheet erosion from 1972 to 2015 was also lower for plots located further away from the crater. Overall, plots further away from the crater have a better environment for vegetation growth and a lower dry density of the volcanic ash surface layer. It is thought that lower dry density results in increased soil permeability, which impedes surface flow. In order to prevent debris-flow disasters, caused by mud and rock flow resulting from impaired soil penetrability, it is essential to promote soil development and restore penetrability by artificial vegetation restoration.

• 대기
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• 제27권3호
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• pp.317-329
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• 2017

Ocean mixed layer (OML) depth affects diurnal cycle of sea surface temperature (SST) induced by change of solar radiation absorption and heat budget in ocean. The diurnal SST variation can lead to convection over the ocean, which can impact on localized precipitation both over coastal and inland. In this study, we investigate the OML characteristics affecting the diurnal cycle of SST for the Korean Peninsula and surrounding areas. To analyze OML characteristics, HYCOM oceanic mixed layer depth (MLD) and wind field at 10 m from ERA-interim during 2008~2016 are used. In the winter, MLD is deeply formed when the strong wind field is located on perpendicular to continental slope over deep seafloor areas. Besides, cooling SST-induced vertical mixing in OML is reinforced by dry cold air originated from Siberia. The OML in summer is shallowly distributed about 20 m. In order to estimate the impact of OML model in high resolution NWP model, four experimental simulations are performed. At this time, the prognostic scheme of skin SST is applied in NWP to simulate diurnal SST. The simulation results show that CNTL (off-OML) overestimates diurnal cycle of SST, while EXPs (on-OML) indicate similar results to observations. The prediction performance for precipitation of EXPs shows improvement compared with CNTL over coastal as well as inland. This results suggest that the application of the OML model in summer season can contribute to improving the prediction for performance of SST and precipitation over coastal area and inland.

• 한국기계가공학회지
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• 제14권1호
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• pp.70-77
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• 2015

This paper develops and evaluates a mechanical machining process which involves drilling on PVS material. According to the material, two treatment experiments were conducted, one involving drilling in a wet condition or using a lubricant and one involving drilling in a dry condition with no lubricant. Drilling in a dry condition showed better performance in terms of the cutting time than in the wet condition. Otherwise, the wet condition has several advantages. The lubricant influenced the burr diameter size and minimized the temperature on the surface of the work piece. During the wet condition drilling process, a smaller burr diameter size was noted as compared to the dry condition. The temperature showed a linear correlation with the drill bit size, where a least-square analysis provided an $R^2$valuewhichexceeded 0.95. The wet condition required more cutting time than the dry condition. In this condition, the water provides a lubrication effect. A thin layer between the cutting edges and the surface of the work piece is formed. The chip formation is affected by the drilling depth. The color on the tips of the chips was darker than in the initial condition. No correlation between the drilling depth and the bore roughness was noted, but the variation of the cutting speed or the RPM influenced the roughness of the bore. The optimum cutting speed ranged from 40 RPM to 45 RPM in the condition which provided the finest roughness surface.

• Restorative Dentistry and Endodontics
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• 제25권2호
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• pp.243-253
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• 2000

