• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.36-36
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• 2019

강원도 설악산 국립공원에는 국내 최장의 토왕성 폭포가 있다. 유역면적이 $0.54km^2$에 불과하여 평소에는 폭포의 물줄기를 볼 수 없지만, 비 온 뒤에는 며칠간 하얀 물줄기의 장관을 연출한다. 본 연구에서는 물리적 기반의 수문모형인 CAT3.0을 이용하여 강우시 토왕성 폭포의 유출량을 분석하고 강우량에 따른 유출지속기간을 산정하여 강우의 누적량 및 지속기간에 따른 폭포의 물줄기를 볼 수 있는 기간을 추정하고자 하였다. CAT 3.0은 다양한 침투방정식중에 Rainfall Excess, Horton Eq., Green-Ampt. Eq.을 이용하여 강우시 토양특성(토양깊이, 투수계수)과 잠재증발산량과 토양수분량에 의한 실제증발산량을 산정하고 유출량을 계산하는 수문모형이다. 토왕성 폭포의 유출 특성을 분석하기 위하여 속초지점의 19년간(2010~2018) 관측자료를 이용하였으며, 토양의 깊이는 10 cm, 30 cm를 가정하여 비교하였다. 유출해석을 위하여 일단위 자료를 사용하였으며, 강우지속일수 및 누가강우량에 따른 유출을 산정하고 폭포의 물줄기가 확연히 보일 수 있는 한계유출량을 추정하였다. 폭포로부터의 유출량을 측정하는 관측지점이 없으므로, 폭포의 물줄기를 볼 수 있는 기간은 방송사 뉴스, 신문기사, SNS 등의 다양한 정보원으로부터 유추해석하였다. 이러한 분석결과로부터 강우에 의한 토왕성 폭포의 물줄기를 볼 수 있는 기간을 제시하였다.

• Journal of Korean Society on Water Environment
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• v.23 no.5
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• pp.683-688
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• 2007

Water flow into unsaturated soils is most often modeled by Richards equation consisting of the mass conservation law and Darcy's law. Three standard forms of Richards equation are presented as the head (${\Psi}$)-based form, the moisture content (${\theta}$) based form, and the mixed form. Numerical solutions of these partial differential equations with highly nonlinear terms can cause poor results along with significant mass balance errors. The numerical solution based on the mixed form of Richards equation is known that the mass is perfectly conserved without any additional computational efforts. The aim of this study is to develop fully implicit numerical scheme of Richards equation for one-dimensional vertical unsaturated flow in homogeneous soils using the finite difference approximation, and then to perform sensitivity analysis of infiltration to the variations in the unsaturated soil properties and to different soil types.

• The Journal of Engineering Geology
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• v.18 no.2
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• pp.127-136
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• 2008

Geophysical survey for establishing a wide site for the distribution of water content, wetting front infiltration due to the rainfall, and distribution of groundwater level has been performed by using 8round penetration radar (GPR) method, electrical resistivity method, and so on. On the other hand, a narrow area survey was performed to use a permittivity method such as time domain reflectometry, frequency domain reflectometry, and amplitude domain reflectometry methods for estimating volumetric water content, soil density, and concentration of contaminant in surface and subsurface. The permittivity methods establish more corrective physical parameters than different found survey technologies mentioned above. In this study for establishment of infiltration behaviors for wetting front in the unsaturated soil caused by an artificial rainfall, soil physical parameters for volumetric water content, pore water pressure, and pore air pressure were measured by FDR measurement device and pore water pressure meter which are installed in the unsaturated weathered granite soil with different depths. Consequently, the authors were proposed to a new establishment method for analyzing the variations of volumetric water content and wetting front infiltration from the responses of infiltrating pore water in the unsaturated soil.

