ScholarWorks@Korea University: Lee, Seung hak

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Lee, Seung hak (이승학)

Graduate School of Energy and Environment (KU-KIST GREEN SCHOOL)

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Vadose zone:8||Environmental forensics:5||Aquifer storage and recovery:4||Source identification:4||Arsenic:4||Injection capacity:3||Groundwater vulnerability:2||Dissimilatory iron reduction:2||Water quality:2||Uniformity coefficient:2||Mapping:2||Diesel:2||Unresolved complex mixture (UCM):2||Sensitivity analysis:2||Soil contamination:2||Refined petroleum products:2||Deep saline aquifer:1||Redox sensitive behavior:1||Sphalerite:1||Natural attenuation:1||Pore network:1||Soil texture:1||Petroleum hydrocarbons:1||Remobilization:1||Sewage sludge:1||Release properties:1||Alginate bead:1||Sorption:1||Fate and transport:1||Visible light activity:1||Titanium dioxide:1||Managed aquifer recharge (MAR):1||Water security:1||Water saturation:1||Nitrate:1||Water saturation degree:1||Groundwaterlevel fluctuation:1||Potential risk:1||Soil microbiome:1||Mobile–immobile model:1||Environmental sustainability:1||Phosphorous recovery:1||Lead isotope:1||Targeted removal:1||Photocatalytic oxidation:1||Seepage velocity:1||Wettingdrying cycle:1||Riverbank filtration:1||Specific capacity:1||Damkohler number:1||Inverse estimation:1||Antimony oxyanions:1||Density functional theory calculations:1||Facetmediated interactions:1||Longterm operation:1||Metal contamination:1||Geogenic source:1||Zinc contamination:1||Nanoscale palladium/zerovalent iron:1||Microbedriven iron reduction:1||Petroleum:1||Thinlayer chromatography (TLC):1||Iron:1||Inverse modeling:1||Chemical mass balance:1||Franklinite:1||Sand filtration:1||Soil organic matter:1||Wetdry cycle:1||Petroleum hydrocarbons (PH):1||Random forest model:1||Calcium silicate hydrates:1||Zinc smelter:1||Sand:1||Inorganic oxidant:1||Alternative electron acceptor:1||Sunscreen:1||Soil column experiment:1||Soil remediation:1||Extraction capacity:1||Skin layer:1||Leaky aquifers:1||Microbial community structure:1||Denitrification:1||Infiltration:1||Ferrihydrite:1||Boehmite:1||Attenuation capacity:1||Metal source identification:1||Natural organic matter:1||Zinc oxide:1||Gas chromatography:1||Attachment efficiency:1||Natural attenuation potential:1||Breakthrough curve:1||Ensemble smoothing:1||Variabledensity flows:1||Dissolved organic carbon attenuation:1||Iron (hydr)oxides:1||Aquifer storage recovery:1||Xray absorption spectroscopy:1||Retardation factor:1||La/CuFe3O4 nanocapsules:1||Phosphate recovery:1||Water disinfection:1||TiO2 nanoparticle:1||Sulfate:1||Pumping capacity:1||Groundwater recharge:1||Organic compounds:1||Electromagnetic control:1||Soil properties:1||Stable Pb isotope:1||Trichlorophenol:1||Charge separation:1||Swimming pool:1||Risk assessment:1||Titanium dioxide nanoparticle:1||Nanoparticle transport:1||Total petroleum hydrocarbons (TPH):1||Minnesota:1||Wellbore storage:1||Microplastics:1||Multiple contaminant sources:1||3D heterogeneous aquifer:1||Nitratedependent iron oxidation:1||Bioattenuation:1||Multiple linear regression:1||Adsorption kinetics:1||

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