Phases package

Coder package

# Equilibrate package¶

The equilibrate module implements a Python interface to the Equilibrate and EquilState classes. It also implements a Python class called MELTSmodel that wraps the objective-C classes: EquilibrateUsingMELTSv102, EquilibrateUsingMELTSv110, EquilibrateUsingMELTSv120, EquilibrateUsingpMELTSv561, EquilibrateUsingMELTSwithDEW, and EquilibrateUsingStixrude.

The Equilibrate class provides methods to calculate an equilibrium phase assemblage given a list of Phase class instances.

You can calculate equilibrium in closed thermodynamic systems under a variety of constraints:

• Temperature and pressure (Gibbs free energy minimization)

• Entropy and pressure (enthalpy minimization)

• Temperature and volume (Helmholtz free energy minimization)

• Entropy and volume (internal energy minimization)

You can also calculate equilibrium under constraints of fixed temperature and pressure in open thermodynamic systems by specifying one or more fixed elemental chemical potentials.

For details of the underlying theory and algorithms implemented in the Equilibrate class, see the notebooks in the PublicNotebooks/Equilibrate folder on the ENKI server.

class equilibrate.Equilibrate(element_l=None, phase_l=None, lagrange_l=None)[source]

Class for minimizing a generic thermodynamic potential in order to calculate an equilibrium phase assemblage.

The default potential is the Gibbs free energy.

Parameters
element_l[], default None

See documentation for element_list attribute.

phase_l[], default None

See documentation for phase_list attribute.

lagrange_l[], default None

See documentation for lagrange_list attribute.

Notes

Alternate potentials are specified by stipulating appropriate Lagrange transformations of the Gibbs potential.

Attributes
A_omni_inv

A matrix that transforms an array/matrix of mole numbers of elements to

bulk_comp

Bulk composition of the system as moles of elements

CTf

Stoichiometric vectors of element concentrations that embody the

element_list

A list of strings that identify the element basis for the system

entropy

Indicates if entropy is an independent variable of the minimal potential

eps_linear

Convergence criteria for the norm of the linear projection phase of the

eps_minimal_energy

Tolerance for establishing criteria for a minimum in the system potential.

eps_quad_optimal

Convergence criteria for the norm of the quadratic projection phase of

eps_quad_suboptimal

Relaxed convergence criteria for the norm of the quadratic projection

eps_rank

Tolerance for establishing the rank of the projected Hessian, which is

equil_cycle_max

Number of addition/removal cycles allowed for a phase before it is

equil_linear_min

Number of successful linear minimization attempts that do not result in a subsequent dimunition of the quadratic norm after which convergence is accepted as a “minimal energy” condition.

lagrange_list

A list of tuples characterizing the Lagrange transformation of the

lagrange_moles

Moles of chemical potential entities stipulated in dictionaries,

lagrange_no_mol_deriv

Produces a simplified gradient and hessian of the generalized

lagrange_use_omni

If set to True, the algorithm uses the omnicomponent phase exclusively to balance non-linear constraint reactions.

max_linear_iters

Maximum number of linear search steps associated with each quadratic

max_quad_iters

Maximum number of Newton quadratic minimization steps allowed in

moles_in

Moles of phase added to the system on detection of saturation

moles_out

Minimum total moles of phase allowed in system

phase_list

A list of class instances for phases that are permitted to form

phase_separ_threshold

Minimum energy in Joules for phase separation

reactions

Balanced reactions pertaining to the Lagrange constraints

rotate_orthog_proj

Prevents creation of a search direction for potential

use_numpy_lstsq

Flag to toggle method used to solve for quadratic search direction

volume

Indicates if volume is an independent variable of the minimal potential

VT_null

Orthogonal projection operator obtained from constraints on chemical

property A_omni_inv

A matrix that transforms an array/matrix of mole numbers of elements to an array/matrix of mole numbers of components of the omnicomponent phase

This matrix is the inverse of a matrix that maps elemental abundances to component mole numbers for the omnicomponent phase. This property is available only if chemical potential constraints are specified in lagrange_list and if there is an omnicomponent phase in the system.

Default is None

Returns
2-d nd_array
property CTf

Stoichiometric vectors of element concentrations that embody the Lagrange constraints

Default is None

Returns
np_array or None
property VT_null

Orthogonal projection operator obtained from constraints on chemical potentials derived from the lagrange_list entries

Default is None

Returns
np array or None
property bulk_comp

Bulk composition of the system as moles of elements

Returns
numpy array
property element_list

A list of strings that identify the element basis for the system

For example,[‘H’,’C’,’O’,’Na’,’Mg’,’Al’,’Si’,’P’,’K’,’Ca’,’Ti’,’Cr’, ‘Mn’,’Fe’,’Co’,’Ni’]

Returns
A Python list
property entropy

Indicates if entropy is an independent variable of the minimal potential and if temperature is a dependent variable

True if yes; False if reverse.

Returns
Flag (bool)
property eps_linear

Convergence criteria for the norm of the linear projection phase of the equilibrium calculation

Returns
Convergence tolerance (number)
property eps_minimal_energy

Tolerance for establishing criteria for a minimum in the system potential.

Successive linear minimization attempts (equil_linear_min) that do not result in a subsequent dimunition of the quadratic norm within this tolerance result in convergence as a “minimal energy” condition.

