Hydrothermal Production of H2 and Magnetite From Steel Slags: A Geo-Inspired Approach Based on Olivine Serpentinization
The interaction between ultramafic rocks and hot seawater at slow-spreading mid-oceanic ridges triggers hydrothermal redox reactions which are known to produce magnetite and H2 under appropriate pressure and temperature conditions. Steel slags share some common properties with ultramafic rocks. They...
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| Natura: | Artigo |
| Lingua: | Inglês |
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Frontiers Media S.A.
2019-03-01
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| Serie: | Frontiers in Earth Science |
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| Accesso online: | https://www.frontiersin.org/article/10.3389/feart.2019.00017/full |
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