• Korean Journal of Soil Science and Fertilizer
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• v.28 no.2
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• pp.123-129
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• 1995

For the propose of increasing the value added, zeolite powder was granulated by adding Polyvinyl Alcohol (PVA) as cementing material. The optimal concentration of PVA for granulation and the physical properties of the prepared granule were investigated. Four percent PVA stock solution was made by adding distilled water at $90^{\circ}C$ water bath and incorporated with zeolite. The contents of water stable granule above 2.0mm in diameter was 98.0% in the case of 0.3% PVA addition and almost 100% in the case of 0.6% PVA addition. Increasing PVA concentration of granules increased the hardness and decreased the infiltration rate and the maximum water holding capacity of granules, However, the drying method hardly affected the physical properties of granules. With the increase in the mixing ratios of kaolinite or bentonite to zeolite, the hardness of granules increased but high water contents of granules resulted in rapid decrease in the hardness of granules. However, when smectite or perlite was mixed with zeolite, the increase in mixing ratios to zeolite resulted in the decrease in hardness, the increase in the infilteration rate and maximum water holding capacity of granules.

• Korean Journal of Soil Science and Fertilizer
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• v.43 no.6
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• pp.823-827
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• 2010

This study was conducted to assess the propriety of models for soil water characteristics estimation in anthropogenic soil through the measurement of soil water content and soil water matric potential. Soil profile was characterized with four different soil layers. Soil texture was loamy sand for the first soil layer (from soil surface to 30 cm soil depth), sand for the second (30~70 cm soil depth) and the third soil layers (70~120 cm soil depth), and sandy loam for the fourth soil layer (120 cm < soil depth). Soil water retention curve (SWRC), the relation between soil water content and soil water matric potential, took a similar trend between different layers except the layer of below 120 cm soil depth. The estimation of SWRC and air entry value was better in van Genuchten model by analytical method than in Brooks-Corey model with power function. Therefore, it could be concluded that van Genuchten model is more desirable than Brook-Corey model for estimating soil water characteristics of anthropogenic soil accumulated with saprolite.

• KSCE Journal of Civil and Environmental Engineering Research
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• v.28 no.5A
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• pp.709-718
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• 2008

Developed is a chloride penetration analysis program in which changes of environmental conditions such as temperature, humidity and external chloride concentration, and the diffusion, convection and binding of chlorides are considered. In order to consider the changes of environmental conditions, analyses for temperature and moisture distribution are implemented simultaneously, and variation of diffusion coefficients due to temperature, humidity and age is also considered. By comparing the calculated total chloride contents with some experimental data, it has been confirmed that the proposed analysis program can trace measured chloride distribution well. Also, through some example analyses, the mechanism of accumulation of chlorides at near surface and acceleration of corrosion of steel reinforcement in case that the moisture distribution changes according to repeated drying and wetting cycles have been verified.

• Proceedings of the Korea Concrete Institute Conference
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• 1992.10a
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• pp.224-227
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• 1992

세그멘탈 교량에 포스트 텐셔닝 힘을 도입할 때 발생하는 가장 큰 문제는 균열의 발생이다. 이러한 균열은 실제 구조물의 강도감소 뿐 아니라, 이 균열은 염분 및 수분 침투의 통로가 되어, 부식 및 동결손상의 주원인이 되어 구조안전도에 큰 문제를 유발한다. 본 연구는 국부 집중 하중을 받는 프리스트레스 정착부의 응력분포 특성을 규명하고, 국부집중응력으로 인한 균열 발생 요인을 규명하여, 균열발생방지방안 및 그 대책을 강구함에 그 근본 목적이 있다. 이를 위하여 텐던에 대한 형상, 국부보강방식, 단일 및 복수텐던의 영향, 구조보강 철근량에 따른 콘크리트 내부 변형도 및 균열양상을 도출하기 위해, 부재를 제작하여 실험을 실시하여 균열의 양상 및 균열발생원인을 조사하고, 그 구체적 보강방안을 찾고자 한다.

