advances in electrolyte thermodynamics... · advances in electrolyte thermodynamics peiming wang,...
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OLI Simulation Conference 2016
Conference organization by
Advances in Electrolyte Thermodynamics
Peiming Wang, Margaret Lencka, Ronald Springer, Jerzy Kosinski, Jiangping Liu, Ali Eslamimanesh, Gaurav Das, and Andre Anderko
Scope
• Structure of OLI’s thermodynamic models
• Progress in thermodynamic modeling • Results for selected chemistries
• How predictive can we be?
• Dielectric constant
• Status of databanks
• Plans for the future
Structure of Thermophysical Property Frameworks
Electrical conductivity
Viscosity
Aqueous (AQ) Framework Mixed-Solvent Electrolyte (MSE) Framework
Self-diffusivity
Thermal conductivity
Surface tension
Interfacial tension
Dielectric constant
MSE thermodynamics
Standard state: HKF EOS (direct)
GEX: MSE No concentration limit
Solids: Thermochemical
properties
Gas phase: SRK equation of state
2nd liquid phase: MSE GEX model (same as for
aqueous phase)
Interfacial phenomena: Ion exchange, surface
complexation, molecular adsorption
AQ thermodynamics Standard state: HKF
EOS (via fitting equations as default)
GEX: Bromley-Zemaitis I < 30 m; xorg < 0.3
Solids: Equilibrium constants
for SLE
Gas phase: SRK equation of state
2nd liquid phase: SRK EOS (same as for gas
phase)
Interfacial phenomena: Ion exchange, surface
complexation, molecular adsorption
Other properties Other properties
Electrical conductivity
Viscosity
Self-diffusivity
Progress in Thermodynamic Modeling: Inorganic systems
• Actinide chemistry • U(IV, VI), Np(IV, V, VI), Pu(III, IV, V, VI), Am(III), Cm(III)
• Oxides, hydroxides, carbonates, chlorides, nitrates
• Redox
• Surface complexation on MnOx
• Rare-earth element chemistry • REE chlorides, sulfates, carbonates, phosphates,
hydroxides, acetates, citrates, gluconates
• Transition metal chemistry • Ru, Rh, Tc fundamental chemistry
• Ag nitrate, sulfate systems
• Ni sulfate systems
Progress in Thermodynamic Modeling: Inorganic systems
• Post-transition metal chemistry • Pb silicate, molybdate, tungstate, acetate, formate, nitrate • Al nitrate and sulfate with corresponding acids • AlF3 - NaF
• Tellurium chemistry • Oxides, hydroxides, nitrates, compounds with Na, Zr, Mo
• Silicate chemistry • Na aluminosilicates, Ca, Mg, Zn, Al, Pb silicates
• Sodium phosphate chemistry
• Chemistry of solutes in CO2 environments • S0, NOx, SOx in CO2
• High-pressure, high-temperature scaling • BaSO4, CaCO3
Progress in Thermodynamic Modeling: Inorganic systems
• C – N – H chemistry • Melamine, melam, ammeline, ammelide, cyanuric acid • Cyanate chemistry
• Chelant chemistry • EDTA and IDA
• Potash chemistry • K2SO4 – KCl • Li2SO4
• Other salts • NaBr • Revisions of Sr – SO4 – CO2 chemistry • Revisions of FeS and FeCO3 chemistry
Progress in Thermodynamic Modeling: Organic systems
• Hydrocarbon chemistry • PVT properties of hydrocarbons • Methanol-hydrocarbon systems • CO2 – hydrocarbon – H2O systems • H2S – hydrocarbon – H2O systems • Methane – higher hydrocarbon systems • Methane – H2O – salt mixtures
• Organic acid chemistry • Maleic acid and anhydride • Acetic and formic acids with hydrocarbons
• Monoethylene glycol chemistry refinements • PVT properties • Effect on SrSO4, FeSO4, FeCO3
