Seasonal variation in dissolved aluminium concentrations in coastal waters and biological limitation of the export of the riverine input of aluminium to the deep sea

Horizontal gradient of the chemical speciation of iron in surface waters of the northeast Atlantic Ocean

“…In contrast with manganese and iron, the aluminium concentration decreased again in the Channel waters after the boundary. The aluminium concentrations found for the Atlantic and the Channel are in reasonable agreement with those found previously (Measures, 1995;Hydes, 1989). The different behaviour of aluminium is in line with expectation: for instance, in the Pacific, aluminium shows clearly its atmospheric source followed by a decrease by scavenging and an increase due to remobilization (Orians and Bruland, 1986); iron on the other hand follows a clear nutrientlike behaviour (Martin et al, 1989).…”

Horizontal gradient of the chemical speciation of iron in surface waters of the northeast Atlantic Ocean

“…In contrast with manganese and iron, the aluminium concentration decreased again in the Channel waters after the boundary. The aluminium concentrations found for the Atlantic and the Channel are in reasonable agreement with those found previously (Measures, 1995;Hydes, 1989). The different behaviour of aluminium is in line with expectation: for instance, in the Pacific, aluminium shows clearly its atmospheric source followed by a decrease by scavenging and an increase due to remobilization (Orians and Bruland, 1986); iron on the other hand follows a clear nutrientlike behaviour (Martin et al, 1989).…”

The role of sea ice formation in cycling of aluminium in northern Marguerite Bay, Antarctica

“…Our dissolved Al concentration concentrations from northern Marguerite Bay are consistent with published values for the Weddell Sea, ranging from 8-22 nM (van Bennekom et al, 1991;Sañudo-Wilhelmy et al, 2002) and other coastal regions (Hydes and Liss, 1977;Hydes, 1989) …”

Distribution and redox speciation of dissolved iron on the European continental margin

“…In the English Channel, the concentrations of both elements were higher, ranging from Hydes 1989). DFe was consistently lower than the surface-water data reported for the same region in March 1998 (Boye et al 2003), when North Atlantic and English Channel surface waters were 0.6-0.9 and 1.0-1.7 nmol L 21 , respectively.…”

Horizontal gradient of the chemical speciation of iron in surface waters of the northeast Atlantic Ocean

“…In contrast with manganese and iron, the aluminium concentration decreased again in the Channel waters after the boundary. The aluminium concentrations found for the Atlantic and the Channel are in reasonable agreement with those found previously (Measures, 1995;Hydes, 1989). The different behaviour of aluminium is in line with expectation: for instance, in the Pacific, aluminium shows clearly its atmospheric source followed by a decrease by scavenging and an increase due to remobilization (Orians and Bruland, 1986); iron on the other hand follows a clear nutrientlike behaviour (Martin et al, 1989).…”

The role of sea ice formation in cycling of aluminium in northern Marguerite Bay, Antarctica

“…Our dissolved Al concentration concentrations from northern Marguerite Bay are consistent with published values for the Weddell Sea, ranging from 8-22 nM (van Bennekom et al, 1991;Sañudo-Wilhelmy et al, 2002) and other coastal regions (Hydes and Liss, 1977;Hydes, 1989) …”

Distribution and redox speciation of dissolved iron on the European continental margin

“…In the English Channel, the concentrations of both elements were higher, ranging from Hydes 1989). DFe was consistently lower than the surface-water data reported for the same region in March 1998 (Boye et al 2003), when North Atlantic and English Channel surface waters were 0.6-0.9 and 1.0-1.7 nmol L 21 , respectively.…”

Horizontal gradient of the chemical speciation of iron in surface waters of the northeast Atlantic Ocean

“…In contrast with manganese and iron, the aluminium concentration decreased again in the Channel waters after the boundary. The aluminium concentrations found for the Atlantic and the Channel are in reasonable agreement with those found previously (Measures, 1995;Hydes, 1989). The different behaviour of aluminium is in line with expectation: for instance, in the Pacific, aluminium shows clearly its atmospheric source followed by a decrease by scavenging and an increase due to remobilization (Orians and Bruland, 1986); iron on the other hand follows a clear nutrientlike behaviour (Martin et al, 1989).…”

The role of sea ice formation in cycling of aluminium in northern Marguerite Bay, Antarctica

“…Our dissolved Al concentration concentrations from northern Marguerite Bay are consistent with published values for the Weddell Sea, ranging from 8-22 nM (van Bennekom et al, 1991;Sañudo-Wilhelmy et al, 2002) and other coastal regions (Hydes and Liss, 1977;Hydes, 1989) …”

Distribution and redox speciation of dissolved iron on the European continental margin

“…In the English Channel, the concentrations of both elements were higher, ranging from Hydes 1989). DFe was consistently lower than the surface-water data reported for the same region in March 1998 (Boye et al 2003), when North Atlantic and English Channel surface waters were 0.6-0.9 and 1.0-1.7 nmol L 21 , respectively.…”