해상 사고에 의한 익수자는 저체온증에 의한 사망 위험에 노출되어 있다. 구명 동의 등을 착용함으로써 부력은 유지할 수 있으 나 해수의 낮은 온도에 의한 신체의 열손실은 짧은 시간 내에 체온을 하강시키고 그에 따른 저체온증 사망이 우려된다. 전통적인 구명 동 의는 고체형 부력체를 사용하여 부력을 향상 시키고 있으나, 구명 동의에 공기를 채움으로써 부력 및 체온 보존 효과를 얻을 수 있을 것으 로 판단된다. 본 연구는 고체형 충진재를 이용한 기존의 비 팽창형 구명 동의와 공기를 채운 팽창형 구명 동의의 단열 성능을 비교하고, 각 각의 방법이 체온 변화에 미치는 영향을 정성적으로 평가하고자 한다. 먼저 열저항 모델을 이용한 대략적인 단열 성능의 비교를 실시하고, 유한요소법을 이용하여 Pennes의 신체 열전달 해석을 수행하여 시간에 따른 체온 변화를 수치적으로 검토하였다.

To compare the effects of two external forcing on track of typhoon, TWRF(Typhoon WRF) based ensemble experiments are carried out in the case of Typhoon Morako which is the 8th typhoon at Northwest Pacific region in 2009. The two forcing are tropical SST and topography induced thermal and mechanical forcing, respectively. According to the result of numerical experiment for five-day forecast, the effect of mechanical forcing is about two times stronger than thermal forcing on the track error of the typhoon. More case study for other typhoon will be done as a next paper.

This study forecasts changes in thermal environment and microclimate change per new building construction and assignment of green space in urban area using Computational Fluid Dynamics(CFD) simulation. The analysis studies temperature, humidity and wind speed changes in 4 different given conditions that each reflects; 1) new building construction; 2) no new building construction; 3) green spaces; and 4) no green spaces. Daily average wind speed change is studied to be; Case 2(2.3 m/s) ＞ Case 3. The result of daily average temperate change are; Case 3(26.5℃) ＞ Case 4(24. 6℃) ＞ Case 2(23.9℃). This result depicts average of 2.5℃ temperature rise post new building construction, and decrease of approximately 1.8℃ when green space is provided. Daily average absolute humidity change is analysed to be; Case 3(15.8 g/kg') ＞ Case 4(14.1 g/kg') ＞ Case 2(13.5 g/kg'). This also reveals that when no green spaces is provided, 2.3 g/kg' of humidity change occurs, and when green space is provided, 0.6 g/kg change occurnd 4(1.8 m/s), which leads to a conclusion that daily average wind velocity is reduced by 0.5 m/s per new building construction in a building complex.

In this study, thermal environment improvements throughout public design improvement project on the urban street space were compared and evaluated. Thermo-Render 3.0, 3D-CAD based thermal environment simulation program, had been used for thermal environment improvement evaluations. Followings are the results. First, clayey blocks which have low heat transfer rate and cool island effect by trees and roof gardens brought cooling effects for buildings and surface of streets. Seconds, MRT values showed low levels because of low radiant mulching materials. Thirds, roof gardens contributed to reduce heat island effect since HIP levels were affected by decreasing heat storage effect of buildings from roof gardens. As a result, reducing heat storage effect throughout selecting and arranging proper materials which would not increase heat island potentials should be performed to improve heat island effects.

The present study explores time and spatial thermal environment for Daegu, which is a city built on a basin area, according to varying land cover conditions of the earth's surface by analyzing data derived from meteorological observation and satellite images. The study has classified land use by utilizing MODIS satellite images and analyzed land surface temperature. Also, by using data acquired from automatic weather system, the study has evaluated the effects of atmospheric heating caused by city pavements by analyzing the sensible heat flux between the city's land surface and the atmosphere.The results are as follows. 1) Classification of land use in the Daegu area shows 46.64% of urban and built-up area, 1.39% of watersides, 35.19% of forest, 11.43% of crops, and 5.37% grasslands. 2) During the weekdays throughout the year, the land surface temperature was high for Dalseogu, Bukgu, and Seogu regions where industrial complexes could be found. Comparatively, lower temperature could be observed in the woodlands. 3) While the land surface temperature displayed the effects of pushing air upwards during the weekdays in urban areas, the reverse was true for forest regions. During the night, the temperature did not exert any significant influence on air movement.

This paper presents hull stress monitoring system installed in LNGC damaged by a Typhoon Elongation/contraction of removed areas has been assessed in terms of possible residual stress that will take place in replaced blocks when the applied load is removed. The bending moment of a vessel changes actually in terms of loss of longitudinal members and the change of weight distribution in repair procedure. The change of bending moment affects mainly in hull stress of longitudinal members. Hull stress monitoring system was installed on upper deck to prove LNGC stable in the criteria to be less than 40MPa during the period of repair procedure. A temperature measuring system was also installed to exclude the additional stress due to thermal effect from the measured hull stress. As a result, the hull stress was modified with the data measured by the temperature measuring system. This hull stress considering thermal effect was used as a guide stress to check the safety of LNGC during the period of repair procedure.

