• 대한환경공학회지
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• 제31권3호
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• pp.208-216
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• 2009

본 연구에서는 토양 중 POPs 오염수준을 토지이용형태별로 구분 조사하여 오염특성을 규명하고 효율적인 토양 중 POPs 오염물질 관리방안 마련에 필요한 자료를 제공하였다. 농약류 중 Heptachlor, Aldrin, Endrin, Mirex, Toxaphene이 모든 지역에서 검출되지 않았고 Dieldrin은 N.D.-12.08 ${\mu}g$/kg, Chlordane은 N.D.-16.08 ${\mu}g$/kg, ${\Sigma}$DDT는 N.D.-38.19 ${\mu}g$/kg, HCB는 N.D.-1.32 ${\mu}g$/kg의 범위를 나타냈다. PCBs는 N.D.-172.12 ${\mu}g$/kg의 범위로 절연유오염지역이 높게 나타났으며, PCDD/Fs는 N.D.-6.68 pg I-TEQ/g으로 공단지역이 비교적 높게 나타났다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2002년도 총회 및 춘계학술발표회
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• pp.179-182
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• 2002

The objective of this study was to evaluate petroleum hydrocarbon degradation processes governing natural attenuation at tile contaminated site and accomplished through conducting on investigation of degradation rate, capacity, and mechanism of the monitored natural attenuation. The monitoring results of the three years indicated that the concentrations of DO, nitrate, and sulfate in the contaminated area were significantly lower than these in the none-contaminated area. The results also showed a higher ferrous iron concentration, a lower redox potential and a neutral pH in the contaminated groundwater, suggesting that biodegradation of TEX is the major on-going process in the contaminated area. However, reduction of TEX in the groundwater was not only biodegradation but also dilution and reaeration during infiltration of uncotaminated surface and groudwater.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.390-393
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• 2004

This study was carried out to evaluate the acid producing potential of geological materials such as pit wall, waste rock and stream sediments near the abandoned Imgi mine. The 17 samples used in this study were collected and then treated by static test such as Acid Base Accounting and etc. Samples of pit wall and waste rocks with high S content display a NAGpH values below 4.5 and net acid potential. Therefore some cost effective measures such as capping and groudwater flow barriers, will be required to reduce the impacts of ARD from the waste rock impoundment and the pit wall on near the stream.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2004년도 학술발표회
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• pp.691-695
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• 2004

In recent years, mary studies for efact estimation of groudwater recharge has been performed. They can be categorized into three groups : analytical method by means of groundwater recession curve, water budget analysis based on watershed, and the method using groundwater model. Since groundwater recharge rate shows the spatial-temporal variability due to hydrogeological heterogeneity, existing studies have various limits to deal with these characteristics. The method of estimating daily recharge rate with spatial-temporal variation based on rainfall-runoff model is suggested in this study for this purpose. This method is expected to enhance existing indirect method by means of reflecting climatic conditions, land use and hydrogeological heterogeneity.

• 대한토목학회논문집
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• 제9권4호
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• pp.103-112
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• 1989

방사성 폐기물 처분장 주변의 지하수 유동 현상을 이해하기 위해 정상상태에서의 지하수 수치모델을 수립하였다. 지하수 수치모델은 절점과 부재로 구성된 network에 의해 균질, 비균질, 다층매질에서 지하수 흐름을 조사하는데 이용되었고 모델의 수치해는 해석해와 일치하는 결과를 가졌다. 또한 지하매질의 수리학적 특성과 균열지역의 영향에 의한 지하수 유동의 물리적 변화현상도 조사되었다. 처분장 주변의 지하매질에 대해 구성된 network과 계산된 지하수 속도의 방향을 이용하여 지하수의 가능한 이동경로를 산정하는 방법이 개발되어 방사성 폐기물 처분장에서 생태계로의 가능한 지하수의 이동속도 및 시간을 예측하였다.

• 농촌계획
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• 제26권2호
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• pp.51-59
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• 2020

In this study, we analyzed the characteristics of 511 agricultural districts through statistical data, and classify these districts as the vulnerable area to drought through correlation and cluster analysis. The criteria for classification was related to ground-water recharge, irrigation water demand, and water supply. As a result, 8 types of agricultural districts were extracted. For example, the type 1 indicated the high priority area for ground-water development, thus the districts which were classified as type 1 showed ground-water use was less than 80 % of maximum capacity, and irrigation water supply was only 37.5 % and 76.5 % of irrigation water demand in upland and paddy field, respectively. As a result, 44 of 511 districts were classified as type 1.36 districts (types 5-8) were areas where groundwater development is limited. The results of this study are expected to provide useful information for establishing the direction of the rural area development project in connection with the revitalization of policy of people return to rural area.

