Article ID Journal Published Year Pages File Type
4698384 Chemical Geology 2016 11 Pages PDF
Abstract

•The data on H2S solubility in water and in NaCl(aq) were analyzed and the reliable data sets selected for correlation.•An activity – fugacity model using the Pitzer interaction theory is presented for calculating H2S solubility in water and NaCl(aq).•The model covers a wide T –P – mNaCl range up to 573 K, 40 MPa and 6 m NaCl, with (or close to) experimental accuracy.•The model uses the most representative equations of state for pure H2S and for its Henry's law constant.•An extension of the new model allows a thermodynamically consistent description of other derivative properties of the liquid phase in the ternary H2S–H2O–NaCl system.

Reliable experimental results were selected from the literature (using over 700 data) to develop a thermodynamic model for calculating the solubility of hydrogen sulfide (H2S) in pure water and in aqueous NaCl solutions between 283 and 573 K, 0.1–40 MPa and ms 0–6 mol·kg− 1. Thermodynamic properties of the pure components were calculated using highly accurate multiparametric equations of state for H2S (Lemmon and Span, 2006) and for H2O (Wagner and Pruss, 2002). Thermodynamic properties of H2S(aq) at infinite dilution were based on the Henry's law constants generated from the SOCW model (Sedlbauer et al., 2000) and reported by Majer et al. (2008). The determined activity coefficients of H2S in pure water and in NaCl solutions were treated using the Pitzer interaction model. The Pitzer parameters for H2S in binary and ternary solutions were newly determined while those for NaCl(aq) in the H2S-free system were adopted from the review of Archer (1992). The experimental solubilities selected for correlation are reproduced by the model with mean relative deviations of 5.2% and 6.1% for the H2S–H2O and for H2S–H2O–NaCl systems, respectively. These values are comparable to the experimental uncertainty of the solubility data. The new model allows a thermodynamically consistent description of numerous other properties of the liquid phase in the ternary H2S–H2O–NaCl system, including the activity coefficients of H2S and NaCl, the osmotic coefficients, the Setchenow constants, and the molar volume and density of the bulk liquid. These properties can be calculated for any H2S and NaCl concentrations up to halite saturation. The model is available as a computer code that is freely distributed.

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