ScholarWorks@Korea University: YUN, Seong Taek

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YUN, Seong Taek (윤성택)

College of Science (Department of Earth and Environmental Sciences)

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Tel 02-3290-3176
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CO2 leakage:13||Hydrochemistry:11||Korea:10||hydrochemistry:7||South Korea:7||Groundwater:7||Heavy metals:6||Seoul:5||Nitrate:5||Groundwater contamination:4||Carbon capture and storage:4||hydrogeochemistry:4||CO2rich springs:3||Arsenic:3||heavy metals:3||Monitoring:3||CO2rich groundwater:3||geochemistry:3||waterrock interaction:3||fluid inclusions:3||Environmental forensics:3||Geological CO2 storage:3||Balneotherapy:3||stable isotopes:3||Denitrification:3||Soil moisture content:2||Deep groundwater:2||Vanadium:2||Reactive media:2||Volume and porosity change:2||Fluid inclusion Introduction:2||Sulfate reduction:2||Sensitivity analysis:2||Selforganizing map (SOM):2||Principal component analysis (PCA):2||Artificial tracer:2||Chemical properties:2||Particle:2||Redox condition:2||Scoria:2||Leakage:2||반응성 용질 이동 모델링:2||Reactive transport modeling:2||Microbial community:2||Geological storage:2||CO2 storage site:2||Immunomodulation:2||Modelbased clustering:2||Contaminated groundwater:2||Deep saline aquifer:2||Cobalt deposit:2||topographical landscape:2||Nearsurface environment:2||Agrolivestock farming:2||Crystalline bedrock aquifer:2||Dynamic factor analysis:2||CO2:2||Kangwon district:2||thermal groundwater:2||Kwangyang:2||theme tourism courses:2||Agrolivestock farming area:2||Vadose zone:2||Natural analogue:2||Mineral waters:2||Principal component analysis:2||urban groundwater:2||trace metals:2||2line ferrihydrite:2||aquifer geology:2||Gyeryongsan national park:2||tourist resources:2||Nitrate contamination:2||CO2rich spring:2||Geogenic source:2||Sulfur and oxygen isotopes of sulfate:2||Hydrogeochemistry:2||Adsorption:2||Atopic dermatitis:2||Waterrock interaction:2||Jeju Island:2||pH:2||Geologic CO2 Sequestration:2||Concurrent injection of SO2:2||Disposal efficiency:2||acid mine drainage:2||nitrogen isotope:2||groundwater quality:2||natural analogue:2||Effective dynamic efficiency:2||Urban groundwater:2||shallow aquifer:2||Acid mine drainage:2||Chemical vapor condensation:2||geologic control:2||Groundwater pollution:2||nitrate pollution:2||Machine learning:2||Noble gas tracing:2||Soil:2||CO2waterrock interaction:2||Redox geochemistry:2||seawater mixing:2||Zinc:2||Mineralogy:2||geomorphological fieldwork:2||Sulfide precipitation:2||Positive matrix factorization:2||temporal changes:1||bacteria:1||CO2 release:1||Geochemical groups:1||trace metal:1||Wellbased denitrification biobarrier (WDB):1||Carbon isotope ratio:1||Nitrate contamination of groundwater:1||Ordinary cokriging (OCK):1||Contamination probability map:1||Shallow groundwater:1||Compositional data analysis:1||Fuzzy cmeans (FCM) clustering:1||Raman lidar:1||CO2 leakage remote sensing:1||Tetracycline:1||Indicator:1||probability density function (PDF):1||Soil contamination:1||Mine drainage:1||Unsaturated zone travel time:1||Scenario:1||waterrockCO2 interaction:1||Risk management:1||Multiple endmembers mixing modeling:1||Bacterial sulfate reduction:1||geologic storage:1||exposure assessment:1||Heterogeneous fluvial aquifer:1||Crop intake pathway:1||Basaltic soils:1||Polyamide:1||Copper