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Transformation of Fe(OH)2 into Fe3O4 with hydrogen release
Schikorr reaction formally describes the conversion of the iron(II) hydroxide (Fe(OH)2) into iron(II,III) oxide (Fe3O4). This transformation reaction
Schikorr_reaction
Rock formed by transformation of olivine
-> 2 Fe3O4 + 3 SiO2 + 2 H2}}} This reaction closely resembles the Schikorr reaction also producing hydrogen gas by oxidation of Fe2+ ions into Fe3+ ions
Serpentinite
Chemical compound
magnetite and molecular hydrogen. This process is described by the Schikorr reaction: 3 Fe ( OH ) 2 ferrous hydroxide ⟶ Fe 3 O 4 magnetite + H 2 hydrogen
Iron(II,III)_oxide
Formation of serpentinite by hydration and metamorphic transformation of olivine
brucite, that is, brucite containing Fe(OH)2, which then undergoes the Schikorr reaction in the anaerobic conditions of serpentinization: Maximum reducing
Serpentinization
Chemical compound
III) oxide) and molecular hydrogen. This process is described by the Schikorr reaction: 3 Fe(OH)2 → Fe3O4 + H2 + 2 H2O Anions such as selenite and selenate
Iron(II)_hydroxide
Chemical element with atomic number 1 (H)
Fe3O4 + SiO2 + H2 Closely related to this geological process is the Schikorr reaction: 3 Fe(OH)2 → Fe3O4 + 2 H2O + H2 This process also is relevant to the
Hydrogen
water to form the mineral magnetite (Fe3O4) in the process called the Schikorr reaction. In general, the anaerobic corrosion of metals, such as iron and copper
Anaerobic_corrosion
Fringe theory about the origin of petroleum
magnetite + hydrogen 3 FeO + H2O → Fe3O4 + H2 This redox reaction closely resembles the Schikorr reaction involving the partial oxidation and conversion of iron(II)
Abiogenic_petroleum_origin
Salt mine in Germany
radioactive waste repository Nuclear decommissioning Schacht Konrad Schikorr reaction Waste Isolation Pilot Plant Herrmann, Albert Günter; Röthemeyer, Helmut
Asse_II_mine
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