Thermodynamics of Actinides • Trivalent actinides
show similar phase behavior
• Weak complexation with Cl-
• Moderate increase in solubility due to Cl complexation
• Model is consistent with both solubility and TRLFS speciation data
Solubility of Am(OH)3
as a function of pH and Cl-
Speciation of Cm(III)
as a function of Cl-
Thermodynamics of Actinides • Dual effect of CO3/HCO3
• Strong complexation
• Formation of carbonate solids
Speciation of Cm(III) as a function of CO3/HCO3
Solubility of Am
as a function of pH and CO2
How does redox affect solubility? Behavior of Np(VI)
Np(VI) is unstable in acidic and neutral environments
May be easily reduced to Np(V) and Np(IV)
Solubility and speciation calculated by including redox equilibria
At near-neutral conditions, Np(V) predominates (red lines)
solubility of Np(VI) is governed by reductive dissolution
At alkaline conditions, Np(VI) predominates (blue lines)
Surface Complexation Np(V) on hausmanite (Mn3O4) in the presence of CO2
• Double-layer surface complexation model • Originally parameterized
for hydrous ferric oxide using AQ bulk thermodynamics
• Applied to actinide sorption on MnO2 (synthetic, biogenic), MnOOH, Mn3O4 using MSE bulk thermodynamics
• Explains relationship between bulk phase and surface speciation
NpO2-Mn3O4·OH0
NpO2+
NpO2OH
NpO2CO3-Mn3O4·OH2-
NpO2(CO3)2-Mn3O4·H2O3-
NpO2(CO3)2-Mn3O4·OH4-
NpO2CO3-
NpO2(CO3)23-
NpO2(CO3)35-
Thermodynamics of Rare Earth Elements
• DOE’s Critical Material Institute • Diversifying supply:
Improving methods to extract REEs from ores and waste
• Recycling and increasing efficiency of materials use
• OLI’s role • Provide tools for
predicting phase and chemical equilibria to optimize new or improved processes
0
2
4
6
8
10
12
14
16
18
20
-70 -40 -10 20 50 80 110 140 170 200
mL
aC
l3
t / oC
Sokolova (1988)Sokolova (1988)Sokolova (1988)Sokolova (1988)Friend (1940)Herkot (1989)Powell (1960)Nikolaev (1971/67/77/78/69)Zhuravlev (1972/74a)Tang (1982)Storozhenko (1988/86)Khutorskoi (1968/68a,b)Sheveleva (1973a,b/58/61/68)Chen, Y. G. (2003)Chen, J. X. (1990)Berecz (1990)Zelikman (1971)Volkov (1970)Zholalieva (1976/78)Alieva (1970)Brunisholz (1969)Petelina (1969)Sergeeva (1976)Voigt (1993)Cui (1997)Fischer (1968)Kost (1980)Li (1995)Liu (1999)Shi (1988)Shirai (1981)Sorokina (1977)Spedding (1977)Wang (2007)Zwietasch (1984)Voigt (1993)Voigt (1993)
LaCl3.H2O
LaCl3.7H2O
LaCl3.3H2O
LaCl3.9H2O
LaCl3.10H2O
Ice
Fundamentals: Phase behavior of LaCl3 – H2O
Thermodynamics of Rare Earth Elements: Application to Bioseparations
• Engineered cell surfaces used to separate REEs from aqueous solutions
• Lanthanide binding tags bind REEs
• Complexing agents are necessary to recover absorbed REEs
• What eluents will work?
* Park et al. Environ. Sci. Technol. 2016, 50 (5), 2735-2742.
Complexation of Tb
• Complexation is necessary to desorb REEs
• Predicted fraction of Tb uncomplexed in solution parallels the observed fraction of Tb that remains bound to the surface
0
0.2
0.4
0.6
0.8
1
0 10 20 30 40 50
Fra
cti
on
of
Tb
un
co
mp
lex
ed
Eluent (Na acetate) / mM
System:TbCl3 10 µm
CaCl2 0 or 150 mmNa acetate 0-50 mm
NaCl 10E-3 m
pH = 5
pH = 6.1
pH = 5 + CaCl2
pH = 6.1 + CaCl2
Ca competes with Tb for complexation with acetate.
