• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2004.04a
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• pp.426-430
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• 2004

현재 복원사업이 진행 중인 서울시 청계천은 상류와 하류에서 하천의 유량이나 하폭 등에서 서로 다른 특성을 보인다. 본 연구에서는 청계천 상류와 하류에서의 지하수 유동을 모델링을 통하여 해석하였다. 그 결과 청계천 상류에서는 하천과 지하수면이 서로 분리되어 있는 분리손실하천의 형태를 보이는 반면, 청계천 하류에서는 하천과 지하수면이 서로 연결되어 있는 연결손실하천의 형태로 나타났다. 또한, 본 연구에서는 지하수 모델링 결과를 이용하여 하천-지하수의 상호작용을 zone analysis 통하여 분석하였다. 청계천 상, 하류 모두 대수층으로 유입되는 대부분의 물이 하천에서 오지만, 하류에서는 대수층에서 하천으로도 물이 유출되는 것을 확인할 수 있었다. 그 외에도 zone analysis의 결과는 손실하천에서의 유량 확보 또는 유지를 위한 계획을 구상하는 데에 있어서 중요한 지표를 제시해줄 수 있다.

• Journal of Soil and Groundwater Environment
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• v.7 no.4
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• pp.17-23
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• 2002

Pumping tests were carried out from seven wells in fractured rocks. The time-drawdown data were obtained from pumping wells and corrected for the elapsed time of step drawdown test using Cooper-Jacob's method. A statistical method. the least square of error, was used to yield the coefficient of aquifer losses, the coefficient of well losses, and the power which indicates the severity of the turbulence. The values of the power range from 1.65 to 6.48. The well losses result mainly from turbulent flow caused by radial flow nearby pumping wells. The turbulent flow depends on Reynolds number. Since the hydraulic characteristics of fractured rocks control the fluid velocity, the value of the power is an important factor to understand the aquifer system of fractured rocks.

• Economic and Environmental Geology
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• v.30 no.5
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• pp.433-442
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• 1997

A dual-permeability fractal model of fluid flow is proposed. The model simulates groundwater flow in fissured dual aquifer system composed of Aquifer 1 and Aquifer 2. For this model. groundwater flow originates only from Aquifer 1 on the pumping well. The model considers wellbore storage and skin effects at the pumping well and then shows exact drawdown at the early time of pumping. Type curves for different flow dimensions and for two cases are presented and analyzed. The case 1 represents the aquifer system which consists of Aquifer 1 with low permeability and high specific storage and Aquifer 2 with high permeability and low specific storage. The case 2 is inverse to the case 1. Dimensionless drawdown curves in Aquifer 1 and Aquifer 2 shows characteristic trend each other. Consequently, the model will be useful to analyze pumping test data of different draw down patterns on the pumping well and observation wells.

• Journal of Life Science
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• v.27 no.9
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• pp.1086-1095
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• 2017

There is growing interest in groundwater resources to overcome the loss of surface water resources due to climate change. An understanding of the microbial community of aquifers is essential for monitoring and evaluating groundwater contamination, as well as groundwater management. Most microorganisms that inhabit aquifer ecosystems are attached to sediment particles rather than planktonic, as is the case in groundwater. Since sampling aquifer sediment is not easy, groundwater, which contains planktonic microorganisms, is generally sampled in microbial community research. Although many studies have investigated microbial communities in contaminated aquifers, there are only a few reports of microbial communities in uncontaminated or pristine aquifers, resulting in limited information on aquifer microbial diversity. Such information is needed for groundwater quality improvement. This paper describes the ecology and community structure of groundwater bacteria in uncontaminated aquifers. The diversity and structures of microbial communities in these aquifers were affected by the concentration or distribution of substrates (e.g., minerals, organic matter, etc), in addition to groundwater characteristics and human activities. Most of the microbial communities in these uncontaminated aquifers were dominated by Proteobacteria. Studies of microbial communities in uncontaminated aquifers are important to better understand the biogeochemical processes associated with groundwater quality improvement. In addition, information on the microbial communities of aquifers can be used as a basis to monitor changes in community structure due to contamination.

• Proceedings of the Korea Water Resources Association Conference
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• 2005.05b
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• pp.743-748
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• 2005

김남원 등(2004a, b)에 의해 개발된 SWAT-MODFLOW 모형은 SWAT 모형과 MODFLOW 모형의 Recharge Package와 River Package를 직렬로 연결한 모형이다. 그러나 MODFLOW 모형에는 지하수 흐름방정식의 해석에 관련된 Package를 제외하더라도 Well, Drain, Evapotranspiration 등의 Package가 더 있어 대수층으로부터의 우물의 함양과 배출, 배수관을 통한 지하수의 배출, 지하수의 증발산으로 인한 손실 등을 수행할 수 있다. MODFLOW 모형의 Well Package는 SWAT 모형에서 대수층의 물이동, Drain Package는 SWAT 모형의 토관배수, Evapotranspiration Package는 SWAT 모형의 얕은 대수층에서의 증발산과 밀접한 관계가 있다. 본 연구에서는 이들 세 개의 Package를 SWAT 모형과 완전 연동시킴으로써 사용자가 좀 더 다양한 조건에 대하여 SWAT-MODFLOW 결합모형을 적용할 수 있도록 기능을 향상시켰다.

