• 한국물환경학회지
• /
• 제22권3호
• /
• pp.546-556
• /
• 2006

The purpose of this study is to improve the polluted stream water quality by pilot-scale five different constructed wetlands (CWs). Cell 1 to 3 are newly designed 2SFCW (Surface-subsurface flow CW) with 1 to 3 flow shifters (FS) in the middle of the wetland system. Cell 4 and 5 are control CW (CCW), but Cell 5 is the same type as Cell 3. The FS, which converts the route of surface and subsurface flow between two wetlands connected in series, was able to enhance the treatability of TN via nitrification and denitrification and of SS due to filtration and sedimentation. The void fraction and dispersion number of Cell 1, 2 and 3 obtained from the RTD analysis were found to be 0.73 and 0.17, respectively. COD and TP removal efficiencies of Cell 1 to 3 were similar to that of Cell 4 and 5. SS removal efficiencies of Cell 1 to 3 and 5 with FS were 5-10% higher than that of Cell 4 without FS. TN removal efficiencies of Cell 1 to 3 were 3-14% higher than that of Cell 4 and 5. The average $R^2$ values of COD, SS, TN and TP obtained from nonlinear regression analysis were similar to the results of other researchers.

• 한국정밀공학회:학술대회논문집
• /
• 한국정밀공학회 2008년도 추계학술대회 논문집
• /
• pp.583-584
• /
• 2008

• 한국정밀공학회:학술대회논문집
• /
• 한국정밀공학회 2008년도 춘계학술대회 논문집
• /
• pp.847-848
• /
• 2008

• 한국토양비료학회지
• /
• 제45권5호
• /
• pp.683-689
• /
• 2012

본 연구는 시설 하우스 재배에서 지중관수 호스 간격 처리가 상추의 무기성분 함량과 흡수량, 수량, 관수량 및 토양화학성에 미치는 영향을 알아보기 위하여 수행되었다. 상추재배는 반촉성 및 억제재배를 하였으며 시험처리는 분수살수 처리와 지중 호스를 30 cm 깊이에 호스의 배치 간격이 각각 30, 40 및 50 cm 되도록 한 지중관수 처리를 포함하여 총 4처리를 하였다. 지중관수 처리에 의한 상추의 무기성분 함량은 처리간에 차이가 없으나 양분 흡수량은 호스 간격 50 cm 처리에서 가장 낮았다. 수량은 50 cm $\leq$ 분수살수 $\leq$ 40 cm $\leq$ 30 cm 순으로 많았고 관수량은 분수살수 처리가 가장 많았으며 지중관수 처리 간격이 넓을수록 적었다. 토양 양분함량 중 지표 하 10 cm에서 질산태 질소는 50 cm> 40 cm> 분수살수> 30 cm 처리 순으로 많았으며 치환성 칼리함량은 50 cm 처리에서, 마그네슘 함량은 40 cm에서 높았고 칼슘은 30 cm 처리에서 낮았다. 결과적으로 상추 재배에서 지상 분수살수와 지중 점적관수 30 cm 깊이에서 30~40 cm 간격 처리는 수량 차이가 없었으나 관수량은 지중관수에서 호스 간격이 넓을수록 적었다. 지중관수에서 작물의 수량 및 토양 중 양분 변화는 호스의 깊이와 점적기 및 호스간격, 토성에 따른 물의 이동과 작물의 양분 반응에 따라 차이가 있을 수 있어 보다 정밀한 연구가 필요한 것으로 생각되었다.

• 한국농림기상학회지
• /
• 제1권2호
• /
• pp.160-164
• /
• 1999

현재 지구상에서 농업에 기인하여 배출되는 $N_2$O의 80% 정도가 지구의 온난화 뿐만 아니라 오존층 파괴에까지 영향을 미친다. 토양에서 수분함량 등과 관련한 유기태 탄소는 지하수면의 계절적 변화에 따라 탈질화를 결정하는 주요 요인이 되기도 하며 심층토의 탈질화 활동은 토양내 유기물을 분해하여 유기태 질소를 일시적으로 토양에 축적시키기도 한다. 그리고 토양의 관리방법, 폐기물의 토양처리, 질소질 비료의 시용 등이 $N_2$O 증가에 결정적 요인이 되기도 한다. 그러나 이러한 효과의 정도는 거의 알려져 있지 않을 뿐만 아니라 질산화나 탈질화와 같은 상반되는 과정과 제한 요소와 관련하여 범용적으로 적용할 수 있는 $N_2$O 방출을 예측하는 측정 계수와 같은 연구는 매우 미미한 상태이다. 그러므로 농업토양에서 비료와 유기물 시용 둥에 의해 발생하는 토양의 $N_2$O배출을 효율적으로 관리하기 위하여 심층토에서의 동적 역학적 $N_2$O 배출 측정과 관리 방법을 개발하여야 한다.

• 환경영향평가
• /
• 제10권2호
• /
• pp.99-108
• /
• 2001

This study was performed to develop an information processing system for the sound conservation of soil and groundwater resources. The system contains numerical models and geographic information systems for underground flow and contamination. Multidimensional Finite Element Model for Subsurface Environment (MFEMSE) was invented to analyze underground flow and pollution problems of water and gas phases. Newly developed and conventional models (MODFLOW, MOC3D, MT3D, PMPATH, PEST, UCODE) were integrated with GIS (ArcView) for the construction of an integrated information management system of subsurface environment. This system was applied to the management of three mineral water companies located in clean high mountain basin. Desirable management criteria and operational strategies were suggested using this system. The system was constructed to be applied for the broad sense of decision supporting tools in related topics of this study, so that it can be used not only for the prevention regulations, but also for clean up projects.

