Ferromanganese nodules (original) (raw)
Ferromanganese nodules form in the oxidizing environment of the abyssal pelagic zone. They are the result of ion exchange reactions that precipitate ore components from the water (sedimentary) or out of the interstitial water of the sediments layers (diagenetic). The composition of Manganese-bearing minerals is dependent on how the nodules are formed; sedimentary nodules, which have a lower Mn2+ content than diagenetic, are dominated by Fe-, Mn-feroxyhyte, and asbolane-buserite while diagenetic nodules are dominated by buserite I, birnessite, todorokite, and asbolane-buserite.
| Property | Value |
|---|---|
| dbo:abstract | Ferromanganese nodules form in the oxidizing environment of the abyssal pelagic zone. They are the result of ion exchange reactions that precipitate ore components from the water (sedimentary) or out of the interstitial water of the sediments layers (diagenetic). The composition of Manganese-bearing minerals is dependent on how the nodules are formed; sedimentary nodules, which have a lower Mn2+ content than diagenetic, are dominated by Fe-, Mn-feroxyhyte, and asbolane-buserite while diagenetic nodules are dominated by buserite I, birnessite, todorokite, and asbolane-buserite. (en) |
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| dbo:wikiPageLength | 1072 (xsd:nonNegativeInteger) |
| dbo:wikiPageRevisionID | 1088314028 (xsd:integer) |
| dbo:wikiPageWikiLink | dbr:Pelagic_zone dbr:Ore dbr:Todorokite dbr:Ion_exchange dbr:Abyssal dbr:Precipitate dbr:Asbolane dbc:Oceanography dbr:Birnessite dbr:Buserite dbr:Feroxyhyte dbr:Ferromanganese dbr:Sediments dbr:Sedimentary dbr:Oxidizing dbr:Vernadite dbr:Wikt:interstitial |
| dbp:wikiPageUsesTemplate | dbt:Cite_journal dbt:Short_description |
| dct:subject | dbc:Oceanography |
| rdfs:comment | Ferromanganese nodules form in the oxidizing environment of the abyssal pelagic zone. They are the result of ion exchange reactions that precipitate ore components from the water (sedimentary) or out of the interstitial water of the sediments layers (diagenetic). The composition of Manganese-bearing minerals is dependent on how the nodules are formed; sedimentary nodules, which have a lower Mn2+ content than diagenetic, are dominated by Fe-, Mn-feroxyhyte, and asbolane-buserite while diagenetic nodules are dominated by buserite I, birnessite, todorokite, and asbolane-buserite. (en) |
| rdfs:label | Ferromanganese nodules (en) |
| owl:sameAs | freebase:Ferromanganese nodules wikidata:Ferromanganese nodules https://global.dbpedia.org/id/4jyyA |
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| foaf:isPrimaryTopicOf | wikipedia-en:Ferromanganese_nodules |
| is dbo:wikiPageRedirects of | dbr:Ferromanganese_nodule |
| is dbo:wikiPageWikiLink of | dbr:Juan_Fernández_Islands dbr:Green_Bay_(Lake_Michigan) dbr:Todorokite dbr:Birnessite dbr:Zealandia dbr:Buserite dbr:Sethunathasarma_Krishnaswami dbr:Trace_metal_stable_isotope_biogeochemistry dbr:Outline_of_oceanography dbr:Ferromanganese_nodule |
| is foaf:primaryTopic of | wikipedia-en:Ferromanganese_nodules |