pygcc.clay_thermocalc
Created on Wed Mar 17 16:02:22 2021
@author: Adedapo Awolayo and Ben Tutolo, University of Calgary
Copyright (c) 2020 - 2021, Adedapo Awolayo and Ben Tutolo, University of Calgary
This program is free software: you can redistribute it and/or modify it under the terms of the GNU General Public License as published by the Free Software Foundation, either version 3 of the License, or (at your option) any later version.
This program is distributed in the hope that it will be useful, but WITHOUT ANY WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the GNU General Public License for more details.
You should have received a copy of the GNU General Public License along with this program. If not, see <http://www.gnu.org/licenses/>.
Module Contents
Functions
This function stores the Molecular weight of all elements |
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This function calculates logK values and reaction parameters of clay reactions using below references: |
Attributes
- pygcc.clay_thermocalc.Molecularweight()[source]
This function stores the Molecular weight of all elements
- pygcc.clay_thermocalc.MW
- pygcc.clay_thermocalc.J_to_cal = 4.184
- pygcc.clay_thermocalc.calclogKclays(TC, P, *elem, dbaccessdic=None, group=None, cation_order=None, Dielec_method=None, ClayMintype=None, ThermoInUnit='cal', **rhoEG)[source]
This function calculates logK values and reaction parameters of clay reactions using below references:
- Parameters:
TC (float, vector) – Temperature [°C]
P (float, vector) – Pressure [bar]
elem (list) – list containing nine parameters with clay names and elements compositions with the following format [‘Montmorillonite_Lc_MgK’, ‘Si’, ‘Al’, ‘FeIII’, ‘FeII’, ‘Mg’, ‘K’, ‘Na’, ‘Ca’, ‘Li’]
dbacessdic (dict) – dictionary of species from direct-access database, optional, default is speq21
group (string) – specify the structural layering of the phyllosilicate, for layers composed of
1 tetrahedral + 1 octahedral sheet (1:1 layer)
- specify ‘7A’,2 tetrahedral + 1 octahedral sheet (2:1 layer)
- specify ‘10A’, or the latter with abrucitic sheet in the interlayer (2:1:1 layer)
- specify ‘14A’ (optional), if not specified, default is based on charge balance on the cations and anionscation_order (string) – specify ordering of Si and Al ions either ‘Eastonite’, ‘Ordered’, ‘Random’, or ‘HDC’ (optional), if not specified, default is based on guidelines by Vinograd (1995)
Dielec_method (string) – specify either ‘FGL97’ or ‘JN91’ or ‘DEW’ as the method to calculate dielectric constant (optional), if not specified, default - ‘JN91’
ClayMintype (string) – specify either ‘Smectite’ or ‘Chlorite’ or ‘Mica’ as the clay type, if not specified default - ‘Smectites’
ThermoInUnit (string) – specify either ‘cal’ or ‘KJ’ as the input units for species properties (optional), particularly used to covert KJ data to cal by supcrtaq function if not specified default - ‘cal’
rhoEG (dict) – dictionary of water properties like density (rho), dielectric factor (E) and Gibbs Energy (optional)
- Returns:
logK_clay (float, vector) – logarithmic K values
Rxn (dict) – dictionary of reaction thermodynamic properties
Usage
The general usage of calclogKclays is as follows:
Without the optional arguments, not on steam saturation curve:
[logK, Rxn] = calclogKclays(TC, P, *elem),
where T is temperature in celsius and P is pressure in bar;
Without the optional arguments, on steam saturation curve:
[logK, Rxn] = calclogKclays(TC, ‘T’, *elem),
where T is temperature in celsius, followed with a quoted char ‘T’
[logK, Rxn] = calclogKclays(P, ‘P’, *elem),
where P is pressure in bar, followed with a quoted char ‘P’.
Meanwhile, usage with any specific dielectric constant method (‘FGL97’) for condition not on steam saturation curve is as follows. Default method is ‘JN91’
[logK, Rxn] = calclogKclays(TC, P, *elem, dbacessdic = dbacessdic, group = ‘10A’, cation_order = ‘HDC’, Dielec_method = ‘FGL97’)
Examples
>>> logK, Rxn = calclogKclays(50, 'T', *['Clinochlore', '3', '2', '0', '0', '5', '0', '0', '0', '0'], group = '14A') >>> logK 57.56820225
References
Blanc, P., Vieillard, P., Gailhanou, H., Gaboreau, S., Gaucher, É., Fialips, C. I., Madé, B & Giffaut, E. (2015). A generalized model for predicting the thermodynamic properties of clay minerals. American journal of science, 315(8), 734-780.
Blanc, P., Gherardi, F., Vieillard, P., Marty, N. C. M., Gailhanou, H., Gaboreau, S., Letat, B., Geloni, C., Gaucher, E.C. and Madé, B. (2021). Thermodynamics for clay minerals: calculation tools and application to the case of illite/smectite interstratified minerals. Applied Geochemistry, 104986.
Vinograd, V.L., 1995. Substitution of [4]Al in layer silicates: Calculation of the Al-Si configurational entropy according to 29Si NMR Spectra. Physics and Chemistry of Minerals 22, 87-98.