• 한국농공학회지
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• 제21권2호
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• pp.81-103
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• 1979

The weathered granite soil involves problems in its stability in soil structures depending upon the reduction of soil strength due to the water absorption, crushability, and content of colored mineral and feldspar. As an attemt to solve the problems associated with soil stability, the crushability of weathered granite soil was investigated by conducting tests such as compaction test, CBR test, unconfined compression test, direct shear test, triaxial compression test, and permeability test on the five soil samples different in weathering and mineral compositions. The experimental results are summarized as follows: The ratio of increasing dry density in the weathered granite soil was high as the compaction energy was low, while it was low as the compaction energy was increased. The unconfined compressive strength. and CBR value were highest in the dry side rather than in the soil with the optimum moisture content, when the soil was compacted by adjusting water content. However, the unconfined compressive strength of smples, which were compacted and oven dried, were highest in the wet side rather than in soil with the optimum moisture content. As the soil becomes coarse grain, the ratio of specific surface area increased due to increased crushability, and the increasing ratio of the specific surface area decreased as the compaction energy was increased. The highest ratio of grain crushability was attained in the wet side rather than in the soil with the optimum moisture content. Such tendency was transforming to the dry side as the compaction energy was increased. The effect of water on the grain crushability of soil was high in the coarse grained soil. The specific surface area of WK soil sample, when compacted under the condition of air dried and under the optimum moisture content, was constant regardless of the compaction energy. When the weathered granite soil and river sand with the same grain size were compacted with low compaction energy, the weathered granite soil with crushability had higher dry density than river sand. However, when the compaction energy reached to certain point over limitation, the river sand had higher dry density than the weathered granite soil. The coefficient of permeability was lowest in the wet side rather than in the optimum moisture content, when the soil was compacted by adjusting soil water content. The reduction of permeability of soil due to the compaction was more apparent in the weathered granite soil than in the river sand. The highly significant correlation coefficient was obtained between the amount of particle breakage and dry density of the compacted soil.

• Applied Biological Chemistry
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• 제42권3호
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• pp.218-222
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• 1999

자당지방산에스테르(SE), 이소말토올리고당(IO) 또는 글리세린(GL)을 첨가한 백설기를 7일간 저장한 후 저장온도, 수분함량 및 첨가물의 농도에 따른 백설기의 텍스쳐에 미치는 영향을 경도, 응집성 및 씹힘성의 관점에서 반응표면 분석법으로 비교분석하였다. SE첨가 백설기 경도는 20, 50 및 $80^{\circ}C$의 저장온도에서 등고선 값은 각각 $1500{\sim}3200,\;500{\sim}1300$ 및 $100{\sim}400\;g_f$로 저장온도가 올라감에 따라서 급격히 감소하였다. $20^{\circ}C$ 및 $50^{\circ}C$의 저장에서는 수분함량과 SE농도 증가에 따라서 경도는 감소하였으나 $80^{\circ}C$의 고온저장에서는 수분함량 증가나 SE첨가효과가 거의 나타나지 않았다. IO나 GL첨가 백설기의 경도는 일반적으로 저장온도가 높아질수록 수분함량 및 첨가물 농도가 증가할수록 감소를 나타내었다. 백설기의 경도에 미치는 영향은 저장온도, 수분함량, 첨가물농도 순이었으며 저장온도 조절이 백설기의 저장성 향상에 가장 효과적이라는 것을 의미한다. 응집성 측면에서 SE 또는 GL첨가 백설기는 저장온도가 $20^{\circ}C$에서 $50^{\circ}C$로 높아짐에 따라서 응집성 증가를 보였으나 $50^{\circ}C$와 $80^{\circ}C$의 저장온도간에는 차이가 거의 없었다. 또한, 수분함량이 40%부근에서 높은 응집성을 나타내었으며 GL첨가 백설기는 농도가 0.5%부근에서 낮은 값을 보였다. 저장온도, 첨가물 농도 및 수분함량 순으로 백설기의 응집성에 영향을 미쳤다. 씹힘성은 첨가물의 종류에 관계없이 저장온도가 높아질수록, 수분함량과 첨가물 농도가 증가할수록 감소하였다. 씹힘성에 영향을 미치는 정도는 저장온도, 수분함량, 첨가물 농도 순이었다.

