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Dissolution of barite for the analysis of strontium isotopes and other chemical and isotopic variations using aqueous sodium carbonate

January 1, 1985

A simple procedure for preparing barite samples for chemical and isotopic analysis is described. Sulfate ion, in barite, in the presence of high concentrations of aqueous sodium carbonate, is replaced by carbonate. This replacement forms insoluble carbonates with the cations commonly in barite: Ba, Sr, Ca and Pb. Sulfate is released into the solution by the carbonate replacement and is separated by filtration. The aqueous sulfate can then be reprecipitated for analysis of the sulfur and oxygen isotopes. The cations in the carbonate phase can be dissolved by acidifying the solid residue. Sr can be separated from the solution for Sr isotope analysis by ion-exchange chromatography. The sodium carbonate used contains amounts of Sr which will affect almost all barite 87Sr86Sr">87Sr86Sr ratios by less than 0.00001 at 1.95θ of the mean. The procedure is preferred over other techniques used for preparing barite samples for the determination of 87Sr86Sr">87Sr86Sr ratios because it is simple, rapid and enables simultaneous determination of many compositional parameters on the same material.

Publication Year 1985
Title Dissolution of barite for the analysis of strontium isotopes and other chemical and isotopic variations using aqueous sodium carbonate
DOI 10.1016/0168-9622(85)90043-0
Authors G. N. Breit, E.C. Simmons, M. B. Goldhaber
Publication Type Article
Publication Subtype Journal Article
Series Title Chemical Geology: Isotope Geoscience Section
Index ID 70013083
Record Source USGS Publications Warehouse