• Journal of Korea Water Resources Association
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• v.34 no.3
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• pp.275-285
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• 2001

Since the majority of streamflow during dry periods is provided by groundwater storage, the streamflow depends on a basin moisture state recharged from rainfall during wet periods. This hydrologic characteristics dives good condition to predict long-term streamflow if the basin state like groundwater recharge is known in advance. The objective of this study is to examine groundwater recharge effect to monthly streamflow, and to attempt monthly streamflow prediction using estimated groundwater recharge. The ground water recharge is used as an independent variable with streamflow and precipitation to construct multiple regression models for the prediction. Correlation analysis was performed to assess the effect of groundwater carry-over to streamflow and to establish the associations among independent variables. The predicted streamflow shows that the multiple regression model involved groundwater recharge gives improved results comparing to the model only using streamflow and precipitation as independent variables. In addition, this paper shows that the prediction model with the effect of groundwater carry-over taken into account can be developed using only precipitation.

• Restorative Dentistry and Endodontics
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• v.18 no.2
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• pp.507-513
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• 1993

The purpose of this study was to observe the effect of immersion in water at 3, 5, 7, and 10 minutes after mixing on the surface of three regular and one light-curing glass-ionomer cement by measuring penetration of a methylene blue solution. Early solubility of these cements was also measured and compared with that of a zinc phosphate and a polycarboxylate cement. A blue-stained zone was observed in all glass-ionomer cement, but an inner, opaque zone was observed in only two of the regular glass-ionomer cements. Extending the time between start of mixing and immersion on water decreased the width of both zones in all cements and markedly lowered the loss of substance from the surface of regular glass-ionomer cements. However, time after mixing had no or only a limited effect on the loss of substance from the light-curing glass-ionomer cement, the zine phosphate cement, or the polycarboxylate cement.

• Proceedings of the Korea Water Resources Association Conference
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• 2017.05a
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• pp.458-458
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• 2017

증발산은 지표면으로부터의 증발이나 식물에 의한 증산에 의해 유역으로부터 물이 제거되는 주요 기작으로서, 유역 물수지 관점에서 보았을 때 강수량과 증발산량의 차이로부터 유출이나 함양되는 양을 추정할 수 있다. 제주도의 경우에는 수자원 이용량의 약 84%를 지하수에 의존하고 있으며, 한편으로 제주도의 지질학적 특성으로 인해 일정 규모 이하의 강수량은 지표유출이나 중간유출의 과정없이 대부분 지하로 침투되기 때문에, 증발산량을 정확하게 파악하는 것이 지하수 함양량의 추정과 제주도 전체 수자원 계획에 큰 영향을 주게 된다. 정확한 증발산량 파악을 위해서는 지속적인 관측과 전문적인 계측장비 등에 의한 직접적인 방법이 있으나 광범위한 유역 단위의 관측값을 확보하는 것이 현실적으로 어렵기 때문에, 물수지법, 열수지법, 공기역학적방법 및 조합방법 등의 간접적인 방법이 많이 활용되고 있다. 간접적인 방법으로 많이 활용되고 있는 Penman-Monteith 법은 일 단위 기반의 정확도 높은 증발산량을 추정할 수 있는 장점이 있으나, 작물생육단계 및 토양수분, 기상 등 많은 변수들에 대한 입력을 요구하고 있기 때문에 복잡한 모델링 과정을 수반하게 되는 단점을 내포하고 있다. 반면, Morton (1978)의 CRAE (Complementary Relationship Areal Evapotranspiration)나 Priestly and Taylor (1973)의 AA (Advection-Aridity)와 같이 잠재증발산량과 실제증발산량간의 보완관계를 이용하는 방법은 지역적인 인자 또는 가용 수분에 대한 조건없이 몇 가지 기상자료만으로 유역의 증발산량을 산정할 수 있다는 장점이 있다. 본 연구에서는 제주도 지역의 4개 하천유역(한천, 천미천, 강정천, 외도천)을 대상으로, Penman-Monteith 법을 적용한 SWAT 모델링를 통해 얻어진 유역의 실제증발산량과 잠재증발산량으로부터, 고도에 따른 기상특성을 반영하여 증발산 보완관계를 검토하였다.