• Journal of the Korean Wood Science and Technology
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• 제24권1호
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• pp.75-80
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• 1996

The purpose of this study is to clarify the mechanism of moisture transfer depend on the thickness of the spruce(Picea sitchensis Carr.). Therefore, as the basic research of moisture transmission, the amount of moisture transmission and the moisture distribution in specimens and temperature of it's surfaces in vapor transmission process were investigated. The experiment was conducted in a steady state. and the moisture distribution was measured by knife cutting and weighing the specimens. The following conclusions were obtained ; 1. It can be found that distribution of moisture in the specimen can be approximated by two different straight lines intersecting at nine or ten percent moisture content. The amount of moisture movement defends on the gradient of moisture in the wood. 2. It is investigated that the wood surface moisture contents(MCs) are less for thinner specimens than for thick ones on the absorption side. On the other hand, the wood surface MCs are greater for thinner specimens than for thick ones on the desorption side. The main factor that affects the EMC of wood would be temperature when the relative humidity of atmosphere is constant. The specimen generate heat with the absorption and desorption process. In addition, the velocities of moisture transmission varied with the thicknesses of specimens. If the temperature of wood becomes greater, its MC decreases. Then the difference between surface MC and EMC of adsorption and desorption side becomes greater for thinner specimens. Therefore it is considered that the coefficients of moisture transfer decreases with the increases of the specimens' thicknesses.

• 한국환경과학회지
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• 제31권10호
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• pp.869-881
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• 2022

In this study, a field study was conducted to investigate the relationship between high-resolution remote images and the volumetric moisture, and the number of compaction. Changes in the shape of the surface and soil moisture content were observed and correlated with the number of compactions using roller equipment. As the compaction is repeated, the surface is flattened and the terrain curvature decreases and converges to zero. In particular, the tangential curvature changes as the number of compactions increase. Due to soil compaction, the vegetation index changed from a positive to a negative value, and most of the test site area was homogenized with a negative index. This suggests a decrease in porosity and an increase in volumetric water content associated with increasing soil compaction. Soil moisture, measured using a frequency domain reflectometry(FDR) sensor, tends to increase proportionately with the number of vibration compactions, but the correlation between the number of compactions and soil moisture is unclear. This study suggests that while it is necessary to consider the reproducibility of the experiments performed, the compaction quality of the soil can be evaluated using high-resolution terrain factors and soil moisture.

• 반도체디스플레이기술학회지
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• 제9권2호
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• pp.33-39
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• 2010

The moisture absorption properties such as diffusion coefficient and moisture content ratio of liquid type epoxy resin systems with the filler were investigated. Bisphenol A type and Bisphenol F type epoxy resin, Kayahard MCD as hardener and 2-methylimidazole as catalyst were used in these epoxy resin systems. The nano-sized spherical type fused silica as filler were used in order to study the moisture absorption properties of these liquid type epoxy encapsulant according to the change of filler size. The temperature of glass transition (Tg) of these epoxy resin systems was measured using Dynamic Scanning Calorimeter (DSC), and the moisture absorption properties of these epoxy resin systems according to the change of time were observed at $85^{\circ}C$ and 85% relative humidity condition using a thermo-hygrostat. The diffusion coefficients in these systems were calculated in terms of modified Crank equation based on Ficks' law. An increase of Tg and diffusion coefficient with filler size in these systems can be observed, which are attributed to the increase of free volume with Tg. The change of maximum moisture absorption ratio according to the filler size and filler content cannot be observed; however, the diffusion coefficients of these systems decreased with filler content. The diffusion via free volume is dominant in the epoxy resin systems with low nano-sized filler content; however, the diffusion with the interaction of absorption according the increase of the filler surface area is dominant in the liquid type epoxy encapsulant with high nano-sized filler content.

