Abstract
The results of a geochemical study of groundwater in an area of dawsonite mineralization are reported. The studied groundwater has a sodium bicarbonate composition, with pH 7.3-9.2, and a salinity of 0.4-7.2 g/L. The equilibrium conditions in the water with respect to dawsonite, calcite, gibbsite, kaolinite, montmorillonite, quartz, albite, anorthite, and analcime were investigated. A comprehensive consideration of groundwater composition and ore-forming properties of the water-rock system led to the conclusion that dawsonite is a product of aluminosilicate rock weathering. However, this mineral is formed only under conditions of reduced water exchange providing a long-term water-rock interaction and accumulation of sufficient amounts of Na +, OH -, HCO 3 -, CO 3 2-, and Al(OH) 4 -.
| Original language | English |
|---|---|
| Title of host publication | Water-Rock Interaction - Proceedings of the 13th International Conference on Water-Rock Interaction, WRI-13 |
| Pages | 747-750 |
| Number of pages | 4 |
| Publication status | Published - 2010 |
| Event | 13th International Conference on Water-Rock Interaction, WRI-13 - Guanajuato, Mexico Duration: 16 Aug 2010 → 20 Aug 2010 |
Other
| Other | 13th International Conference on Water-Rock Interaction, WRI-13 |
|---|---|
| Country | Mexico |
| City | Guanajuato |
| Period | 16.8.10 → 20.8.10 |
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ASJC Scopus subject areas
- Geology
Cite this
Hydrogeochemical processes of dawsonite formation : Evidence for evolution of a water-rock system. / Shvartsev, S. L.
Water-Rock Interaction - Proceedings of the 13th International Conference on Water-Rock Interaction, WRI-13. 2010. p. 747-750.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Hydrogeochemical processes of dawsonite formation
T2 - Evidence for evolution of a water-rock system
AU - Shvartsev, S. L.
PY - 2010
Y1 - 2010
N2 - The results of a geochemical study of groundwater in an area of dawsonite mineralization are reported. The studied groundwater has a sodium bicarbonate composition, with pH 7.3-9.2, and a salinity of 0.4-7.2 g/L. The equilibrium conditions in the water with respect to dawsonite, calcite, gibbsite, kaolinite, montmorillonite, quartz, albite, anorthite, and analcime were investigated. A comprehensive consideration of groundwater composition and ore-forming properties of the water-rock system led to the conclusion that dawsonite is a product of aluminosilicate rock weathering. However, this mineral is formed only under conditions of reduced water exchange providing a long-term water-rock interaction and accumulation of sufficient amounts of Na +, OH -, HCO 3 -, CO 3 2-, and Al(OH) 4 -.
AB - The results of a geochemical study of groundwater in an area of dawsonite mineralization are reported. The studied groundwater has a sodium bicarbonate composition, with pH 7.3-9.2, and a salinity of 0.4-7.2 g/L. The equilibrium conditions in the water with respect to dawsonite, calcite, gibbsite, kaolinite, montmorillonite, quartz, albite, anorthite, and analcime were investigated. A comprehensive consideration of groundwater composition and ore-forming properties of the water-rock system led to the conclusion that dawsonite is a product of aluminosilicate rock weathering. However, this mineral is formed only under conditions of reduced water exchange providing a long-term water-rock interaction and accumulation of sufficient amounts of Na +, OH -, HCO 3 -, CO 3 2-, and Al(OH) 4 -.
UR - http://www.scopus.com/inward/record.url?scp=84860140112&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84860140112&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:84860140112
SN - 9780415604260
SP - 747
EP - 750
BT - Water-Rock Interaction - Proceedings of the 13th International Conference on Water-Rock Interaction, WRI-13
ER -