• 지질공학
• /
• 제15권4호
• /
• pp.407-421
• /
• 2005

본 연구는 부산광역시 도심지역 중 부산진구 양정동부터 동구 수정동까지 지역에 대한 수리지질 특성을 파악하였다. 이를 위하여 양정동의 암반대수층과 부산진구 부산진역 부근의 미 고결층에서 양수시험을 실시하였다. 특히 양정동의 암반대수층은 동래단층대와 만나는 지 역으로서 동래단층의 수리지 질 특성을 파악하는데 중점을 두었고, 부산진구 부산진역 부근의 미고결층에서 행한 양수시험에서는 해안매립지와 해안퇴적층(미고결층)의 수리지질 특성을 파악하였다. 양정동의 암반대수층에 대해서는 Moench의 구상체 이중공극모델이 적합한 것으로 나타났으며, 부산진역 부근의 미고결층에 대해서는 Neuman의 자유면대수층 모델이 적당한 것으로 나타났다. 암반대수층의 평균 투수량계수는 $2.75\times10^{-5}m^2/s$, 평균 저류계수는 $6.41{\times}10^-5}$이고, 미고결층의 투수량계수는 $8.24\times10^{-4}m^2/s$, 저류계수는 $3.70\times10^{-3}$이다. 한편 순간충격 시험에 의한 평균 투수량계수와 평균 저류계수는 각각 $9.84{\times}10^{-4}m^2/s\;와\;1.21{\times}10^-4}$이다.

• 한국지하수토양환경학회:학술대회논문집
• /
• 한국지하수토양환경학회 2003년도 추계학술발표회
• /
• pp.565-569
• /
• 2003

One-year-long groundwater-level data have been collected from 18 wells in Cheon-an area. The result of barometric efficiency, autocorrelation, cross-correlation and statistical distribution evaluated from the measurement data shows that groundwater-level measurements from observation wells are the principal source of information about aquifer characteristics. Data from WA-2 has high barometric efficiency as well as steady decreasing auto-correlation coefficient, which means nonleaky confined aquifer, Most aquifers in this study show the unconfined properties so that barometric efficiencies are mostly low and the coefficients of cross-correlation between groundwater-level and precipitation are commonly high. This study showed that the long-term groundwater-level monitoring data without artificial stress such as pumping would give accurate information about aquifer characteristics.

• 한국지하수토양환경학회:학술대회논문집
• /
• 한국지하수토양환경학회 2006년도 총회 및 춘계학술발표회
• /
• pp.92-96
• /
• 2006

Borehole geophysical techniques were adopted for characterizing aquifer properties of crystalline rock formation in Bongmyong borehole test site, Kangwon National University. Specific fractures and/or fracture zones accompanying groundwater flow were delineated well by high resolution flowmeter and dilution measurements, and could be confirmed fromconventional well log methods. These geophysical techniques have been proved to be the most effective in aquifer characterization in crystalline rock formation.

• 한국지하수토양환경학회:학술대회논문집
• /
• 한국지하수토양환경학회 2006년도 총회 및 춘계학술발표회
• /
• pp.371-374
• /
• 2006

To quantify the hydraulic connection between river and aquifer, riverbed leakance values are required to be estimated. Silt, clay, and organic materials are often deposited in rivers resulting in the streambed having a lower hydraulic conductivity than the underlying alluvial aquifer The riverbed hydraulic conductivities are measured through vertical and oblique permeameter test. Anisotropic and heterogeneous properties of riverbed hydraulic conductivity were identified. Grain size analysis and flood wave response technique were checked along with the permeameter test for the riverbed hydraulic conductivity.

• 한국지하수토양환경학회지:지하수토양환경
• /
• 제20권1호
• /
• pp.65-75
• /
• 2015

An artificial recharge test aimed at investigating transport characteristics of the injected water plume in a fractured rock aquifer was conducted. The test used an injection well for injecting tap water whose temperature and electrical conductivity were different from the groundwater. Temporal and depth-wise variation of temperature and electrical conductivity was monitored in both the injection well and a nearby observation well. A highly permeable fracture zone acting as the major pathway of groundwater flow was distinctively revealed in the monitoring data. A finite element subsurface flow and transport simulator (FEFLOW) was used to investigate sensitivity of the transport process to associated aquifer parameters. Simulated results showed that aperture thickness of the fracture and the hydraulic gradient of groundwater highly affected spatio-temporal variation of temperature and electrical conductivity of the injected water plume. The study suggests that artificial recharge of colder water in a fractured rock aquifer could create a thermal plume persistent over a long period of time depending on hydro-thermal properties of the aquifer as well as the amount of injected water.

• 자원환경지질
• /
• 제54권2호
• /
• pp.247-257
• /
• 2021

The study area has been contaminated with explosive materials and heavy metals for several decades. For the design of the pump and treat remediation method, groundwater flow before and during groundwater pumping in a contaminated aquifer system was simulated, calibrated, and predicted using a generalized multidimensional hydrological numerical model. A three-dimensional geologic formation model representing the geology, hydrogeology, and topography of the aquifer system was established. A steady-state numerical simulation with model calibration was performed to obtain initial steady-state spatial distributions of groundwater flow and groundwater table in the aquifer system before groundwater pumping, and its results were illustrated and analyzed. A series of transient-state numerical simulations were then performed during groundwater pumping with the four different pumping rates at a potential location of the pumping well. Its results are illustrated and analyzed to provide primary reference data for the pump and treat remediation method. The results of both steady-state and transient-state numerical simulations show that the spatial distribution and properties of the geologic media and the topography have significant effects on the groundwater flow and thus depression zone.

