• Economic and Environmental Geology
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• v.35 no.1
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• pp.13-23
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• 2002

The chemical compositions of groundwaters from the granite areas mainly belong to Ca-HC0$_{3}$ and Na-HC0$_{3}$type, and some of these belong to Ca-(CI+S0$_{4}$) and Na-(CI+S0$_{4}$) type. Spring waters and groundwaters from anorthosite areas belong to Ca-HC03 and Na-HC03 type, respectively. The result of reaction path modeling shows that the chemical compositions of aqueous solution reacted with granite evolve from initial Ca-CI type, via CaHC0$_{3}$ type, to Na-HC0$_{3}$ type. The result of rain water-anorthosite interaction is similar to evolution path of granite reaction and both of these results agree well with the field data. In the reaction path modeling of rain watergranite/anorthosite reaction, as a reaction is progressing, the activity of hydrogen ion decreases (pH increases). The concentrations of cations are controlled by the dissolution of rock-forming minerals and precipitation and re-dissolution of secondary minerals according to the pH. The continuous addition of granite causes the formation of secondary minerals in the following sequence; gibbsite plus hematite, Mn-oxide, kaolinite, silica, chlorite, muscovite (a proxy for illite here), calcite, laumontite, prehnite, and finally analcime. In the anorthosite reaction, the order of precipitation of secondary minerals is the same as with granite reaction except that there is no silica precipitation and paragonite precipitates instead of analcime. The silica and kaolinite are predominant minerals in the granite and anorthosite reactions, respectively. Total quantities of secondary minerals in the anorthosite reaction are more abundant than those in the granite reaction.

• Journal of Korean Tunnelling and Underground Space Association
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• v.7 no.3
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• pp.219-226
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• 2005

The result that analyze for 6 years a groundwater influx quantity of total 60 catch-pit established in subway line 5 appeared with $0.77m^3/min$. When comparing design approaches of the catch-pit with design approaches of the box structure $2m^3/min$ and the tunnel structure $3m^3/min$, it is found that it has a surplus. Red sedimentation substance contains large portion of Fe. The earth retaining structure of a tunnel and groundwater containing more portion of Fe than other area rue the major factor of this substance. In case of white sedimentation substance, the most frequently founded ingredient is CaO, which is occurred in case grouting injection materials for ground reinforcement is transmitted into a tunnel system by ground water. This substance is doesn't affect safety of a tunnel.

• Food Science and Preservation
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• v.10 no.4
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• pp.482-487
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• 2003

The filtration effects of glass membrane filters and hollow fiber membranes with different pore size to prevent the haze of a commercial foxtail millet Yakju were investigated. The most particles(haze precusors) present in the Yakju were removed by using 1.2 $\mu\textrm{m}$ glass membrane filter. In case of using 0.45$\mu\textrm{m}$ hollow fiber membrane system, the permeate flux on the Yakju filtration was calculated to 342.8 lmh. During the 3 month storage at 4$^{\circ}C$ and room temperature for each 48 hrs in turn, alittle fine haze was observed from the Yakju even if it was filtered by using 0.7 $\mu\textrm{m}$ glass membrane filter. Anything of haze was, however, observed from the Yakju filtered by using all of hollow fiber membranes. Therefore, the 0.45$\mu\textrm{m}$ hollow fiber membrane system was effective as a final filtration process of the Yakju.

• The Journal of Engineering Geology
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• v.13 no.1
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• pp.29-50
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• 2003

Physicochemical Properties of acid mine water of the Chonam-ri Creek and the Sagok-ri Creek in the Kwangyang Au-Ag mine area were determined using geochemical approaches. Metal contamination (Cd, Cu, Pb, Zn) is more serious in the Chonam-ri Creek than in the Sagok-ri Creek. However, the contents of Al and Fe is higher in the Sagok-ri Creek. Such differences between the two creeks probably reflect the abundance and composition of ore minerals. The attenuation processes for acid mine water in both creeks were investigated. In the Chonam-ri Creek, a small retention pond which contains limestone plays an important role in the removal of heavy metals by adsorption or coprecipitation due to increase of pH. The capacity of metal scavenging in this pond depends on the seasonal variation of inflow volume. Reddish yellow precipitates sampled in the Chonam-ri Creek were analyzed by XRD, SEM-EDS, EPMA, and chemical decomposition. The precipitates mainly consist of goethite and are also enriched in Al, Mn, Cu and Zn. This inditates that precipitation of goethite is important for scavenging those trace elements, possibly due to adsorption or coprecipitation. In the Sagok-ri Creek, on the other hand, hydrologic mixing of uncontaminated tributaries results in removal of heavy metals with iron hydroxides precipitation due to the pH increase. The mechanisms proposed for metal attenuation at the confluence between contaminated mine water and uncontaminated tributary water are also explained by the property-property plots.

