Coastal sources, sinks and strong organic complexation of dissolved cobalt within the US North Atlantic GEOTRACES transect GA03
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
Coastal sources, sinks and strong organic complexation of dissolved cobalt within the US North Atlantic GEOTRACES transect GA03 ; volume:14 ; number:11 ; year:2017 ; pages:2715-2739
Biogeosciences ; 14, Heft 11 (2017), 2715-2739
- Urheber
-
Noble, Abigail E.
Ohnemus, Daniel C.
Hawco, Nicholas J.
Lam, Phoebe J.
Saito, Mak A.
- DOI
-
10.5194/bg-14-2715-2017
- URN
-
urn:nbn:de:101:1-2017110125197
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:21 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Noble, Abigail E.
- Ohnemus, Daniel C.
- Hawco, Nicholas J.
- Lam, Phoebe J.
- Saito, Mak A.
Ähnliche Objekte (12)
Cobalt Deposition from Ionothermally Dissolved Cobalt Oxides
Sources, sinks, and cycling of dissolved organic copper binding ligands in the ocean
Overlooked shelf sediment reductive sinks of dissolved rhenium and uranium in the modern ocean
Anthropological Urban Transect
Colloid-bound and dissolved phosphorus species in topsoil water extracts along a grassland transect from Cambisol to Stagnosol
Spontaneous Isomerization [trans-B20H18]2– → [iso-B20H18]2– during Cobalt(II) Complexation with Phenanthroline
8. Sources and sinks.
Fractional nonlinear energy sinks
Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
Stable carbon isotopes of dissolved inorganic carbon for a zonal transect across the subpolar North Atlantic Ocean in summer 2014
Cobalt‐Ion Superhygroscopic Hydrogels Serve as Chip Heat Sinks Achieving a 5 °C Temperature Reduction via Evaporative Cooling
Cobalt Deposition from Ionothermally Dissolved Cobalt Oxides
Sources, sinks, and cycling of dissolved organic copper binding ligands in the ocean
Overlooked shelf sediment reductive sinks of dissolved rhenium and uranium in the modern ocean
Anthropological Urban Transect
Colloid-bound and dissolved phosphorus species in topsoil water extracts along a grassland transect from Cambisol to Stagnosol
Spontaneous Isomerization [trans-B20H18]2– → [iso-B20H18]2– during Cobalt(II) Complexation with Phenanthroline
8. Sources and sinks.
Fractional nonlinear energy sinks
Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
Stable carbon isotopes of dissolved inorganic carbon for a zonal transect across the subpolar North Atlantic Ocean in summer 2014
Cobalt‐Ion Superhygroscopic Hydrogels Serve as Chip Heat Sinks Achieving a 5 °C Temperature Reduction via Evaporative Cooling
Cobalt Deposition from Ionothermally Dissolved Cobalt Oxides
Sources, sinks, and cycling of dissolved organic copper binding ligands in the ocean
Overlooked shelf sediment reductive sinks of dissolved rhenium and uranium in the modern ocean
Anthropological Urban Transect
Colloid-bound and dissolved phosphorus species in topsoil water extracts along a grassland transect from Cambisol to Stagnosol
Spontaneous Isomerization [trans-B20H18]2– → [iso-B20H18]2– during Cobalt(II) Complexation with Phenanthroline
8. Sources and sinks.
Fractional nonlinear energy sinks
Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
Dissolved Pb and Pb isotopes in the North Atlantic from the GEOVIDE transect (GEOTRACES GA-01) and their decadal evolution
Stable carbon isotopes of dissolved inorganic carbon for a zonal transect across the subpolar North Atlantic Ocean in summer 2014