Gramm-Osipov, Lev M. (1996) Formation of solid phases of manganese in oxygenated aquatic environments, in Manganese Mineralization: Geochemistry and Mineralogy of Terrestrial and Marine Deposits. Geological Society, London, Special Publications, 119 (1). 301-308 doi:10.1144/gsl.sp.1997.119.01.19
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Formation of solid phases of manganese in oxygenated aquatic environments | ||
| Journal | Geological Society, London, Special Publications | ||
| Authors | Gramm-Osipov, Lev M. | Author | |
| Year | 1996 (December 3) | Volume | 119 |
| Page(s) | 301-308 | Issue | 1 |
| Publisher | Geological Society of London | ||
| URL | |||
| DOI | doi:10.1144/gsl.sp.1997.119.01.19Search in ResearchGate | ||
| Generate Citation Formats | |||
| Classification | Not set | LoC | Not set |
| Mindat Ref. ID | 428129 | Long-form Identifier | mindat:1:5:428129:4 |
| GUID | 0 | ||
| Full Reference | Gramm-Osipov, Lev M. (1996) Formation of solid phases of manganese in oxygenated aquatic environments, in Manganese Mineralization: Geochemistry and Mineralogy of Terrestrial and Marine Deposits. Geological Society, London, Special Publications, 119 (1). 301-308 doi:10.1144/gsl.sp.1997.119.01.19 | ||
| Plain Text | Gramm-Osipov, Lev M. (1996) Formation of solid phases of manganese in oxygenated aquatic environments, in Manganese Mineralization: Geochemistry and Mineralogy of Terrestrial and Marine Deposits. Geological Society, London, Special Publications, 119 (1). 301-308 doi:10.1144/gsl.sp.1997.119.01.19 | ||
| In | Nicholson, K., Hein, J. R., Bühn, B., Dasgupta, S. - Eds. (1997) Manganese Mineralization: Geochemistry and Mineralogy of Terrestrial and Marine Deposits. Special Publication Vol. 119. Geological Society of London | ||
| Abstract/Notes | Abstract The article describes a thermodynamic analysis of the formation process of solid manganese phases in oxygenated aquatic environment. The first step of this process is the formation of the compound MnOOH. In the second step the latter in a disproportionation reaction is transformed into a complicated oxohydroxide [(MnO 2 ) 2 n −3 (MnOOH) 4−2 n ] with O/Mn ranging from 1.700 to 1.999. As an example of using results of thermodynamic analyses the behaviour Mn system in the ocean is described. It is shown that Mn 3 O 4 and MnOOH respectively control concentrations and distribution of the manganese in the upper (150–600 m) and lower oceanic water column. | ||
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