• 물과 미래
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• 제8권2호
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• pp.56-60
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• 1975

Traditional descriptions of water movement in soils and of calculations of infiltration rates neglect the air movement and its compressibility. The movement of two fluids in the bounded layered porous medium is treated analytically and computer simulations are conducted for given boundary conditions and initial saturation profiles. The movement of a given saturation across the interface between the different soil layers is theoretically developed by considering the conservation of mass. It is shown that the existence of the interface affects the infiltration rate when the average total velocity is greater than zero. The transition from one layer to another layer cause a change in the capillary drive and consequently influences the infiltration rate.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2010년도 추계 학술발표회 2차
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• pp.192-199
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• 2010

This research produced internal model tester ($2.0m{\times}2.0m{\times}1.0m$) to evaluate the field application of Paju Unjeong District water recycling system for small streams eco-friendly river bed disparity method for the first time in Korea and conducted comparative analysis of the Paju Unjeong District water recycling system field test results and infiltration rate result of internal tests by each rainfall intensity following surface material. Infiltration rate result of internal tests concrete pavement by rainfall intensity following surface material, asphalt pavement, bentonite mate, stabilized soil construction and mixed soil construction manifested low infiltration rate. On the contrary, compaction soil, grassland and water permeable packaging materials resulted in significant amount of infiltration rate. As for the field permeability test results, they were manifested similar tendency as indoor permeability test results and they satisfied the standard for standard of water permeability of domestic disparity facility (less than $1.0{\times}10-7cm$/sec). As compaction rate increased, unconfined compression strength increased as well while coefficient of water permeability decreased.

• 상하수도학회지
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• 제19권2호
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• pp.221-227
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• 2005

This study has suggested the base data for decision of maintenance ranking and estimation of maintenance effect in the maintenance project of sewers as based on investigation of the defective rate in the sewer through Infiltration/Inflow(I/I) and CCTV analysis. It also analyzed the correlation between I/I and defective rate of sewer. As the result of this study, (1) Defective items of sewer was found out one item each 12.97m with an average. (2) By regression analysis, I/I has high correlation with defective rate of sewer like that $R^2$ is 0.7806. (3) The first thing in the item with bad influence on the I/I was joint badness and secondary was cross connection.

• 생물환경조절학회지
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• 제24권2호
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• pp.100-105
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• 2015

온실의 난방부하 중 틈새환기전열부하 산정방법은 설계 기준마다 제각각이고, 온실의 규모에 따라 각각의 방법에는 큰 차이가 있으므로 보다 정확히 국내에 적용할 수 있는 방법을 정립할 필요가 있다. 본 연구에서는 원예시설의 환경설계 중 난방부하 산정방법 정립에 필요한 기초자료를 제공할 목적으로 다양한 종류의 보온커튼을 설치한 단동 및 연동 플라스틱 온실에서 추적가스법을 이용하여 틈새환기율을 실측하였으며, 온실의 틈새환기 전열부하 산정방법을 검토하였다. 연동온실의 틈새환기율은 $0.042{\sim}0.245h^{-1}$의 범위로 측정되었으며 단동온실의 틈새환기율은 $0.056{\sim}0.336h^{-1}$의 범위로 측정되어 단동온실이 약간 큰 것으로 나타났다. 온실의 틈새환기율은 단동, 연동 구분없이 보온커튼의 층수에 따라 크게 감소하는 것으로 나타났다. 또한 틈새환기율은 온실의 실내외 기온차가 커질수록 증가하는 경향을 보였으나, 실험기간 동안의 낮은 풍속 범위에서 외부 풍속에 따른 틈새환기율의 변화는 일정한 경향을 찾을 수 없었다. 온실의 난방설계를 위한 틈새환기율은 적정 실내외 기온차에서의 값을 제시할 필요가 있고, 최대난방부하 산정의 기준이 되는 낮은 풍속 범위에서 풍속에 따른 틈새환기율의 변화는 고려하지 않아도 되는 것으로 고찰되었다. 다만 강풍지역에서는 열관류율을 포함하여 최대난방부하를 약간 증가시키는 보정계수의 적용이 필요할 것으로 판단되었다. 온실의 틈새환기전열부하 산정방법을 검토한 결과 틈새환기전열계수와 온실의 피복면적을 이용하는 방법은 문제가 있는 것으로 나타났으며, 틈새환기율과 온실의 체적을 이용하는 방법이 합리적인 것으로 판단되었다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2021년도 학술발표회
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• pp.130-130
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• 2021

The increasing effect of urbanization has been more apparent through flooding and downstream water quality especially from heavy rainfalls. In response, stormwater runoff management solutions have focused on runoff volume reduction and treatment through infiltration. However, there are areas with low infiltration soils or are experiencing more dry days and even drought. In this study, a lab-scale infiltration system was used to compare the applicability of two types of soil as base layer in gravel-filled infiltration systems with emphasis on runoff capture and suspended solids removal. The two types of soils used were sandy soil representing a high infiltration system and clayey soil representing a low infiltration system. Findings showed that infiltration rates increased with the water depth above the gravel-soil interface indicating that the available depth for water storage affects this parameter. Runoff capture in the high infiltration system is more affected by rainfall depth and inflow rates as compared to that in the low infiltration system. Based on runoff capture and pollutant removal analysis, a media depth of at least 0.4 m for high infiltration systems and 1 m for low infiltration systems is required to capture and treat a 10-mm rainfall in Korea. A maximum infiltration rate of 200 mm/h was also found to be ideal to provide enough retention time for pollutant removal. Moreover, it was revealed that low infiltration systems are more susceptible to horizontal flows and that the length of the structure may be more critical that the depth in this condition.

