• 제목/요약/키워드: Groundwater quality index

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지하수 수질측정망 자료를 활용한 시간적 오염도 추이변화 분석 (Temporal Trend Analysis of Contamination using Groundwater Quality Monitoring Network Data)

  • 방사라;유근제;박준홍
    • 한국물환경학회지
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    • 제27권1호
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    • pp.120-128
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    • 2011
  • Korea Groundwater Quality Monitoring Network is a database of annual groundwater quality survey results to prevent groundwater pollution. We estimated contamination index (CI) values for each type of land use, and analyzed temporal trends of pollutant concentration data in the Groundwater Quality Monitoring Network from 2001 to 2009. Among the pollutants considered in the database, the concentrations of nitrate and chloride were higher than their standards. In the case of nitrate, recreation parks, golf courses and general waste dumping regions showed increasing trends according to linear regression analysis, whereas industrial complexes and residential regions of urgan and recreation parks showed increasing trends in the chloride concentration data. According to multiple variable linear regression analysis, EC, pH and topography were major factors influencing CI values. These results suggest that groundwater with a high CI value and increasing trend is vulnerable for potential contamination, which requires more careful groundwater pollution control.

대수층 계간 축열시스템 적용을 위한 지하수의 화학적 특성 변화 (The Influences of Aquifer Thermal Energy Storage (ATES) System on Geochemical Properties of Groundwater)

  • 최한나;이홍진;심병완
    • 한국지하수토양환경학회지:지하수토양환경
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    • 제26권3호
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    • pp.14-24
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    • 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.

제주도 지하수 관정 내 질산성질소 오염도 평가 (Evaluation of Nitrate Nitrogen Contamination Degree in Groundwater Wells, Jeju Island)

  • 송성호;황보동준;장기영;김진성;서상기;양원석
    • 한국지하수토양환경학회지:지하수토양환경
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    • 제26권4호
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    • pp.8-19
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    • 2021
  • In this study, the evaluation standard for nitrate nitrogen contamination degree (WELCUP) was established using six factors that influence the groundwater quality in Jeju Island. To do this, weightings, ranges, and ratings were assigned for each factor and the relative possibility of nitrate nitrogen contamination degree was evaluated using WELCUP index for each well. As a result of calculating the WELCUP index using groundwater quality data of 5,112 wells in Jeju Island for 27 years (1993-2019), all 61 wells with the WELCUP index value higher than 100 are distributed in Daejung and Hangyung watershed with relatively large area of farmland in Jeju Island. In particular, as the ratio of private wells is more than 64%, it is necessary that systematic management is needed for private wells in terms of nitrate nitrogen contamination. Consequently, based on the results of applying the WELCUP evaluation standard, it is necessary to select the prioritization of nitrate nitrogen contamination pathways project for groundwater wells in Jeju Island.

Geochemical evaluation of groundwater quality of Peshawar Basin, Pakistan

  • Akhter, Gulraiz;Mand, Bilal A.;Shah, Munir H.
    • Advances in environmental research
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    • 제10권1호
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    • pp.43-57
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    • 2021
  • Evaluation of groundwater quality is vital due to its diverse use for several purposes. In the present study, groundwater quality and suitability from the Peshawar basin, Pakistan, were evaluated for drinking and irrigation purposes. The water samples were analysed for major cations (Ca, Mg, Na and K) and anions (chloride, bicarbonate and sulphate) along with other physicochemical parameters (pH, electrical conductivity, total dissolved solids, and total hardness). About 95% of the water samples were found to be within the WHO, US-EPA and Pak-EPA permissible levels for drinking purposes. Seventy percent (70%) of the water samples belonged to the hard water category. Irrigation water quality parameters, such as, chloride, residual sodium bicarbonate, sodium adsorption ratio, percent sodium, magnesium adsorption ratio, Kelly's ration and permeability index were evaluated which demonstrated that the groundwater was highly to moderately suitable for irrigation. A correlation study was conducted to find out the mutual associations among the variables. Piper diagram indicated the overall chemical nature of the study area was calcium-magnesium bicarbonate type. Cluster analysis revealed mutual apportionment of various parameters in the groundwater of the Peshawar basin, Pakistan.