sulfide:1||Hydrochemical parameters:1||Finite normal (Gaussian) mixture model:1||Methanogenesis:1||Bedrock groundwater quality:1||Geochemical modeling:1||SelfOrganizing Map (SOM) approach:1||Indoor air quality:1||crystallization reagent:1||Formic acid:1||NOx:1||Star block copolymer:1||limestone terrain:1||Cytokines:1||Nuclear waste disposal:1||Surface complexation:1||Remediation of polluted soils:1||Uncertainty estimation:1||Roadway tunnel:1||Military air weapons shooting:1||Sorption mechanisms:1||riverside agricultural field:1||hydrochemistry and environmental isotopes:1||Shallow alluvial aquifer:1||Factorial kriging:1||Redox control of agricultural contaminants:1||Carbonate precipitates:1||water quality:1||지구화학:1||Subway tunnel seepage:1||Dissolved Mn and Fe:1||acid and alkaline rains:1||sulfaterich geothermal water:1||geothermometer:1||west sea of South Korea:1||kaolinte clay:1||atmospheric pollution:1||OFKOREA:1||STABLEISOTOPE:1||SOUTHKOREA:1||cluster analysis:1||Mankyeong watershed:1||5가 비소(비산염):1||hydrothermal goldsilver deposits:1||meteoric water interaction:1||지중(지질) 처분:1||tunnel seepage water:1||우라늄 이동 및 흡착:1||riverside alluvium:1||물질흐름분석:1||자원관리:1||Exhumation stage:1||Mesothermal gold:1||Bismuth mine:1||Hydrothermal:1||Natural attenuation:1||Inherent tracers:1||bedrock aquifer:1||& nbsp:1||(LDGP):1||Fecal microorganism:1||Classification model:1||Soil CO2 flux:1||CO2 origin:1||δ13CCO2:1||Water chemistry and environmental isotope:1||geogenic soil CO2 flux:1||Welllog estimation:1||Hierarchical cluster analysis (HCA):1||Transit time:1||Carbon capture and storage (CCS):1||lithofacies interpretation:1||Methanogen:1||CO2 sequestration:1||Geochemical tracing:1||Subsurface properties:1||Nitrification and denitrification:1||CO2rich spring water:1||Sulfide oxidation pathways:1||RDX:1||Scenedesmus:1||trend analysis:1||Pearson correlation:1||Wavelet based clustering:1||Geochemical indicators of mining impacts:1||Delayed gravitational flow:1||Pointsource pollutant loading:1||Numerical modeling:1||controlled release test:1||Stormwater:1||River water quality:1||carbon dioxide:1||leakage detection:1||ecosystems:1||microorganisms:1||plants:1||Titanium dioxide:1||Water type:1||Alginate bead:1||Crystallization:1||Dual isotopes:1||Bacterial sulfate reduction (BSR):1||Arsenate:1||sulfide crystallization:1||V4+/5+:1||Photocatalysis:1||Fenton reaction:1||Advanced oxidation technology:1||Visible light activity:1||Removal of agricultural nitrate:1||Rice paddy soil:1||Toxicity:1||calcite dissolution:1||Geostatistical approaches:1||Air pollution:1||Nanoparticle:1||colour:1||Spatial variation of nitrate:1||agricultural pollution:1||심부 암반 대수층:1||광물 트래핑:1||speciation:1||zinc removal:1||geothermometers:1||MINING DISTRICT:1||MINE:1||mesothermaltype gold deposits:1||BoseongJangheung and Youngdong areas:1||sedimentary terrain:1||sulphate:1||OH isotopes:1||water chemistry:1||magnetic material:1||태백산 광화대:1||부화도:1||Tourism geology:1||지질:1||groundwater mixing1. INTRODUCTIONOne of the most common concerns for drinking waterquality in relation to human health in rural areas is thegroundwater polution:1||Oxygen and hydrogen isotopes:1||toluene:1||Autoregressive lithofacies:1||Kmeans cluster analysis:1||Diesel:1||Water saturation:1||Monitoring well network:1||Artificial injection test:1||Carcass leachate leakage:1||Groundwaterlevel fluctuation:1||Potential risk:1||GCHRMS:1||Chemical