• 대기
• /
• 제26권4호
• /
• pp.553-563
• /
• 2016

Land evaporation contribution to precipitation over East Asia is studied to understand terrestrial moisture source of continental precipitation. Moisture recycling of precipitation relying on terrestrial evaporation is estimated based on the analysis method of Van der Ent et al. (2010). We utilize HadGEM2-AO simulations for the period of 1970~1999 and 2070~2099 from RCP8.5. Globally, 46% of terrestrial precipitation is depending from continental evaporation. 58% of terrestrial evaporation returns as continental precipitation. Over East Asia, precipitation has been affected by local evaporation and transported moisture. The advection of upwind continental evaporation results from the prevailing westerlies from the midwestern of Eurasian continent. For the present-day period, about 66% of the precipitation over the land of East Asia originates from land evaporation. Regionally, the ratios change and the ratios of precipitation terrestrial origin over the Northern inland and Southern coast of East Asia are 82% and 48%, respectively. Seasonally, the continental moisture recycling ratio is larger during summer (JJA) than winter (DJF). According to RCP8.5, moisture recycling ratio is expected to change. At the end of the 21st century, the impact of continental moisture sources for precipitation over East Asia is projected to be reduced by about 5% compared to at the end of 20th century. To understand the future changes, moisture residence time change is investigated using depletion and replenishment time.

• 한국환경과학회지
• /
• 제22권1호
• /
• pp.119-129
• /
• 2013

We compared equilibrium evaporation($E_{equili}$) eddy-covariance($E_{eddy}$) with soil moisture data($E_{SMseries}$) which were measured with a 2 hours sampling interval at three points for a humid forest hillslope from May 5th to May 31th in 2009. Accumulations of $E_{eddy}$, $E_{equili}$ for the study period were estimated as 2.52, 3.28 mm and those of $E_{SMseries}$ were ranged from 1.91 to 2.88 mm. It suggested that the eddy-covariance method considering the spatial heterogeneity of soil evaporation is useful to evaluate the soil evaporation. Method A, B and C were proposed using mean meterological data and daily moisture variation and the computations were compared to eddy-covariance method and equilibrium evaporation. The methods using soil moisture data can describe the variations of soil evaporation from eddy-covariance through simple moving average analysis. Method B showed a good matched with eddy-covariance method. This indicated that Dry Surface Layer (DSL) at 14:00 which was used for method B is important variable for the evaluation of soil evaporation. The total equilibrium evaporation was not significantly different to those of the others. However, equilibrium evaporation showed a problem in estimating soil evaporation because the temporal tendency of $E_{equili}$ was not related with the those of the other methods. The improved understanding of the soil evaporation presented in this study will contribute to the understandings of water cycles in a forest hillslope.

• 한국의류학회지
• /
• 제24권6호
• /
• pp.810-818
• /
• 2000

The purpose of this study was to analyze the effect of geometrical structure on the moisture transport properties of nonwoven batting materials. Two types of nonwovens were used such as single and double layered nonwovens. Steady and dynamic state water vapor transport properties were measured by absorption, evaporation and cobaltous chloride method respectively. The results of this study were as follows: 1) Geometrical structure affected water vapor evaporation, but there were no differences between single and double layered nonwovens in moisture absorption. Thickness and air permeability were influencing factor on water vapor transport rate. 2) Directionality of double layered nonwoven was observed both in steady and dynamic state moisture transport. There were differences between upper and lower layer of double layered nonwoven both in moisture absorption rate and color change by cobaltous chloride method. 3) In dynamic state of water vapor transport rate, single layered nonwoven reached more rapidly at the established relative humidity. It was confirmed that geometrical structure affected water vapor evaporation and hydrophilicity of fiber affected moisture absorption because there were much more water vapor transport rate by evaporation than absorption within the same period of time.

• 한국건축시공학회:학술대회논문집
• /
• 한국건축시공학회 2012년도 추계 학술논문 발표대회
• /
• pp.75-76
• /
• 2012

In this study, it was evaluated about creep properties of high strength concrete according to compressive strength and moisture evaporation condition. As a results, creep strain and creep coefficient was greatly affected by moisture evaporation conditions rather than compressive strength. Also, the effect of fiber mixed was not show big difference.

