Supporting Information Experimental studies and modeling of CO2 solubility in high temperature aqueous CaCl2, MgCl2, Na2SO4, and KCl solutions Haining Zhao, Robert M. Dilmore, and Serguei N. Lvov, 1. Web-based computational interface of PSUCO2 model. We developed a web-based computational interface for the proposed PSUCO2 model, please use the link: http://www.carbonlab.org/psuco2/. The calculation procedure is: (1). Select a system (2). Input pressure, temperature and salt concentration (3). Click "Calculate" button, then the results will come out shortly Figure S1. Web-based computational interface of the proposed PSUCO2 model. (Can be accessed via the link: http://www.carbonlab.org/psuco2/) 2. Procedure to evaluate coefficients ππ ~ππ in Eqs. (10) and (11) We starting from Eq. (9), π ln(πCO2 πΎCO2 ) = ln(πCO πΎπ ) 2 CO2 π πCO 2 ln (π CO2 o ) = lnπΎCO2 − lnπΎCO 2 (9) (S2.1) Substituting Eqs. (7) and (8) into the right side of Eq. (S2.1), we obtain: π πCO 2 ln (π CO2 ) − πΆ = 2πsalt πΉ (S2.2) where C and F in Eq.(S2.2) are given by Eqs. (S2.3) and (S2.4) as below: o 2 o πΆ = 2πnn (πCO2 − πCO ) + 3ππππ (πCO − (πCO )2 ) 2 2 2 πΉ = π΅CO2−salt + π£+π£− 2 πsalt ππππ + 3πCO2 πΆCO2 −CO2−salt (S2.3) (S2.4) and, from Eq. (S2.2) π πCO 2 πΉ = (ππ (π CO2 ) − C) /(2πsalt ) (S2.5) By equating Eqs. (S2.4) and (S2.5), we obtain πΉ = π΅CO2−salt + π£+π£− 2 ππ CO2 )−C) πCO 2 (ln( πsalt ππππ + 3πCO2 πΆCO2 −CO2−salt = (2πsalt ) (S2.6) The parameter C can be calculated by Eq. (S2.3) using experimental CO2 solubility data in both the CO2-H2O and CO2-salt-H2O systems. In order to determine the combined Pitzer interaction parameters π΅πΆπ2 −π πππ‘ and πΆπΆπ2 −πΆπ2 −π πππ‘ in Eq. (7), a function for F was chosen for the data fitting process as shown in Eq. (S2.7).21 100 π πΉ = π1 + π2 π−π + π3 1000 + π4 π(π₯) + π5 3ππΆπ2 + π6 π£+π£− 2 ππ πππ‘ (S2.7) For each salt species, π1 to π6 are coefficients determined by fitting of Eq. (S2.7) to the corresponding experimental data. Comparing Eqs. (S2.6) and (S2.7), we obtain 100 π π΅πΆπ2 −π πππ‘ = π1 + π2 π−π + π3 1000 + π4 π(π₯) (S2.8) πΆπΆπ2−πΆπ2 −π πππ‘ = π5 (S2.9) 2 where π=228K, π(π₯) = π₯ 2 (1 − (1 + π₯)π −π₯ ) , π₯ = πΌ1 πΌ 0.5 , and πΌ1 = 2.0 kg0.5 mol-0.5. For each CO2-salt-H2O system, suppose the number of available experimental CO2 solubility data is n (at different P-T-x points), Eq. (S2.7) can then be written in matrix form as: π΄π₯ = π (S2.8) where 1(1) π΄= 1(2) .. . (π) (1 100 π (1) π (1) −θ 100 1000 π (2) π (2) −θ 1000 100 π (π) π (π) −θ 1000 .. . .. . (1) π£+π£− (2) 2 π£+π£− π(1) (π₯) 3πCO2 π(2) (π₯) . . . 