• Journal of the Korean earth science society
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• v.30 no.7
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• pp.801-809
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• 2009

The Salinas Grandes borate deposit located in Jujuy state, northern Argentina can be categorized into the playatype evaporite deposit. Major borate mineral is ulexite ($NaCaB_5O_9{\cdot}H_2O$), which boron could be originated from volcanic rocks nearby playa. The eastern part of the Jujuy state in northern Argentina belongs to the Altiplano-Puna platform which shows high altitude and semiarid climate. Lots of Mesozoic and Cenozoic volcanics that are source of boron as well as playas that are the basin for borate precipitation in the area are essential for boron evaporite deposit. Therefore, the extensive explorations for the playa-type evaporite deposit are need.

• Proceedings of the Korean Society of Surveying, Geodesy, Photogrammetry, and Cartography Conference
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• 2007.04a
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• pp.431-434
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• 2007

빗물 및 폐수가 흘러가는 하수관은 자연 유하식으로 하수가 흘러갈 수 있도록 설계되어있는 관의 특성상 침전물이 많이 발생하며, 집중호우로 발생하는 다량의 빗물이 빠른 유속으로 관을 흐르기 때문에 관내부를 손상시키는 요인으로 작용하고 있다. 이에 본 연구에서는 관 내부를 촬영할 수 있는 궤도차량을 통해 동영상 자료를 획득하고 영상의 이미지 보정 단계를 거쳐 그래픽 파일로 변환한후 관련 정보를 입력, 저장하는 시스템 개발을 본 연구의 주요 범위로 한다. 이미지보정은 동영상을 거리의 함수를 가지는 이미지 파일로 변환하고 각각의 획득된 이미지를 영상정합기법을 사용하여 하나의 연속된 이미지 형태로 저장하여 영상 해석을 통해 균열, 침전등의 사항을 도출하여 도출된 사항은 지리정보 체계와 연동할 수 있는 파일 체계를 갖추도록 개발하였다.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
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• 2004.09a
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• pp.172-174
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• 2004

본 논문은 광산산성배수(AMD)에서 철 및 알루미늄 제거 효과가 입증되고 ARD(Acid Rock Drainage)에서의 비소제거 효과가 확인된 인회석을 침전제로 사용하여 철, 알루미늄 및 비소가 아닌 다른 중긍속의 제거효율을 알아보기 위해 도금폐수를 이용하여 실내실험을 실시하였다. 실험결과, 도금폐수의 수질분석결과에 의하면 '수질환경보존법 오염물질 배출허용기준' <가>지역 방출수 기준을 초과하는 것은 pH, Zn, Fe, Cu, Cr 및 P였다. 실험 결과 인회석 40번체 통과분-100번체 잔류분을 사용하는 것이 가장 적절할 것으로 생각되며 유속은 1kg의 인회석에 11의 도금폐수를 3시간 동안 반응시키면 경제적, 시간적 측면에서 가장 적절한 것으로 사료된다. 이 경우 pH는 1.98에서 5.30으로 증가하고 Cr, Fe, Cu 및 Zn은 각각 77.10%, 99.58%, 99.39% 및 40.77% 제거되는 것으로 나타났다. 용해율은 0.3619 g/min/kg으로 계산되었다. 그러나 3시간의 반응시간으로는 크롬 및 아연을 기준치 이하로 제거하지 못하므로 인회석 반응조를 다단계로 하는 실험을 수행해 그 결과를 평가해야 할 것이다.

• Economic and Environmental Geology
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• v.34 no.4
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• pp.319-328
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• 2001

The Fe-REE deposit of the Hongcheon-Jaeun district occurs in Precambrian gneiss, and is classified into two ore bodies: the Jaeun ore body (northern ore body) and the Hongcheon ore body (southern ore body). Ecomonically important minerals consist of magnetite, monazite, strontianite and barite. Based on mineral assemblages and textures, the mineralization can be classified into two stages (Na-carbonatite stage and Fe-carbonatite stage). Main REE minerals were precipitated during the Fe-carbonatite stage. Some evidences of the carbonatite origin include: 1) strontianite-monazite exolution texture, 2) strontianite-barite exolution texture, 3) the occurrence of acmite of igneous origin at the area with abundant rare earth minerals, 4) the occurrence of the mineral assemblage consisting of carbonate minerals + magnetite + REE minerals. Therefore, we suggest that Fe-REE mineralization in the study area was related to carbonatite of igneous origin.

