Microwave-induced self-organization in mineral systems. IV. FeCl3 colloid (450 W; 2.45 GHz)
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
2019
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| _version_ | 1867171012484792320 |
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| author | Gradov, Oleg V Gradova, Margaret A |
| author_facet | Gradov, Oleg V Gradova, Margaret A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Membraneous structure self-organization in FeCl3 colloids under microwave treatmet (450 W, 2.45 GHz) occurs due to the hydrolytic polycondensation of the ferric oxohydroxides. A gentle 1 min MW treatment results in various structure formation, while the longer exposition leads to either amorphous or partially crystallyzed mineral patterns. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_897649 |
| institution | PANGAEA |
| language | en |
| publishDate | 2019 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Microwave-induced self-organization in mineral systems. IV. FeCl3 colloid (450 W; 2.45 GHz) Gradov, Oleg V Gradova, Margaret A Acageneite (β-FeOOH); Colloid particle self-assembly; Ferrihydrite; Goethite (α-FeOOH); Hematite; Hydrolytic polymerization and condensation; Lepidocrocite (γ-FeOOH); Maghemite; Self-organization in mineral systems Membraneous structure self-organization in FeCl3 colloids under microwave treatmet (450 W, 2.45 GHz) occurs due to the hydrolytic polycondensation of the ferric oxohydroxides. A gentle 1 min MW treatment results in various structure formation, while the longer exposition leads to either amorphous or partially crystallyzed mineral patterns. |
| title | Microwave-induced self-organization in mineral systems. IV. FeCl3 colloid (450 W; 2.45 GHz) |
| topic | Acageneite (β-FeOOH); Colloid particle self-assembly; Ferrihydrite; Goethite (α-FeOOH); Hematite; Hydrolytic polymerization and condensation; Lepidocrocite (γ-FeOOH); Maghemite; Self-organization in mineral systems |
| url | https://doi.org/10.1594/PANGAEA.897649 |