오염원에 의한 지하수 수질의 변화 (Change of Groundwater Quality derived from Contaminant Sources)

  • 배상근
    • 한국환경과학회지
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    • 제4권5호
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    • pp.75-75
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    • 1995
  • In order to provide for the guidance on groundwater quality monitoring network design and also, to suggest the index to the solution of the contaminated groundwater remediation problems in the lake watershed, it is necessary to analyze the contaminant transport in the groundwater. The solute transport was analyzed in the lake watershed to investigate the behavior of the injected contaminant sources depend on the relationships between the point of contaminant sources and position of the lake. Three hypothetical groundwater flow systems, which is composed of a flow-through lake and two solute sources, were considered. The lakes located in the upper, middle, and lower portions of a watershed respectively. The transported contaminant was numerically simulated for five years by using MT3D contaminant transport model under the three-dimentional steady state conditions. From the above simulations, it can be concluded that the contaminant concentration was high as the contaminant source located at the upper position of a watershed, and the influence of the contaminant injection was large as the solute source located at the lower position. When the injection of contaminant was continued for one year without regard to the position of contaminant source and the lake, the influence of contaminant source was reached to bedrock.

오염원에 의한 지하수 수질의 변화 (Change of Groundwater Quality derived from Contaminant Sources)

  • 배상근
    • 한국환경과학회지
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    • 제4권5호
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    • pp.461-468
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    • 1995
  • In order to provide for the guidance on groundwater quality monitoring network design and also, to suggest the index to the solution of the contaminated groundwater remediation problems in the lake watershed, it is necessary to analyze the contaminant transport in the groundwater. The solute transport was analyzed in the lake watershed to investigate the behavior of the injected contaminant sources depend on the relationships between the point of contaminant sources and position of the lake. Three hypothetical groundwater flow systems, which is composed of a flow-through lake and two solute sources, were considered. The lakes located in the upper, middle, and lower portions of a watershed respectively. The transported contaminant was numerically simulated for five years by using MT3D contaminant transport model under the three-dimentional steady state conditions. From the above simulations, it can be concluded that the contaminant concentration was high as the contaminant source located at the upper position of a watershed, and the influence of the contaminant injection was large as the solute source located at the lower position. When the injection of contaminant was continued for one year without regard to the position of contaminant source and the lake, the influence of contaminant source was reached to bedrock.

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제주도 서부지역의 지하수 오염취약성 작성 연구

  • 이용두;송희경
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2006년도 총회 및 춘계학술발표회
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    • pp.316-318
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    • 2006
  • The purpose of this research is to write out vulnerability for western area in Jeju island by using drastic method which is the most frequently utilized among the writing techniques of underground water vulnerability. In case of aquifer, it was divided into two types, gravel layer or not and rated. And soil media was rated two kinds of method. Plan 1 is concerned with only soil class and plan 2 is concerned with soil class and gravels (or rocks), Vadose zone was rated differently according to the ratio of gravel layer. In case of plan 1, the scope of drastic index is from the minimum 77 to the maximum 176, on the other hand, plan 2, the scope of drastic index is from the minimum 79 to the maximum 182. In case of using the water quality data of Nitrate from 1994 to 2004, Pearson correlation coefficient are 0.164(Plan 1) and 0.124(Plan 2) and Spearman correlation coefficient are 0.132(Plan 1) and 0.113.

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울산지역 토지이용도에 따른 지하수 수질 및 오염특성 (Groundwater Quality and Contamination Characteristics Associated with Land Use in Ulsan Area)

  • 이병대;윤욱;성익환
    • 한국지하수토양환경학회지:지하수토양환경
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    • 제12권6호
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    • pp.78-91
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    • 2007
  • 금번 연구에서 울산지역의 토지이용도에 따른 지하수 수질 및 오염특성을 파악하고, 지하수의 오염 정도를 평가하고 도면으로 시각화하는 방법인 오염지수를 산출하였다. 연구지역내 216개 시료에 대한 지하수의 화학조성은 매우 다양하게 나타나며, 전기전도도의 경우, $100{\sim}31,360\;{\mu}S/cm$로 매우 큰 변화를 보이고 있다. pH값은 $4.6{\sim}8.57$의 범위로 산성 내지 약알카리를 보이며 평균값은 7.0이다. 연구지역 지하수의 화학조성은 토지용도에 따라 많은 영향을 받는 것으로 해석되었다. 수질유형은 $Ca-HCO_3$, $Ca-Na-HCO_3$, 유형이 우세하며, 주거/상업지역과 공업지역 지하수의 경우는 농업지역과 녹지지역 지하수에 비해 Cl이 풍부한 (Na, Ca)-Cl 유형으로 변하고 있다. 연구지역 오염지수의 범위는 $1.1{\sim}117.6$으로 평균은 9.56으로 산출되었다.

