Trace Element Chemistry of Antarctic Saline Lakes and FjordsEntry ID: ASAC_568
Abstract: From the referenced paper:
The frigid concentration or freezing of seawater is an important natural phenomenon in the polar regions and results in the precipitation of a different sequence of salts - and thus produces brines of different composition - to that formed during isothermal evaporation under temperate conditions (about 20-25 degrees C). Seawater freezing, however, has been studied less ... extensively than evaporation and somewhat greater uncertainty exists over the exact nature of the compositional pathway followed. Most investigators have shown that the precipitation of mirabilite (Na2SO4 - 10 H2O) or gypsum (CaSO4 - 2 H2O), which both occur at the same seawater concentration factor (SWCF), is the critical difference between frigid and evaporative concentration, respectively, a consequence of the very different temperature dependence of the solubilities of these salts, as well as the effect of sodium chloride on these properties. This difference can be considered to represent a temperature-dependent chemical divide in the closed-basin concentration of seawater because it determines significantly the major ion composition of the brine and the salt mineral assemblage precipitated on further evolution of the system. Recently new insights into seawater freezing have been achieved through improvements in existing chemical equilibrium models. Along with the results of some associated experimental work, this has provided evidence for the formation of gypsum during freezing, contradicting the accepted Ringer-Nelson-Thompson model of frigid concentration firmly established in the 1950's and through subsequent studies, but validating an alternative model proposed by Gitterman two decades later.
(Click for Interactive Map)
Start Date: 1992-10-01Stop Date: 1995-03-31
Quality Dates provided in temporal coverage are approximate only.
Access Constraints A PDF copy of the referenced paper is available for download from the provided URL to AAD staff only.
Use Constraints This data set conforms to the PICCCBY Attribution License
Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=ASAC_568 when using these data.
Data Set Progress
Distribution Media: HTTP
Distribution Size: 1476 KB
Distribution Format: PDF
Role: TECHNICAL CONTACT
Role: DIF AUTHOR
Phone: +61 3 6226 2173
Fax: +61 3 6226 2186
Email: B.Ogrady at utas.edu.au
Department of Chemistry GPO BOX 252-75 University of Tasmania
Province or State: Tasmania
Postal Code: 7001
Stark S.C., O'Grady B.V., Burton H.R., Carpenter P.D. (2003), Frigidly concentrated seawater and the evolution of Antarctic saline lakes, Australian Journal of Chemistry, 56, 181-186
Creation and Review Dates
DIF Creation Date: 2000-08-02
Last DIF Revision Date: 2011-11-22