Detailed Information on Publication Record
2005
Total dynamics of quartz-water system at ambient conditions
FAIMON, JiříBasic information
Original name
Total dynamics of quartz-water system at ambient conditions
Name in Czech
Celková dynamika systému křemen-voda za normálních podmínek
Authors
FAIMON, Jiří (203 Czech Republic, guarantor)
Edition
Aquatic Geochemistry, Netherlands, Springer Netherlands, 2005, 1380-6165
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
Geochemistry
Country of publisher
Netherlands
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 0.963
RIV identification code
RIV/00216224:14310/05:00030986
Organization unit
Faculty of Science
UT WoS
000228868000002
Keywords (in Czech)
komplex; rozpouštění; dynamika; tok; růst; modelování; PHREEQC; křemen; povrch
Keywords in English
complex; dissolution; dynamics; flux; growth; modeling; PHREEQC; quartz; surface
Tags
International impact, Reviewed
Změněno: 23/9/2009 15:29, doc. Ing. Jiří Faimon, Dr.
V originále
New data on the dissolution and growth of quartz in acid, nearly neutral and slightly alkaline solutions at ambient conditions are presented. During batch dissolutions, aqueous Si-concentrations increased nonlinearly towards limit values. During parallel growth experiments, however, the high Si-concentrations corresponding to 13-fold supersaturation with respect to quartz did not decreased. To interpret these results, two dynamic models (1) a reaction model and (2) a surface-complexation model, were derived. Both models were focused on (a) reversible dissolution/growth of bulk quartz and b) irreversible dissolution of disturbed quartz (weakly bounded Si-atoms) on new surface.
In Czech
New data on the dissolution and growth of quartz in acid, nearly neutral and slightly alkaline solutions at ambient conditions are presented. During batch dissolutions, aqueous Si-concentrations increased nonlinearly towards limit values. During parallel growth experiments, however, the high Si-concentrations corresponding to 13-fold supersaturation with respect to quartz did not decreased. To interpret these results, two dynamic models (1) a reaction model and (2) a surface-complexation model, were derived. Both models were focused on (a) reversible dissolution/growth of bulk quartz and b) irreversible dissolution of disturbed quartz (weakly bounded Si-atoms) on new surface.
Links
MSM0021622412, plan (intention) |
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