• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2001년도 추계학술발표회
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• pp.88-91
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• 2001

The purpose of this study is to localize the recharge rate into the national scale, calculated by use of the groundwater level from the 123 monitoring stations. The soil type, land use type, and bedrocks are selected for the influential factors over recharge rate. The main hypothesis is that the recharge rate can be expressed by the sum of the weighted averages of recharge rates of each factors. The optimized weights of soil type, land-use time and bedrocks from 119 stations are 0.80, 0.18 and 0.02 respectively. So this study offers that localization is available from the recharge rates calculated by groundwater level monitoring results.

• 한국지하수토양환경학회지:지하수토양환경
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• 제11권6호
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• pp.8-17
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• 2006

현장비원위치(Ex-situ) 공법 적용이 불가능한 부지에서, 디젤로 오염된 오염 토양과 지하수를 동시에 복원하기 위하여 과산화수소를 이용한 현장원위치 화학적 산화법(chemical oxidation)과 공기분사법(air-sparging)을 연계한 복합 복원 공정의 정화 효율 규명을 위한 실내 실험을 실시하였다. TPH 농도가 2,401 mg/kg(A 토양)과 9,551 mg/kg(B 토양)인 두 종류의 현장 오염 토양을 대상으로 과산화수소용액을 이용한 화학적 산화법의 디젤 제거 효율 규명을 위한 배치(회분식) 실험 결과, 과산화수소 50% 용액에 의해 토양 초기 TPH 농도의 18%와 15%까지 감소하였다. 과산화수소 용액 20%를 이용한 칼럼 세정 실험 결과, 세정에 의해서 A 토양과 B 토양의 경우 각각 초기 TPH 양의 78%와 72%가 제거되었다. 칼럼 실험에서 과산화수소의 산화반응에 의해 완전 분해되어 무기가스상(주로 $CO_2$과 $H_2O$)으로 제거된 양까지 고려한다면, 과산화수소용액이 오염 토양과 접촉하면서 충분한 산화과정을 거쳐 대부분의 유류가 토양으로부터 제거되었음을 알 수 있었다. 공기분사법을 이용한 디젤 오염 지하수 정화 실험의 경우, TPH 농도가 820 mg/L인 고농도의 인공 지하수 경우에도 공기분사 72시간 이내에 폐수배출허용기준인 5 mg/L 보다 낮아져, 디젤 제거 효율이 매우 높은 것으로 나타났다. 다만, 오염 토양 내 다량의 디젤 자유상이 존재하는 경우 토양으로부터 지하수로의 지속적인 자유상 디젤의 질량 이동에 의하여, 공기분사법의 지하수 정화 효율은 매우 낮았다. 마지막으로, 과산화수소를 이용한 현장원위치 화학적 산화법과 공기분사법을 연계한 복합 공정의 디젤 정화 효율을 규명하는 박스 실험을 실시하였다. 토양 내 자유상 디젤을 먼저 제거하기 위해 과산화수소 용액을 이용한 토양세정법을 실시한 후, 토양 내 TPH가 제거 되는 정도에 따라 후차적으로 공기분사법을 적용함으로써 토양 및 지하수로부터 디젤을 효과적으로 제거할 수 있었다. 20% 과산화수소 용액의 23 L 세정과 2,160 L의 공기분사에 의해 토양의 TPH 농도는 9,551 mg/kg에서 390 mg/kg으로 낮아졌으며, 오염 지하수의 TPH 농도도 5 mg/L 이하로 낮출 수 있었다. 본 실험들에서 얻어진 결과를 바탕으로 실제 현장에서 대단위 공정을 운영하는데 필요한 복원 공정의 최적 조건들을 도출해 낼 수 있으리라 판단되며, 유류로 오염된 토양 뿐 아니라 오염 지하수까지 동시에 정화할 수 있는 복합 공정 개발을 위한 중요한 기술 자료로 이용될 수 있을 것으로 판단된다.

