Metal-ion partitioning during low-temperature precipitation and dissolution of anhydrous carbonates and sulphates

Michael E. Böttcher, Martin Dietzel

Research output: Contribution to journalArticleResearchpeer-review

Abstract

Anhydrous carbonate and sulphate-bearing solids are formed on Earth under very different environmental conditions and are the most abundant constituents in so-called chemical sediments. At low temperatures, both biogenic and abiotic formation mechanisms are observed and their occurrence ranges from freshwater, via open marine to hypersaline aquatic environments. To understand individual mechanisms of mineral formation and the impact of boundary environmental conditions such as reaction temperature, composition of the aqueous mother fluid and precipitation rate, geochemical tracers such as trace metals or stable isotopes are needed. The thermodynamics of element partitioning in solid solutions-aqueous solutions (SS-AS) systems provides a frame for the evaluation of e.g. the impact of reaction kinetics, vital activity, or ionic strength. The presence of metastable phases may influence further reactions by providing the necessary reactants and surfaces for dissolution, adsorption, and reprecipitation reactions, thereby changing reaction kinetics in comparison to reactions in homogeneous solutions. The evaluation of trace-element substitution requires the combination of modelling approaches, in particular with experimental calibrations, but also empirical relationships. In this communication, the authors focus on selected binary carbonate and sulphate SS-AS systems at low temperatures. Systems involving the partitioning of Mg2+, Mn2+ and Sr2+ and others are discussed in more detail. They give a presentation of relevant current topics related to low-temperature metal-ion partitioning during complex precipitation and dissolution behaviour. The aim of this contribution is to stimulate future research in the highly relevant, low-temperature carbonate and sulphate SS-AS systems.

Original languageEnglish
Pages (from-to)139-187
Number of pages49
JournalEuropean Mineralogical Union Notes in Mineralogy
Volume10
Issue number1
DOIs
Publication statusPublished - 2010

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Carbonates
Sulfates
Metal ions
Dissolution
partitioning
dissolution
solid solution
sulfate
carbonate
aqueous solution
ion
metal
reaction kinetics
Solid solutions
Reaction kinetics
environmental conditions
hypersaline environment
Bearings (structural)
Temperature
formation mechanism

ASJC Scopus subject areas

  • Geochemistry and Petrology

Cite this

Metal-ion partitioning during low-temperature precipitation and dissolution of anhydrous carbonates and sulphates. / Böttcher, Michael E.; Dietzel, Martin.

In: European Mineralogical Union Notes in Mineralogy, Vol. 10, No. 1, 2010, p. 139-187.

Research output: Contribution to journalArticleResearchpeer-review

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