3πCO2 . . . π(π) (π₯) 3πCO2 (π) 2 π£+π£− 2 (1) πsalt π1 πΉ (1) π2 πΉ (2) π3 .. ;π₯= π ;π= 4 π5 . (πΉ (π) )π×1 (π6 )6×1 (2) πsalt . . . (π) πsalt ) π×6 The least-squares solution (π₯Μ) for Eq. (S2.8) is [π΄π π΄]6×6 [π₯Μ]6×1 = [π΄π π]6×1 (S2.9) where π΄π is the transpose of matrix A. The parameters (π1 ~π6 ) for each CO2-salt-H2O system are obtained by solving Eq. (S2.9). The results are shown in Table 2. As a result, the parameters π΅πΆπ2 −π πππ‘ and πΆπΆπ2 −πΆπ2−π πππ‘ can be calculated by Eqs. (10) and (11). Following Eqs. (S2.6) and (S2.7), it appears that ππππ equals π6 , which means ππππ is a constant at any P-T-x condition for a CO2-salt-H2O system. However, we can better correlate our experimental CO2 solubility data by adjusting ππππ at different temperatures and salt concentrations as described in the paper. 3. Pitzer ion-ion interaction parameters for aqueous CaCl2, MgCl2, Na2SO4, and KCl solutions. (0) (1) The empirical function f(T,P) to calculate Pitzer ion-ion interaction parameters (π½ππ , π½ππ and π πΆππ ) at the desired temperatures and pressures for the system of CaCl2-H2O, Na2SO4-H2O, MgCl2-H2O and KCl-H2O are summarized as below: 3.1. CaCl2-H2O system1 π(π, π) = πΉ0 + πΉ1 (π) + πΉ2 (π)2 (S3.1) where P is the system pressure in bar. Fo, F1 and F2 are functions of temperature only and given by Eqs. (S3.2) to (S3.4), 1 1 1 1 5 π πΉ0 = π1 + 2 π2 π + 6 π3 π 2 + 12 π4 π 3 + 6 π5 π 2 {lnπ − 6} + π6 {2 + π7 {2 ππ¦ π + 1} lnπy 1 πΉ1 = π8 + π9 π + π10 π + π11 π 2 + ππ₯−1 π12 + ππ¦−1 π13 1 πΉ2 = π14 + π15 π + π16 π + π17 π 2 3π22 2π + π2 ππ₯ π lnππ₯ } + (S3.2) (S3.3) (S3.4) where T1 = 647K, T2 = 227 K, Tx = (T-T2), and Ty = (T1-T). The constants q1~q17 were listed in Table S1. 3.2. Na2SO4-H2O system2,3 π 1 π(π) = π1 + π2 (π 2 − ππ 2 ) + π3 (π − ππ ) + π4 ln (π ) + π5 (π−π − π π 1 ππ (ππ 1 1 1 1 π −π1 ) + π6 π2 (π(π−π ) − 2 1 ) + π΄ (π − π ) −π ) 2 (S3.5) π π΄ = π7 + π8 ππ + π9 ππ 2 + π10 ππ 3 + 2π1 π11 (π 1 π −π1 + 2(π π1 π −π1 )2 ) + 2π2 π12 (2(π π2 π −π2 1 )2 − π −π ) 2 π (S3.6) where ππ is the reference temperature which is conveniently set at 298.15πΎ. π1 is 263πΎ and π2 is 263 or 680 K depending on which ion-interaction parameter is to be calculated (Table S2). 