• 한국지하수토양환경학회지:지하수토양환경
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• 제21권6호
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• pp.80-86
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• 2016

Earthquakes of M5.1, M5.8 and M4.5 occurred in September 12 and 19 respectively in Gyeongju, Gyeongbuk Province. Theses earthquakes inflated fears of people and highlighted necessity of detailed countermeasures because we have considered our country is safe to earthquakes. In the meanwhile, earthquake also impacts groundwater and thus it was recently reported that the Gyeongju Earthquakes affected groundwater there. This study evaluates daily groundwater data collected from five national groundwater monitoring stations (Geoncheon, Sannae, Oedong, Yangbuksin, Cheonbuk) in Gyeongju. The analysis revealed that only groundwater level of bedrock monitoring well hosted in andesite exhibited earthquake impact while no wells in the other four stations hosted in sedimentary rocks showed substantial responses to the earthquakes. This may be derived from the difference of seismic velocity of hosting rocks as well as epicenter distance. Special interest on groundwater monitoring is required to predict earthquakes as precursory phenomena.

• 한국지하수토양환경학회지:지하수토양환경
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• 제12권6호
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• pp.92-99
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• 2007

우리나라 지하수수질측정망은 2007년 현재 환경부가 관리하고 있는 오염우려지역 781개 지점 및 일반지역 1,240개 지점과 건설교통부에서 관리하고 있는 국가지하수관측망 478지점을 합쳐 총 2,499지점으로 구성되어 운영되고 있다. 1999년 이후 측정망 운영에 따른 지하수의 수질분석 결과를 매년 발표하고 있지만, 지하수수질측정망 지점에 대한 관정의 현황 정보는 제공하지 못하였다. 이에 본 연구에서는 지하수수질측정망의 운영현황, 지점선정 및 관정 정보등 현황을 평가하여 특성을 파악하고자 하였으며, 이를 통하여 향후 지하수수질측정망의 개선방안을 고찰하고자 하였다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 총회 및 춘계학술발표회
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• pp.259-262
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• 2003

In the Republic of Korea, Ministry of Construction & Transportation and Korea Water Resources Corporation manage the national groundwater monitoring network at the 169 stations and will organize the supplementary groundwater monitoring network at the 10,000 stations by 2011 year. The method that organizes the monitoring network was developed using the Analytic Hierarchy Process with pairwise comparison. Several estimation factors for the estimating every district were selected to reflect each district conditions. Their weighting value was decided by pairwise comparison and questions to the experts about groundwater The optimal number of groundwater monitoring well was calculated through the developed method. To verify this method, groundwater was monitored in Jeonju city by way showing the example. The study area In Jeonju city needs 7 stations for the supplementary groundwater monitoring network. The results monitored in 7 stations inferred the groundwater level around the study area by Kriging. The mean of residual between inferred groundwater level value from Kriging and actual groundwater level is rather low. Furthermore, the mean and standard deviation of residual between inferred groundwater level change and actual groundwater change is much lower. The Fact that 7 monitoring stations are sufficient for observing the groundwater condition in the study area makes it possible for suggested monitoring number to be proper.

• 지질공학
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• 제21권4호
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• pp.337-348
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• 2011

제주도 지하수위, 지하수온, 전기전도도의 변동특성 및 상관관계를 평가하고 또 지하수위변동법을 이용하여 지하수 함양률을 추정하였다. 자기상관분석을 통하여 각 관정 별 수위의 지연시간과 조절시간을 산정한 결과 자기상관성은 JM안성 관정이 가장 컸다. 그라고 교차상관분석으로 전기전도도-수위, 강수량-수위, 기온-수온간의 상관성을 분석하고 비교하였다. 분석결과 전기전도도-수위는 JR서광2, 강수량-수위는 JD하모, 기온-수온은 JI원종장2가 상호연관성이 가장 높았다. 지하수 함양률과 함양량을 산정한 결과 함양률은 평균 39.61%, 함양량은 평균 1,153,490,407 $m^3/yr$으로 산정되어 기존의 연구결과와 유사하였다.

• Environmental Engineering Research
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• 제15권2호
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• pp.85-91
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• 2010

Romania aims to adopt and implement the European Union's legislation, also including that for the field of water management. Like other countries, groundwater in Romania is locally polluted from point sources, such as leaking landfills, as well as from diffuse pollution sources, include fertilizers, pesticides and leakages from sewers, in urbanized areas. Diffuse pollution can also occur indirectly, by over-exploitation of groundwater wells, resulting in salt water intrusion, as well as from mining and exploitation of mineral aggregates. Romania has quite an intensive monitoring scheme to measure groundwater quality in phreatic and confined aquifers. The purpose of the work resumed in this paper was to derive natural background levels (NBL) for groundwater in order to distinguish the natural elevated concentrations of some substances (natural phenomena) from point and diffuse pollution (anthropogenic phenomena). Based on these NBLs, threshold values (TV) for groundwater will be set according to the requirements of the European Water Framework Directive and the related Groundwater Directive. This paper describes the results of a study for the derivation of NBL and TV in a pilot Groundwater Body. Also, the process and draft results for extrapolating this work for all Romanian groundwater bodies is explained, as well as points for future consideration with respect to monitoring and management.

