• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 총회 및 춘계학술발표회
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• pp.492-494
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• 2004

The purpose of this study is to investigate the hydrochemical characteristics of groundwater in the Umsung area, and to elucidate the effect of host rock type, well depth and mineralization zone on the groundwater chemistry, We carried out chemical analysis, isotopic analysis, statistical analysis of Box-Whisker and trigging analysis for this study. The chemical and isotopic compositions of the groundwater is distinguished into two areas according to host rocks(Cretaceous sedimentary rocks and Jurassic granite) and recharge altitude, and is not greatly influenced by mineralization zone of the mines.

• 상하수도학회지
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• 제28권1호
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• pp.61-72
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• 2014

Study on effluent organic matter (EfOM) characteristic and removal efficiency is required, because EfOM is important in regard to the stability of effluents reuse, quality issues of artificial recharge and water conservation of aqueous system. UV technology is widely used in wastewater treatment. Many reports have been conducted on microbial disinfection and micro pollutant reduction with UV treatment. However, the study on EfOM with UV has limited because low/medium pressure UV lamp is not sufficient to affect refractory organics. The high intensity of pulsed UV would mineralize EfOM itself as well as change the characteristics of EfOM. Chlorine demand and DBPs formation is affected on the changed amounts and properties of EfOM. The objective of this study is to investigate the effect on EfOM, chlorine residual, and chlorinated DBPs formation with low pressure and pulsed UV treatment. The removal of organic matter through low pressure UV treatment is insignificant effect. Pulsed UV treatment effectively removes/transforms EfOM. As a result, the chlorine consumption is changed and chlorine DBPs formation is decreased. However, excessive UV treatment caused problems of increasing chlorine consumption and generating unknown by-products.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2012년도 학술발표회
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• pp.944-944
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• 2012

Urbanization leads to a change of hydrologic responses because impervious area is increased by urbanization. Decrease of groundwater recharge and increase of overland flow are general hydrologic characteristics caused by urbanization. This can be a source of damages such as increased flooding and reduced groundwater levels. Daily streamflow in Gabcheon watershed, South Korea is simulated by ARCSWAT model, an extension of SWAT2005. After calibration and validation of model, the simulated daily streamflow from 1997 to 2001 are statistically analyzed. The phenomenon that $T_{Qmean}$ is inversly proportional to coefficient of variation for the simulated daily streamflow is demonstrated. Also, hydrologic response was more influenced by weather than land use for high flow. This study also examines the effect of land use change on daily streamflow with spatially and quantitatively different land use maps. The simulated stream flow is tested by Mann-Whitney method. The median between stream flows simulated for 1990 and 2000 land use maps is significantly different, but the simulated streamflow for spatially different land use maps is almost unchanged.

• 한국농공학회논문집
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• 제54권1호
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• pp.55-62
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• 2012

This study is to assess the reduction of nonpoint source pollution by applying Best Management Practice (BMP) in Chungju-dam watershed (6,585.1 $km^2$) using Soil and Water Assessment Tool (SWAT). The model was calibrated using 3 years (1998-2000) daily streamflow at 3 locations and monthly water quality of sediment (SS), total nitrogen (T-N) and total phosphorus (T-P) data at 2 locations and validated for another 3 years (2001-2003) data. The 5 BMPs of streambank stabilization, porous gully plugs, recharge structures, terrace, and contour farming were applied to stream and area with the specific criteria of previous researches. Through the parameter sensitivity analysis, the farming practice P-factor and Manning's roughness of stream were sensitive. Overall, the NPS reduction effect was high for streambank stabilization, terrace, and contour farming. At the watershed outlet, the SS, T-P, and T-N were reduced by 64.4 %, 62.8 % and 17.6 % respectively.

• Advances in concrete construction
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• 제8권4호
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• pp.305-309
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• 2019

Pervious concrete pavements are the need of the day to avoid urban flooding and to facilitate ground water recharge. However, the strength of pervious or porous concrete is considerably less compared to conventional concrete. In this experimental investigation, an effort is made to improve the strength of pervious concrete by adopting fibres and a small amount of fine aggregate. A porous concrete with cement to aggregate ratio of 1:5 and a water-powder ratio of 0.4 is adopted. 30% of the cement is replaced by cementitious material ground granulated blast furnace slag (GGBS) for better strength and workability. Recron fibres at a dosage of 0.5, 1.0 and 1.5% by weight of cement were included to improve the impact strength. Since concrete pavements are subjected to impact loads, the impact strength was also calculated by "Drop ball method" in addition to compressive strength. The effect of fine aggregate and recron fibres on workability, porosity, compressive and impact strength was studied. The investigations have shown that 20% inclusion of fine aggregate and 1.5% recron fibres by weight of cement give better strength with an acceptable range of porosity.