난분 함수량에 따른 생육반응에서 건중에 비해 생체중의 변화가 현저하였다. 특히 난분 함수량이 0%± 5인 C point는 100%± 5인 A point에 비해 16.1g에서 4.7g으로 지하부의 생체중 감소가 매우 격감하였으나, 지상부의 생체중에서는 3.5g에서 2.1g으로 다소 감소하는 경향을 볼 수 있었다. 건중에서는 현저한 차이를 볼 수 없었다. 또한 엽록소와 총수용성 탄수화물(Total soluble carbohydrate)에서 용토 내의 함수량에 따른 현저한 차이를 볼 수 있었으나, 지상부와 지하부에 따른 다른 현상을 볼 수 있었다. 체내 총수용성 탄수화물량의 변화를 살펴보면, 지상부는 난분 내의 함수량이 0%± 5의 C point시점에서 0.2mg/g DW로 다소 감소함을 알 수 있었으나, 근권부에서는 100%± 5인 A point에서 0.14mg/g DW에 비해 50%± 5(B point) 그리고 0%± 5(C point)의 시점에서 0.22mg/g DW로 보다 증가함을 알 수 있었다. 난분 함수량에 따른 proline 축적량 변화는 100%± 5인 A point에 0.05mg/g FW 비해 0%± 5인 C point의 시점에서 0.6mg/g FW로 큰 변화를 볼 수 없었다. 한편, glycinebetaine에서는 지상부에서는 변화가 없었으나, 근권부인 뿌리에서 함수량이 100%± 5(A point)의 0.11mg/g DW에서 0%± 5인 C point의 시점에서 0.26mg/g DW로 2배의 증가를 불 수 있었다.

In order to work out statistics of environmental functions of indoor landscape plants in architectures, this study aims to conduct a simulation of how much control plants have over overheating phenomena in atria in summer, involve themselves in air current speed and maintain indoor comfort index, with a numerical analysis model. Thus, nine kinds of representative plants which are usually used for indoor environments were selected, and purified with two irrigations a day for two weeks. And then, their transpiration and photosynthesis amounts were measured three times with a photosynthesis analysis system LICO-6400 at 38℃, which is the highest temperature in the atrium in summer. The data were organized, and another three plants with similar transpiration and photosynthesis amounts were selected. The leaf area which accounts for 10% green zone rate inside the atrium was calculated, and the leaf surplus was removed. And then, the plants were left inside the atrium, and transpiration amount and temperature change were automatically measured for three hours. The maximum temperature change by transpiration of plants was found to be 2.21~2.92℃, which means 0.21~0.23℃ per every 100cm² of leaf area.It is hard to see air current change in atria as convection by plants as the change is at undetectible level with a distribution of 0.08~0.005m/s. However, if air current change is made with fans even in natural air current situations, air current becomes active inside atria as rather cold air moves upward. Therefore, if 0.5 m/s of air current change is made with upward and downward fans in atrium models, the air current speed in the entire atrium converges to the level which gives the most comfort to human.

To verify the accuracy of the numerical experiment of Part I, measurements at the matured rice canopy located around Junam reservoir were performed at August 14, 1995. According to the measured data, the foliage temperature recorded the highest value, and the ground temperature was the lowest around noon, and these results coincided with those of the numerical experiment using the combined model of Part I. From the estimation using measured data, the maximum value of the latent heat flux was 380 Wm2, the highest value among energy balance terms, and the energy redistribution ratio of the latent heat flux was averaged as 0.5, the highest values among redistribution ratios. These results are the same as those of the numerical experiment in tendency, but they reveals a little lower in the absolute values than those from the numerical experiment.

To estimate the thermal effect of the vegetation canopy on the surface sublayer environment numerically, we used the combined model of Pielke's1) single layer model for vegetation and Deardorff's2) Force restore method(FRM) for soil layer. Application of present combined model to three surface conditions, ie., unsaturated bare soil, saturated bare soil and saturated vegetation canopy, showed followings; The diurnal temperature range of saturated vegetation canopy is only 20K, while saturated bare soil and unsaturated bare soil surface are 30K, 35K, respectively. The maximum temperature of vegetation canopy occurs at noon, about 2 hours earlier than that of the non-vegetation cases. The peak latent heat fluxes of vegetation canopy is simulated as a 600Wm2 a at 1300 LST. They have higher values during afternoon than beforenoon. Furthermore, the energy redistribution ratios to latent heat fluxes also increased in the late afternoon. Therefore, oasis effect driving from the vegetation canopy is reinforced during late afternoon compared with the non-vegetated conditions.

Based on the X-ray powder diffraction (XRD) and M ssbauer spectroscopy, the thermal behavior and phase transformations of two clays are investigated for raw and fired conditions, which are collected from Kwangryeongli and Ildo district in Cheju Island. M ssbauer spectra at room temperature and 20for two clays show that paramagnetic Fe3- is the structural iron of the layer silicate and ferrihydrite, and superparamagnetic goethite has about 50% of total iron contents. The XRD peaks of hematite for the fired clays appear from 800℃ in Kwangryeongli clay and from 600℃ in Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 400℃ for Kwangryeongli clay and 500℃~600℃ for Ildo district clay, respectively. The structural Fe2+ was completely oxidized into Fe3- at 400℃. For the temperature ranging from 400℃ to 700℃~800℃, two fired clays exhibit the dehydroxylation of the clay mineral. A disintegration of the clay mineral structure is observed from 700℃~800℃ to 1100℃, followed by the onset and spread of vitrification process. It is also shown that well-crystallized hematite phase is formed at the temperature higher than 1100℃ and the relative absorption area decreases, which might be related to the recrystallization of alluminosilicate matrix.