• 제목/요약/키워드: groundwater level change

검색결과 214건 처리시간 0.024초

산악 터널시공에 따른 주변 지하수위 변화에 대한 수리 및 수문학적 해석 (Hydraulic and hydrological study on the change in groundwater level during tunnel construction)

  • 김선명
    • 한국터널지하공간학회 논문집
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    • 제13권2호
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    • pp.97-114
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    • 2011
  • 산악터널이 건설되는 지역에 있는 우물이나 작은 하천들은 흔히 주민들의 일상생활용수원으로 사용되고 있다. 이때 터널이 굴착됨에 따라 우물의 수위 저하와 같은 문제들이 발생할 수 있다. 따라서 본 연구에서는 설계단계에서 터널 주위의 지하수에 대한 부정적인 영향을 경감시키기 위해 MODFOLOW와 같은 수치모델링 기법을 사용하여 터널내 지하수 유입량과 지하수위 저하 지역에 대한 평가를 실시하였다. 또한 수문학적인 방법에 의해서 터널주변 지역의 지하수의 용수량을 평가하였다.

Savitzky-Golay 필터와 미분을 활용한 LSTM 기반 지하수 수위 예측 모델의 성능 비교 (Performance Comparison of LSTM-Based Groundwater Level Prediction Model Using Savitzky-Golay Filter and Differential Method )

  • 송근산;송영진
    • 반도체디스플레이기술학회지
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    • 제22권3호
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    • pp.84-89
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    • 2023
  • In water resource management, data prediction is performed using artificial intelligence, and companies, governments, and institutions continue to attempt to efficiently manage resources through this. LSTM is a model specialized for processing time series data, which can identify data patterns that change over time and has been attempted to predict groundwater level data. However, groundwater level data can cause sen-sor errors, missing values, or outliers, and these problems can degrade the performance of the LSTM model, and there is a need to improve data quality by processing them in the pretreatment stage. Therefore, in pre-dicting groundwater data, we will compare the LSTM model with the MSE and the model after normaliza-tion through distribution, and discuss the important process of analysis and data preprocessing according to the comparison results and changes in the results.

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Remediation of Contaminated Groundwater: Change of Paradigm for Sustainable Use

  • Lee, Jin-Yong;Lee, Kang-Kun
    • 한국지하수토양환경학회지:지하수토양환경
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    • 제18권6호
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    • pp.1-7
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    • 2013
  • Groundwater development and use have been increasing in Korea causing frequent occurrences of related hazards such as groundwater level decline, land subsidence, and groundwater contamination. To tackle these groundwater problems, central and local governments have set-up and maintained many groundwater monitoring programs such as the National Groundwater Monitoring Network and the Groundwater Quality Monitoring Network, which collect very valuable data on the overall status of domestic groundwater to aid proper groundwater management. However, several problems mainly related to the remediation of contaminated groundwater remain unresolved. Recently, there have been some incidents related to the contamination of groundwater, and these have drawn the concern of the Korean people. Although groundwater contamination has been investigated in detail, actual groundwater remediation work has not yet been implemented. The remediation of the contaminated groundwater must begin immediately in order to sustain the eco-system service of clean groundwater and enhance the welfare of the Korean people.

Estimating Groundwater Level Change Associated with River Stage and Pumping using Time Series Analyses at a Riverbank Filtration Site in Korea

  • Cheong, Jae-Yeol;Hamm, Se-Yeong;Kim, Hyoung-Soo;Lee, Soo-Hyoung;Park, Heung-Jai
    • 한국환경과학회지
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    • 제26권10호
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    • pp.1135-1146
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    • 2017
  • At riverbank filtration sites, groundwater levels of alluvial aquifers near rivers are sensitive to variation in river discharge and pumping quantities. In this study, the groundwater level fluctuation, pumping quantity, and streamflow rate at the site of a riverbank filtration plant, which produces drinking water, in the lower Nakdong River basin, South Korea were interrelated. The relationship between drawdown ratio and river discharge was very strong with a correlation coefficient of 0.96, showing a greater drawdown ratio in the wet season than in the dry season. Autocorrelation and cross-correlation were carried out to characterize groundwater level fluctuation. Autoregressive model analysis of groundwater water level fluctuation led to efficient estimation and prediction of pumping for riverbank filtration in relation to river discharge rates, using simple inputs of river discharge and pumping data, without the need for numerical models that require data regarding several aquifer properties and hydrologic parameters.