• Proceedings of the Korea Water Resources Association Conference
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• 2020.06a
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• pp.210-210
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• 2020

LID (Low Impact Development, 저영향개발)는 산업화 및 도시화 진행 지역에서 비점오염원으로부터 배출되는 오염물질을 제어해 개발지역 내 자연순화 기능을 최대한 유지하고, 물순환 기능증대를 통해 강우 유출수를 지역 내에서 관리하는 것을 목표로 한다. 비점오염원 저감 LID 시설에는 자연형과 장치형 시설이 있다. 자연형 시설에는 저류형, 침투, 식생형 시설 등이 있다. 특히, 침투시설에는 대표적으로 투수블럭이 있으며, 이는 투수성 포장재를 통해 강우 유출수를 지하로 침투시켜 여과나 흡착 등으로 비점오염물질을 제어하는 시설이다. 장치형 시설로는 여과재나 망을 이용해 비점오염물질을 분리하는 여과형 및 스크린형 시설, 응집과 침전을 통해 비점오염물질을 분리하는 응집·침전 시설 등이 있다. 이에 본 연구는 2016년부터 2018년 3년간 전주 서곡지구 지역 내 설치된 필터형 투수블럭, 틈새형 투수블럭에서 진행했다. 각각의 투수블럭에서 총 19회, 20회의 강우 모니터링을 실시했고, 오염물질 유입 및 유출 EMC 등의 분석을 통해 유출 및 오염물질 저감효과를 분석했다. 연구 대상 각 투수블럭의 주요 제원은 시설 용량 14.4㎥, 시설 면적은 14.4㎡이다. 모니터링 결과값을 분석한 결과 필터형 투수블럭의 경우 유출 저감율은 17.4 ~ 100%, 틈새형 투수블럭은 29.6 ~ 100%이었다. 필터형 투수블럭과 틈새형 투수블럭의 단위면적당 유량 저감량은 각각 0.014 ~ 0.583㎥/㎡, 0.035 ~ 0.588㎥/㎡이었다. 오염물질 저감효율을 분석한 결과 유기물 항목(BOD, TOC)의 경우 틈새형 투수블럭에서의 저감효율(BOD 93.59%, TOC 90.39%)이 필터형 투수블럭에서의 저감효율(BOD 89.99%, TOC 86.94%) 보다 다소 높게 나타났다. 영양염류 항목(T-N, T-P)의 경우 필터형, 틈새형 모두 비슷한 저감효율(필터형 T-N 89.02%, 필터형 T-P 98.12%, 틈새형 T-N 90.41%, 틈새형 T-P 98.04%)을 보였다.

• The Journal of Engineering Geology
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• v.27 no.3
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• pp.293-304
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• 2017

This study was performed in order to hydrogeological analysis of aquifer, which is a necessary part for evaluating the efficiency of the combined well and open-closed loops geothermal (CWG) systems. CWG systems have been proposed for the effective utilization of geothermal energy by combining open loop geothermal systems and closed loop geothermal systems. Small aperture CWG systems and large aperture CWG systems were installed at a green house land with water curtain facilities in Chungju City. Aquifer tests include pumping tests and step-drawdown tests were conducted to analyse hydrogeological characteristics of aquifer in the study area. The transmissivity was estimated in the range of $13.49{\sim}58.99cm^2/sec$, and the storativity was estimated in the range of $1.13{\times}10^{-5}{\sim}5.20{\times}10^{-3}$. The geochemical analysis showed $Ca^{2+}$ ion and ${HCO_3}^-$ ion were dominant in groundwater. The Langelier Saturation Index and the Ryznar Stability Index showed low scaling potential of groundwater. In the analysis of vertical water temperature change, the geothermal gradient was estimated as $2.1^{\circ}C/100m$, which indicated the aquifer was enough for geothermal systems. In conclusion, groundwater is rich, can stably use geothermal heat, and it is less likely to cause deterioration of thermal energy efficiency by precipitation of carbonate minerals in study area. Therefore, the study area is suitable for installation of the combined geothermal system.