Returns
Tolerance (number)
property eps_quad_optimal

Convergence criteria for the norm of the quadratic projection phase of the equilibrium calculation

Returns
Convergence tolerance (number)
property eps_quad_suboptimal

Relaxed convergence criteria for the norm of the quadratic projection phase of the equilibrium calculation

Returns
Convergence tolerance (number)
property eps_rank

Tolerance for establishing the rank of the projected Hessian, which is needed to compute a valid quadratic search direction

Returns
Tolerance (number)
property equil_cycle_max

Number of addition/removal cycles allowed for a phase before it is suppressed from the equilibrium assemblage

Returns
Iteration limit (int)
property equil_linear_min

Number of successful linear minimization attempts that do not result in a subsequent dimunition of the quadratic norm after which convergence is accepted as a “minimal energy” condition.

Returns
Iteration limit (int)
execute(self, t=1000.0, p=1000.0, bulk_comp=None, state=None, con_deltaNNO=None, debug=0, stats=False)[source]

Calculates an equilibrium assemblage, returning the results as an instance of the EquilState class

Parameters
tfloat, default 1000.0

Temperature in Kelvins

pfloat, default 1000.0

Pressure in bars

bulk_compnumpy array, default None

Bulk composition of the system. Array of element concentrations, of the length and order of self.element_list

stateEquilState, default None

An instance of the EquilState class generated by this method. This parameter is only specified for a sequence of equilibrium calculations where the state of the system is initialized from a previous computation.

con_deltaNNOfloat or None

A non-None value for this parameter is ignored unless the system contains an omnicomponnet liquid phase of either 15 or 16 endmember components modeled after Ghiorso and Sack (1995) or Ghiorso and Gualda (2015), i.e. a MELTS silicate liquid thermodynamic model. If a value is set, the liquid is constrained to follow the nickel- nickel oxide oxygen buffer plus the offset value, con_deltaNNO, which is specified in log 10 fO2 units. For example, a value of 1.0 will force the system to equilibrate on the NNO+1 oxygen buffer by adjusting the ratio of ferric and ferrous iron according to the Kress and Carmichael (1991) calibration. Setting a value permits the system to be open to oxygen transfer; the bulk moles of oxygen in the system is no longer constrained by input bulk composition.

debugint, default 0

Level of detail printed by the method:

• 0, no information

• 1, minimal progress information

• 2, normal debugint output level

• 3, verbose debuging output level

statsbool, default False

Toggle printing of statistics associated with calculation progress

Returns
state: EquilState

An instance of the EquilState class that contains the equilibrium state of the system

Notes

Both the bulk_comp and state parameters cannot be set simultaneously.

kc_ferric_ferrous(self, t, p, m, mtype='components', compute='logfO2', deltaNNO=0.0, debug=0)[source]

Calculates oxygen fugacity or ferric-ferrous ratio for silicate melts using the Kress and Carmichael (1991) calibration

Parameters
tfloat

Temperature in Kelvins

pfloat

Pressure in bars

mnumpy ndarray

An array of moles of endmember liquid components correcponding to the model of Ghiorso and Sack (1995) (m has length 15) or the model of Ghiorso and Gualda (2015) (m has length 16)

mtypestr, default ‘components’

Type of values in m.

computestr, default ‘logfO2’

Type of output requested, see Returns.

deltaNNOfloat, default 0.0

If ferric-ferrous computation if requested (see compute), the ratio will be computed at log 10 f O2 = nickel-nickel oxide + deltaNNO

debugint, default 0

Level of detail printed by the method:

• 0, no information

• 1, minimal progress information

• 2, normal debugint output level

• 3, verbose debuging output level

Returns
resultfloat

log 10 f O2, if compute is set to ‘logfO2’ (default) excess chemical potential of O2, if compute is set to ‘chem_pot’

resultnumpy ndarray

array of oxide values, with the computed ferric-ferrous ratio appropriate to the imposed log f O2. The oxides are in standard order: SiO2, TiO2, Al2O3, Fe2O3, Cr2O3, FeO, MnO, MgO, NiO, CoO, CaO, Na2O, K2O, P2O5, H2O, [CO2]

kc_print_state(self, state=None, silent=False)[source]

Prints information about the current system state in terms of the Kress and Carmichael (1991) ferrous-ferric equilibrium model

Parameters
stateEquilState, default None

An instance of the EquilState class generated by this method. This parameter is only specified for a sequence of equilibrium calculations where the state of the system is initialized from a previous computation.

silentbool, default False

Flag to silence printing

Returns
resulttuple or None

Returns None if state is None or the system does not contain an omnicomponent phase name ‘Liquid’, else returns a tuple with the computer log 10 fO2 of the liquid phase relative to the NNO oxygen buffer, the value of log 10 fO2 on the buffer, and the total number of moles of oxygen in the system

property lagrange_list

A list of tuples characterizing the Lagrange transformation of the Gibbs free energy to form the operative thermodynamic potential

Each tuple has two terms:

1. Either of the following:

• A string with content ‘T’ or ‘P’

• A dictionary keyed on element symbols with values corresponding to stoichiometric coefficients of element chemical potentials. These linear combinations of potentials are fixed by the constraint.

2. A function to compute values for the constraints specified in (1)

The function has a signature func(T, P, state), where T is temperature in K, P is pressure in bars, and state is an instance of the EquilState class.