0
0.2
0.4
0.6
0.8
1
0 5 10 15 20
Fra
cti
on
of
Tb
un
co
mp
lex
ed
Eluent (Na citrate) / µM
System:TbCl3 10 µm
CaCl2 0 or 150 mmNa citrate 0-50 mm
NaCl 10E-3 m
pH = 5 - No CaCl2
pH = 6.1 - No CaCl2
pH = 5 + CaCl2
pH = 6.1 + CaCl2
Ca does not effectively compete with Tb for complexation with citrate.
Acetate is inefficient for desorption and
Ca interferes with desorption
Small concentration of citrate is sufficient
for desorption
Modeling systems containing elemental sulfur
• What are the chemical transformations of SOx, NOx H2S, and O2 in CO2 transportation pipelines?
• Hence, what are the limits of safe operation?
• Part 1: Model the solubility of S0 in CO2-rich phases in order to predict whether solid S0 can drop out
• Systems analyzed: Pure S0, S0 – H2O, S0 – CO2
• Speciation of sulfur
• Species up to S020 have been detected
• S01 through S0
8 have been assumed • S0
8 is dominant at moderate conditions in gas phase
• Lower multimers become prevalent at higher temperatures
• In liquid phase, S08 predominates
• In CO2 phase, solvated S0 – CO2 species appears
S08
Solubility of S0 in CO2
• Two segments of solubility curves at each T corresponding to gas (or gas-like) and liquid (or liquid-like) CO2
• Transition is sharp for subcritical CO2 and gradual for supercritical CO2
1E-07
1E-06
1E-05
1E-04
1E-03
50 100 150 200 250 300 350 400 450
S8, m
ole
fra
cti
on
Pressure, atm
Kennedy and Wieland (1960)
Gu etal (1993)
Serin etal (2010)
Dugstad et al (2015)
Svenningsen et al (2016)
25C
45C
60C
90C
110C
120C
Pushing the Limits of Complexity: NaOH + H3PO4 + H2O
Temperature range:
to 350C
Chemical equilibria
• PO4-3, HPO4
-2,
H2PO4-1, etc.
• Association of
Na+/H2PO4-1
Phase equilibria
• Vapor-liquid
• Solid-liquid, sodium pyrophosphate (T
> 250C)
• Liquid-liquid (T >
270C)
Liquid-Liquid Equilibria at High Temperatures
• Increased ion pairing at high T drives liquid phase demixing
• Lower critical temperature
• LLE depends on the Na/P ratio
• If the solubility drops with T, LLE will not appear
How to Deal with Near-Critical Behavior?
• Classical models do not represent near critical behavior
• Crossover models would not be practical for highly speciated reactive systems
• A local model gives a fully quantitative representation of LLE in the high-T region
Modeling Silicates: Importance of Metastable Phases PbO – SiO2 – H2O
• Multiple competing silicate phases
• Both stable and metastable phases
1.E-09
1.E-08
1.E-07
1.E-06
1.E-05
1.E-04
1.E-03
1.E-02
1.E-01
1.E-05 1.E-04 1.E-03 1.E-02
m S
iO2
m PbO
SiO2 amorphous
SiO2 quartz
PbSiO3 alamosite
Pb2SiO4
Pb11Si3O17
PbO yellow
PbO red
SiO2 (quartz)
SiO2 (am)
Pb2SiO4
PbSiO3
Pb11Si3O17
PbO red PbO yellow
25 C 300 C
Mixtures of Hydrocarbons with Acetic Acid
• Reproducing vapor-liquid and liquid-liquid equilibria
• Generalization of parameters for normal alkanes to handle pseudocomponents
-20
-10
0
10
20
30
40
50
60
70
0.2 0.4 0.6 0.8 1
t / °C
x acetic acid
C7
C9
C10
C11
C12
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 0.2 0.4 0.6 0.8 1
x a
ceti
c aci
d
x hexane
fuse&Iguchi (1970), 25°C
Rao&Rao (1957), 31°C
acetic acid + hexane + water
P=1atm.
LLE for HAc – hexane – H2O ternary LLE for HAc – hydrocarbon binaries: Miscibility gap increases with carbon number
How Predictive Is the Model?