• The Journal of Engineering Geology
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• v.34 no.2
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• pp.217-228
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• 2024

During deep drilling, confined aquifers can present various challenges such as the inability to remove cuttings, rapid groundwater influx, and mud loss. Particularly in flowing well conditions, it is essential to apply the suitable mud density since the aquifer can generates an overpressurized condition. This paper proposes a method for determining the suitable mud density while drilling (SMD) through confined aquifers using mud window analysis and applies it to a case study. The minimum mud density at each depth, which represents the lower limit of the mud window, is determined by the equivalent mud density pore pressure gradient (or by adding a trip margin) at that depth. The pore pressure gradient of a confined aquifer can be calculated using the piezometric level or well head pressure of the aquifer. As the borehole reaches the confined aquifer, there is a significant increase in pore pressure gradient, which gradually decreases with increasing depth. The SMD to prevent a kick can be determined as the maximum value among the minimum mud densities in the open hole section. After entering the confined aquifer, SMD is maintained as the minimum mud density at the top of the aquifer during the drilling of the open hole section. Additionally, appropriate casing installation can reduce the SMD, minimizing the risk of mud loss or invasion into the highly permeable aquifer.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2003.09a
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• pp.206-209
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• 2003

hillslope에서 하천주위에 수리적으로 연관된 대수층의 지하수 수위와 하천수위는 그 수리경사의 방향에 따라서 이득하천과 손실하천으로 구분되며 이득하천이라도 홍수 시 손실하천으로 역전될 수 있다. 이러한 현상은 hillslope에서 기저유출의 발생여부를 좌우한다. 시간에 따른 하천의 수리경사 변화곡선으로 기저유출의 기여도와 지하수-하천수 수위곡선을 이용하여 그 양상을 비교하였다. 전라남도 곡성군 삼기천 소유역에서 연구기간 중 지하수관측지점에서 기저유출의 기여도는 37.4%이며 지하수-하천 수위곡선의 변화양상은 시계방향이다.

• The Journal of Engineering Geology
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• v.4 no.2
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• pp.127-138
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• 1994

The stationary dual-porosity model is not sufficient to describe the hydraulic characteristics of fractured aquifers as the groundwater flow in fractured aquifers is often controlled by the fractal geometry of fractures. This study deals with new stationary dual-porosity fractal model. This model simulates pseudo-steady state flow from matrix block to fissure in the fractal aquifer. Furthermore, it considers storage capacity and well loss effect at the production well. Type curves for different flow dimensions with different drainage factors are plotted. This new model has been applied to experimental data. The result of the interpretation shows a good accordance between the theoretical model and the observed data.

• The Journal of Engineering Geology
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• v.4 no.3
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• pp.283-295
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• 1994

A new nonstationary dual-porosity fractal model is presented which simulates a nonsteady state block-to-fissure flow with or without fracture skin between the block and the fissure in a fractal aquifer. The model includes weilbore storage and well loss effects on the production well. Type curves for different flow dimensions with different values of hydraulic parameters are created. The application of the model to experimental data in fractured aquifer is described.

• Journal of Nuclear Fuel Cycle and Waste Technology(JNFCWT)
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• v.10 no.1
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• pp.1-11
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• 2012

The equation of the step-drawdown test "$s_w=BQ+CQ^p$" written by Rorabaugh (1953) is suitable for drawdown increased non-linearly in the fractured rocks. It was found that value of root mean square error (RMSE) between observed and calculated drawdowns was very low. The calculated $C$ (well head loss coefficient) and $P$ (well head loss exponent) value of well head losses ($CQ^p$) ranged $3.689{\times}10^{-19}{\sim}5.825{\times}10^{-7}$ and 3.459~8.290, respectively. It appeared that the deeper depth in pumping well the larger drawdowns due to pumping rate increase. The well head loss in the fractured rocks, unlike that in porous media, is affected by properties of fractures (fractures of aperture, spacing, and connection) around pumping well. The $C$ and $P$ value in the well head loss is very important to interpret turbulence interval and properties of high or low permeability of fractured rock. As a result, regression analysis of $C$ and $P$ value in the well head losses identified the relationship of turbulence interval and hydraulic properties. The relationship between $C$ and $P$ value turned out very useful to interpret hydraulic properties of the fractured rocks.