Returns
A Python list of tuples
property lagrange_moles

Moles of chemical potential entities stipulated in dictionaries, which are contained in the lagrange_list constraints

Default is None

Returns
np.array or None
property lagrange_no_mol_deriv

Produces a simplified gradient and hessian of the generalized Khorzhinskii potential

Assume that the generalized Khorzhinkii potential is constructed so that the imposed chemical potential is not a function of mole numbers of any phase in the system. Alternatively, the imposed potential is stoichiometrically assembled using reaction coefficients involving equilibrium phases in the assemblage. This option produces a simplified gradient and hessian of the generalized Khorzhinskii potential, but does not affect construction of the equality constraint matrix nor the Lagrange multiplier terms in the hessian of the Lagrangian function. It is seldom necessary to set this flag to True.

Default is False

Returns
Flag (bool)
property lagrange_use_omni

If set to True, the algorithm uses the omnicomponent phase exclusively to balance non-linear constraint reactions.

Default is True

Returns
Flag (bool)
log10NNO(self, t, p)[source]

Calculates the base 10 logarithm of oxygen fugacity along the nickel- nickel oxide buffer

Parameters
tfloat

Temperature in Kelvins

pfloat

Pressure in bars

Returns
resultfloat

log (10) f O2

Notes

Algorithm from O’Neill and Pownceby (1993, Contributions to Mineralogy and Petrology, 114, 296-314) using the pressure correction suggested by Frost (1991, Mineralogical Society of America, Reviews in Mineralogy, v. 25, 1-9)

property max_linear_iters

Maximum number of linear search steps associated with each quadratic iteration

Returns
Number of linear search steps (int)
property max_quad_iters

Maximum number of Newton quadratic minimization steps allowed in computation

Returns
Number of steps allowed (int)
property moles_in

Moles of phase added to the system on detection of saturation

Returns
property moles_out

Minimum total moles of phase allowed in system

If there is less than this quantity, the phase is discarded.

Returns
Minimum moles allowed (number)
mu0O2(self, t, p)[source]

Calculates the chemical potential of oxygen gas in the standard state of unit fugacity at one bar and any tenperature

Parameters
tfloat

Temperature in Kelvins

pfloat

Pressure in bars

Returns
resultfloat

standard state chemical potential in Joules/mole of O2 gas

Notes

Algorithm from Berman (1988).

muNNO(self, t, p, delta=0.0)[source]

Calculates the excess chemical potential of oxygen along the nickel- nickel oxide (+ delta offset) buffer

Parameters
tfloat

Temperature in Kelvins

pfloat

Pressure in bars

deltafloat, default 0.0

Offset in base 10 log units relative to the nickel-nickel oxide oxygen buffer

Returns
resultfloat

Excess chemical potential of oxygen in Joules/mole of O2

Notes

See definition of function log10NNO(t, p)

property phase_list

A list of class instances for phases that are permitted to form

These instances must derive from the PurePhase or SolutionPhase classes, which are defined in the phases module.

Returns
A Python list
property phase_separ_threshold

Minimum energy in Joules for phase separation

Gibbs free energy threshold that must be attained in order to add another instance of a phase to the equilibrium assemblage. In the phase unmixing (immiscibility) algorithm, candidate compositions are tested and if one is found with a Gibbs free energy below the projected tangent plane to the input composition by this amount, then the new phase instance is added to the system. The value is in Joules and should always be negative. Values larger than the default will likely encourage the detection of false unmixing events; values more negative will likely prevent the detection of unmixing and result in metastable assemblages. Use caution when altering the default value.

Default is -0.1

Returns
Threshold value (number)
property reactions

Balanced reactions pertaining to the Lagrange constraints

Default is None

Returns
np.array or None
property rotate_orthog_proj

Prevents creation of a search direction for potential minimization that has unwanted coupling of oxygen-bearing components

The basis vectors of the orthogonal projection matrix, VT_null, generated from the lagrange_list attribute, are rotated to zero to minimize the contribution of oxygen to the null space. This flag is enabled to avoid creating a search direction for potential minimization that has unwanted coupling of oxygen-bearing components (for more information, see method _compute_null_space(…)). This option is seldom needed and can be applied only if no omnicomponent phase is present in the system.

Default is False

Returns
Flag (bool)
property use_numpy_lstsq

Flag to toggle method used to solve for quadratic search direction

The quadratic search direction, dn, is computed by solving a system of equations given by H dn = -g, where H is the projected Hessian and g the projected gradient of the system potential (e.g., the system Gibbs free energy). If use_numpy_lstsq is True (default), the solution method is numpy’s linalg.lstsq method. If False, a QR decomposition method from the Python package statsmodels is utilized. The numpy method uses SVD decomposition and is slower, but more tolerant of rank deficient solutions (e.g., near phase rule violations).

Returns
Flag (bool)
property volume

Indicates if volume is an independent variable of the minimal potential and if pressure is a dependent variable

True if yes; False if reverse.

Returns
Flag (bool)
class equilibrate.EquilState(elements_l, phases_l)[source]

Class for holding the phase state for an equilibrium model determined by Equilibrate

Parameters
elements_l[]

A list of strings identifying the chemical elements present in the system

phases_l[]

A list of class instances for phases that are in the system. These instances must derive from the PurePhase or SolutionPhase classes, which are defined in the phases module.