• E2M - 전기 전자와 첨단 소재
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• 제1권1호
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• pp.70-77
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• 1988

This paper describes the influence of the electrode materials, moisture content, electrolyte density, temperature, surface state, ion absorbent on the C.T.I of phenolic resin by the I.E,C, 112 method. C.T.I are increased for electrode materials with low hydrogen overvoltage and high soluble point. Increusing moisture content of samples increased by logarithmical on the droplet number to tracking breakdown. Increasing electrolyte temperature region above 70-80(.deg.C) decreased hydrogen over-voltage, following the density changes are decreased by C.T.I=1/aD$^{2}$-bD+C.

• 한국연초학회지
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• 제18권2호
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• pp.150-159
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• 1996

In this study, to obtain the basic data for the optimum moisture control system, moisture adsorption characteristics, adsorption isotherms models for water and surface physical characteristics of burley and flue-cured tobacco were investigated. By the hypothesis' the phenomenon of moisture adsorption of tobacco is the same as the first order reaction, the wetting constant (k) and equilibrium moisture content were obtained. And activation energy, frequency factors were also calculated by applying its data to Arrhenius equation. The Kamei's empirical formula of moisture adsorption isotherms showed the best agreement with the experimental data and its correlation coefficient (r) was 0.997. It can be seen that specific surface area of burley is 157 m2/g, that of flue-cured is 152 m2/g, -△H1 of adsorbed monolayer is 45,972 J/mol, 45,486 J/mol, respectively, and the condensation heat (40,595 J/mol) being caught in adsorbed multilayer is less than that of monolayer.

• Journal of the Korean Wood Science and Technology
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• 제2권2호
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• pp.5-7
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• 1974

본 논문은 필자가 미국 미쉬간대학에 유학중 실시된 연구로서 동대학 목재가공학과에 설치된 소형 목재인공건조장치를 사용하여 일정한 건조조건(건구 온도 $150^{\circ}F{\risingdotseq}65.5^{\circ}C$, 습구온도 $1250^{\circ}F{\risingdotseq}51.7^{\circ}C$, 관계습도 48%, 평형함수율 6.9%)하에 공기 순환속도를 매분당 250ft., 400ft, 및 650ft.로 변경할 때 얻어지는 건조속도를 측정하고, 시간당 건조율을 산출하여 비교 검토한 것이다. 본 실험에 사용한 수종은 북미산소나무 Northern white pine (Pinus strobus L.)로서 시편의 크기는 길이 60cm, 넓이 12.5mm(5in.), 두께 18.7mm(3/4in.)이며 공시목의 표면은 증발조건을 균일히 하기 위하여 포삭하였으며, 마구리(end grain)에는 end coating 하였다. 또한 공기순환속도 측정은 상기대학에 비치된 velometer를 사용하였다. 1. 목재의 섬유포화점(함수율 30%) 이상에 있어서 공시목의 건조율은 건조실내 공기순환속도의 증가에 따라서 증가된다. 즉 공시목의 건조율 증감은 공기 순환속도에 대략 비례한다. 그러나 섬유포화점 이하에 있어서는 공기순환속도의 증강은 건조율 증감에 거의 영향을 이치지 아니한다(그림 1, 2 참조). 2. 실험한 건조조건하에 있어서는 공시목의 초기 함수율이 높을수록 높은 건조율을 얻을 수 있다. 즉 공시목의 초기 함수율(MC30% 이상)이 동일하지 아니한 경우에도 공기순환속도를 증가하면 건조 최종기에 있어서 비교적 빨리 대체로 같은 함수율의 공시목을 얻을 수 있다(실험한 초기 함수율, 건조조건 및 공기순환 속도등은 심한 건조 결함을 유발하지 아니하였음). 3. 본연구 결과에 의하면 공시목의 건조율은 섬유포화점(대략 MC30%)에 있어서 현저한 변화를 나타내고 있다. 즉 공시목의 함수율에 대한 건조율 곡선은 그림 3으로 표시된 바와 같이 섬유포화점 이상에 있어서는 건조율 곡선은 X축(MC)에 대하여 요(凹)형(concave)을 나타냈는데, 섬유포화점 이하의 함수율 범위 30%에서 20%에 있어서는 건조율 곡선은 X축에 대하여 철(凸)형(convex)을 나타냈으며 함수율 20% 이하에 있어서는 재차 심한 요(凹)형을 나타내고 있음을 알 수 있다. 이와감은 결과를 요약표시한 원문 그림4에 있어서, 건조율 곡선의 반곡점은 대략 섬유포화점인 MC 30%와 MC 20%에 위치하고 있음을 알 수 있다. 이와같이 섬유 포화점으로 알려져 있는 MC 30%와 20%에 있어서 건조율이 급변하는 반곡점 즉 한계점을 표시하는 것은 다음과 같은 야유에 의한 것으로 고려된다. 즉 세포막에 흡수된 결합수의 증발은 세포강, 세포간격 및 기타의 미세한 공간에 존재하는 자유수의 증발보다 훨씬 곤란하므로, 함수율 30%에서 20%의 범위에 있어서는 철(凸)형을 나타낸다. 즉 함수율 30%에서 20% 의 범위에 있에서 세포막의 모세관 응축수(capillary-condensed water)의 증발은 대략 동일한 감소율을 나타내나, 공시목의 함수율이 20%에 접근됨에 따라서 한층 강한 결합상태하에 있는 수분(표면 결합수 및 그 부근에 있는 수분)이 증발하게 되나, 그와 같은 수분의 증발은 한층 곤란하므로 함수율 20% 이하에 있어서 건조율곡선은 재차 요(凹)형을 표시하는 것으로 사료된다. 이상의 관계를 요약 표시한 원문 그림 4에 있어서, 반곡점을 가지지 아니한 점선 곡선 AC 와 2개의 반곡점을 가지는 실선곡선 BD를 비교하면, BD곡선은 AC곡선보다 함수율범위 30%에서 20%에 있어서 그 건조율은 현저히 감소되고 또한 D점을 반곡점으로 해서 그 건조율은 가일층 감소되고 있음을 알 수 있다. 이상을 요약하면 생재에서 함수율 30%(섬유포화점)까지는 큰 건조율을 표시하니 함수율 범위 30%에서 20%에 있어서는 그 건조율은 점감되고 함수율 20% 이하에 있어서는 그 건조율은 현저히 감소됨을 표시한다.

