• 터널과지하공간
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• 제13권6호
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• pp.465-475
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• 2003

본 논문은 지하공동이 건설되는 지역을 대상으로 공동내 지하수 유입량을 계산하기 위하여 영국의 AEA Technology에서 개발한 NAPSAC과 NAMMU를 이용하여 수치 모델링을 실시하였다. 이것은 3차원의 파쇄된 매질에서 지하수 유동에 대하여 아주 유효한 유한요소 소프트웨어 패키지이다. 모델링에 사용된 입력자료는 지표조사, 시추조사, 단일공 수리시험 자료 등을 이용하여 산출하였다. 공동내 지하수 유입량을 보다 정확히 산출하기 위하여 이방성 수리전도도를 고려하였으며 이방성 수리전도도값은 연구지역에 분포하는 균열체계의 확률적 분포특성이 반영된 균열망에서 역산되었다. 연속체 개념의 수치모델링을 통하여 평수기, 갈수기와 풍수기시의 지하 공동내 유입량, 유동시간, 유동경로의 변화를 계산하였다.

• Geomechanics and Engineering
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• 제21권2호
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• pp.165-170
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• 2020

The groundwater during tunnel excavation not only affects the stability of the tunnel and constructability but also causes the subsidence of the upper ground due to the lowering of groundwater. Generally, the cutoff grouting is applied as a countermeasure to reduce the groundwater inflow during tunnel excavation, and the cutoff grouting is often applied in the range of plastic zone around the tunnel. However, grouting in the plastic zone is only appropriate for ground reinforcement purposes, and guidelines for the application range of cutoff grouting and the targeted permeability coefficient of the grouting zone are required. In this study, the relationship between groundwater inflow into tunnel and application range of cutoff grouting and permeability coefficient is proposed and compared with numerical analysis results. It was found that grouting with tunnel radius thickness is appropriate to reduce the groundwater inflows effectively. More than 90% reduction in groundwater inflow can be achieved when the annular area of the tunnel radius thickness is grouted with a permeability reduction ratio of 1/50~1/200.

• Geomechanics and Engineering
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• 제13권4호
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• pp.671-683
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• 2017

Groundwater control is a significant issue in most underground construction. An estimate of the inflow rate is required to size the pumping system, and treatment plant facilities for construction planning and cost assessment. An estimate of the excavation-induced drawdown of the initial groundwater level is required to evaluate potential environmental impacts. Analytical and empirical methods used in current engineering practice do not adequately account for the effect of the jointed-rock-mass anisotropy and heterogeneity. The impact of geostructural anisotropy of fractured rocks on tunnel inflows is addressed and the limitations of analytical solutions assuming isotropic hydraulic conductivity are discussed. In this paper the unexcavated Zagros tunnel route has been classified from groundwater flow point of view based on the combination of observed water inflow and numerical modeling results. Results show that, in this hard rock tunnel, flow usually concentrates in some areas, and much of the tunnel is dry. So the remaining unexcavated Zagros tunnel route has been categorized into three categories including high Risk, moderately risk and low risk. Results show that around 60 m of tunnel (3%) length can conduit the large amount of water into tunnel and categorized into high risk zone and about 45% of tunnel route has moderately risk. The reason is that, in this tunnel, most of the water flows in rock fractures and fractures typically occur in a clustered pattern rather than in a regular or random pattern.

• Geomechanics and Engineering
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• 제12권6호
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• pp.1003-1020
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• 2017

Estimation of groundwater inflow into underground opening is of critical importance for the design and construction of underground structures. Groundwater inflow into a pilot underground storage facility in China was estimated using analytical equations, numerical modeling and field measurement. The applicability of analytical and numerical methods was examined by comparing the estimated and measured results. Field geological investigation indicated that in local scale the high groundwater inflows are associated with the appearance of open joints, fractured zone or dykes induced by shear and/or tensile tectonic stresses. It was found that 8 groundwater inflow spots with high inflow rates account for about 82% of the total rate for the 9 caverns. On the prediction of the magnitude of groundwater inflow rate, it was found that could both (Finite Element Method) FEM and (Discrete Element Method) DEM perform better than analytical equations, due to the fact that in analytical equations simplified assumptions were adopted. However, on the prediction of the spatial distribution estimation of groundwater inflow, both analytical and numerical methods failed to predict at the present state. Nevertheless, numerical simulations would prevail over analytical methods to predict the distribution if more details in the simulations were taken into consideration.