Attributes
c_matrix

Numpy matrix that maps elements to moles of endmembers

c_omni

Numpy conversion matrix for the omnicomponent phase (if one exists)

c_omni_qr

Tuple of Numpy matrices of the Q,R decomposition of c_omni

c_qr_decomp

Tuple of Numpy matrices of the Q,R decomposition of the c_matrix

element_l

List of atomic numbers of elements in the system

phase_d

A dictionary of dictionaries that holds properties of system phases

pressure

Pressure of the assemblage, in bars

temperature

Temperature of the assemblage, in Kelvins

G(self, t=1000.0, p=1000.0)[source]

Returns Gibbs free energy of the system; a scalar

affinities(self, phase_name=None)[source]

Returns affinity of phases in the system

Parameters
phase_namestr, default None

Name of phase in system. If None, returns a dictionary of system phases, with names as keys and ‘stable’ or ‘unstable’ as values.

property c_matrix

Numpy matrix that maps elements to moles of endmembers

Moles of endmembers are indexed by row, and moles of elements are indexed by column.

Returns
Numpy 2-D array
c_matrix_for_phase(self, phase_name)[source]

Returns a slice of c_matrix relevant to the specified phase_name

Parameters
phase_namestr

Name of a system phase

property c_omni

Numpy conversion matrix for the omnicomponent phase (if one exists)

Moles of endmembers are indexed by row, and moles of elements are indexed by column.

Returns
np 2-D array
property c_omni_qr

Tuple of Numpy matrices of the Q,R decomposition of c_omni

Returns
tuple
property c_qr_decomp

Tuple of Numpy matrices of the Q,R decomposition of the c_matrix

Returns
tuple
compositions(self, phase_name=None, ctype='components', units='moles')[source]

Returns compositions of phases in the system

Parameters
phase_namestr, default None

Name of phase in system

ctypestr, default ‘components’

Compositional descriptor. Permitted: ‘components’, ‘oxides’, ‘elements’

unitsstr, default ‘moles’

Units of composition. Permitted: ‘moles’, ‘mole_frac’, ‘wt%’

Returns
resultnumpy array

One dimensional vector

Notes

If units is set to ‘oxides’ or ‘elements’, results are returned in an array of standard length and order.

d2GdP2(self, t=1000.0, p=1000.0)[source]

Returns the second pressure derivative of the Gibbs free energy of the system; a scalar, and the negative of the volume times the system’s coefficient of isothermal compressibility

d2GdPdn(self, t=1000.0, p=1000.0)[source]

Returns the second derivative of G of the system with respect to pressure and mole numbers; a 1-D numpy array

d2GdT2(self, t=1000.0, p=1000.0)[source]

Returns the second temperature derivative of the Gibbs free energy of the system; a scalar, and the negative of the temperature times the system heat capacity

d2GdTdP(self, t=1000.0, p=1000.0)[source]

Returns the cross temperature-pressure derivative of the Gibbs free energy of the system; a scalar, and the volume times the system’s coefficient of isothermal expansion

d2GdTdn(self, t=1000.0, p=1000.0)[source]

Returns the second derivative of G of the system with respect to temperature and mole numbers; a 1-D numpy array

d2Gdn2(self, t=1000.0, p=1000.0, element_basis=True)[source]

Returns the second molar derivative of G of system; a 2-D numpy array

Parameters
element_basisbool, def True

If True, returns a projected Hessian on an element basis

d3GdP2dn(self, t=1000.0, p=1000.0)[source]

Returns the third derivative of G of the system with respect to pressure twice and mole numbers once; a 1-D numpy array

d3GdP3(self, t=1000.0, p=1000.0)[source]

Returns the third pressure derivative of the Gibbs free energy of the system; a scalar

d3GdPdn2(self, t=1000.0, p=1000.0)[source]

Returns the first pressure and second molar derivative of G of system; a 2-D numpy array

d3GdT2dP(self, t=1000.0, p=1000.0)[source]

Returns the third pressure derivative of the Gibbs free energy of the system; a scalar

d3GdT2dn(self, t=1000.0, p=1000.0)[source]

Returns the third derivative of G of the system twice with respect to temperature and once with respect to mole numbers; a 1-D numpy array

d3GdT3(self, t=1000.0, p=1000.0)[source]

Returns the third temperature derivative of the Gibbs free energy of the system; a scalar

d3GdTdP2(self, t=1000.0, p=1000.0)[source]

Returns the third pressure derivative of the Gibbs free energy of the system; a scalar

d3GdTdPdn(self, t=1000.0, p=1000.0)[source]

Returns the third derivative of G of the system with respect to temperature, pressure and mole numbers; a 1-D numpy array

d3GdTdn2(self, t=1000.0, p=1000.0)[source]

Returns the first temperature and second molar derivative of G of system; a 2-D numpy array

d3Gdn3(self, t=1000.0, p=1000.0, phase=None, cmp=None)[source]

Returns the third molar derivative of G system for the cmp component of the phase named phase as a 2-D numpy array

Parameters
phasestr, def None
cmpint, def None

for the phase named phase d3Gdn3[cmp][*][*] is returned

dGdP(self, t=1000.0, p=1000.0)[source]

Returns the pressure derivative of the Gibbs free energy of the system; a scalar, and the system volume

dGdT(self, t=1000.0, p=1000.0)[source]

Returns the temperature derivative of the Gibbs free energy of the system; a scalar, and the negative of the system entropy

dGdn(self, t=1000.0, p=1000.0, element_basis=True, full_output=False, use_omni_phase=False)[source]

Returns the first molar derivative of G of the system; a 1-D numpy array

Parameters
element_basisbool, def True

If True, returns a projected array of element chemical potentials

full_outputbool, def False

If True, returns a tuple with full output from numpy lstlq method

use_omni_phasebool, def False

If True, returns a projected array of element chemical potentials using the omnicomponent phase as a basis. The system must have an omnicomponent phase, and element_basis must be set to True for this keyword to have effect.