저영향개발(Low Impact Development) 기법 적용 지역 토양·지하수 환경 영향 평가 방법론 제안 연구 (Proposed Methodological Framework of Assessing LID (Low Impact Development) Impact on Soil-Groundwater Environmental Quality)

  • 김종모;김성훈;이윤규;최한나;박준홍
    • 한국지반환경공학회 논문집
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    • 제15권7호
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    • pp.39-50
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    • 2014
  • 본 연구에서는 도시개발 시 저영향개발(Low Impact Development, LID) 기법을 적용하였을 때, 토양 지하수 환경과 생태경관에 미치는 영향을 총체적으로 평가하는 방법의 framework 구축을 목적으로 문헌조사 연구를 수행하였다. 그 결과 토양 지하수 환경생태 건강성은 (i) 수리지질학적 지하수 오염 취약성, (ii) 생화학적 오염도와 (iii) 토양의 오염 정화능력의 여러 요소들에 의해서 측정되어 종합 및 평가되는 것이라는 개념을 설정하였고, 이들 각각의 요소에 미치는 영향 평가를 위한 측정 항목 선정과 각 요소의 측정치를 종합화해서 등급화 및 지표화하는 방법을 제시하였다. 또한 토양 지하수 환경 건강성과 기존의 환경 영향 평가에서 고려하는 생태 및 경관 요소를 GIS(Geographic Information System)와 AHP(Analytic Hierachy Process) 기반을 활용 및 접목하여 토양 지하수뿐만 아니라 생태 경관 등 LID의 자연환경에 미치는 영향을 총체적으로 평가하는 측정 항목 및 지표 산정과 그에 따른 활용 방법을 제시하였다. LID 기술의 계획 및 설계 단계에서 활용할 수 있는 최적화를 위해서 LCIA(Life Cycle Impact Assessment) 방법상의 framework로 활용하는 것을 본 연구에서는 제안하였다.

Hydrogeochemical and geostatistical study of shallow alluvial groundwater in the Youngdeok area

  • Kim, Nam-Jin;Yun, Seong-Taek;Kwon, Man-Jae;Kim, Hyoung-Soo;Kim, Chang-Hoon;Koh, Yong-Kwon
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2000년도 추계학술대회
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    • pp.232-236
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    • 2000
  • Multi-regression statistical analyses were applied for the water quality data of shallow alluvial ground water (n = 47) collected from the Youngdeok area, in order to quantitatively generalize the natural (non-anthropogenic) causes of regional water quality variation. Seven samples having the high contamination index ( $C_{a}$ > 3) reflect the striong effects by anthropogenic activity. Most of the alluvial groundwaters have acquired their quality primarily due to the dissolution of carbonate minerals. The results of multi-regression analysis show that chlorine is mainly derived from seawater effect. Sulfur isotopic compositions of dissolved sulfur and the S $O_4$/Cl ratio also enable us to discriminate the samples (n = 18) which are affected by atmospheric input of marine aerosol (sea-spray) and also by mixing between freshwater and seawater. Hydrogen and oxygen isotope data of the samples collected lie close to the local meteoric water line obtained from nearby Pohang city but has lower slope (5.45) on the $\delta$D-$^{18}$ O plot, indicating that alluvial groundwater was recharged from infiltrated meteoric water which has undergone some degree of kinetic evaporation. The estimated initial isotopic composition of the recharged water ($\delta$D = -74.8$^{0}$ /$_{00}$, $\delta$$^{18}$ O = -10.8$^{[-1000]}$ /$_{[-1000]}$ ) suggests that the alluvial ground water recharge largely occurs during summer storm events.s.s.

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