수리지질학적 과학수사 기법에 의한 도로 터널이 지하수 변화에 미치는 영향 (Influence of Road Tunnel on Groundwater Change Determined Using Forensic Hydrogeological Technique)

  • 윤설민;함세영
    • 한국환경과학회지
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    • 제33권4호
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    • pp.269-277
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    • 2024
  • Scientific forensic techniques are used to verify environmental impact of groundwater pollution, surface water pollution, air pollution, noise, and vibration according to residents' complaints in connection with construction and civil engineering works. In this study, we investigated the contamination of groundwater and the lowering of the groundwater level in an area surrounding a tunnel excavation site for the Andong-Yeongdeok national road, using a forensic hydrogeological technique. We reviewed the groundwater level and water quality of well GW1 in the area surrounding the tunnel excavation site as well as tunnel construction information and then we analyzed the correlations among the obtained data. Before tunnel excavation, the water level of well GW1 was lower than the tunnel elevation. Considering the relationship between the precipitation, tunnel discharge, tunnel depth, and groundwater level of well GW1, the groundwater flowed from the tunnel to well GW1. Moreover, the tunnel discharge and groundwater levels were not related to each other. The pH of well GW1 was 8.4 before tunnel excavation. During excavation, the pH declined to 8.1-8.2 at the beginning, and increased to 8.8 at the end of the excavation. The fluorine concentration in well GW1 was 2.49 mg/L, 1.91-3.22 mg/L, and 1.7-2.67 mg/L, respectively, before, during, and after the excavation. The sulfate ion concentration was very high, over 2,000 mg/L, before and during the excavation; after the excavation, it was between 200 and 323 mg/L. Turbidity was 1.47, 10.5, and 4.51 NTU before, during, and after tunnel excavation, respectively. Therefore, the excavation of this tunnel is not related to the groundwater quality of well GW1.

기름 유출로 인한 토양 및 지하수의 오염

  • 김동진;양재의;유진열;김희갑;김기동
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2006년도 총회 및 춘계학술발표회
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    • pp.424-427
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    • 2006
  • Soil contamination with petroleum oil around a military army was investigated. It showed that soils of a riverside highland, an entrance of the military army, and nearby roads were contaminated with total petroleum hydrocarbons (TPH) released from the military army to the depth of approximately 2 m. The measured concentrations were as high as 15,277 mg/kg. A wide range of soil in the riverside highland was contaminated by the movement of oil to the surface soil, which occurred with the vertical movement of groundwater table caused by the change of river water level and groundwater level. Spilled petroleum oil components were released into Wonju Stream by the increase of hydraulic conductivity and the groundwater flow.

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수위변동에 따른 포화/불포화 매질의 체적함수비 변화 특성 평가 (Properties of the variations of volumetric water content on the saturated/unsaturated media by water-level fluctuations)

  • 김만일;임헌태;김형수
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2006년도 춘계 학술발표회 논문집
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    • pp.1076-1082
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    • 2006
  • This study measured the change of media properties using Time domain Reflectometry (TDR) and Tensionmeter (TM) to measure volumetric water content of soil affecting in land subsidence and pollutant diffusion under saturation/unsaturated condition by water-level fluctuations. Also, actual water content compared their changes aspect by dry oven test for quantitative determinations of these measured values. In the case of TM, initial unsaturated condition confirmed that range in dimension of each other different according to their establishment depth, but measured values of TM can know that is shown measured value in almost similar measuring range under drain condition after the first injection. Also, the results of TDR showed that can measure enough change of volumetric water content in saturation/unsaturated condition by water-level fluctuations. Therefore, we are judged that TDR measurement equipment is very effective to measure the variations of volumetric water content and water-level being caused in groundwater level fluctuations.