• 자원환경지질
• /
• 제26권4호
• /
• pp.541-549
• /
• 1993

The main goal of this paper is to determine hydraulic properties and to predict drawdown for the efficient and stable development of groundwater in the Daejong-Chun area, North of Kyungsang-Do. Based on geological survey and analysis of well logging data conducted in 1991, it is found that the type of aquifer of this area is considered to be an anisotropic unconfined aquifer with saturated thickness of 19.8 m. In order to characterize this aquifer pumping test was conducted, and the resulting drawdown data were utilized for the analysis by applying both type curve matching technique and semi-log straight line method. As a result, the average specific yield of this aquifer is estimated as 32.3%, and the average ratio of $K_H$ to $K_V$ is only 2.7, which means that gravitational effect is not significant factor for this type of aquifer. For the validation of the estimated hydraulic properties, the analytical model which was developed with Newton-Raphson iteration procedure in this study, was employed to generate the drawdown. And, the resulting drawdown was compared against actual drawdown data and it shows the excellent matches. The actual drawdown data for 9 hours of pumping were used for history matching purposes and relatively satisfactory matches were achieved in this match. Then, the model was run by using the tuned parameters that are obtained during history matching stage, and the drawdown was predicted for the next 30 years of pumping with $3,000m^3/day$ of constant pumping rate. Its result indicates that the drawdown was stabilized as 1.41 m from 20 days with $3,000m^3/day$ of constant pumping rate, which is the required amount of water to be safely supplied to this area.

• 지질공학
• /
• 제22권1호
• /
• pp.27-37
• /
• 2012

미고결대수층에서 우물 굴착 시 대수층 교란이 수리특성에 미치는 영향을 파악하기 위하여 우물굴착 이후의 우물개량 공법인 서지블록과 에어서징을 실시하였다. 그리고 우물 굴착 및 개량의 대수층 변화를 비교 분석하기, 위하여 단계 및 장기 양수시험을 수행하였다. 그 결과 우물 굴착 및 개량 이후의 단계양수시험에서 동일 양수율 $700m^3/day$에 대한 수위강하와 비교하였을 때 수위강하는 각각 26.01 m, 21.62 m로 4.39 m정도 감소되었다. 이때 우물특성을 파악하기 위한 우물 굴착 및 개량 이후의 스킨계수는 7.92에서 5.04로 감소되어 우물상태가 개선된 것으로 나타났다. 우물 굴착 및 개량 이후의 장기양수시험에서 양수정을 중심으로 주변 MW-2, 3, 4호정의 투수량계수 범위는 각각 $1.684{\times}10^{-3}{\sim}4.490{\times}10^{-3}m^2/sec$, $4.002{\times}10^{-3}{\sim}4.939{\times}10^{-3}m^2/sec$ 범위로 우물개량 이후의 수리전도도 값이 조금 증가되었으며, MW-1호정은 $1.018{\times}10^{-2}m^2/sec$에서 $6.988{\times}10^{-3}m^2/sec$로 감소되었다. 이는 서징하는 동안 대수층의 공기 차단 및 폐색의 잠재적인 요인으로 인하여 MW-1호정 주변 대수층의 투수성이 미세하게 감소되는 효과로 나타났다. 따라서 미고결대수층에서 우물 굴착 시 미세입자가 양수정 주변의 수리특성에 영향을 미칠 수 있음을 반드시 유의해야 한다.

• 한국지하수토양환경학회지:지하수토양환경
• /
• 제25권4호
• /
• pp.87-97
• /
• 2020

In this study, the applicability of the geostatistical evolution strategy as an inverse analysis method of estimating hydraulic properties of small-scale basin was tested. The geostatistical evolution strategy is a type of data assimilation method that can effectively estimate aquifer hydraulic conductivity by combining a global optimization model of the evolution strategy and a local optimization model of the ensemble Kalman filtering. In the applicability test, the geometry, hydraulic boundary conditions, and the distribution of groundwater monitoring wells of Hanlim-Eup were employed. On the other hand, a synthetic hydraulic conductivity distribution was generated and used as the reference property for ease of estimation quality assessment. In the estimations, two different cases were tested where, in Case I, both groundwater levels and hydraulic conductivity measurements were assumed to be available, and only the groundwater levels were available, in Case II. In both cases, the reference and estimated hydraulic conductivity fields were found to show reasonable similarity, even though the prior information for estimation was not accurate. The ability to estimate hydraulic conductivity without accurate prior information suggests that this method can be used effectively to estimate mathematical properties in real-world cases, many of which little prior information is available for the aquifer conditions.

• 한국지하수토양환경학회지:지하수토양환경
• /
• 제26권3호
• /
• pp.14-24
• /
• 2021

Aquifer thermal energy storage (ATES) system uses groundwater thermal energy for cooling and heating of buildings, and it is also often utilized to provide warm water to crops and plants for the purpose of enhancing agricultural yields. This study investigated the potential influences of a ATES system on the geochemical properties of groundwater by simulating the variation of hydrochemistry and saturation index of groundwater during ATES operation. The test bed was installed at an agricultural field, which is mainly composed of an groundwater-rich alluvial plain. The simulation results showed no significant precipitation of mineral phases such as manganese-iron oxide, carbonate and sulfate around the ATES test bed, as well as no debasement of other important water quality parameters. The implementation of ATES system in the study area was appropriate and effective for utilizing the thermal energy of groundwater for agricultural use.