• 대한토목학회논문집
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• 제35권6호
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• pp.1259-1267
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• 2015

우리나라에서는 기존에 경험하지 못한 농촌의 지하수 개발문제가 새로운 도전으로 대두되고 있다. 이른바 수막재배(Water Curtain Cultivation : WCC)라 불리우는 동절기 농업활동이 주된 이슈이다. 본 연구에서는 대상지역인 충북 청원군 수막재배지역내 충적대수층의 물수지를 검증하기 위해 3차원 유한차분모형인 MODFLOW를 구축하였다. 세계적인 추세인 학제간 융합방식을 현장규모에 맞게 도입한 지하수 모델링을 수행하였고, 특히 정밀한 지하수 함양량의 입력을 위해 SWAT모형을 이용한 소유역 지하수 함양량을 계산하였으며 양질의 현장자료를 기반으로 모형의 신뢰성을 확보하기 위한 검보정이 진행되었다. 본 연구의 목표는 하천의 보와 배수 시스템과 같은 인위적인 경계조건하에서 지하수 양수가 진행될 때 하천과 대수층의 다양한 상호작용을 모의하는 것이다. 또한 부지내의 누적 물수지의 계절변화를 분석함으로써 지하수 고갈과 회복량을 정량화할 수 있었다.

• 한국농공학회논문집
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• 제53권6호
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• pp.67-74
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• 2011

The objective of this study was to compare concentrations of nutrients such as total nitrogen (TN), nitrate nitrogen ($NO_3$-N) total phosphorous (TP), and phosphate phosphorous ($PO_4$-P) in groundwater under paddy and upland fields, and surface water recharging from a rural mixed land-use watershed. Chinese cabbage and hot pepper were cultivated on the upland field plot. The TN concentrations in upland groundwater showed double peaks (4.7, 4.3 mg/L, respectively) in April 2009 shortly after fertilizer application, indicating that TN concentrations are greatly influenced by fertilization. However, the TN concentrations in paddy groundwater were always lower than 2.0 mg/L irrespective of fertilization. Whereas the mean concentrations of TN and $NO_3$-N in upland groundwater significantly (p<0.05) higher than those in surface water, the mean concentrations of TP and $PO_4$-P in upland groundwater were significantly lower than those in surface water. On the other hand, the mean concentrations of TN, $NO_3$-N, TP and $PO_4$-P in paddy groudwater were significantly (p<0.05) lower than those in surface water. The TN concentrations in upland groundwater were generally higher than those in surface water during early April to early December due to the effect of fertilization, but vice versa in the other periods. In contrast, the TP concentrations in upland groundwater were always lower than those in surface water due to the sorption of inorganic phosphorous by soil. Moreover, the TN and TP concentrations in paddy groundwater were always lower than those in surface water, and therefore paddy groundwater may dilute nutrient concentrations in surface water when paddy groundwater and surface water mix.

• 지질공학
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• 제24권4호
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• pp.597-608
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• 2014

전 세계적으로 해안지방에서의 지하수자원 이용은 점차 증가하고 있다. 또한 해수침투와 같은 자연재해로 인한 피해는 점차 가중될 것으로 예상되며 기후변화와 같은 환경의 변화는 재해의 속도를 가속화시키고 세계 곳곳에서 상당히 큰 대규모 재해의 형태까지 속출하고 있다. 해안 지하수 및 관련 재해 관련 연구개발은 각국의 대표적 실증 부지 중심으로 기술을 시험하고 검증하는 추세이다. 본 논문에서는 전세계적인 해안 지하수 및 관련 재해 연구의 추세를 파악하고 질적, 양적 성장을 확인하였으며 향후 발전방향을 전망하였다. 또한 해안 지하수의 해석기술을 간략하게 소개하였다. 현재 우리나라 실증 부지 중 제주도의 수문지질학적 특징에 대해 살펴보고 국지적인 해수침투 발생 현황을 파악하였다. 마지막으로 제주도와 규모와 형태가 비슷한 화산섬인 하와이 Oahu 지역의 대수층을 대상으로 해외 연구 동향 및 연구 내용에 대해 소개함으로써 앞으로 제주 지역 및 국내 해안 대수층의 지하수 유동 및 오염에 관한 연구에 접목할 수 있는 연구 방식에 대해 고찰하였다.

• 한국광물학회지
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• 제10권1호
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• pp.33-44
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• 1997

The reaction path of water-gneiss in 200m borehole at the Soorichi site of Yugu Myeon, Chungnam was simulated by the EQ3NR/EQ6 program. Mineral composition of borehole core and fracture-filling minerals, and chemical composition of groundwater was published by authors. In this study, chemical evolution of groundwater and formation of secondary minerals in water-gneiss system was modelled on the basis of published results. The surface water was used as a starting solution for reaction. Input parameters for modelling such as mineral assemblage and their volume percent, chemical composition of mineral phases, water/rock ratio reactive surface area, dissolution rates of mineral phases were determined by experimental measurement and model fit. EQ6 modelling of the reaction path in water-gneiss system has been carried out by a flow-centered flow through open system which can be considered as a suitable option for fracture flow of groundwater. The modelling results show that reaction time of 133 years is required to reach equilibrium state in water-gneiss system, and evolution of present groundwater will continue to pH 9.45 and higher na ion concentration. The secondary minerals formed from equeous phase are kaolinite, smectite, saponite, muscovite, mesolite, celadonite, microcline and calcite with uincreasing time. Modeling results are comparatively well fitted to pH and chemical composition of borehole groudwater, secondary minerals identified and tritium age of groundwater. The EQ6 modelling results are dependent on reliability of input parameters: water-rock ratio, effective reaction surface area and dissolution rates of mineral phases, which are difficult parameters to be measured.