• 한국토양비료학회지
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• 제48권6호
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• pp.658-665
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• 2015

Temporal and spatial variation of soil moisture is important for understanding patterns of climate change, for developing and evaluating land surface models, for designing surface soil moisture observation networks, and for determining the appropriate resolution for satellite-based remote sensing instruments for soil moisture. In this study, we measured several soil moistures in upland soil using Advanced Microwave Scanning Radiometer 2 (AMSR2) Soil Moisture Content (SMC) during eight-month period in Chungbuk province. The upland soil moisture properties were expressed by simple statistical methods (average, standard deviation and coefficient of variation) from the monthly context. Supplementary studies were also performed about the effect of top soil texture on the soil moisture responses. If the results from this study were utilized well in specific cities and counties in Korea, it would be helpful to establish the countermeasures and action plans for preventing disasters because it was possible to compare with the relationship between soil moisture and top soil texture of each region. And it would be the fundamental data for estimating the effect of future agricultural plan.

• 한국지역사회생활과학회지
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• 제25권3호
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• pp.383-388
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• 2014

This study was examined the physical characteristics (geometry, yield strength, thousand-seeds weight, true density, and moisture content) required for mechanization-related technologies such as (harvesting, washing, transport, and drying). Large differences in the size and shape of boxthorn berries(Jangmyeong, Bullo, Chungmyeong, and Hokwang) are used to analyze these physical properties. The average diameter, volume, surface area, and sphericity rate are calculated using long and short diameters of the boxthorn berry according to its variety. Hokwang has the largest measured surface area, and Bullo, the smallest. Average yield strength is 1.78 kPa and the mechanical pressure of soft boxthorn berries is not more than 1 kPa. Bullo has the highest true density. The optimum drying time for the measurement of moisture content is 4 hours at the drying temperature of $100^{\circ}C$.