USGS · tm10C10
Determination of the δ 34 S of sulfate in water; RSIL lab code 1951
Abstract
The purpose of the Reston Stable Isotope Laboratory (RSIL) lab code 1951 is to determine the δ( 34 S/ 32 S), abbreviated as δ 34 S, of dissolved sulfate. Dissolved sulfate is collected in the field and precipitated with BaCl 2 at pH 3 to 4 as BaSO 4 in the laboratory. However, the dissolved organic sulfur (DOS) is oxidized to SO 2 , and the carbonate is acidified to CO 2 . Both are degassed from the water sample before the sulfate is precipitated. The precipitated BaSO 4 is filtered and dried before introduction into an elemental analyzer (EA) Carlo Erba NC 2500. The EA is used to convert sulfur in a BaSO 4 solid sample into SO 2 gas, and the EA is connected to a continuous flow isotope-ratio mass spectrometer (CF-IRMS), which determines the differences in the isotope-amount ratios of stable sulfur isotopes ( 34 S/ 32 S) of the product SO 2 gas. The combustion is quantitative; no isotopic fractionation is involved. Samples are placed in a tin capsule and loaded into the Costech Zero Blank Autosampler of the EA. Under computer control, samples are dropped into a heated tube reaction tube that combines the oxidation and reduction reactions. The combustion takes place in a helium atmosphere containing an excess of oxygen gas at the oxidation zone at the top of the reaction tube. Combustion products are transported by a helium carrier through the reduction zone at the bottom of the reaction tube to remove excess oxygen and through a separate drying tube to remove any water. The gas-phase products, mainly CO 2 , N 2 , and SO 2 , are separated by a gas chromatograph. The gas is then introduced into the isotope-ratio mass spectrometer (IRMS) through a Finnigan MAT (now Thermo Scientific) ConFlo II interface, which also is used to inject SO 2 reference gas and helium for sample dilution. The IRMS is a Thermo Scientific Delta V Plus CF-IRMS. It has a universal triple collector with two wide cups and a narrow cup in the middle. It is capable of measuring mass/charge ( m/z ) 64 and 66 simultaneously. The ion beams from SO 2 are as follows: m/z 64 = SO 2 = 32 S 16 O 16 O; m/z 66 = SO 2 = 34 S 16 O 16 O primarily.
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Kinga Revesz, Haiping Qi, Tyler B. Coplen. 2006. Determination of the δ 34 S of sulfate in water; RSIL lab code 1951. https://doi.org/10.3133/tm10c10
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