property element_l

List of atomic numbers of elements in the system

Returns
A Python list
moles_elements(self, phase_name)[source]

Returns array of moles of elements in phase

Parameters
phase_namestr

Name of a system phase

Returns
resultnp_array

Numpy array of mole numbers of the reduced set of elements in the phase

moles_v(self, reaction_v)[source]

Computes of a reaction product

moles (scalar) = (mole vector of all endmembers of all active phases in the system) x (input mole vector of reaction coefficients)

Parameters
reaction_vndarray

Array of reaction coefficients

Returns
molesfloat

Moles of reaction product

omni_phase(self)[source]

Returns first omnicomponent phase in the phase dictionary

oxide_comp(self, phase_name, output='wt%', prune_list=True)[source]

Returns a dictionary of concentrations of oxides in phase

Parameters
phase_namestr

Name of a system phase

outputstr, default “wt%”

Units of output: ‘wt%’ (default), ‘moles’, ‘grams’

prune_listbool, default True

Remove zeroed valued entries

Returns
resultcollections.OrderedDict

Dictionary of oxide concentration values, keyed by oxide

property phase_d

A dictionary of dictionaries that holds properties of system phases

Returns
Dictionary of phases in the system (dict)
property pressure

Pressure of the assemblage, in bars

Returns
float
print_state(self, level='summary', wt_as_oxides=True)[source]

Prints results about the system state

Parameters
levelstr

Level of detail to be printed

wt_as_oxidesbool, default True

Print wt% values on an oxide basis; otherwise print wt% of endmember components.

properties(self, phase_name=None, props=None, units=False)[source]

Returns properties of phases in the system

Parameters
phase_namestr, default None

Name of phase in system. If None, returns a dictionary of system phases, with names as keys and ‘stable’ or ‘unstable’ as values.

propsstr, default None

Name of property to be retrieved. If None, a list of valid properties is returned.

unitsbool, default False

Property units are provided as the second entry of a returned tuple.

set_phase_comp(self, phase_name, cmp, input_as_elements=False)[source]

Sets the endmember moles and total moles a phase in the system

Parameters
phase_namestr

Name of a system phase

cmpndarray

1-D Numpy array with compositional data

input_as_elementsbool, def False

If True, convert input array from moles of elements to moles of endmember components.

Returns
validbool

True if input composition is valid for phase

property temperature

Temperature of the assemblage, in Kelvins

Returns
float
tot_grams_phase(self, phase_name)[source]

Returns total grams of phase

Parameters
phase_namestr

Name of a system phase

tot_moles_elements(self)[source]

Returns array of moles of elements in system

Returns
resultnp_array

Numpy array of mole numbers of the reduced set of elements in the system

tot_moles_phase(self, phase_name)[source]

Returns total moles of phase

Parameters
phase_namestr

Name of a system phase

class equilibrate.MELTSmodel(version='1.0.2')[source]

Class for creating an instance of the Equilibrate PhaseObjC class that is tailored to calculate equilibrium phase assemblages using one of the MELTS calibrations.

Valid initializers are version=’1.0.2’, ‘1.1.0’, ‘1.2.0’, ‘5.6.1’, ‘DEW’, ‘OnlyDEW’

add_sheet_to_workbook_named(self, wb, sheetName)[source]

Creates a new sheet in an existing Excel workbook.

Parameters
wbtype Workbook

A pointer to an existing Excel workbook

sheetNamestring

New sheet name in the specified Excel workbook

Returns
wstype Worksheet

A pointer to an Excel worksheet in the specified workbook, wb

Notes

Part of the Excel workbook functions subpackage

equilibrate_sp(self, S_a, P_a, initialize=False)[source]

Determines the equilibrium phase assemblage at an entropy-pressure point or along a series of S-P points.

The bulk composition of the system must first be set by calling the function:

set_bulk_composition

Parameters
S_afloat or numpy array of floats

Entropy in Joules per Kelvins. Either a scaler values or a numpy array of float values must be provided.

P_afloat or numpy array of floats

Pressure in mega-Pascals. Either a scaler values or a numpy array of float values must be provided.

NOTE: If both t_a and p_a are arrays, then they must both be the same length.

initializebool, optional

True if this is a S-, P-point that starts a sequence of calculations.

False if this is a continuation S-,P-pair or series of pairs.

Returns
output_aan array of tuples

tuple = (status, T, P, xmlout):

• status is a string indicating the status of the calculation: success/failiure, Reason for success/failure.

• T is a float value corresponding to the temperature in degrees centigrade.

• P is a float value corresponding to the pressure in mega-Pascals.

• xmlout is an xml document tree of the type xml.etree.ElementTree. The xml tree contains information on the masses and abundances of all phases in the system. xmlout is utilized as input for a number of functions in this package that retrieve properties of the equilibrium assemblage.

Notes

The xmlout document tree will be expanded to include thermodynamic properties of the phases and chemical affinities of phases not present in the equilibrium assemblage.

equilibrate_sv(self, S_a, V_a, initialize=False)[source]

Determines the equilibrium phase assemblage at an entropy-volume point or along a series of S-V points.

The bulk composition of the system must first be set by calling the function:

set_bulk_composition

Parameters
S_afloat or numpy array of floats

Entropy in Joules per Kelvins. Either a scaler values or a numpy array of float values must be provided.

V_afloat or numpy array of floats

Volume in Joules per bar. Either a scaler values or a numpy array of float values must be provided.

