Abstract
The article considers study outcomes of hydrogenous mineral neoformations precipitated on deferrization filters of Tomsk water intake facility from underground sources. Compositionally, these precipitations are colloform and polymineral including ferrous, carbonate and aluminosilicate mineral phases. Ferrous phase predominates and embraces ferric hydroxides (ferrihydrate, goethite, hematite and lepidocrocite) and ferrous hydrophosphates (vivianite, strengite, strunzite and rockbridgeit). Carbonate and aluminosilicate minerals are calcite and kaolinite-group, respectively.
| Original language | English |
|---|---|
| Article number | 012017 |
| Journal | IOP Conference Series: Earth and Environmental Science |
| Volume | 33 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 15 Apr 2016 |
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Fingerprint Dive into the research topics of 'Hydrogenous mineral neoformations in Tomsk water intake facility from underground sources'. Together they form a unique fingerprint.
Cite this
Dutova, E., Vologdina, I., Pokrovsky, D., Nalivaiko, N., Kuzevanov, K., & Pokrovsky, V. (2016). Hydrogenous mineral neoformations in Tomsk water intake facility from underground sources. IOP Conference Series: Earth and Environmental Science, 33(1), [012017]. https://doi.org/10.1088/1755-1315/33/1/012017