• 한국지하수토양환경학회지:지하수토양환경
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• 제26권6호
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• pp.130-143
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• 2021

Wetlands are one of the most representative groundwater dependent ecosystems(GDEs) that require access to groundwater on a permanent or intermittent basis to maintain their biological communities and ecological processes. In this study, the seasonal characteristics of the GDEs in Baekseok Reservoir Wetland were evaluated through the monitoring of the temporal and spatial community of benthic macroinvertebrates in the wetland. The appearance of benthic macroinvertebrates appearance was changed seasonally depending on environmental factors such temperature, precipitation and water level for their habitat and it also showed the clear spatial difference in the wetland. The scores of Diversity index(H'), Richness Index (R1) and the Ecological score of benthic macroinvertebrates (TESB/AESB) were relatively high at St.3 and 4(i.e., north area) where groundwater inflows into wetland(i.e., high ²²²Rn conc.). The statistical analysis (ANOVA test and PCA) investigated the correlation among the benthic macroinvertebrates' community, groundwater level, wetland water level and water quality. The results showed that the community of benthic macroinvertebrates at St. 3 and 4 in Baekseok Reservoir Wetlands was spatially dependent on groundwater level and groundwater inflow. The characterization and assessment of GDEs requires understanding the hydrological, biogeochemical and biological process and this study will provide information for characterization and assessment of GDEs.

• 지질공학
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• 제10권1호
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• pp.79-93
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• 2000

일반적으로 공동 주변에 분포하고 있는 지질구조는 지하 암반 공동 굴착시 지수, 보강, 지하수 유동 등에 상당한 영향을 주게 되므로 지질구조의 분포 및 특성을 아는 것이 매우 중요하다. 본 연구에서는 거제 지역에 기 시행된 지하 비축시설의 조사, 설계 및 시공자료를 토대로 지질구조와 공동 누수량 상호 관계를 분석한 결과, 본역에 발달하고 있는 주 함수구조대의 방향은 N50∼60W, 경사는 거의 수직이며 인장 단열로서 추정된다. 이 구조대는 양수 시험시 타원형의 장축 방향과 일치하고 N10∼30E 방향의 단열들과 교차하고 있으며, 화강섬록암에서 나타나는 전형적인 장방형 단열계를 나타낸다.

• 한국수자원학회논문집
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• 제40권6호
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• pp.431-446
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• 2007

지하수 유동 모델에 반영되는 유역의 수리지질학적, 수문학적 특징들은 지하수 유동 특성에 주요한 영향을 미칠 수 있는 현장 특성들이다. 상기 특징들을 최대한 반영하기 위하여 438개의 관정자료를 토대로 갑천 유역(유역 면적$648.3km^2$)의 대수층 구조 특성을 분석하고, 24개의 하천 자료를 이용하여 지하수 유동 모델을 구축하였다. 그리고 검 보정된 준분포형 유출모형(SWAT)의 소유역별 지하수 함양량 결과를 3차원 지하수 유동 모델(MODFLOW)과 연계하여 갑천 유역의 광역 지하수 유동 특성을 평가하였다. 모의된 지하수위와 86개 지하수 관측정의 지하수위 비교에서 결정계수는 0.99, 유역 전체의 물교환량의 상대오차율이 약 0.57%로 갑천 유역의 지하수 유동 특성을 잘 반영하였다. 갑천 유역의 지하수는 지형 및 대수층 특성과 하천의 영향에 의하여 전반적으로 유역 남쪽에서 북쪽으로 유동하는데 산지 지역에 존재하는 하천들은 손실과 이득 하천의 형태를 반복하는 반면, 갑천 중 하류 부분과 갑천-유등천 합류 부근은 이득하천의 형태를 보이고 있다. 그리고 소유역별 지하수 물교환량 분석한 결과, 상기 지역을 포함하는 소유역의 하천 공급원이 해당 유역의 지하수 함양량보다 지하수 유동 체계에 따라 인근 소유역에서 공급되는 지하수 유입량 비율이 훨씬 높은 것으로 분석되었다. 반면 유등천 중 상류 지역의 소유역을 제외한 산지 지역의 경우는 하천 공급원이 지하수 유동 체계에 의한 유입량보다 해당 유역 내에서 공급되는 지하수 함양량 비율이 높은 것으로 분석되었다. 따라서 지표수와 지하수의 상호작용 및 하천 유출에 지하수 유동 특성이 주요한 영향을 미치는 것으로 평가되었다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2001년도 총회 및 춘계학술발표회
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• pp.3-6
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• 2001