NOTE: If both t_a and p_a are arrays, then they must both be the same length.

initializebool, optional

True if this is a S-, V-point that starts a sequence of calculations.

False if this is a continuation S-,V-pair or series of pairs.

Returns
output_aan array of tuples

tuple = (status, T, P, xmlout):

• status is a string indicating the status of the calculation: success/failiure, Reason for success/failure.

• T is a float value corresponding to the temperature in degrees centigrade.

• P is a float value corresponding to the pressure in mega-Pascals.

• xmlout is an xml document tree of the type xml.etree.ElementTree. The xml tree contains information on the masses and abundances of all phases in the system. xmlout is utilized as input for a number of functions in this package that retrieve properties of the equilibrium assemblage.

Notes

The xmlout document tree will be expanded to include thermodynamic properties of the phases and chemical affinities of phases not present in the equilibrium assemblage.

equilibrate_tp(self, T_a, P_a, initialize=False)[source]

Determines the equilibrium phase assemblage at a temperature-pressure point or along a series of T-P points.

The bulk composition of the system must first be set by calling the function:

set_bulk_composition

Parameters
t_afloat or numpy array of floats

Temperature in degrees centigrade. Either a scaler values or a numpy array of float values must be provided.

p_afloat or numpy array of floats

Pressure in mega-Pascals. Either a scaler values or a numpy array of float values must be provided.

NOTE: If both t_a and p_a are arrays, then they must both be the same length.

initializebool, optional

True if this is a T-, P-point that starts a sequence of calculations.

False if this is a continuation T-,P-pair or series of pairs.

Returns
output_aan array of tuples

tuple = (status, T, P, xmlout):

• status is a string indicating the status of the calculation: success/failiure, Reason for success/failure.

• T is a float value corresponding to the temperature in degrees centigrade.

• P is a float value corresponding to the pressure in mega-Pascals.

• xmlout is an xml document tree of the type xml.etree.ElementTree. The xml tree contains information on the masses and abundances of all phases in the system. xmlout is utilized as input for a number of functions in this package that retrieve properties of the equilibrium assemblage.

Notes

The xmlout document tree will be expanded to include thermodynamic properties of the phases and chemical affinities of phases not present in the equilibrium assemblage.

equilibrate_tv(self, T_a, V_a, initialize=False)[source]

Determines the equilibrium phase assemblage at a temperature-volume point or along a series of T-V points.

The bulk composition of the system must first be set by calling the function:

set_bulk_composition

Parameters
T_afloat or numpy array of floats

Temperature in degrees centigrade. Either a scaler values or a numpy array of float values must be provided.

V_afloat or numpy array of floats

Volume in Joules per bar. Either a scaler values or a numpy array of float values must be provided.

NOTE: If both t_a and p_a are arrays, then they must both be the same length.

initializebool, optional

True if this is a T-, V-point that starts a sequence of calculations.

False if this is a continuation T-,V-pair or series of pairs.

Returns
output_aan array of tuples

tuple = (status, T, P, xmlout):

• status is a string indicating the status of the calculation: success/failiure, Reason for success/failure.

• T is a float value corresponding to the temperature in degrees centigrade.

• P is a float value correcponding to the pressure in mega-Pascals.

• xmlout is an xml document tree of the type xml.etree.ElementTree. The xml tree contains information on the masses and abundances of all phases in the system. xmlout is utilized as input for a number of functions in this package that retrieve properties of the equilibrium assemblage.

Notes

The xmlout document tree will be expanded to include thermodynamic properties of the phases and chemical affinities of phases not present in the equilibrium assemblage.

fractionate_phases(self, root, frac_coeff)[source]

Fractionates phases from the system. Partitions and maintains an internal dictionary of fractionates and automatically modifies system bulk composition to reflect fractionation.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_xx

frac_coeffdictionary

A dictionary keyed on phase names with values that indicate the fraction of each phase that should fractionate.

See get_dictionary_of_default_fractionation_coefficients().

Returns
dictdictionary

A dictionary keyed on phase names with values corresponding to a dictionary of phase properties. Keys are property names.

get_composition_of_phase(self, root, phase_name='System', mode='oxide_wt')[source]

Returns the composition of a phase in the specified equilibrium assemblage as a dictionary, with composition tabluated in the specified mode.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_xx

phase_namestring, optional

The name of the phase whose abundance is requested, or the string ‘System’, which returns the combined mass of all phases in the system. Default value is ‘System’.

modestring, optional

Controls the contents of the returned dictionary.

• ‘formula’ returns a dictionary with the string ‘formula’ as key and value set to a string representation of the phase formula. For pure component phases, this is the standard phase formula. For solutions, this is the actual formula constructed by weighting the endmember components by their mole fractions.

• ‘oxide_wt’ returns a dictionary of oxide string keys with values in wt%. This is a valid mode for all phase_name entries.

• ‘component’ returns a dictionary of endmember component keys with values in mole fraction. The length of this dictionary will vary dependening on the number of components that describe the solution. Pure phases return an empty dictionary, as does phase_name set to ‘System’.

The default value of mode is ‘oxide_wt’.