• 한국물환경학회지
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• 제24권1호
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• pp.107-117
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• 2008

Infiltration facilities are effective instruments to mitigate flood and can increase base runoff in urban watersheds. In order to analyze effects of infiltration trenches physical model experiments were conducted. The physical model facility consists of two soil tanks, artificial rainfall generators, tensiometers, and piezometers. The experiment was conducted by nine times and each case differed in rainfall intensity, rainfall duration and the type of ground surface. Measured quantities in the experiments are as follows: surface runoff, subsurface runoff, trench pipe runoff, groundwater level, water content, etc. The following resulted from the model experiment: The volume of subsurface runoff at trench watershed was maximum 78.3% compared with rainfall. This value is bigger than that of ordinary rate of subsurface runoff, and shows a groundwater recharge effect of trench. The time of runoff passing through the trench became earlier and the volume of runoff became larger with the increase of inflow into the trench, while trench exfiltration into ground became relatively smaller. The results of this study presented above show that infiltration trenches are effective instruments to increase base runoff during dry periods.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2020년도 학술발표회
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• pp.290-290
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• 2020

연구지역인 충청남도 홍성군 갈산면 신곡마을은 상시 가뭄지역으로서 농번기 물부족을 겪고 있으며, 물 확보의 수단으로서 지하수 인공함양이 고려되고 있다. 본 연구에서는 수치모델을 이용하여 수직정 방식의 지하수 인공함양시 주입 효과를 예비 평가하였다. 모델 지역은 가로 세로 2,450 × 2,350 m로서 10 × 10 m 간격의 격자로 구성하였으며, 현장에서 실시된 지하수위 조사 및 9공의 시추조사, 1개공의 양수시험 결과로부터 수리전도도, 지층분포 등을 구성하였다. 정류모델결과, 실측 및 예측 지하수위의 표준오차(Standard error of the estimate)는 0.53 m, 표준화제곱근오차(Normalized RMS)는 6.79%, 상관계수는 0.99%로 나타났다. 수직정을 통한 주입 효과를 평가하기 위하여, 주입량을 5 ㎥/d, 10 ㎥/d, 15 ㎥/d, 20㎥/d, 주입기간을 1일, 3일, 7일, 우물의 개수를 1개, 3개, 5개일 때 등 다양한 조건하에서의 부정류 모델을 수행하였다. 이로부터 주입의 효과인 지하수위 상승량 및 상승 범위 등을 토대로 물 부족 기간의 인공함양 시나리오(주입정의 위치, 갯수, 심도, 기간 등)를 예비적으로 제시하였으며, 추후 정밀 모델 및 실제 현장 주입 시험 등을 토대로 인공함양 설계를 추진할 예정이다.

• 물과 미래
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• 제16권4호
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• pp.245-252
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• 1983

근년에 이르러 국내 지표수의 오염 현상은 사회적으로 매우 심각한 문제를 야기시키고 있어 수자원의 보호문제가 매우 중요한 시점에 이르렀다. 한강유역내에 발달 분포된 천층의 충적 퇴적층과 결정질암내에 저유된 지하수에 대해 동위원소를 이용한 환경 조사를 시행하였으며 결과를 분석한 바 다음과 같은 가정을 확인하였다. 1) 천층지하수의 함양원은 서울 도심지역은 하천수였고, 교외 외각의 농촌 지역은 강우의 직접 지하 침투에 의해 일어나고 있으며, 2) 충적 퇴적층으로 피복된 결정질 암은 상부충적퇴적층내에 저유된 천층 지하수가 충진원의 역할을 한다. 한강하류부의 해안 가까운 곳에 분포된 일부 충적층과 그 하부의 결정질암내에 저유된 지하수는 $H^3$의 함량이 매우 낮은치를 나타내는데 이는 핵실험이전의 기상수가 상당히 먼곳에서 충진되었기 때문으로 시료된다. 안정동위원소 조사에 의하면 한강상류에 분포된 석회암 대수층의 함양지역은 하류부의 충적층과는 달리 비교적 고지대였으며 석회암 대수층내에서 지하수의 체제 시간은 수개월 정도였다. 지하수의 포함된 극소량의 Pb, Mn, Zn 량과 충진메카니즘을 대비하려고 시도하였으나 명확한 관계가 나타나지 않았다.

