The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment in the Atlantic sector of the Southern Ocean deviates strongly from ambient natural waters. Three iron additions (ferrous sulfate solution) were conducted, resulting in elevated dissolved iron concentrations and significant Fe(II) levels. Repeated vertical profiles for dissolved (filtrate 200 kDa–200 kDa
The distribution of dissolved iron and its chemical speciation (organic complexation and redox speci...
The characteristics of the dissolved iron (DFe) binding organic ligands were determined during 3 Dut...
To investigate the biogeochemistry of iron in the waters of the European continental margin, we dete...
The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment i...
An in situ iron enrichment experiment was carried out in the Southern Ocean Polar Frontal Zone and f...
The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment i...
Measurements of Fe(II) and H2O2 were carried out in the Atlantic sector of the Southern Ocean during...
The chemical speciation of iron was determined in the Southern Ocean along a transect from 48 to 70°...
A transect across the eastern North Atlantic from 42°N, 23°W towards the European continental shelf ...
The distribution of dissolved iron and its chemical speciation (organic complexation and redox speci...
The characteristics of the dissolved iron (DFe) binding organic ligands were determined during 3 Dut...
To investigate the biogeochemistry of iron in the waters of the European continental margin, we dete...
The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment i...
An in situ iron enrichment experiment was carried out in the Southern Ocean Polar Frontal Zone and f...
The speciation of strongly chelated iron during the 22-day course of an iron enrichment experiment i...
Measurements of Fe(II) and H2O2 were carried out in the Atlantic sector of the Southern Ocean during...
The chemical speciation of iron was determined in the Southern Ocean along a transect from 48 to 70°...
A transect across the eastern North Atlantic from 42°N, 23°W towards the European continental shelf ...
The distribution of dissolved iron and its chemical speciation (organic complexation and redox speci...
The characteristics of the dissolved iron (DFe) binding organic ligands were determined during 3 Dut...
To investigate the biogeochemistry of iron in the waters of the European continental margin, we dete...