The purpose of this in vitro study was to evaluate dentin bonding by two different dentin bonding systems(DBS) using acetone based primer or adhesive [All Bond 2(AB2), One Step(OS)] when they were applied by wet or dry bonding technique. Morphology of resin-dentin interface and hybrid layer thickness(HLT) were investigated using Confocal Laser Scanning Microscope(CLSM) and compared to shear bond strength(SBS). 72 extracted sound human molars were randomly divided into 4 groups of 18 teeth each - Group 1.(AW); AB2 by wet bonding. Group 2(AD); AB2 by dry bonding. Group 3.(OW); OS by wet bonding, Group 4.(OD); OS by dry bonding. In 6 teeth of each group, notch-shaped class V cavities(depth 2mm) were prepared on buccal and lingual surface at the cementoenamel juction(12 cavities per group). To obtain color contrast in CLSM observation, bonding resins of each DBS were mixed with rhodamine B and primer of AB2 was mixed with sodium fluorescein. Prepared teeth of each group were treated with AB2, OS, respectively according to the manufacturer's instructions except for dentin surface moisture treatment after acid etching. In group 1 and 3, after acid etching, excess water was removed with wet tissue(Kimwipes), leaving consistently shiny, visibly hydrated dentin surface. In group 2 and 4, dentin surface was dried for 10 seconds at 1 inch distance. The treated teeth were then packed with composite resin(${\AE}$litefil) and light-cured. 12 microscopic samples($60{\sim}80{\mu}m$ thickness) of each group were obtained after longitudinal section and grinding(Exakt cutting and grinding system). Morphological investigation of resin-dentin interface and HLT measurement using CLSM were done. For measurement of SBS, remaining 12 teeth of each group were flattened occlusally to remove all enamel and grinded to 500 grit SiC(Pedemet Specimen Preparation Equipment). After applying DBS on the exposed dentin surface, composite resin was applied in the shape of cylinder, which has 5mm diameter, 1.5mm thickness, and light cured. SBS was measured using Instron with a crosshead speed of 0.5mm/min. It was concluded as follows, 1. HLT of AW(mean: $2.59{\mu}m$) was thicker than any other group, and followed by AD, OW, OD in descending order(mean; 2.37, 2.28, $1.92{\mu}m$). Only OD had statistically significant differences(p<0.05) to AW and AD. 2. There were intimate contact of resin and dentin at the interface in wet bonding groups, but gaps or irregular interfaces were observed in dry bonding groups. 3. The length, diameter, density of resin tags were various even in the same group without significant differences between groups and lots of adhesive lateral branches were observed. 4. There were no statistically significant difference of SBS between AB2 and OS, but SBS of wet bonding groups were significantly higher(p<0.05) than dry bonding groups. 5. There were no consistent relationships between HLT and SBS.

• 한국토양비료학회지
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• 제42권5호
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• pp.364-370
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• 2009

벼 재배시 하해혼성층 논토양의 전북통과 지산통 작토층과 경반층의 특성을 2년간(2005~2006)조사 분석한 결과를 요약하면 다음과 같다. 하해혼성층적층 대표토양인 전북통과 곡간충적층 대표토양인 지산통을 10개소에서 조사한 결과 작토심은 전북통 12.6 cm, 지산통 12.7 cm 이었고 플라우 경운깊이는 120필지에서 조사한 결과 10.5 cm 이었으며 전북통에서 경도와 작토심과는 부의 상관을, 경도와 경반층 두께와는 정의 상관을 나타냈다. 경반층 경도는 전북통 $14.7kg\;cm^{-2}(25.3mm)$, 지산통 $8.7kg\;cm^{-2}(22.1mm)$ 이었고, 두께는 전북통 22.3 cm, 지산통 17.8 cm 이었으며 경반층 출현깊이는 전북통 15 cm, 지산통 20 cm에 있었다. 경반층 지온은 작토층과의 차이를 보면 전북통에서는 봄 $-2.0^{\circ}C$, 여름 $-2.5^{\circ}C$, 가을 $-1.0^{\circ}C$를 지산통은 봄 $-2.1^{\circ}C$, 여름 $-1.8^{\circ}C$, 가을 $-0.7^{\circ}C$를 나타냈고 전북통에서 산화환원전위차 변화는 작토층은 유수형성기부터 환원상태를 경반층은 출수후기까지 산화상태를 나타냈다. 토양물리성은 두 토양통 공히 경반층에서 용적밀도, 고상율이 높고 공극율, 기상율이 낮았다. 또한 토양화학성은 경반층에서 총질소가 낮았고, 유기물 및 유효 인산함량이 적은 반면에 pH가 높고, 유효규산, 치환성칼슘 및 마그네슘 함량이 많았다. 양이온치환용량은 전북통에서 작토층 및 경반층 비슷한 경향이었으나 지산통은 경반층에서 다소 낮은 경향을 나타냈다. 무기태질소 함량은 토양통 공히 작토층에서 많았고, 가용성 미량성분 함량은 경반층에서 많았으며 지산통에서 많은 경향을 나타냈다. 감수심은 전북통에서 심경구, 지산통 경운구는 로타리구보다 빠르고, 계절별 감수심 변화는 6월 하순까지는 감수심이 빨랐으나 7~8월에는 1~3 mm로 늦었으며 9월부터는 빠른 경향을 나타냈다. 벼 뿌리분포는 로타리 25 cm, 심경 30 cm, 경운 20 cm까지 신장하였고, 출수기 뿌리 건물중은 심경>로타리>경운 순으로 무거웠다.

