From f385cf576e43acc8fcd4e874aa092f4a891c10a1 Mon Sep 17 00:00:00 2001 From: David Parkhurst Date: Wed, 10 Mar 2021 10:07:19 -0700 Subject: [PATCH] Tony's updates March 10, 2021 --- pitzer.dat | 22 +++++++++++----------- 1 file changed, 11 insertions(+), 11 deletions(-) diff --git a/pitzer.dat b/pitzer.dat index dda0ea5b..a9f55c91 100644 --- a/pitzer.dat +++ b/pitzer.dat @@ -1,5 +1,5 @@ # Pitzer.DAT for calculating pressure dependence of reactions -# and temperature dependence to 200 °C. With +# and temperature dependence to 200 °C. With # molal volumina of aqueous species and of minerals, and # critical temperatures and pressures of gases used in Peng-Robinson's EOS. # Details are given at the end of this file. @@ -237,7 +237,7 @@ Calcite CaCO3 = CO3-2 + Ca+2 log_k -8.406 delta_h -2.297 kcal - -analytic -237.04 -0.1077 0 102.25 6.79e5 # ref. 3 + data from Ellis, 1959, Plummer and Busenberg, 1982 + -analytic 8.481 -0.032644 -2133 # ref. 3 + data from Ellis, 1959, Plummer and Busenberg, 1982 -Vm 36.9 Carnallite KMgCl3:6H2O = K+ + Mg+2 + 3Cl- + 6H2O @@ -266,8 +266,9 @@ Diopside Vm 67.2 Dolomite CaMg(CO3)2 = Ca+2 + Mg+2 + 2 CO3-2 - log_k -17.083 + log_k -17.09 delta_h -9.436 kcal + -analytic -120.63 -0.1051 0 54.509 # 50–175°C, Bénézeth et al., 2018, GCA 224, 262-275. -Vm 64.5 Enstatite MgSiO3 + 2 H+ = - H2O + Mg+2 + H4SiO4 # llnl.dat @@ -477,7 +478,7 @@ Ntg(g) T_c 126.2 ; -P_c 33.50 ; -Omega 0.039 Mtg(g) Mtg = Mtg - -analytic 10.44 -7.65e-3 -6669 0 1.014e6 # CH4 solubilities 25 - 100°C + -analytic 10.44 -7.65e-3 -6669 0 1.014e6 # CH4 solubilities 25 - 100°C T_c 190.6 ; -P_c 45.40 ; -Omega 0.008 H2Sg(g) H2Sg = H+ + HSg- @@ -670,7 +671,7 @@ PITZER Ca+2 CO2 0.183 Ca+2 H4SiO4 0.238 # ref. 3 Cl- CO2 -0.005 - CO2 CO2 -1.34e-2 348 0.803 # new VM("CO2"), CO2 solubilities at high P, 0 - 150°C + CO2 CO2 -1.34e-2 348 0.803 # new VM("CO2"), CO2 solubilities at high P, 0 - 150°C CO2 HSO4- -0.003 CO2 K+ 0.051 CO2 Mg+2 0.183 @@ -911,7 +912,6 @@ SURFACE_SPECIES Hfo_wOH + H4SiO4 = Hfo_wH2SiO4- + H+ + H2O ; log_K -3.22 Hfo_wOH + H4SiO4 = Hfo_wHSiO4-2 + 2H+ + H2O ; log_K -11.69 - END MEAN GAM CaCl2 @@ -968,15 +968,15 @@ END # W * QBrn is the energy of solvation, QBrn is the pressure dependence of the Born equation, # W is fitted on measured solution densities. # z is charge of the solute species. -# Av is the Debye-Hückel limiting slope (DH_AV in PHREEQC basic). -# a0 is the ion-size parameter in the extended Debye-Hückel equation: +# Av is the Debye-Hückel limiting slope (DH_AV in PHREEQC basic). +# a0 is the ion-size parameter in the extended Debye-Hückel equation: # f(I^0.5) = I^0.5 / (1 + a0 * DH_B * I^0.5), # a0 = -gamma x for cations, = 0 for anions. # For details, consult ref. 1. # -# ref. 1: Appelo, Parkhurst and Post, 2014. Geochim. Cosmochim. Acta 125, 49-67. -# ref. 2: Procedures from ref. 1 using data compiled by Laliberté, 2009, J. Chem. Eng. Data 54, 1725. -# ref. 3: Appelo, 2015, Appl. Geochem. 55, 62-71. +# ref. 1: Appelo, Parkhurst and Post, 2014. Geochim. Cosmochim. Acta 125, 49–67. +# ref. 2: Procedures from ref. 1 using data compiled by Laliberté, 2009, J. Chem. Eng. Data 54, 1725. +# ref. 3: Appelo, 2015, Appl. Geochem. 55, 62–71. # http://www.hydrochemistry.eu/pub/pitzer_db/appendix.zip contains example files # for the high P,T Pitzer model and improvements for Calcite. # ref. 4: Appelo, 2017, Cem. Concr. Res. 101, 102-113.