indicators:1||Groundwater quality monitoring:1||Isometric logratio (ILR) transformation:1||controlling factors:1||earthquake:1||evolutionary process:1||Fumarate:1||Biological heterotrophic denitrification:1||spectral facies:1||Nitrogen loading:1||CO2 capture and storage (CCS):1||Nearsurface geochemical monitoring:1||Leakage of carcass leachate:1||Rulebased percolation model:1||Hydrogeochemistry and quality:1||Aminefunctionalized acrylic fiber:1||Real industrial plating wastewater:1||photodegradation:1||quantitative index for distribution shift (QI(shift)):1||hydrogeochemical modeling:1||cybertwin:1||Subagging regression method:1||Freshening of salinized aquifer:1||Uncertainty analysis:1||Urban mining:1||Geochemical monitoring:1||Photooxidation:1||UVLED:1||Human health risk assessment:1||Desalination:1||Targeted removal:1||Rural groundwater:1||Nanoparticles:1||Reverse ion exchange:1||Low temperature:1||Mesocosm:1||Stable isotopes:1||Vehicle emission:1||nephrite:1||Permeable reactive barrier:1||Dyeing industry complex:1||Republic of Korea:1||Statistics:1||Oxbow lake:1||Synthetic coal fly ash aggregate:1||이산화탄소 지중처분:1||carbonate minerals:1||부피 및 공극률 변화:1||처분 효율:1||Kwangyang mine, South Korea:1||adsorption kinetics:1||기술 동향:1||Sobaegsan Massif:1||roadside sediments:1||multivariate statistics:1||지하수 환경:1||groundwater environment:1||geochemical models:1||Carlintype Au deposit:1||geological and geomorphological landscape resources:1||Fluid inclusion:1||Bedrock aquifer:1||Riverbank filtration:1||Carbon capture, utilization, and storage:1||Net zero:1||Area of effective electric field:1||Soil fertility:1||Resilience:1||External forces:1||Oxygen and hydrogen isotopes of precipitation:1||Hydrochemical processes:1||Heavy metal(loid)s:1||Specific gravity:1||Distribution mechanism:1||Data labeling and feature selection:1||soil contamination:1||Soil contaminants:1||Metal(loid)s:1||Hydrogeochemical characterization:1||EU policies:1||Groundwater pollution index (GPI):1||CO2 flux:1||Sewage and pit latrine:1||Groundwater nitrate:1||CFCs dating and dual nitrate isotopes:1||seismically inactive:1||Soil CO2 efflux:1||archaea:1||Metal contamination:1||welllog data:1||Nitrogen application limit:1||High soil CO2:1||N2O:1||CO2induced geochemical processes:1||Livestock mortality burial pits:1||Supervised classification scheme:1||Pollutant loading:1||Monitoring network design:1||Enhanced weathering:1||Soil surface CO2 flux:1||Ground and surface water in mine area:1||Ion exchange fiber:1||Chromium(VI):1||alkaline hydrolysis:1||Electrospun nanofibrous membranes:1||Antifouling:1||Jeju:1||monitoring:1||Bentonite:1||Source identification:1||Multiresolution crosscorrelation:1||Unsaturated zone:1||Cyberphysical system (CPS):1||Organic solvent:1||Soil enzymes:1||elemental carbon:1||workplace:1||environmental impact assessment:1||Natural analogue study:1||Bioconcentration factor (BCF):1||Geochemical conditions:1||Molecular layerbylayer:1||Nanoscale palladium/zerovalent iron:1||Calciumcoated sand:1||Anthropogenic polluted level:1||National Groundwater Monitoring Network of South Korea:1||Contamination:1||2Line ferrihydrite:1||Sorption kinetics:1||NO2:1||결정화 시약:1||유동층 반응기:1||황화물 결정화:1||NH3SCR activity:1||Hydrophobicity:1||coastal shallow groundwater:1||CD4(+) T cells:1||Geologic carbon storage:1||Voltammetry:1||Colloid:1||Estimation of spatial extent and volume of polluted