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Merge pull request #612 from bobmyhill/macaw
added MACAW EoS
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from __future__ import absolute_import | ||
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# This file is part of BurnMan - a thermoelastic and thermodynamic toolkit | ||
# for the Earth and Planetary Sciences. | ||
# Copyright (C) 2012 - 2024 by the BurnMan team, released under the GNU | ||
# GPL v2 or later. | ||
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import scipy.optimize as opt | ||
from . import equation_of_state as eos | ||
import warnings | ||
import numpy as np | ||
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# Try to import the jit from numba. If it is | ||
# not available, just go with the standard | ||
# python interpreter | ||
try: | ||
from numba import jit | ||
except ImportError: | ||
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def jit(fn): | ||
return fn | ||
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@jit(nopython=True) | ||
def make_params(K0, K0_prime, K_infinity_prime): | ||
a = ( | ||
16.0 * np.power(K0_prime, 3.0) | ||
+ 84.0 * np.power(K0_prime, 2.0) | ||
+ 192.0 * K0_prime | ||
- 972.0 * K_infinity_prime | ||
+ 1177.0 | ||
) | ||
b = 2.0 * np.power(K0_prime, 2.0) + 7.0 * K0_prime - 27.0 * K_infinity_prime + 38.0 | ||
omega = np.power((a + np.sqrt(a * a - 32.0 * b * b * b)), 1.0 / 3.0) | ||
C = ( | ||
(11.0 / 6.0) | ||
+ (1.0 / 3.0) * K0_prime | ||
- K_infinity_prime | ||
+ (np.power(2, -1.0 / 3.0) / 6) * omega | ||
+ (np.power(2, 1.0 / 3.0) / 3) * (b / omega) | ||
) | ||
B = K_infinity_prime - 1.0 | ||
A = K0 / (B - 0.5 * C + np.power(B + C, 2.0)) | ||
return A, B, C | ||
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class MACAW(eos.EquationOfState): | ||
""" | ||
Class for the MACAW equation of state | ||
detailed in Lozano and Aslam (2022; https://doi.org/10.1063/5.0076897). | ||
This equation of state has no temperature dependence. | ||
""" | ||
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def isothermal_bulk_modulus_reuss(self, pressure, temperature, volume, params): | ||
""" | ||
Returns isothermal bulk modulus :math:`K_T` :math:`[Pa]` as a function of pressure :math:`[Pa]`, | ||
temperature :math:`[K]` and volume :math:`[m^3]`. | ||
""" | ||
A, B, C = make_params(params["K_0"], params["Kprime_0"], params["Kprime_inf"]) | ||
Vrel = volume / params["V_0"] | ||
term1 = A * np.power(Vrel, -(B + 1)) | ||
term2 = np.exp((2.0 / 3.0) * C * (1 - np.power(Vrel, 1.5))) | ||
term3 = np.power(C * np.power(Vrel, 1.5) + B, 2.0) - ( | ||
0.5 * C * np.power(Vrel, 1.5) - B | ||
) | ||
return term1 * term2 * term3 | ||
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def volume(self, pressure, temperature, params): | ||
""" | ||
Get the Vinet volume at a reference temperature for a given | ||
pressure :math:`[Pa]`. Returns molar volume in :math:`[m^3]` | ||
""" | ||
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def delta_pressure(x): | ||
return self.pressure(0.0, x, params) - pressure | ||
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V = opt.brentq(delta_pressure, 0.1 * params["V_0"], 1.5 * params["V_0"]) | ||
return V | ||
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def pressure(self, temperature, volume, params): | ||
""" | ||
Returns pressure :math:`[Pa]` as a function of volume :math:`[m^3]`. | ||
""" | ||
A, B, C = make_params(params["K_0"], params["Kprime_0"], params["Kprime_inf"]) | ||
Vrel = volume / params["V_0"] | ||
term1 = A * np.power(Vrel, -(B + 1.0)) | ||
term2 = np.exp((2.0 / 3.0) * C * (1.0 - np.power(Vrel, 1.5))) | ||
term3 = C * np.power(Vrel, 1.5) + B | ||
return term1 * term2 * term3 - A * (B + C) + params["P_0"] | ||
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def molar_internal_energy(self, pressure, temperature, volume, params): | ||
""" | ||
Returns the internal energy :math:`\\mathcal{E}` of the mineral. :math:`[J/mol]` | ||
""" | ||
A, B, C = make_params(params["K_0"], params["Kprime_0"], params["Kprime_inf"]) | ||
Vrel = volume / params["V_0"] | ||
I1 = -params["V_0"] * ( | ||
np.power(Vrel, -B) * np.exp((2.0 / 3.0) * C * (1.0 - np.power(Vrel, 1.5))) | ||
- 1.0 | ||
) | ||
I0 = (-A * (B + C) + params["P_0"]) * params["V_0"] * (Vrel - 1.0) | ||
return -A * I1 - I0 | ||
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def gibbs_free_energy(self, pressure, temperature, volume, params): | ||
""" | ||
Returns the Gibbs free energy :math:`\\mathcal{G}` of the mineral. :math:`[J/mol]` | ||
""" | ||
return ( | ||
self.molar_internal_energy(pressure, temperature, volume, params) | ||
+ pressure * volume | ||
) | ||
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def isentropic_bulk_modulus_reuss(self, pressure, temperature, volume, params): | ||
""" | ||
Returns adiabatic bulk modulus :math:`K_s` of the mineral. :math:`[Pa]`. | ||
""" | ||
return self.isothermal_bulk_modulus_reuss(pressure, temperature, volume, params) | ||
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def shear_modulus(self, pressure, temperature, volume, params): | ||
""" | ||
Returns shear modulus :math:`G` of the mineral. :math:`[Pa]` | ||
""" | ||
return 1.0e99 | ||
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def entropy(self, pressure, temperature, volume, params): | ||