• Desirable scenario: • Develop model parameters based on binary data
• Predict the behavior of multicomponent systems
• If the model is physically correct, this works • Caveat: As long as there is no chemistry change in a
multicomponent system
• Two cases to illustrate predictions
Case 1: Mixed Chloride - Sulfate
Systems • Binary systems
• Regressed parameters • Cation-anion interaction
parameters
• Thermochemical properties of solids
• Based on experimental data • Solubilities
• VLE/osmotic coefficients
• Activity coefficients
• Enthalpies of dilution
• Heat capacity
• Density
Na2SO4 (rhombic)
Na2SO4 (monoclinic) Na2SO4 ·10H2O
Ice
Ice
NaCl ·2H2O
NaCl
NaCl – H2O
Na2SO4 – H2O
Case 1: Mixed Chloride - Sulfate Systems
• Ternary system
• Regressed parameters • Cl- - SO4
2- interactions
• Second-order correction
• Binary in nature but obtained from ternary data
• Full complexity of ternary behavior is reproduced
NaCl - Na2SO4 – H2O
Case 1: Mixed Chloride - Sulfate Systems: Pure Prediction
KCl – K2SO4 – H2O • Behavior of ternary
system is accurately predicted without any further parameter adjustment
• Parameters are fully transferable
• No new ternary chemical effects
Case 2: Mixed Al and Na Salts
• Binary and ternary systems
• Interactions regressed • Cation-anion
parameters
• Al3+ - Na+ cation-cation parameters
NaF – H2O
AlF3 – H2O
AlF3
Case 2: Mixed Al and Na Salts
AlF3 – NaF – H2O
• Although NaF and AlF3 are fairly soluble, solubility in the ternary system AlF3 – NaF – H2O is dramatically lower
• Specific ternary chemistry effect: Formation of sparingly soluble double salts • Cryolite, Na3AlF6, and chiolite, Na5Al3F14
• Ternary chemical effects need to be incorporated but cannot be simply predicted from the properties of binary or other ternary systems
Na3AlF6
Na5Al3F14
AlF3.3H2O
NaF
Predicting Dielectric Constant of Mixtures
• Calculating polarization • Kirkwood theory
• Mixing rule for polarization
• Good approximation without binary parameters
kT
g
v
Np A
33
4
9
121 2
n
i
ii
n
i
n
j
ijji
m
vx
vpxx
p
1
ijjjiiij kpvpvvp 1
2
1
Monoethylene glycol – water
Predicting Dielectric Constant
• Effect of ionic components
• Predicts universal decrease with ionic composition
• Effect of ion pairs is more complex
ionsXiii
0ss
IB1xA1 )ln(
NaCl at 25 C
NaCl at various T
AQ and MSE Databanks: A Comparison Databank Aqueous model:
Number of species Mixed-solvent electrolyte model: Number of species
General-purpose (process chemistry) PUBLIC 5407 (5407 in 10/2014)
MSEPUB 2590 (2150 in 10/2014)
Geochemical (solids formed on a geological timescale)
138 135
Corrosion (corrosion-related solids) 367 321
Urea (enabling urea-related reactions) Not available 8
Surface complexation, double layer 120 57
Ion exchange 13 0
Ceramics (ceramic solids) 36 Not applicable – included in MSEPUB
Low temperature (extension to calculate properties below 0 C)
227 Not relevant (MSEPUB works below 0 C)
Plans for the Future • Thermodynamics of rare-earth elements
• Applications to diversifying the supply, separation and recycling
• High-pressure, high-temperature scaling • Solubility of ZnS, PbS and CaSO4 in produced water
environments
• Chemistry of CO2 transmission • Predicting formation of corrosive phases in dense-phase
CO2
• Chemistry of silicates • Application to silica removal processes including surface
complexation and kinetics
Plans for the Future
• Potash chemistry • K – Na – Li – Ca – SO4 – Cl systems
• Amines and amine hydrochlorides • Towards further improvement of predictions
• Finalizing improvements of hydrocarbon chemistry
• Mutual diffusivity • Applications to mass-transfer separations
• Future client-driven projects