Various Parameters such as stream velocities, discharges, and dispersion coefficients of dissolved solutes were estimated by fitting 1-D nonreactive solute transport model to the time-series chemistry data. This study was done for the reaches of Mankyung River lower than the Jeonju Wastewater Treatment Plant (Jeonju WTP). Korea. Concentrations of inorganic chemicals in the stream waters are strongly influenced by mixing with the chemically distinct effluent from Jeonju WTP. Sulfate, EC. and the total major cation were proved to be nearly conservative in the study area front their relationships with chloride, the conservative chemical species. The solute transport model was constrained to the time-series concentrations for these 4 conservative species. The variations of concentration and discharge of Jeonju WTP were used as input parameters, and the stream velocities, dispersion coefficients, and concentrations and discharges of some inflows were optimized. The differences between the observed arid simulated values for alkalinities and nitrates are inversely correlated and show diurnal fluctuations, indicating the photosynthesis. The parameters obtained front this mode] range from 550 to 774 kcmd (stream discharge at the outlet of the study area), from 0.06 to 0.10 m/sec (flow velocity), and from 0.7 to 6.4 m$^2$/sec (dispersion coefficient). The history of Jeonju WTP discharge was well predicted when optimized, indicating the validity of the model results.

• 지질공학
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• 제20권2호
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• pp.147-153
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• 2010

투수성이 낮은 매질로 설치되는 차수벽(Cut-off wall)은 댐 지역 비상여수로 터널 지역에서 지하수의 흐름을 차단하기 위한 기능을 갖는다. 임하댐의 3개 비상여수로 터널 입구부에 차수벽 설치시 지하수 유입의 차단 효과를 평가하기 위하여 MODFLOW 모델링을 활용하였다. 규모와 설치 방향 등을 고려하여 3가지 차수벽 설치 방안이 검토되었는데, 모델링을 통하여 추정된 비상여수로 터널내로 유입되는 지하수량은 약 64.26~65.49 $m^3/day$이며, 이중에서 차수벽 구간을 통과하여 유입되는 지하수량은 약 44.08~45.31 $m^3/day$로서 방안별로 유사한 것으로 나타났다. 따라서, 본 연구지역에서는 방안별 차수 효과보다는 시공성, 환경파괴의 최소성 등을 고려하여 최적의 차수벽 설치 방안을 제안하였다.

• 한국물환경학회지
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• 제34권6호
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• pp.678-687
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• 2018

The purpose of this study was to understand the unique and complicated feature of urban stream receiving various inflows. The Yangjae stream, the second tier of the Han River, runs through the southern parts of Seoul, Korea and its middle part flows on the boundary of Seoul where land use is actively changing. Stream flow was greatly influenced by rainfall. Other than rainfall events, effluent discharge from wastewater treatment plant (WWTP) comprised 51 % of stream flux. As a result, majority ions water chemistry was changed at the receiving zone of the discharged effluent (Zone A). Its contribution increased to 69.9 % at the second sampling period with low stream flow. In the middle zone, inflows from the northern area, recently developed to a residential district showed low $NO_3-N$ and high $HCO_3$, Ca, $SO_4$, and $SiO_2$ indicating the effects of groundwater and concrete. One inflow (T-8), with extremely high Na and Cl, median $SiO_2$, was assessed to have anthropogenic influence, however its contribution to main stream was under 1 %. Road construction near Y-13 also affected water chemistry leading to the highest Na and Cl concentration. These hydro chemical changes can be critically used to evaluate the changes in water budget and fate of chemicals in a peri-urban watershed occasioned by human activities on the Yangjae.