• 한국지반환경공학회 논문집
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• 제18권5호
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• pp.35-43
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• 2017

지하수위 저하를 방지하기 위한 방법으로 지반 굴착에 따라 배출된 지하수를 대상 지반에 다시 재주입함으로써 흙막이 벽체 배면의 지반함몰 및 침하를 방지하는 방법에 관한 연구이다. 지하수 재주입에 따른 흙막이 벽체 배면의 지반함몰 및 침하를 분석하기 위해 지하수 재주입 여부와 흙막이 벽체 배면으로부터 거리 등 조건을 달리하며 재주입정 위치별 효과를 확인할 수 있는 실내모형실험을 수행하였다. 실험을 통해 지하수위에 영향을 미치는 인자와 흙막이 벽체 배면의 지반함몰 및 침하경향을 분석하고, 지하수 재주입에 따른 지반함몰 방지효과에 대한 연구를 수행하였다. 지하수위의 영향을 고려한 침하분석 결과, 흙막이 전면을 굴착할 때 지하수위 저하에 따라 지표면 침하가 발생, 흙막이 벽체 배면에서 최대가 된다. 또한 흙막이 길이를 기준으로 흙막이 벽체 배면으로부터 재주입정 위치별 거리 비에 따라 침하량이 달라지는 것으로 분석되었다. 지하수의 영향에 의한 지반함몰 및 침하를 방지하기 위한 방법으로 흙막이 벽체 배면으로부터 가까운 위치에 지하수를 재주입 할 때 지반함몰 및 침하 방지 효과가 크고 최대 침하영향거리도 감소하는 것으로 분석되어 지하수 재주입정 공법의 지반함몰 방지효과를 확인하였다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.121-121
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• 2004

The groundwater in the Pocheon area occurs from both a fractured bedrock aquifer in igneous and metamorphic rocks and an alluvial aquifer with a thickness of <50 m, and forms a major source of domestic and agricultural water supply. In this study, we performed a hydrogeochemical study in order to identify the control of geochemical processes on groundwater quality. For this study, groundwater level and physicochemical parameters (EC, Eh, pH, alkalinity) were monitored once a month from a total of 150 groundwater wells between June 2003 to August 2004. A total of 153 water samples (13 surface water, 66 alluvial groundwater, 74 bedrock groundwater) were also collected and analyzed in February 2004. Groundwater chemistry in the study area is very complex, depending on a number of major factors such as geology, degree of chemical weathering, and quality of recharge water. Hydrochemical reactions such as the leaching of surficial and near-solace soil salts, dissolution of calcite, cation exchange, and weathering of silicate minerals are proposed to explain the chemistry of natural groundwater. Alluvial groundwaters locally have very high TDS concentrations, which are characterized by their chloride(nitrate)-sulfate-bicabonate facies and low Na/Cl ratio. Their grondwater levels are highly fluctuated according to rainfall event. We suggest that high nitrate content and salinity in such alluvial groundwaters originates from the local recharge of sewage effluents and/or fertilizers. Likewise, high concentrations of nitrate were also locally observed in some bedrock groundwaters, suggesting their effect of anthropogenic contamination. This is possibly due to the bypass flow taking place through macropores. Tile degree of the weathering of silicate minerals seems to be a major control of the distribution of major cations (sodium, calcium, magnesium, potassium) in bedrock groundwaters, which show a general increase with increasing depth of wells. Thermodynamic interpretation of groundwater chemistry shows that the groundwater in the study area is in chemical equilibrium with kaolinite and Na-montmorillonite, which indicates that weathering of plagioclase to those minerals is a major control of hydrochemistry of bedrock groundwater. The interpretation of the molar ratios among major ions, as well as the mass balance calculation, also indicates the role of both dissolution/precipitation of calcite and Ca-Na cationic exchange as bedrock groundwaters evolves progressively.