• Geomechanics and Engineering
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• 제1권1호
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• pp.35-52
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• 2009

A significantly thick zone of steep slopes is commonly encountered above groundwater table and the soils within this zone are unsaturated with negative pore-water pressures (i.e., matric suction). Matric suction contributes significantly to the shear strength of soil and to the factor of safety of unsaturated slopes. However, infiltration during rainfall increases the pore-water pressure in soil resulting in a decrease in the matric suction and the shear strength of the soil. As a result, rainfall infiltration may eventually trigger a slope failure. Therefore, understanding of shear strength characteristics of saturated and unsaturated soils under shearing-infiltration (SI) conditions have direct implications in assessment of slope stability under rainfall conditions. This paper presents results from a series of consolidated drained (CD) and shearing-infiltration (SI) tests. Results show that the failure envelope obtained from the shearing-infiltration tests is independent of the infiltration rate. Failure envelopes obtained from CD and SI tests appear to be similar. For practical purposes the shear strength parameters from the CD tests can be used in stability analyses of slopes under rainfall conditions. The SI tests might be performed to obtain more conservative shear strength parameters and to study the pore-water pressure changes during infiltration.

• Membrane and Water Treatment
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• 제10권1호
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• pp.67-74
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• 2019

Apparent changes in the natural hydrologic cycle causing more frequent floods in urban areas and surface water quality impairment have led stormwater management solutions towards the use of green and sustainable practices that aims to replicate pre-urbanization hydrology. Among the widely documented applications are infiltration techniques that temporarily store rainfall runoff while promoting evapotranspiration, groundwater recharge through infiltration, and diffuse pollutant reduction. In this study, a laboratory-scale infiltration device was built to be able to observe and determine the factors affecting flow variations and corresponding solids removal through a series of experiments employing semi-synthetic stormwater runoff. Results reveal that runoff and solids reduction is greatly influenced by the infiltration capability of the underlying soil which is also affected by rainfall intensity and the available depth for water storage. For gravel-filled structures, a depth of at least 1 m and subsoil infiltration rates of not more than 200 mm/h are suggested for optimum volume reduction and pollutant removal. Moreover, it was found that the length of the structure is more critical than the depth for applications in low infiltration soils. These findings provide a contribution to existing guidelines and current understanding in design and applicability of infiltration systems.

• 한국습지학회지
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• 제22권2호
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• pp.145-152
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• 2020

고속도로는 많은 자동차 운행대수와 함께 높은 주행속도 및 급격한 주행속도 변화구간(휴게소, 영업소 등)으로 인하여 비점오염물질의 배출이 높은 지역에 해당한다. 국내 고속도로는 절토층 및 성토층에 조성됨으로써 적정 토양침투량 확보가 어려워 다양한 종류의 비점오염저감시설이 설치되지 못하고 있다. 본 연구는 토양치환 기법에 대한 연구를 통해 고속도로에 설치 가능한 시설의 종류를 확대하고 비용효율적 침투시설의 설계를 유도하기 위하여 수행되었다. 침투율이 낮은 원지반에 토양치환을 수행할 경우 시설 내 체류시간이 약 30% 지연되고, 시설 내 침투 및 저류율은 약 20% 증대하며, 비점오염물질 Total Suspend Soiled (TSS), Chemical Oxygen Demand (COD), Biological Oxygen Demand(BOD), Total Nitrogen(TN) 및 Total Phosphorus(TP) 제거효율이 약 20% 증가하는 것으로 나타났다. 원지반 내 침투율이 낮은 곳에 토양치환을 수행할 경우 저류량, 체류시간 및 침투면적이 증가하여 침투율이 향상되는 것으로 나타났다. 원지반 토양의 침투능이 낮은 토양에 침투시설을 적용하기 위해서는 물환경보전법 시행규칙 별표17(비점오염저감시설의 설치기준)의 개선이 필요하며, 이 경우 토양 침투율이 시간당 13 mm 이하일 때 토양치환을 통해 법적 처리용량을 확보하도록 요구할 수 있다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2000년도 추계학술대회
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• pp.74-77
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• 2000

Infiltration and water flow in the upper soil layer of a deep water table aquifer are modeled for multistorm runoff events. The infiltration process is developed using the sharp wetting front model of Green and Ampt, and the following redistribution process is modeled using the gravity drained rectangular approximation. The Brooks-Corey model [Brooks and Corey, 1966] is adopted to relate the effective soil saturation, the tension head, and the unsaturated hydraulic conductivity Firstly, the infiltration and redistribution model is developed for a single stom runoff event. Then a couple of events combined for multistorm runoff events. In the later case, infiltration rate of the second rainfall is strongly influenced by the length of the rainfall hiatus and soil moisture profile.

• 한국분말재료학회지
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• 제6권1호
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• pp.36-41
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• 1999

The present work has attempted to investigate the dependence of Cu infiltration kinetics on in-situ structure modification of W powder skeleton in W-Cu system. In-situ structure modification of W skeleton by addition of 0.3wt%Ni-P eutectic alloy was designed to proceed during heat-up of the W compact for Cu infiltration process. It was found that the Ni-P added W skeleton underwent remarkable stucture change only during heating-up. its structure was composed of large necks of W particles above 0.5 in the ratio of neck to particle size and smooth pore channels. The infiltration experiment showed that the infiltration kinetics for the W-Ni-P followed well the linear relationship of h vs. $t^{1/2}$ the rate constant K of which was in good agreement with the theoretical value. On the other hand, in case of the pure W skeleton a lower K value by 20% than the theoretical one was obatined. Such discrepancy is discussed in terms of skeleton structure induced infiltration mechanics.