Returns
dictdictionary

A dictionary describing the composition of phase_name according to the mode specified. The dictionary will be empty if phase_name is not present in the equilibrium assemblage. It will also be empty for certain cases described above under mode.

get_dictionary_of_affinities(self, root, sort=True)[source]

Returns an ordered dictionary of tuples of chemical affinity and phase formulae for undersaturated phases in the system.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_xx

sortboolean

A flag when set to sort the dictionary in order of ascending affinities

Returns
dictOrderedDict

A Python ordered dictionary. Dictionary keys are strings naming the phases not in the equilibrium assemblage but known to the system. These phases are by definition undersaturated. Dictionary values are tuples consisting of a float value and a string: (affinity, formula). For a solution phase, the formula is the composition closest to equilibrium with the reported phase assemblage. Dictionary ordering corresponds to array order in get_phase_names(), unless sorted is set to True; then entries are ordered by ascending chemical affinity.

get_dictionary_of_default_fractionation_coefficients(self, fracLiq=False, fracSolid=True, fracFluid=True, fracCoeff=1.0)[source]

Returns a dictionary of default coefficients for phase fractionation.

These coefficients may be modified by the user. They are used when setting the extent to which a phase will fractionate from the equilibrium assemblage.

Parameters
fracLiqbool, optional

Flag to indicate if liquid phases should be fractionated from the system. Default is False.

fracSolidsbool, optional

Flag to indicate if solid phases should be fractionated from the system. Default is True.

fracFluidsbool, optional

Flag to indicate if fluid phases should be fractionated from the system. Default is True.

fracCoefffloat, optional

Fractionation coefficient, which gives the fractional extend to which the mass of the phase is extracted during phase fractionation. Default is 1.0 (100%).

Returns
dictdictionary

A Python dictionary keyed on phases with values giving the extent (in fractional units) that a phase will fractionation mass.

Notes

This dictionary is provided as input to the function fractionate_phases(). The default configuration fractionates all solid/fluid phases and retains liquid.

get_list_of_phases_in_assemblage(self, root)[source]

Returns a list of phases in the specified equilibrium assemblage.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_xx

Returns
listlist

A Python list of all phases in the equilibrium assemblage

get_list_of_properties(self)[source]

Returns a list of properties reported for each phase in an equilibrium assemblage.

Returns
listlist

A Python list of all properties of phases in an equilibrium assemblage

get_mass_of_phase(self, root, phase_name='System')[source]

Returns the mass of a phase in the specified equilibrium assemblage.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_xx

phase_namestring, optional

The name of the phase whose abundance is requested, or the string ‘System’, which returns the combined mass of all phases in the system. Default value is ‘System’.

Returns
valuefloat

The mass of the phase in the equilibrium assemblage specified by root, in grams. If the specified phase is not in the equilibrium assemblage, a value of zero is retuned.

get_object_for_phase(self, phase_name)[source]

Retrieve an object instance for the named phase.

Parameters
phase_name: string

Name of phase

Returns
object: instance of a phase class

null if the phase is not in the stable assemblage

get_oxide_names(self)[source]

Retrieves a list of system oxides

Composition of the system can be expressed in terms of these oxides.

Returns
arraystrings

An array of strings naming system components in terms of oxides

get_phase_inclusion_status(self)[source]

Retrieves a dictionary of the inclusion status of each phase

Returns
dictdictionary

A dictionary of boolean values indicating the inclusion status of each phase (key) known to the system

get_phase_names(self)[source]

Retrieves a list of system phases

Names of phases known to the system

Returns
arraystrings

An array of strings naming system phases

get_properties_of_DEWFluid(self, property_name='species', T=1000, P=1000)[source]

Retrieves a dictionary of properties of the specified type

DEWFluid must exist in the equilibrium assemblage; otherwise an empty dictionary is returned.

Parameters
property_name: string, optional

‘species’ (default) returns a dictionary of species mole fractions in the equilibrated solution.

‘mu’ returns a dictionary of species chemical potentials in the equilibrated solution.

‘activity’ returns a dictionary of species activities in the equilibrated solution.

Tfloat optional

Temperature in degrees centigrade (default is 1000°C)

Pfloat optional

Pressure in bars (default is 1000 bars)

Returns
dictionary: a python dictionary

Keys are species names (strings).

Values are species concentrations in mole fraction, or chemical potential, or thermodynamic activity, depending on the value of property_name.

get_property_of_phase(self, root, phase_name='System', property_name='Mass')[source]

Returns the specified property of a phase in the specified equilibrium assemblage.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_xx

phase_namestring, optional

The name of the phase whose property is requested, or the string ‘System’, which returns the combined property of all phases in the system. Default value is ‘System’.

property_namestring, optional

The name of the property to be returned. Default value is ‘Mass’.

Returns
valuefloat

The property of the phase in the equilibrium assemblage specified by root, in standard units. If the specified phase is not in the equilibrium assemblage, a value of zero is returned. If the property is not in the standard list, a value of zero is returned.

get_thermo_properties_of_phase_components(self, root, phase_name, mode='mu')[source]

Returns a dictionary of the specified component thermodynamic properties of the designated phase.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_xx.

phase_namestring

The name of the phase whose abundance is requested.

modestring, optional

Controls the contents of the returned dictionary.

• ‘mu’ returns a dictionary of endmember component keys with values of chemical potential. The length of this dictionary will vary depending on the number of components that describe the solution. Pure phases return a dictionary of unit length, with the phase name as key and their specific Gibbs free energy as value (J/g).

• ‘excess’ returns a dictionary of endmember component keys with values of excess chemical potential. The length of this dictionary will vary depending on the number of components that describe the solution. Pure phases return a dictionary of unit length, with the phase name as key and zero as value.

• ‘activity’ returns a dictionary of endmember component keys with values of component activity. The length of this dictionary will vary depending on the number of components that describe the solution. Pure phases return a dictionary of unit length, with the phase name as key and unity as value.