• Structural Engineering and Mechanics
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• 제61권4호
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• pp.519-526
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• 2017

In the present paper, the effects of cutting parameters and coating material on the performances of cutting tools in turning of AISI 52100 steel are discussed experimentally. A comparative study was carried out between uncoated and coated (with TiCN-TiN coating layer) cermet tools. The substrate composition and the geometry of the inserts compared were the same. A mathematical model was developed based on the Response Surface Methodology (RSM). ANOVA method was used to quantify the effect of cutting parameters on the machining surface quality and the cutting forces. The results show that feed rate has the most effect on surface quality. However, cutting depth has the significant effect on the cutting force components. The effect of coating layers on the surface quality was also studied. A lower surface roughness was observed when using PVD (TiCN-TiN) coated insert. A second order regression model was developed and a good accuracy was obtained with correlation coefficients in the range of 95% to 97%.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2010년도 추계 학술발표회
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• pp.3-25
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• 2010

The paper deals with two bearing capacity problems of shallow footing under combined loading. The first is a FEM study of shallow strip footing on two-layer clay deposits subjected to a vertical, horizontal and moment combined loading, while the second is a centrifuge study of shallow rectangular footing on dry sand under double eccentricity. The FEM results revealed that the existence of top soft layer sensitively affects more on horizontal and moment capacity than vertical capacity for cases of footing on soft clay overlying stiff clay. Practical design charts are presented to evaluate bearing capacities of footing for various combinations of the ratio of the depth of the upper layer to the footing width and the ratio of undrained strength of the upper layer to that of the lower. The centrifuge tests indicated that current design practice of calculating failure load of rectangular surface footing under double eccentricity underestimates the centrifuge loading test data. This trend is more marked when the eccentricity becomes larger. The decreasing trend in failure load with an increase of double eccentricity is rather uniquely expressed by a single curve, using a newly defined resultant eccentricity and the diagonal length of the footing base.

• 한국수자원학회논문집
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• 제45권6호
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• pp.557-568
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• 2012

산림사면에서 수문학적 과정을 이해하는데, 증발산 중 토양증발을 구분하여 규명하고 정량화하는 것은 도전적이지만 중요한 연구 주제이다. 본 연구에서는 2009년 5월 22일부터 31일까지 총 10일 동안에 습윤한 산림사면에서 세 지점에서 깊이별 토양수분을 집중 측정하고, 분석하여 토양증발과 관련 기작에 대해 연구하였다. 토양증발을 평가하는 방법은 토양수분자료의 물질수지($E_{SM}$), Penman식(1948) 그리고 수정된 Penman식(Staple (1974), Konukcu (2007), 평형증발($E_{equili}$))이다. $E_{SM}$을 계산하기 위해서는 지표면의 에너지 균형식을 이용하여 토양내의 증발깊이(DSL, dry surface layer)를 평가하였다. 그 결과, 각 지점(A, B, C)의 2시간별 10일 동안의 누적 증발량($E_{SM}$)은 약 2.09, 1.80 그리고 2.88mm으로 평가되었다. Penman식(1948), Staple (1974), Konukcu (2007), 평형증발($E_{equili}$)의 누적 증발값은 각각 4.91, 8.80, 8.63 그리고 3.28mm으로 $E_{SM}$보다 높은 값들을 보여주고 있다. 산림 내 토양증발은 직접적인 복사량과 바람의 영향보다는 낙엽층과 DSL으로 인해 토양 내의온도상승과 대기와의 상호작용을 통해서 일어난다. 이는 $E_{SM}$는 복사량의 변화보다 2~4시간 정도의 시간적 지체(time lag)가 보이기 때문이다. DSL과 지표저항($r_s$)은 토양수분이 감소함에 따라 선형적으로 증가하였다. 관측된 장력 및 토양수분의 수직적 분포를 분석함으로써 확보되는 DSL 값은 에너지 방정식에 의해서 추정된 값과 유사하게 나타났다.