""" | ||
Returns the molar entropy :math:`\\mathcal{S}` of the mineral. :math:`[J/K/mol]` | ||
""" | ||
return 0.0 | ||
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def molar_heat_capacity_v(self, pressure, temperature, volume, params): | ||
""" | ||
Since this equation of state does not contain temperature effects, return a very small number. :math:`[J/K/mol]` | ||
""" | ||
return 1.0e-99 | ||
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def molar_heat_capacity_p(self, pressure, temperature, volume, params): | ||
""" | ||
Since this equation of state does not contain temperature effects, return a very small number. :math:`[J/K/mol]` | ||
""" | ||
return 1.0e-99 | ||
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def thermal_expansivity(self, pressure, temperature, volume, params): | ||
""" | ||
Since this equation of state does not contain temperature effects, return zero. :math:`[1/K]` | ||
""" | ||
return 0.0 | ||
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def grueneisen_parameter(self, pressure, temperature, volume, params): | ||
""" | ||
Since this equation of state does not contain temperature effects, return zero. :math:`[unitless]` | ||
""" | ||
return 0.0 | ||
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def validate_parameters(self, params): | ||
""" | ||
Check for existence and validity of the parameters. | ||
The value for :math:`K'_{\\infty}` is thermodynamically bounded | ||
between 5/3 and :math:`K'_0` :cite:`StaceyDavis2004`. | ||
""" | ||
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if "E_0" not in params: | ||
params["E_0"] = 0.0 | ||
if "P_0" not in params: | ||
params["P_0"] = 1.0e5 | ||
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# Check that all the required keys are in the dictionary | ||
expected_keys = ["V_0", "K_0", "Kprime_0", "Kprime_inf"] | ||
for k in expected_keys: | ||
if k not in params: | ||
raise KeyError("params object missing parameter : " + k) | ||
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# Finally, check that the values are reasonable. | ||
if params["P_0"] < 0.0: | ||
warnings.warn("Unusual value for P_0", stacklevel=2) | ||
if params["V_0"] < 1.0e-7 or params["V_0"] > 1.0e-3: | ||
warnings.warn("Unusual value for V_0", stacklevel=2) | ||
if params["K_0"] < 1.0e9 or params["K_0"] > 1.0e13: | ||
warnings.warn("Unusual value for K_0", stacklevel=2) | ||
if params["Kprime_0"] < 0.0 or params["Kprime_0"] > 10.0: | ||
warnings.warn("Unusual value for Kprime_0", stacklevel=2) | ||
if params["Kprime_inf"] < 1 + 45.0 / 29.0: | ||
warnings.warn("Value for Kprime_inf below recommended value", stacklevel=2) | ||
if params["Kprime_inf"] > params["Kprime_0"]: | ||
warnings.warn("Kprime_inf should be less than Kprime_0", stacklevel=2) |
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from __future__ import absolute_import | ||
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# This file is part of BurnMan - a thermoelastic and thermodynamic toolkit | ||
# for the Earth and Planetary Sciences. | ||
# Copyright (C) 2012 - 2024 by the BurnMan team, released under the GNU | ||
# GPL v2 or later. | ||
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from burnman.tools.eos import check_eos_consistency | ||
from burnman import Mineral | ||
import numpy as np | ||
import matplotlib.pyplot as plt | ||
import matplotlib.image as mpimg | ||
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HMX_params = { | ||
"P_0": 1.0e5, | ||
"V_0": 1.0e-6, # arbitrary value | ||
"K_0": 15.22e9, | ||
"Kprime_0": 7.54, | ||
"Kprime_inf": 2.63, | ||
"molar_mass": 0.296155, | ||
"equation_of_state": "macaw", | ||
} | ||
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HMX = Mineral(HMX_params) | ||
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if check_eos_consistency(HMX, tol=1.0e-5, including_shear_properties=False): | ||
print("The MACAW EoS is internally consistent.\n") | ||
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pressures = np.linspace(0.0, 100.0e9, 6) | ||
temperatures = 0.0 + 0.0 * pressures | ||
V, K_T = HMX.evaluate(["V", "K_T"], pressures, temperatures) | ||
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for i in range(6): | ||
print( | ||
f"{pressures[i]/1.e9:3.0f} GPa: " | ||
f"V/V_0 = {V[i]/HMX_params['V_0']:.3f}, " | ||
f"K_T = {K_T[i]/1.e9:6.2f} GPa" | ||
) | ||
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pressures = np.linspace(0.0, 100.0e9, 101) | ||
temperatures = 0.0 + 0.0 * pressures | ||
K_T = HMX.evaluate(["K_T"], pressures, temperatures)[0] | ||
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fig1 = mpimg.imread("figures/Lozano_Aslam_2022_Fig6c_HMX.png") | ||
plt.imshow(fig1, extent=[0.0, 100.0, 0, 500.0], aspect="auto") | ||
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plt.plot(pressures / 1.0e9, K_T / 1.0e9, linestyle=":", c="red") | ||
plt.show() |
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The MACAW EoS is internally consistent. | ||
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0 GPa: V/V_0 = 1.000, K_T = 15.22 GPa | ||
20 GPa: V/V_0 = 0.704, K_T = 127.87 GPa | ||
40 GPa: V/V_0 = 0.626, K_T = 218.49 GPa | ||
60 GPa: V/V_0 = 0.579, K_T = 300.87 GPa | ||
80 GPa: V/V_0 = 0.546, K_T = 378.32 GPa | ||
100 GPa: V/V_0 = 0.520, K_T = 452.36 GPa |