• 한국수자원학회논문집
• /
• 제34권4호
• /
• pp.403-411
• /
• 2001

본 연구에서는 지표하층과 암반층 사이의 지표하흐름을 기존 TOPMODEL의 구조에 연계시킨 수정 TOPMODEL의 국내 유역 적용성을 검증하였다. 지표하층에 존재하고 있는 대공극은 신속한 유출발생을 위한 수문경로를 제공하고 있으며, 수문감쇠곡선 분석을 위한 이중저류체계의 필요성을 의미한다. 설마천 유역을 대상으로 2개월간의 연속적인 유역수문거동을 모의한 결과 수정 TOPMODEL은 기존 TOPMODEL에 비해 유출발생과정을 모다 포괄적이고, 현실적으로 재현할 수 있는 것으로 밝혀졌다. Monte-Carlo 방법을 도입한 매개변수 산정결과도 수정 TOPMODEL의 경우가 물리적으로 타당한 것으로 밝혀졌다.

• 한국수자원학회:학술대회논문집
• /
• 한국수자원학회 2001년도 학술발표회 논문집(I)
• /
• pp.25-34
• /
• 2001

A grid-based KIneMatic wave soil-water EROsion and deposition Model (KIMEROM) that predicts temporal variation and spatial distribution of sediment transport in a watershed was developed. This model uses ASCII-formatted map data supported from the regular gridded map of GRASS (U.S. Army CERL, 1993)-GIS (Geographic Information Systems), and generates the distributed results by ASCIIl-formatted map data. For hydrologic process, the kinematic wave equation and Darcy equation were used to simulate surface and subsurface flow, respectively (Kim, 1798; Kim et al., 1993). For soil erosion process, the physically-based soil erosion concept by Rose and Hairsine (1988) was used to simulate soil-water erosion and deposition. The model adopts sing1e overland flowpath algorithm and simulates surface and subsurface water depth, and sediment concentration at each grid element (or a given time increment. The model was tested to a 162.3 km$^2$ watershed located in the tideland reclaimed area of South Korea. After the hydrologic calibration for two storm events in 1999, the results of sediment transport were presented for the same storm events. The results of temporal variation and spatial distribution of overland flow and sediment areas are shown using GRASS.

• Geomechanics and Engineering
• /
• 제22권5호
• /
• pp.375-384
• /
• 2020

In this study, the application of conventional cubic law to a deep depth condition was experimentally evaluated. Moreover, a modified equation for estimating the rock permeability at a deep depth was suggested using precise hydraulic tests and an effect analysis according to the vertical stress, pore water pressure and fracture roughness. The experimental apparatus which enabled the generation of high pore water pressure (< 10 MPa) and vertical stress (< 20 MPa) was manufactured, and the surface roughness of a cylindrical rock sample was quantitatively analyzed by means of 3D (three-dimensional) laser scanning. Experimental data of the injected pore water pressure and outflow rate obtained through the hydraulic test were applied to the cubic law equation, which was used to estimate the permeability of rock fracture. The rock permeability was estimated under various pressure (vertical stress and pore water pressure) and geometry (roughness) conditions. Finally, an empirical formula was proposed by considering nonlinear flow behavior; the formula can be applied to evaluations of changes of rock permeability levels in deep underground facility such as nuclear waste disposal repository with high vertical stress and pore water pressure levels.

• 한국지하수토양환경학회지:지하수토양환경
• /
• 제15권3호
• /
• pp.34-43
• /
• 2010

The fate of hydrophobic organic contaminants (HOCs) in ground water is highly affected by the distribution and property of the carbonaceous materials (CMs) in subsurface sediments. CMs in soils consist of organic matters (e.g., cellulose, fulvic acid, humic acid, humin, etc.) and black carbon such as char, soot, etc. The distribution and property of CMs are governed by source materials and geological evolution (e.g., diagenesis, catagenesis, etc.) of them. In this study, the distribution and property of CMs in subsurface sediments near the Imjin river in the Republic of Korea and HOC sorption property to the subsurface sediments were investigated. The organic carbon contents of sand and clay/silt layers were about 0.35% and 1.37%, respectively. The carbon contents of condensed form of CMs were about 0.13% and 0.45%, respectively. The existence of black carbon was observed using scanning electron microscopes with energy dispersive spectroscopy. The specific surface areas (SSA) of CMs in heavy fraction(HFrCM) measured with N2 were $35-46m^2/g$. However, SSAs of those HFrCM mineral fraction was only $1.6-4.3m^2/g$. The results of thermogravimetric analysis show that the mass loss of HFrCM was significant at $50-200^{\circ}C$ and $350-600^{\circ}C$ due to the degradation of soft form and condensed form of CMs, respectively. The trichloroethylene (TCE) sorption capacities of sand and clay/silt layers were similar to each other, and these values were also similar to oxidzed layer of glacially deposited subsurface sediments of the Chanute Air Force Base (AFB) in Rantoul, Illinois. However, these were 7-8 times lower than TCE sorption capacity of reduced layer of the Chanute AFB sediments. For accurate prediction of the fate of hydrophobic organic contaminants in subsurface sediments, continuous studies on the development of characterization methods for CMs are required.