• 한국지하수토양환경학회지:지하수토양환경
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• 제28권3호
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• pp.12-28
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• 2023

Each national groundwater monitoring well showed distinct change patterns in groundwater levels and electrical conductivity (EC) in the Nakdong River Estuary, implying different external forces (EFs) on each well. According to the annual average data in 1997-2020, seawater was invaded into Well C. The desalination rate of -1,062 µS/cm/year represents the adaptive capacity of the well to seawater intrusion. The water levels and EC in Well E responded to precipitation, indicating the low absorptive capacity to climate changes. Meanwhile, Well B showed constant increases in water levels, suggesting that problems by rising groundwater should be considered in the study area where confined aquifers are overlaid by clay aquitards. The other wells showed consistent water levels and EC, indicating resilience to EFs. Here, resilience is the capacity of a well to resist changes by EFs, including the absorptive and adaptive capacity. The resilience of Wells E and F to climate changes was quantitatively compared using a resilience cost (RC). The RC showed Well F was more resilient than Well E, and the bedrock aquifer was more resilient than the alluvium aquifer, supporting the usefulness of RC. The resilience assessment against EFs (e.g., changes in land use and climate) helps sustainable groundwater management.

• 한국지하수토양환경학회지:지하수토양환경
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• 제12권5호
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• pp.86-97
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• 2007

현재 운영중인 국가지하수관측소의 지하수위 변동 특성을 파악하고자, 2003년부터 2005년까지의 156주 동안의 202개 암반관측정과 112개 충적관측정을 대상으로 주성분분석을 실시하였다. 암반 및 충적관측정의 지하수위에 대하여 80% 정도 설명 가능한 8개 주성분을 각각 추출하였으며 이중 충적관측정에 대해서는 주성분 인자적재값을 이용하여 군집분석을 실시한 결과 강우에 대한 지하수위의 반응(군집 1: 4.6일, 군집 2: 24.1일, 군집 3: 1.4일), 수위 변동추세(군집 1: $2.05{\times}10^{-4}$ m/day, 군집 2: $-7.85{\times}10^{-4}$ m/day, 군집 3: $-3.51{\times}10^{-5}$ m/day), 수위 변동 폭(군집 1 < 군집 2 < 군집3) 등에 의하여 설명되는 3개의 군집으로 분류되었으며, 각 군집은 유의수준 0.05에서 인근 하천과의 거리(군집 3 < 군집 2 < 군집 1), 지하수 함양율(군집 3 < 군집 2 < 군집 1) 및 지형 경사 특성(군집 3이 평야지대, 군집 1은 급경사 지역) 등에 차이를 보이는 것으로 나타났다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제21권4호
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• pp.30-41
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• 2016

The amount of groundwater related data is drastically increasing domestically from various sources since 2000. To justify the more expansive continuation of the data acquisition and to derive valuable implications from the data, continued employments of sophisticated and state-of-the-arts statistical tools in the analyses and predictions are important issue. In the present study, we employed a well established machine learning technique of Gaussian Process Regression (GPR) model in the trend analyses of groundwater level for the long-term change. The major benefit of GPR model is that the model provide not only the future predictions but also the associated uncertainty. In the study, the long-term predictions of groundwater level from the stations of National Groundwater Monitoring Network located within Han River Basin were exemplified as prediction cases based on the GPR model. In addition, a few types of groundwater change patterns were delineated (i.e., increasing, decreasing, and no trend) on the basis of the statistics acquired from GPR analyses. From the study, it was found that the majority of the monitoring stations has decreasing trend while small portion shows increasing or no trend. To further analyze the causes of the trend, the corresponding precipitation data were jointly analyzed by the same method (i.e., GPR). Based on the analyses, the major cause of decreasing trend of groundwater level is attributed to reduction of precipitation rate whereas a few of the stations show weak relationship between the pattern of groundwater level changes and precipitation.

• 한국농공학회논문집
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• 제64권6호
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• pp.13-23
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• 2022

The purpose of this study was to analyze the impact of greenhouse cultivation area and groundwater level changes due to the water curtain cultivation in the greenhouse complexes, which are mainly situated along rivers where water resources are easy to secure. The groundwater observation network in Miryang, Gyeongsangnam-do, located downstream of the Nakdong River, was selected for the study area. We classified the groundwater monitoring well into the greenhouse (riverside) and field cultivation areas (plain and mountain) to compare the groundwater impact of water curtain cultivation in the greenhouse complex. The characteristics of groundwater level changes classified by terrain type were analyzed using the observed data. Riverside wells have significant permeability coefficients and are close to rivers, so they are greatly affected by river flow and precipitation changes so that water level shows a specific pattern of annual changes. Most plain wells do not show a constant annual change, but observation wells near small rivers and small-scale greenhouse cultivation areas sometimes show annual and daily changes in which the water level drops during winter. Compared to other observation wells, mountain wells do not show significant yearly changes in water level and show general characteristics of bedrock aquifer well with a low permeability coefficient.

• 한국지하수토양환경학회지:지하수토양환경
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• 제10권1호
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• pp.65-74
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• 2005

한국수자원공사는 전국을 대상으로 지하수의 수위 및 수질의 변동을 관측하고 국내 지하수자원의 보전 관리를 위한 기반 구축을 위하여 국가지하수 관측소를 설치${\cdot}$운영하고 있다. 자동 관측장비를 관측정 내에 설치하여 6시간 간격으로 지하수위, 온도, 전기전도도를 관측하고 있다. 주기적인 관측소 현장점검과 노후화된 혹은 고장난 관측장비 교체 및 수리 등의 작업에도 불구하고 자동 관측 및 전송의 내재적 한계로 인하여 부분적으로 이상값이 발생하고 있다. 그런데 이러한 이상값의 발생으로 인한 자료의 교란이나 관측 발생기간을 줄이기 위해서는 빠른 인지와 대처가 필요하다. 본 단보에서는 한강유역 국가 지하수 관측소 2000년도 지하수 관측 원자료에 대하여 이상값이 발생되는 시기와 빈도를 분석하였고 그 결과 지하수위는 급하강, 수온은 무변동 그리고 전기전도도는 급하강 이상이 가장 많이 발생하는 것으로 나타났다. 또한 각 해당항목에 대해 이상값 판단기준을 실례로 제시하였다.