soil:1||Substrates:1||North Westland:1||Li normalization:1||Trace metals:1||National groundwater monitoring station:1||Nitrogen and oxygen isotopes:1||contamination model:1||modelbased clustering:1||탄산염 광물:1||geologic alkaline source:1||anthropogenic acidic source:1||geothermal potential:1||groundwater:1||batch dissolution:1||Seawater mixing index (SMI):1||land use and contamination:1||land use:1||distribution coefficient:1||lead [Pb(II)]:1||electrokinetic removal:1||soil pH:1||streams:1||rock weathering:1||FLUID INCLUSION:1||VEIN DEPOSITS:1||BEARING:1||MINERALIZATION:1||adsorption:1||hydrochemical modeling:1||denitrification:1||geochemical modeling:1||Daerae mine:1||metallogeny:1||mesothermal gold:1||central Inner Mongolia:1||transport and adsorption of uranium:1||magnetic monitoring:1||fluoride and fluorosis:1||비소/안티모니 이상대:1||national park:1||계룡산 국립공원:1||hydrogeochemical evolution:1||Granitoid:1||combustion:1||Fractionation:1||Iron:1||Inverse modeling:1||Chemical mass balance:1||geological heterogeneity:1||Hydrochemical indicators:1||natural background levels (NBLs):1||Carbon dioxide:1||System impact:1||Jeju Samdasoo watershed:1||Isotopic composition:1||Livestock burial:1||Gaussian Mixture Model (GMM):1||multivariate:1||Field evaluation:1||Petroleum hydrocarbons (PH):1||Leakage scenario:1||Deep geologic disposal:1||Underground research laboratory (URL):1||LCHRMS (Liquid chromatographyhighresolution mass spectrometry):1||Adit water:1||Nitrate Directive and Groundwater Directive:1||Temporal change:1||Urbanization:1||Bidirection LSTM (BiLSTM):1||Deepseated CO2:1||CO2 concentration measurement:1||Fiberoptic spectroscopy:1||electrical resistivity tomography:1||Hillslope:1||Geochemical Monitoring:1||Gaussian mixture model:1||rockcore digital images:1||Quantile regression:1||Vulnerability:1||Mountain recharge:1||Sequential Gaussian cosimulation (SGCS):1||Driving forces:1||Mine tailings and wastes:1||denitration:1||KCOSEM:1||Green engineering:1||Swelling:1||Groundwater level fluctuation:1||Water table fluctuation:1||Datadriven model:1||Processbased model:1||Data model:1||Early warning system (EWS):1||Transboundary river:1||Microbial community composition:1||Metamodeling:1||Rare earth ore deposits:1||carbon capture and storage:1||CO2rich water:1||Leaching experiments:1||Forward osmosis:1||Fedbatch fluidized bed reactor:1||Smoking room:1||Tobacco:1||Seawater intrusion:1||Nanocomposites:1||Sorption equilibria:1||National Groundwater Monitoring Network:1||Vanadium oxide:1||Chlorophenols:1||Copper:1||The urbanrural composite area:1||Intertidal sediments:1||heterogeneous alluvial aquifer:1||Riverside alluvium aquifer:1||Clustering of time course data:1||geologic CO2 sequestration:1||고염도 심부 대수층:1||isotopes:1||CO2rich and alkaline:1||CARBONDIOXIDE:1||흡착반응:1||흡착등온선:1||As(V) (arsenate):1||adsorption isotherm:1||geologic sequestration:1||geochemical concepts:1||Dalseong mine:1||gold:1||argonargon age:1||tectonics:1||schlumberger array:1||칼린형 금광상:1||자원이용지수:1||지형경관자원:1||Collision environment:1||Yucheon:1||Zn and Cd isotopes:1||hydrograph separation:1||Noble gas:1||Automated monitoring:1||CO2 exsolution:1||Iron oxyhydroxides precipitation:1||Livestock manurederived groundwater plume & nbsp:1||Uniformity coefficient:1||Recovery effort:1||Ground penetrating radar:1||Geochemical affinity:1||Suspect/nontarget screening:1||SNTS:1||2019 Green Deal:1||Climatology:1||Water