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Impact of predicted climate change on groundwater resources of small islands : Case study of a small Pacific Island

  • Babu, Roshina;Park, Namsik
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2018년도 학술발표회
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    • pp.145-145
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    • 2018
  • Small islands rely heavily on groundwater resources in addition to rainwater as the source of freshwater since surface water bodies are often absent. The groundwater resources are vulnerable to sea level rise, coastal flooding, saltwater intrusion, irregular pattern of precipitation resulting in long droughts and flash floods. Increase in population increases the demand for the limited groundwater resources, thus aggravating the problem. In this study, the effects of climate change on Tongatapu Island, Kingdom of Tonga, a small island in Pacific Ocean, are investigated using a sharp interface transient groundwater flow model. Twenty nine downscaled General Circulation Model(GCM) predictions are input to a water balance model to estimate the groundwater recharge. The temporal variation in recharge is predicted over the period of 2010 to 2099. A set of GCM models are selected to represent the ensemble of 29 models based on cumulative recharge at the end of the century. This set of GCM model predictions are then used to simulate a total of six climate scenarios, three each (2010-2039, 2040-2069, and 2070-2099) under RCP 4.5 and RCP 8.5. The impacts of predicted climate change on groundwater resources is evaluated in terms of freshwater volume changes and saltwater ratios in pumping wells compared to present conditions. Though the cumulative recharge at the end of the century indicates a wetter climate compared to the present conditions the large variability in rainfall pattern results in frequent periods of groundwater drought leading to saltwater intrusion in pumping wells. Thus for sustaining the limited groundwater resources in small islands, implementation of timely assessment and management practices are of utmost importance.

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한국의 지하수위와 강우이동평균간의 상관관계 (The Correlation Between the Moving Average of Precipitation and Groundwater Level in Korea)

  • 양정석;김남기
    • 대한토목학회논문집
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    • 제31권3B호
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    • pp.265-276
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    • 2011
  • 한반도와 제주를 포함한 전국의 강우 자료와 국가지하수위 관측소에 관측된 지하수위 관측 자료를 수집하였다. 강우와 지하수위의 관계를 분석한 후 강우자료를 이용하여 이동평균을 취한 후 지하수위와의 상관관계를 분석하였다. 또한 유역평균 일최대침투량인 한계침투량을 고려한 후, 강우이동평균과 지하수위간의 상관계수를 산정하였다. 한계침투량 고려시 상관계수가 0.6 이상인 곳을 최종적으로 선정하였고, 선정된 지역의 공통점과 지역 특성에 따른 차이점 등을 비교 분석하였다. 총 26개 지역이 선정되었고 행정구역별로 경기도가 4개소, 강원도가 4개소, 충청도가 5개소, 전라도가 3개소, 경상도가 9개소, 제주도가 1개소이다. 상관계수가 높을수록 강우사상 발생에 따른 지하수위 변동은 뚜렷하게 나타났으며, 강우와 상관없는 요인에 의한 지하수위의 변동이 거의 없는 것으로 나타났다. 본 연구를 토대로 강우 예측 시나리오를 활용한다면 상관계수가 높은 지역에서 지하수위 또한 예측이 가능할 것으로 기대된다.

장기모니터링을 통한 지하수계의 이해 - 광릉소유역 사례 연구 (Understanding the Groundwater System through the Long-term Monitoring - a case Study of Gwangneung Headwater Catchment)

  • 이재민;우남칠
    • 한국지하수토양환경학회지:지하수토양환경
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    • 제17권4호
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    • pp.51-62
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    • 2012
  • Effects of climate change on groundwater system requires understanding the groundwater system in temporal and spatial scales through the long-term monitoring. In this study, the spatio-temporal variations of groundwater were analyzed through the continuous observation of water level, electrical conductivity (EC) and water temperature with automatic data-loggers and sampling in a Gwangneung catchment, Korea, for the four years from 2008 to 2011. Groundwater monitoring were performed at the nest-type wells, MW1 and MW2, located in upsteam and downstream of the catchment, respectively. During the survey period, both the total amount of annual precipitation and the frequency of concentrated rainfall have increased resulting in the elevation of runoff. Water level of MW1 showed no significant fluctuations even during the rainy season, indicating the confined groundwater system. In contrast, that of MW2 showed clear seasonal changes, indicating the unconfined system. The lag-time of temperature at both wells ranged from one to three months depending on the screened depths. Results of chemical analyses indicated that major water compositions were maintained constantly, except for the EC decreases due to the dilution effect. Values of the stable-isotope ratios for oxygen and deuterium were higher at MW2 than MW1, implying the confined system at the upstream area could be locally developed.