ScholarWorks@Hanyang University ERICA Campus: Hyun, Jung Ho

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Hyun, Jung Ho (현정호)

ERICA 공학대학 (ERICA 해양융합공학과)

Research Area: 해양미생물 생태/생지화학, 미생물해양학, 퇴적물 생지화학, Marine Microbial Ecology and Biogeochemistry, Microbial Oceanography, Sediment Biogeochemistry

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Sulfate reduction:16||Benthic nutrient flux:9||Yellow Sea:8||Ulleung Basin:7||East Sea:6||Iron reduction:5||Benthicpelagic coupling:4||Bacterial production:4||Antarctica:3||Amundsen Sea:3||Upwelling:3||Organic carbon oxidation:3||bacterial production:3||Ulleung basin:3||Polynya:3||East Sea (Japan Sea):3||Amundsen Sea polynya:3||sulfate reduction:3||Denitrification:2||Phytoplankton:2||Bioturbation:2||Genomics:2||biological pump:2||Organic carbon:2||16S rRNA gene:2||microbial loop:2||climate change:2||Sediment oxygen demand:2||Carbon remineralization:2||Aquaculture:2||Metatranscriptomics:2||Suaeda japonica:2||Sulfate reduction rate:2||Sulfatereducing bacteria:2||Yeongsan River estuary:2||gas hydrate:2||AOM:2||Han River estuary:2||aquaculture:2||Sulfurovum:2||Northeast equatorial pacific:2||iron reduction:2||CALANUSFINMARCHICUS:1||CARBON:1||CLIPPERTON FRACTUREZONE:1||CO2:1||COASTAL MARINESEDIMENTS:1||COMB. NOV:1||COMMUNITY:1||CONTINENTALMARGIN SEDIMENTS:1||CYTOPHAGAULIGINOSA ZOBELL:1||Carbon mineralization:1||Carbon neutrality:1||Carbon stable isotope ratios:1||Chromium reducible sulfur:1||ClarionClipperton Fracture Zone (CCFZ):1||Climate change:1||Colorimetric sensor:1||Continental margin:1||Convergence:1||Crassostrea gigas:1||DEEPOCEAN:1||DIATOMS:1||DILUTION:1||DISSOLVED ORGANICMATTER:1||DOC:1||DOM:1||Deep sea fauna:1||Dilution method:1||Dissolve Organic Matter:1||Dissolved organic matter:1||Divergence:1||Diversity:1||Drake passage:1||EAST SEA:1||EAST/JAPAN SEA:1||EEMPARAFAC:1||EGGPRODUCTION:1||ESTUARINE SEDIMENT:1||East sea (Japan sea):1||Eddy:1||Elemental sulfur:1||Environmental impact:1||Environmental impact assessment:1||Enzymatic extract:1||Epiphytes:1||Estuary:1||Expanded polystyrene:1||Fe and P cycles:1||Fe oxide:1||Fe(III) reduction:1||Fe2:1||Federated States of Micronesia:1||Feeding guild:1||Feeding pellet:1||Filtration methods:1||Fish farm:1||Fish farming:1||Freezing seawater:1||Freshwater Rinoff:1||Freshwater Sediments:1||GREENALGAE:1||Ganghwa intertidal sediment:1||Ganghwa intertidal wetland:1||Gas hydrate:1||Gas hydrates:1||Getz Ice Shelf:1||Glyoxylate:1||Grazing impact:1||Grazing rate:1||HEMIPELAGIC SEDIMENTS:1||HS:1||Halocynthia roretzi:1||Halophila nipponica:1||Heterotrophic Prokaryote:1||Heterotrophic bacteria:1||Heterotrophic dinoflagellates:1||Heterotrophy:1||Hg(II) methylation:1||Hg(II)methylating microbial communities:1||Hypoxic environment:1||INTACT SEDIMENT CORES:1||Impoundment:1||Inorganic Carbon:1||Inorganic Nutrient:1||Inorganic nutrients:1||Intertidal sediments:1||Intertidal wetland:1||Invasive Spartina anglica:1||Iron oxide:1||Japan Sea:1||Korean coast:1||LEVEL:1||Lake Shihwa:1||Latitudinal distribution:1||Leaching:1||Lipid biomarker:1||Longline oyster culture:1||Longline sea squirt and oyster aquaculture:1||MARINE ECOSYSTEMS:1||MARINESEDIMENTS:1||MATTER MINERALIZATION:1||MAXIMUMLIKELIHOOD:1||MEMBER:1||MICROBIAL FOODWEB:1||MPN counts:1||Macrophthalmus japonicus:1||Macrotidal environment:1||Macrozoobenthos:1||Manganese oxide:1||Manganese oxides:1||Manila clam:1||Marine aquaculture:1||Marine group:1||Mass balance:1||MeHg demethylation:1||Mesoscale spatial variations:1||Metabolic balance:1||Methane:1||Microbial:1||Microbial biomass:1||Microbial carbon pump:1||Microbial ecology:1||Microbial loop:1||Microbially induced carbonate precipitation:1||Microbiology:1||Microscopic enumeration:1||Mn nodule:1||Mn nodule mining:1||Mn oxide:1||Mycobacterium gilvum PYRGCK:1||NEC:1||NECC:1||NH4+:1||NORTHATLANTIC:1||Nanoand microzooplankton:1||Northeast Equatorial Pacifc:1||Nutrient dynamics:1||OITHONASIMILIS:1||ORGANICCARBON OXIDATION:1||OXYGEN MINIMUM ZONE:1||Ocean alkalinity:1||Ocean negative carbon emission:1||Organic Carbon:1||Organic carbon mineralization:1||Organic matter:1||Organicmatter