State of the Art on Fe Precipitation in Porous Media: Hydrogeochemical Processes and Evolving Parameters
The mixing of terrestrial groundwater and seawater creates dynamic reaction zones in intertidal areas, where land-derived Fe(II) is oxidized to Fe(III) and then precipitates as Fe hydroxides at the groundwater–seawater interface. These hydrogeochemical processes contribute to the formation of iron b...
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| Autori principali: | , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
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MDPI AG
2024-04-01
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| Serie: | Journal of Marine Science and Engineering |
| Soggetti: | |
| Accesso online: | https://www.mdpi.com/2077-1312/12/4/690 |
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