• 한국의류학회지
• /
• 제25권1호
• /
• pp.61-70
• /
• 2001

As important factors determining human sensorial comfort, liquid moisture management and surface properties of heat resistant workwear materials were examined. To figure out liquid moisture management properties of the test materials, absorption capacity, rate of absorption, and evaporation properties were assessed. A modified GATS(Gravimetric Absorbency Testing System) was used to measure the liquid moisture accumulation associated with the wicking of liquid moisture from sweating skin. The GATS procedure measures demand wettability of materials to take up liquid in a direction perpendicular to the fabric surface and it was modified to incorporate a special test cell and cover to assess absorption behavior in the presence of evaporation. Fabric stiffness, smoothness, number and the length of surface fibers, and an estimate of the contact area between the skin and fabric surface were measured to characterize the mechanical and surface properties of the test materials. Also an estimate of the force with which a fabric clings to moist skin was made using as wet-cling index.

• 한국건축시공학회:학술대회논문집
• /
• 한국건축시공학회 2012년도 춘계 학술논문 발표대회
• /
• pp.289-290
• /
• 2012

In this study, it was evaluated about shrinkage properties of high strength concrete according to poly mix fiber and moisture evaporation condition. As a results, When concrete was mixed with poly mix fiber of spalling control, it reduced effect of shrinkage independent of the evaporation conditions of unsealed and sealed.

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

• 한국환경과학회지
• /
• 제4권5호
• /
• pp.427-435
• /
• 1995

In order to discuss the differences among the SMP(Surface Moisture Availability Parameter), by previous researchers on the basis of their own theoretical and empirical background, we assessed the SMP according to the soil types and volumetric soil water contents. The results are as follows. There are differences among all the five SMAPs. There's a tendency that the larger grain size, the higher value of parameters. And they divided into two groups for their value: one group has parameters with exponential function and the other with cosine and linear function. The maximum difference between the two groups appears when the volumetric soil water contents are 0.07m3m-3 for sand, 0.l1m3m-3 for loam, 0.12 for clay, and 0.13m3m-3 for silt loam. So, these differences must be considered when we estimate the surface evaporation rate. From field data, the paddy field soil around Junam reservoir is classified as a silt has high wetness, 0.56. So, the parameter obtained from the field measurement is much higher than that of Clapp and Hornberger(1978)'s Table. This study treated the SMP for a certain point of time in winter season. But if we measured the soil water contents continuously, we could obtain better time-dependent parameter. Key words : SMAP(Surface Moisture Availability Parameter), Paddy field, Volumetric soil water content, Evaporation, Capillary potential.

• 에너지공학
• /
• 제18권4호
• /
• pp.213-220
• /
• 2009

수분의 함량이 높은 저품위탄을 건조시키기 위하여 유중 건조 방법에 대해 조사하였다. 최적의 건조 조건을 선정하기 위하여 최종온도, 석탄과 등유의 혼합비율, 석탄 또는 등유의 양, 혼합물의총량, 교반방법에 따른 석탄의 건조 특성을 관찰하였다. 최종온도가 $120^{\circ}C$ 이하일 때는 완전한 증발이 이루어지지 않았으며, $130^{\circ}C$ 이상인 경우에는 수분의 증발량에 큰 차이가 나타나지 않았다. 석탄과 등유의 혼합비율에서 석탄의 양이 증가 할수록 수분의 증발이 잘 이루어짐에 따라, 열에너지의 전달이 수분의 증발에 미치는 영향보다 증발한 수분이 등유 속에서 배출되기 위하여 필요한 에너지가 더 큰 것으로 나타났다. 혼합물의 총량이 많은 경우에는 건조후의 수분 함량이 더 낮아지지만 많은 시간이 소모되는 반면, 적은 경우에는 수분 함량을 일정한 수준 이하로 낮추기 어려운 반면에 짧은 시간에 일정한 함량까지 수분을 증발시킬 수 있는 것으로 나타났다. 따라서 등유와 석탄 혼합물의 유동성이 확보되는 한도 내에서 등유의 양을 가능한 줄이는 것이 석탄의 건조에 유리한 것으로 판단되었다. 한편, 질소를 이용한 교반과 진공을 개별적으로 적용한 경우에는 증발량이 향상되었다.

• 한국의류학회지
• /
• 제8권1호
• /
• pp.95-106
• /
• 1984

This experiment was conducted to determine the heat loss by the amount of perspiration from human body. Warmth keeping ratio determined by using cooling methods were as follows ; 1) The higher amount of moisture evaporation, the higher amount of heat loss was resulted 2) The cold feeling was found at the level of moisture content in clothes above 0.017 cc/$cm^3$ (amount of moisture evaporation; $160\times10^{-3}cc/cm^2{\cdot}min$) 3) There was no relationship between the characteristics of fabrics(kinds, density, were factor, moisture transpiration) and heat loss at the same moisture content.