removal:1||Outwelling:1||Oxygen minimum zone:1||Oxygen penetration:1||Oyster farm:1||P dynamics:1||P limitation:1||P regeneration:1||Pacific Ocean:1||Phaeocystis bloom:1||Phaesocystis antarctica:1||Phosphorus speciation:1||PhyloChip:1||Planctomycetes:1||Plastic debris:1||Polar front:1||Polycyclic aromatic hydrocarbons:1||Pore water:1||Primary production:1||Prokaryotic Abundance:1||Prokaryotic heterotrophic production:1||Proteomics:1||Protozooplankton:1||Pylaiella littoralis:1||RECLASSIFICATION:1||RNASIP:1||Radical scavenging activity:1||Rhizosphere:1||River:1||S cycles:1||SALTMARSH SEDIMENTS:1||SEQUENCES:1||SMTZ:1||SPRING BLOOMS:1||SULFATE REDUCTION:1||SURFACE SEDIMENTS:1||Salinity:1||Seawater warming:1||Sediment:1||Sediment Core Incubation:1||Sediment oxygen consumption:1||Shikimate:1||Source identi fication index:1||Sov2:1||Spartina anglica:1||Standards of practice:1||Storage of bacterial cells:1||Styrene oligomers:1||Sulfidic conditions:1||Sulfuroxidizing bacteria:1||Sulphidic environment:1||Surface Mixed Layer:1||Synechococcus:1||TRFLP:1||TIDAL FLAT SEDIMENT:1||TREES:1||TROPHIC INTERACTIONS:1||Thaumarchaeota:1||Total Nitrogen:1||Total oxygen uptake:1||Total sediment oxygen uptake:1||Total volatile basic nitrogen (TVBN):1||Typhooninduced rainfall:1||Ulleung warm eddy:1||Uncoupling:1||Vegetated intertidal sediment:1||Vertical distribution:1||Viability:1||Water column structure:1||Western Scotia Sea:1||YSCW:1||YSWC:1||Yellow Sea Cold Water:1||Yellow Sea Warm Current:1||Yeongsan River dyke:1||Zostera marina:1||anticyclonic eddy:1||bacterial respiration:1||bacterioplankton:1||benthic environment:1||benthic microbial community:1||benthic nutrient flux:1||benthicpelagic coupling:1||biogenic apatite P:1||biogeochemistry:1||biological carbon pump:1||biological invasion:1||burrow:1||carbon cycling:1||carbon sequestration:1||cellulose:1||ciliates:1||circumpolar deep water:1||continental slope and rise:1||copepod nauplii:1||deepsea sediment:1||dilution:1||dissolved organic carbon (DOC):1||disturbance:1||divergence:1||dsrAB gene:1||eacterioplankton:1||environmental gradients:1||facultative methanotrophy:1||feeding behavior:1||food sensor:1||freshness monitoring:1||fungi:1||global climate change:1||heterotrophic dinoflagellates:1||heterotrophic nanoflagellates:1||hgcA gene:1||intertidal sediment:1||intertidal wetland:1||intrathermocline eddy:1||macrofauna:1||manganese reduction:1||marginal seas:1||marine sediment:1||mcrA gene:1||meltwater:1||microbial community:1||microbial community structure:1||microbial diversity:1||mixotrophy:1||mudflat:1||nanoand microzooplankton:1||northeast equatorial Pacific:1||nutrients:1||organic carbon:1||organic carbon mineralization:1||organic carbon oxidation:1||phosphorus speciation:1||phytoplankton community composition:1||polynya:1||rainfall:1||salimity:1||screening:1||sediment trap:1||sedimentderived DOM:1||sedimentwater interface:1||sizefractionated phytoplankton:1||spring bloom:1||sulfatemethane transition zone:1||thiotrophy:1||tidal flat:1||upwelling:1||west coast of Korea:1||wetland:1||xylanase:1||담수 퇴적물:1||빈산소 환경:1||시화호:1||알루미늄 결합 인:1||영산강 하구:1||영양염:1||영양염 용출:1||유기물 분해:1||유기탄소:1||인 존재형태:1||저층 용출:1||퇴적물 코어 배양법:1||황산염 환원:1||16S rRNASIP:1||1944 REICHENBACH 1989:1||3,5dinitrosalicylic acid:1||ACID VOLATILE SULFIDE:1||ANAEROBIC AMMONIUM OXIDATION:1||ATP:1||Abalone:1||Abundance:1||Acetateoxidizing bacteria:1||Acid volatile sulfide:1||Aluminum bound phosphorus:1||Amplicon sequencing:1||Amundsen Sea Polynya:1||Anaerobic ammonium oxidation:1||Anaerobic oxidation of methane:1||Antarctic:1||Antioxidant activity:1||Aquaculture impacts:1||Archaeal diversity:1||Artificial dyke:1||BACTERIAL SULFATE REDUCTION:1||BCG:1||BENTHIC DENITRIFICATION:1||Bacteria:1||Bacterial cell number:1||Bacterial growth:1||Bacterial growth efficiency:1||Bacterial indicator:1||Bacterial respiration:1||Bacterioplankton:1||Behavior:1||Benthic–pelagic coupling:1||Benthic C oxidation:1||Benthic Flux:1||Benthic P flux:1||Benthic flux:1||Benthic metabolism:1||Benthic microbial communities:1||Biodeposit:1||Biological pump:1||Bottom Water:1||

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