Conceptid (3090) | Preflabel |
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FCO2ANOM | Fugacity anomaly (water - air) of carbon dioxide {CO2 CAS 124-38-9} in the water body |
FCO2ECAL | Fugacity of carbon dioxide {CO2 CAS 124-38-9} {fCO2} in the experiment water sample by computation |
FCO2EQTX | Fugacity of carbon dioxide {fCO2 CAS 124-38-9} in the water body by equilibration with air, drying and constant temperature non-dispersive infra-red gas analysis and computation from pCO2 corrected to 1 bar at 100% humidity |
FCO2IG02 | Fugacity of carbon dioxide {fCO2 CAS 124-38-9} in the atmosphere by drying and constant temperature non-dispersive infra-red gas analysis and computation from pCO2 corrected to 1 bar at 100% humidity |
FCO2TK02 | Fugacity of carbon dioxide {fCO2 CAS 124-38-9} in the water body by equilibration with air, drying and constant temperature non-dispersive infra-red gas analysis and computation from pCO2 corrected to 1 bar at 100% humidity at in-situ temperature (Takahashi correction) |
FCO2WCAL | Fugacity of carbon dioxide {CO2 CAS 124-38-9} {fCO2} in the water body by computation |
FCO2WTAT | Fugacity of carbon dioxide (at 100% humidity) {CAS 124-38-9} in the atmosphere |
FCO2XXXX | Fugacity of carbon dioxide (at 100% humidity) {fCO2 CAS 124-38-9} in the water body |
FCSDECAL | Fugacity standard deviation of carbon dioxide {CO2 CAS 124-38-9} {fCO2} in the experiment water sample by computation |
FCSDWCAL | Fugacity standard deviation of carbon dioxide {CO2 CAS 124-38-9} {fCO2} in the water body by computation |
FE56MSPW | Enrichment of total iron-56 {total_56Fe CAS 14093-02-8} {delta(56)Fe} in the sediment pore water [dissolved plus reactive particulate <0.2um phase] by anion exchange chromatography and inductively-coupled plasma mass spectrometry |
FE56SDPW | Enrichment standard deviation of total iron-56 {total_56Fe CAS 14093-02-8} {delta(56)Fe} in the sediment pore water [dissolved plus reactive particulate <0.2um phase] by anion exchange chromatography and inductively-coupled plasma mass spectrometry |
FE57MSPW | Enrichment of total iron-57 {total_57Fe} {delta(57)Fe} in the sediment pore water [dissolved plus reactive particulate <0.2um phase] by anion exchange chromatography and inductively-coupled plasma mass spectrometry |
FE57SDPW | Enrichment standard deviation of total iron-57 {total_57Fe} {delta(57)Fe} in the sediment pore water [dissolved plus reactive particulate <0.2um phase] by anion exchange chromatography and inductively-coupled plasma mass spectrometry |
FELSCVD5 | Log ligand binding strength of iron-complexing organic ligands {Fe_org_ligands} in the water body [dissolved plus reactive particulate <0.2um phase] by filtration and cathodic stripping voltammetry |
FELSCVDN | Log ligand binding strength of iron-complexing organic ligands {Fe_org_ligands} in the water body [dissolved plus reactive particulate <10**6 Dalton phase] by filtration and cathodic stripping voltammetry |
FELSCVE6 | Log ligand binding strength standard error of iron-complexing organic ligands {Fe_org_ligands} in the water body [dissolved plus reactive particulate <0.2um phase] by filtration and cathodic stripping voltammetry |
FELSCVLL | Log ligand binding strength of iron-complexing organic ligands (iron-complexing, lower limit calculated from filtered (<0.2um) Fe) in the water body [dissolved plus reactive particulate phase] by cathodic stripping voltammetry |
FELSCVUL | Log ligand binding strength of iron-complexing organic ligands (iron-complexing, upper limit calculated from unfiltered iron concentration) in the water body [dissolved plus reactive particulate phase] by cathodic stripping voltammetry |
FELSCVZZ | Log ligand binding strength of iron-complexing organic ligands {Fe_org_ligands} in the water body [dissolved plus reactive particulate phase] by cathodic stripping voltammetry |
FEMNGS01 | Proportion of particles (Fe-Mn nodules) in the sediment 160-315um |
FEMNGS02 | Proportion of particles (Fe-Mn nodules) in the sediment 315-630um |
FEMNGS03 | Proportion of particles (Fe-Mn nodules) in the sediment 630-1250um |
FEMNGS04 | Proportion of particles (Fe-Mn nodules) in the sediment 1250-2500um |