management:1||Long shortterm memory (LSTM):1||Optical fiber sensor:1||Hollow core fiber:1||Photonic crystal fiber:1||CO2 flux:1||Reaction pathways and mixing:1||Headwater catchment:1||Metal source identification:1||CCS:1||Highstrength nitrate:1||multilayer neural network:1||Ammoniaoxidizing microbes:1||CH4:1||Carbon13 isotope:1||Pollution potential:1||Groundwater age:1||Recharge source:1||Monte Carlo simulation:1||Equilibrium phase modeling:1||pointbar alluvial setting:1||site investigation:1||nitramines:1||Graphene oxide:1||poly(vinylidene fluoride):1||Environmental impact assessment:1||Porous media:1||Visualization:1||Waste regeneration:1||Supercritical CO2:1||Groundwater quality:1||Mine pollution index:1||Air:1||Mining impacts:1||Sulfatesulfur and nitrateN isotopes:1||Geologic CO2 sequestration:1||Ionadsorption:1||CCS monitoring:1||Dermatitis:1||Cyanide:1||Soil analytical method:1||Jeju Island groundwater:1||Thin film composite membranes:1||Sodium sulfide pentahydrate:1||Orthogonal regression of PCA:1||CO:1||Chemical vapor condensation (CVC):1||Psoriasis:1||Xray absorption spectroscopy:1||fluidized bed reactor:1||heavy metal:1||중금속:1||Photocatalytic degradation:1||Porphyrin:1||Heterogeneous alluvial aquifer:1||hydrogeochemical modelling:1||Granitic rocks:1||Gypsum and carbonates:1||Recharge:1||Denitrifying bacteria:1||weathering rind:1||Geochemical dispersion:1||Sequential extraction:1||Zeolitic rocks:1||multilevel monitoring:1||Dams, Rockfill:1||Sinkholes:1||mixture model:1||Jungwon area, Korea:1||anodic striping voltammetry (ASV):1||fluorine:1||cation exchange:1||Langmuir and Freundlich isotherms:1||enhancement:1||alluvial groundwater:1||As(III) (arsenite):1||Pocheon spaland area, Korea:1||이산화탄소 배출량 조절 및 저감:1||anodic stripping voltammetry (ASV):1||breccia pipe CuW mineralization:1||지화학 모델:1||지속가능한:1||Mining area:1||A longrange spatial information:1||Solubilitytrapping:1||Performance indicator:1||Key performance indicators:1||Leachate from poultry burial:1||Electrokinetic remediation:1||bottled water:1||Pervasive agricultural contamination:1||Natural attenuation potential:1||CO2 release experiment:1||Site characterization:1||Fracture:1||machine learning:1||TPH:1||Sulfide oxidation:1||Human risk assessment:1||Annual emission:1||Electrical resistivity:1||Biomarker:1||Carcass leachate:1||Compositional data analysis (CoDa):1||Robust principal component analysis (RPCA):1||Spatial model:1||Periurban, Mongolia:1||Legacy effect:1||nonvolcanic and:1||Endmember mixing analysis (EMMA):1||Meteorological:1||CO2 mass:1||Stable isotope:1||Dissolved silica:1||Soil acidification:1||Streamaquifer interaction:1||Spatial distribution of soil contaminants:1||Waveletbased multiresolution analysis:1||Fixedbed column:1||Nanomaterial recycling:1||nitrate:1||Alteration:1||quantitative index for distribution pattern (QI(tail)):1||Zincconcentrates:1||Behavior of metals:1||CO2 concentration:1||Chemical accident:1||carbon dioxide geologic storage:1||VOCs:1||Metal plating wastewater:1||Fe2O3carbon foam:1||Northern Mongolia:1||Pyrosequencing:1||Diversity:1||Preservation:1||Recycling:1||carbon nanotube:1||Multilevel sampling:1||Isotopes:1||pH neutralization:1||Photocatalyst:1||Hydroxyl radical:1||Geochemical controls:1||Bayesian mixing model (MixSIR):1||Normal (Gaussian) mixture model:1||Reaction path:1||Classification and characterization:1||Daycare center:1||Roadside:1||Impregnation:1||Agricultural