Returns
dictdictionary

A dictionary describing the thermodynamic properties of components in phase_name according to the mode specified. The dictionary will be empty if phase_name is not present in the equilibrium assemblage.

get_units_of_property(self, prop='Mass')[source]

Returns the units of a specified property.

Returns
stringstring

The units of the specified property. Returns ‘none’ if property is invalid.

output_summary(self, root, printT=True, printP=True, printMass=False, printSysWt=False, printSysM=False, printPhs=True, printPhsWt=False, printPhsM=False)[source]

Prints information about the specified equilibrium phase assemblage.

Parameters
roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_tp

printTbool, optional, default=True

Print the system temperature in degrees centigrade

printPbool, optional, default=True

Print the system pressure in mega-Pascals

printMass ; bool, optional, default=False

Print the mass of the system in grams

printSysWtbool, optional, default=False

Print the composition of the system in wt% oxides

printSysMbool, optional, default=False

Print the composition of the system in moles of elements

printPhsbool, optional, default=True

Print the phases present in the system, their masses (in grams) and their chemical formulas

printPhsWtbool, optional, default=False

Print the composition of each phase in wt% oxides (most often used in conjunction with printPhs=True)

printPhsMbool, optional, default=False

Print the composition of each phase in moles of endmember components (most often used in conjunction with printPhs=True)

print_default_settings(self)[source]

Prints list of options and tolerance settings for algorithm.

set_bulk_composition(self, oxide_d={})[source]

Sets the bulk composition of the system

This function first tests if the composition is feasible before setting the bulk composition of the system. You should check to make sure that the composition is feasible before proceeding.

Parameters
oxide_da python dictionary

A dictionary of oxide names and values, e.g. {‘SiO2’:77.8, ‘Al2O3’:12.0, …, ‘H2O’:3.74}

Returns
booleanTrue or False

True if the composition is feasible, in which case the composition of the system is defined.

False if the composition is infeasible, in which case the composition of the system is undefined.

Notes

Feasibility call has yet to be implemented: (Objective-C method call:) -(BOOL)compositionIsFeasible:(NSArray *)compositionInWtPercentOxides forSolution:(id <SolutionPhaseProtocol>)omniComponentPhase;

set_debug_state(self, debugS=False, debugV=False)[source]

Sets debug output level for Equilibrate class and subclasses

Parameters
debugSboolean, optional

Sets on or off low level debug output. Default is off (False).

debugVboolean, optional

Sets on or off high level debug output. Default is off (False).

set_entropy(self, s)[source]

Sets the entropy of the system and reinitializes a calculation sequence

Parameters
sfloat

Float value to set the system entropy in J/K.

set_phase_inclusion_status(self, status_d)[source]

Sets the inclusion status of specified phases

Parameters
status_ddictionary

A dictionary of phase name keys and boolean values. True sets inclusion, and False prevents inclusion of a phase in the equilibrium assemblage. Note that the chemical affinity of the phase will still be calculated even if the inclusion level is set to False.

set_pressure(self, p_mpa=200.0)[source]

Sets the pressure of the system and reinitializes a calculation sequence

Parameters
p_mpafloat optional

Float value to set the system pressure in mega-Pascals. Default is 200 MPa.

set_temperature(self, t_c=800.0)[source]

Sets the temperature of the system and reinitializes a calculation sequence

Parameters
t_cfloat optional

Float value to set the system temperature in degrees centigrade. Default is 800 °C.

set_volume(self, v)[source]

Sets the volume of the system and reinitializes a calculation sequence

Parameters
vfloat

Float value to set the system volume in J/bar

start_excel_workbook_with_sheet_name(self, sheetName='Summary')[source]

Create an Excel workbook with one named sheet.

Parameters
sheetNamestring

Sheet name in the new empty Excel workbook

Returns
wbtype Workbook

A pointer to an Excel workbook

Notes

Part of the Excel workbook functions subpackage

update_excel_workbook(self, wb, root)[source]

Writes the specified equilibrium system state to the specified Excel workbook.

Parameters
wbtype Workbook

A pointer to an existing Excel workbook

roottype xml.etree.ElementTree

An xml document tree returned by the function equilibrate_tp

Notes

The workbook is structured with a Summary worksheet and one worksheet for each equilibrium phase. The evolution of the system is recorded in successive rows. Row integrity is maintained across all sheets. This function may be called repeatedly using different root objects. Part of the Excel workbook functions subpackage.

write_excel_workbook(self, wb, fileName='junk.xlsx')[source]

Writes the specified Excel workbook to disk.

Parameters
wbtype Workbook

A pointer to an existing Excel workbook

fileNamestring, optional

Name of the file that will contain the specified Excel notebook. Default file name is ‘junk.xlsx’.

Notes

Part of the Excel workbook functions subpackage

write_to_cell_in_sheet(self, ws, col, row, value, format='general')[source]

Writes information into the specified row, col on the specified worksheet.

Parameters
wstype Worksheet

A pointer to a previously created Excel worksheet (see add_sheet_to_workbook_named)

colint

Column number to write entry to. Numbering starts at column one.

rowint

Row number to write entry to. Numbering starts at row one.

valuefloat

Value to place at entry

formatstring, optional

Format to use for value

• ‘general’ is the default; no formatting applied

• ‘number’ formats as ‘0.00’

• ‘scientific’ formats as ‘0.00E+00’

Notes

Part of the Excel workbook functions subpackage