_version_ 1867170989994934272
author Goldberg, Edward D
author_facet Goldberg, Edward D
collection Datos científicos de ciencias marinas y ambientales
contents The ability of the hydrated oxides of manganese and iron to adsorb ions from solution (scavenging) is considered in relation to some problems in marine geology, chemistry, and biology. In the ferruginous sediments of the Pacific Ocean, iron oxides are accompanied by titanium, cobalt, and zirconium in amounts proportional to the iron content. Similarly, copper and nickel are linearly related to the manganese content. These observations are explained on the basis of scavenging. An electrochemical theory for the formation of manganese nodules is presented. Marine sediments are classified on the basis of the geosphere in which the solid phases originate. The distribution of certain ionic species in sea water between the solid and aqueous phases is considered on the basis of scavenging and co-ordination compound theory. The concentration of minor elements by members of the marine biosphere is explained either by the direct uptake of the element or by the uptake of iron or manganese oxides with the accompanying scavenged element.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_858479
institution PANGAEA
language en
publishDate 1954
publisher PANGAEA
record_format pangaea
spellingShingle (Table 2, Page 252) Average chemical composition of 11 manganese nodules and crust from the Pacific Ocean
Goldberg, Edward D
Aluminium; CHA-160; Challenger1872; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Event label; GC; GOLDHW1; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Henderson Seamount, Pacific Ocean; Horizon; Identification; Iron; Manganese; MDPC02HO-MP-026A-3; MDPC02HO-MP-037A; MDPC03HO-043K; MIDPAC; MPC-26A-3; MPC-37A; MPC-43J; MPC-43K; NEL-HEND; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North Pacific Ocean; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D1; NTHL-D7; Pacific Ocean; PAS-19121; Phosphorus; Spectrophotometer, Beckmann DU; Titanium; Wired profile sonde; WP; Zirconium
The ability of the hydrated oxides of manganese and iron to adsorb ions from solution (scavenging) is considered in relation to some problems in marine geology, chemistry, and biology. In the ferruginous sediments of the Pacific Ocean, iron oxides are accompanied by titanium, cobalt, and zirconium in amounts proportional to the iron content. Similarly, copper and nickel are linearly related to the manganese content. These observations are explained on the basis of scavenging. An electrochemical theory for the formation of manganese nodules is presented. Marine sediments are classified on the basis of the geosphere in which the solid phases originate. The distribution of certain ionic species in sea water between the solid and aqueous phases is considered on the basis of scavenging and co-ordination compound theory. The concentration of minor elements by members of the marine biosphere is explained either by the direct uptake of the element or by the uptake of iron or manganese oxides with the accompanying scavenged element.
title (Table 2, Page 252) Average chemical composition of 11 manganese nodules and crust from the Pacific Ocean
topic Aluminium; CHA-160; Challenger1872; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; Dredge; Dredge, rock; DRG; DRG_R; Event label; GC; GOLDHW1; Grab; GRAB; Gravity corer; H.M.S. Challenger (1872); Henderson Seamount, Pacific Ocean; Horizon; Identification; Iron; Manganese; MDPC02HO-MP-026A-3; MDPC02HO-MP-037A; MDPC03HO-043K; MIDPAC; MPC-26A-3; MPC-37A; MPC-43J; MPC-43K; NEL-HEND; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North Pacific Ocean; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; NTHL-D1; NTHL-D7; Pacific Ocean; PAS-19121; Phosphorus; Spectrophotometer, Beckmann DU; Titanium; Wired profile sonde; WP; Zirconium
url https://doi.org/10.1594/PANGAEA.858479