Raman spectral quantification of Li2SO4, Na2SO4, K2SO4 and Cs2SO4 at 25 to 250 °C and its potential implications for the determination of sulfate contents in natural fluid inclusions

The quantitative study of the sulfate content in natural fluid inclusions (FIs) will help our understanding of the processes of metal transport and related mineralization. The sulfate-rich FIs typically contain several types of sulfates with diverse cations such as Na + , K + , and so on. In order to get the sulfates contents in natural FIs, in situ Raman spectral quantitative calibration method is used to calibrate the Li 2 SO 4 , Na 2 SO 4 , K 2 SO 4 and Cs 2 SO 4 solutions at temperatures ranging from 25 °C to 250 °C in our study. The results show that the A (SO 4 2− )/ A (H 2 O) ratio increases linearly with increasing m SO 4 2− in sulfate solutions containing single cation of Li, Na, K or Cs at the set temperatures, where A is Raman peak area and m is molality (mol/kg H 2 O), and a negative linear relationship exists between k (quantitative calibration coefficient) and temperature for sulfate solutions with specific cations up to 250 °C. Meanwhile, the slopes and the intercepts of the k-T correlation curves are obviously different among sulfate solutions with different cations, and the coefficients k of these sulfate solutions at certain temperature decrease with the increase of atomic number of the cation, in accordance with the following order: Li +  > Na +  > K +  > Cs + . As Na + and K + are the main cations in the natural sulfate-bearing FIs, the quantification of the multi-cation (Na ± K ± Li) sulfate solutions was evaluated by using the Raman quantitative calibration curves of Li 2 SO 4 , Na 2 SO 4 , K 2 SO 4 and Cs 2 SO 4 separately, the errors exist due to the use of calibration curves with different cations; the average concentration errors derived from the use of Na 2 SO 4 or K 2 SO 4 Raman quantitative calibration curves are within about 5 %, while those from the use of Li 2 SO 4 or Cs 2 SO 4 Raman quantitative calibration curves are within about 15 %. Therefore, the acceptable errors suggest that the calibration curves of individual sulfates can be applied to the determination of sulfate content of natural sulfate-bearing FIs.