contamination:1||Skin inflammation:1||Dedolomitization:1||Speciation:1||Discharge:1||USA and EU:1||New Zealand:1||Mass balance modeling:1||Korea, South:1||Groundwater mixing:1||mineral trapping:1||reactive transport model:1||Water quality:1||Jecheon:1||Bugok:1||nonparametric statistical analysis:1||stream sediment:1||sequential extraction:1||mineral equilibrium:1||3가 비소(아비산염):1||hydrologic mixing:1||fluid geochemistry:1||riverside alluvial aquifer:1||sulfur isotope:1||Sangju area:1||pollution:1||vertical Electric Sounding (VES):1||roadside dust:1||Mt. Taebaek mining district:1||alluvial groundwaters:1||chemical accident:1||metabolomics:1||Longand shortterm memory:1||Bidirectional long and shortterm memory:1||Sulfate:1||karstic spring:1||flow type:1||Physicochemical stratification:1||Carbon mineralization:1||Electrode configuration:1||Hydrogeochemical tracer:1||Siliciclastic aquifers:1||Groundwater recharge:1||geoscience data (geodata):1||Oxidative treatment:1||Nextgeneration sequencing:1||Geochemical mixing model:1||groundwater nitrate:1||volcanic area:1||Global warming:1||Groundwater Quality Index (GQI):1||Livestock farming:1||Conditional variational autoencoder:1||Probabilistic estimation:1||Carbon isotope:1||Carbon dioxide capture and storage:1||groundwater ecosystems:1||Crystalline bedrock:1||Stable Pb isotope:1||longterm impact:1||Metal(loid)s leaching:1||Portable Xray fluorescence (PXRF) and ICPAES:1||Urban water management:1||riverbank filtration:1||subsurface geology:1||Breakthrough curve model analysis:1||Monitoring technique:1||Convection:1||pH indicator:1||Endoflife products:1||Shrinkage:1||Wavelet analysis:1||Crosscorrelogram:1||CyberPhysical System (CPS):1||Cation exchange:1||Land surface:1||Risk assessment:1||black carbon:1||nanomaterial:1||bioindicators:1||Permeable reactive kiddle:1||Heavy metal contamination:1||Occurrence:1||Trichlorophenol:1||Background level and threshold of nitrate:1||Shallow alluvial groundwater:1||Natural versus anthropogenic processes:1||Heat treatment:1||Geological CO2 sequestration:1||Bath:1||Bedrock groundwater:1||NC/Nga mice:1||Tungsten oxide:1||HaCaT cells:1||Hydrogeochemical evolution:1||Clay mineralogy:1||Onroad measurement:1||Geologic CO2 storage:1||environmental regulatory framework:1||groundwater recharge:1||Hydrogeology:1||Rare earth elements:1||Coal fly ash:1||deep bedrock aquifer:1||반응성 용질 이동 모델:1||이산화탄소 지중 처분:1||이산화황의 동시 주입:1||Hydrochemical modeling:1||rainwater chemistry:1||spa:1||granite and biotite:1||coastal groundwater:1||anthropogenic contamination:1||volatile organic compounds:1||sorption:1||0.1 NHCl extraction:1||reservoir temperature:1||redox reaction:1||factor analysis:1||흡착반응속도론:1||control and reduction of CO2 emissions:1||technological development:1||지화학적 개념:1||mine drainage:1||reactive transport models:1||heavy metal pollution:1||bedrock groundwater:1||As/Sb anomaly:1||Mobility:1||Enrichment factor:1||Functional enzyme (nirS, nosZ):1||16s rRNA:1||Lithofacies sequence estimation:1||Geophysical welllog data:1||Integrated hydrochemical index:1||Recharge altitude:1||Sources:1||Gold mining and processing:1||During and after drilling:1||Hotspot:1||Highlevel radioactive waste (HLW):1||Contamination plume:1||environmental forensics:1||Soil leachate:1||sustainable management:1||soil CO2:1||Logistic mixture:1||

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