3.3. MgCl2-H2O system4 Wang and Pitzer (1998) developed a general model that describes the thermodynamic properties of MgCl2(aq) based on an ion-interaction treatment of a variety of thermodynamic properties. (0) (1) (0) (1) The equations for calculating the ion interaction parameters (π½ππ , π½ππ ,πΆππ , πΆππ ) are given below, π π 2 π(π, π) = πΉ0 + πΉ1 (10) + πΉ2 (10) /2 (S3.7) where P is the system pressure in bar. F0, F1 and F2 are functions of temperature only and given by Eqs. (S3.8) to (S3.11) 1 πΉ0 = π1 + π2 lnπ + π3 π + π4 π 2 + π5 π 3 + π6 π 10 + π7 (π −π) 2 (S3.8) 1 2 1 πΉ1 = π8 + π9 lnπ + π10 π + π11 π 2 + π12 π 3 + π13 π 10 + π14 (π −π) (S3.9) 1 1 2 πΉ2 = π15 + π16 lnπ + π17 π + π18 π 2 + π19 π 3 + π20 π 10 + π21 (π −π) 1 π (0) (1) (2) πΆππ = 2[πΆππ + πΆππ exp(−π₯π1 ) + πΆππ exp(−π₯π2 )] (S3.10) (S3.11) where π₯π1 = πΌπ1 πΌ; π₯π2 = πΌπ2 πΌ, πΌπ1 = 0.4 kg mol−1, πΌπ2 = 0.28 kg mol−1 , and T1 = 647K. The constants q1~q21 are shown in Table S3. 3.4. KCl-H2O system5 1 1 π π(π) = π1 + π1 (π − π ) + π3 ln (π ) + π4 (π − ππ ) + π5 (π 2 − ππ 2 ) + π6 ln(π − 260) π π where π1 -π6 are constants listed in Table S4, and ππ is 298.15 K. (S3.12) (0) (1) Table S1. Constants of Eqs. (S3.1) to (S3.4) for calculating Pitzer ion-interaction parameters (π½ππ , π½ππ π and πΆππ ) of CaCl2(aq).1 (0) Const. (1) π(π, π) = π½ππ π π(π, π) = πΆππ π(π, π) = π½ππ π1 0 0 -1.3455 10-1 π2 4.9213 10-3 -1.3814 10-1 0 π3 -3.5512 10-5 1.6522 10-2 3.0401 10-4 π4 4.7629 10-8 6.3784 10-6 1.3136 10-7 π5 0 -3.1030 10-3 -5.8863 10-5 π6 0 -2.0329 10-2 -6.4986 10-4 π7 -3.5549 10-4 0 0 π8 1.1021 10-3 0 -9.0317 10-7 π9 -1.3924 10-1 0 0 π10 -2.8663 10-6 1.0935 10-6 0 π11 2.9609 10-9 -4.0084 10-9 5.9573 10-12 π12 2.3285 10-3 0 0 π13 -2.1508 10-2 0 0 π14 0 0 -5.5630 10-9 π15 0 0 1.7685 10-6 π16 -1.2534 10-10 0 0 π17 3.5462 10-13 0 0 (0) (1) Table S2. Constants in Eqs. (S3.5) – (S3.6) for calculating Pitzer ion-interaction parameters (π½ππ , π½ππ π and πΆππ ) of Na2SO4(aq).3 (0) Const. π(π) = π½ππ (1) π π(π) = πΆππ π(π) = π½ππ * π1 1.869 10-2 1.0994 5.54900 10-3 π2 -1.03611 10-5 -3.2355 10-4 0 π3 3.00299 10-2 5.76552 10-1 5.14316 10-5 π4 -1.43441 10+1 -1.88769 10+2 0 π5 -6.66894 10-1 -2.05974 10-1 0 π6 0 -1.46744 10+3 3.45791 10-1 π7 -2.081437 10+2 -5.29421 10+2 4.25799 10+1 π8 -1.43441 10+1 -1.88769 10+2 0 π9 3.00299 10-2 5.76552 10-1 5.14316 10-5 π10 -2.07222 10-5 -6.471 10-4 0 π11 6.66894 10-1 2.05974 10-1 -3.45791 10-1 π12 0 1.46744 10+3 0 (1) *When calculating π½ππ , T2 in Eqs. (A5) and (A6) is 680K, otherwise T2 is 263K (0) (1) π Table S3. Constants of Eqs. (S3.7) – (S3.10) for calculating Pitzer ion-interaction parameters (π½ππ , π½ππ and πΆππ ) of MgCl2 (aq).4 (0) Coeff. (1) π(π, π) = π½ππ π π(π, π) = π½ππ (0) (1) (2) πΆππ = 2 [πΆππ + πΆππ exp(−π₯π1 ) + πΆππ exp(−π₯π2 )] (Eq. (A11)) (0) (1) π(π, π) = πΆππ (2) π(π, π) = πΆππ π(π, π) = πΆππ π1 -5.50111455 10+1 7.21220552 10+1 5.92428240 0 0 π2 1.50130326 10+1 -1.77145085 10+1 -1.65126386 -1.02256042 0 π3 -1.58107430 10-1 1.14397153 10-1 1.89399822 10-2 3.77018617 10-2 -2.28040769 10-3 π4 2.30409919 10-4 0 -2.99972128 10-5 -7.91682934 10-5 1.37425889 10-5 π5 -1.31768095 10-7 -1.43588435 10-7 1.89174291 10-8 5.91314258 10-8 -1.94821902 10-8 π6 -1.26699609 10-28 1.72952766 10-27 0 0 1.04649784 10-28 π7 2.82197499 10+2 3.41920714 10+3 5.49030201 10+1 -2.28493084 10+2 0 π8 0 0 4.50114048 10-2 0 0 π9 0 2.28440612 10-4 -1.08427926 10-2 0 0 π10 8.39661960 10-5 0 7.41041864 10-5 -7.79259941 10-5 0 π11 -4.60207270 10-7 0 -5.99961498 10-8 4.28675876 10-7 0 π12 6.21165614 10-10 0 0 -5.77509662 10-10 0 π13 8.43555937 10-31 -1.77573402 10-29 0 0 0 π14 0 -2.29668879 10+2 -4.60562847 0 0 π15 0 0 0 -5.13962051 10-4 0 π16 0 0 0 9.30761142 10-5 0 π17 0 -2.71485086 10-7 0 0 0 π18 0 0 0 0 0 π19 0 0 -1.39016981 10-15 -7.43350922 10-13 0 π20 0 0 0 0 0 π21 -1.11176553 1.01000272 10+1 1.40556304 10-1 1.12721557 0 (0) (1) π Table S4. Constants of Eq. (S3.12) for calculating Pitzer ion-interaction parameters (π½ππ , π½ππ and πΆππ ) of KCl(aq).5 (0) Const. (1) π(π) = π½ππ π π(π) = πΆππ π(π) = π½ππ π1 4.808 10-2 4.76 10-2 -7.88 10-4 π2 -7.5848 10+2 3.039 10+2 9.127 10+1 π3 -4.7062 1.066 5.8643 10-1 π4 1.0072 10-2 0 -1.298 10-3 π5 -3.7599 10-6 0 4.9567 10-7 π6 0 4.7 10-2 0 Supporting Information References 1. Holmes HF, Busey RH, Simonson JM, Mesmer RE CaCl2(aq) at elevated temperatures. Enthalpies of dilution, isopiestic molalities, and thermodynamic properties. Journal of Chemical Thermodynamics. 1994;26:271-298. 2. Rogers PSZ, Pitzer KS. High-temperatue thermodynamic properties of aqueous sodium sulfate solutions. Journal of Physical Chemistry. 1981;85:2886-2895. 3. Rumpf B, Maurer G. An Experimental and Theoretical Investigation on the Solubility of Carbon Dioxide in Aqueous Solutions of Strong Electrolytes. Berichte der Bunsengesellschaft für physikalische Chemie. 1993;97:85-97. 4. Wang P, Pitzer KS. Thermodynamic properties of aqueous magnesium chloride solutions from 250 to 600 K and to 100 MPa. Journal of Physical and Chemical Reference Data. 1998;27:971-991. 5. Holmes HF, Mesmer RE. Thermodynamic Properties of aqueous solutions of the alkali metal chlorides to 250 oC. Journal of Physical Chemistry. 1983;87:1242-1255.