• 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.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.453-454
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• 2004

Hydrogeochemical and isotopic characteristics were investigated for groundwater of Tertiary basin in southeastern part of Korea where deep drilling is in progress for geothermal investigation. According to geology, aquifer was distinguished as alluvial, tertiary sedimentary bedrock (bedrock groundwater), and fractured volcanic rock (deep groundwater). Groundwater of each aquifer is distinctively separated in Eh-pH conditions and concentrations of Cl, F, B and HCO$_3$. Deep groundwater has very low level 3H and 14C whereas alluvial groundwater has those of recent precipitation level. However one of deep groundwater show mixed characteristics in terms of hydrochemistry which indicates effect of pumping. Deep groundwater have temperature of 38 to 43$^{\circ}C$ whereas bedrock and alluvial groundwater have temperature less than 2$0^{\circ}C$. Fractured basement rock aquifer has different hydrogeologicalsetting from bedrock and alluvial aquifer considering hydrogeochemical and isotopic characteristics, and temperature.

• 한국지하수토양환경학회지:지하수토양환경
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• 제19권3호
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• pp.33-38
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• 2014

This study was performed to evaluate the applicability of pump and treat technology as well as to identify the changes of groundwater level by continuous pumping at the petroleum contaminated site. A total of 9 monitoring wells were installed at the site and the contaminant concentrations, TPH, benzene, toluene, ethylbenzene and xylene, of groundwater were measured. With the results of the groundwater monitoring, a total of 9 wells were set up for pumping contaminated groundwater in 3 locations. The waste water treatment facility with a capacity of $10m^3/hr$ was installed in the site and operated for about 1 year. The concentrations of the contaminated groundwater from the 3 pumping wells were exceeded groundwater regulation for benzene and TPH. However, the effluent concentration of benzene and TPH was under the regulation showing the maximum level of 0.011 mg/L and 1.2 mg/L during the operation periods. Groundwater levels were decreased by continuous pumping and those were not recovered during the operation period. Groundwater levels of PW-1,2, PW-3,4,5,6 and PW-7,8,9 were decreased about 5 m, 0.7 m, 2 m, respectively. The hydraulic conductivity (K) of the region of PW-1,2, PW-3,4,5,6 and PW-7,8,9 was estimated to be $6.143{\times}10^{-5}cm/sec$, $2.675{\times}10^{-5}cm/sec$, $1.198{\times}10^{-4}cm/sec$. Groundwater level was seemed to be affected not by hydraulic conductivity but by morphological effect. These results show that the pump and treat technology has high applicability for the restoration of petroleum contaminated groundwater but needs continuous monitoring to prevent rapid groundwater drawdown.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 INTERNATIONAL SYMPOSIUM ON SOIL & GROUNDWATER ENVIRONMENT
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• pp.166-168
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• 2005

• 한국지하수토양환경학회지:지하수토양환경
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• 제20권2호
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• pp.1-9
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• 2015

Groundwater has been a very precious resource for human life and economic development in the world. With increasing population and food demand, the groundwater use especially for agriculture is largely elevated worldwide. The very much large groundwater use results in depletion of major aquifers, land subsidences in many large cities, anthropogenic groundwater contamination, seawater intrusion in coastal areas and accompanying severe conflicts for water security. Furthermore, with the advent of changing climate, securing freshwater supply including groundwater becomes a pressing and critical issue for sustainable societal development in every country because prediction of precipitation is more difficult, its uneven distribution is aggravating, weather extremes are more frequent, and rising sea level is also threatening the freshwater resource. Under these difficulties, can groundwater be sustaining its role as essential element for human and society in the near future? We have to focus our efforts and wisdom on answering the question. Korean government should increase its investment in securing groundwater resources for changing climate.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 INTERNATIONAL SYMPOSIUM ON SOIL & GROUNDWATER ENVIRONMENT
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• pp.4-4
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• 2005

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2000년도 창립총회 및 춘계학술발표회
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• pp.163-163
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• 2000

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 1996년도 국제환경심포지엄
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• pp.33-39
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• 1996