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Mineralogical reactions and thermodynamics (fwd)
Sender: Dean Biddle <dbiddle@waite.adelaide.edu.au>
Subject: WSN: Mineralogical reactions and thermodynamics
Could I please have feedback on the following approach for
calculating the spontaneity of mineralogical reactions from
elementary thermodynamics. If anyone can tell me of references
existing for this approach, I would be greatful.
The following spreadsheet, with cell formulas listed at the
bottom, can be used to derive the magnitude of entropy, enthalpy
and Gibb's free energy of mineralogical reactions.
A B C D E F G H
1 Standard Thermodynamic Quantities of Reaction @ 25 =F8C
2
3 react1 react2 react3 prod1 prod2 prod3
4 formula ---> NaAlSi3O H+ H2O ---> Al(OH)3 H4SiO4 Na+
5 coefficient ---> 1 1 7 1 3 1
6 S (J/K-mol) 207.4 0 69.95 68.44 180 58.4
7 H (kJ/mol) -3935.1 0 -285.83 -1293.1 -1460 -240.3
8 G (kJ/mol) -3711.7 0 -237.14 -1154.9 -1308 -261.9
9
10 Order -30.2
11 Endothermic 22.5
12 Nonspontaneous 30.92
where the active cell formulas are:
A10: @IF(B10=3D0,"No Change",@IF(B10>0,"Disorder","Order"))
A11: @IF(B11=3D0,"No Change",@IF(B11>0,"Endothermic","Exothermic"))
A12: @IF(B12=3D0,"At Equilibrium",@IF(B12>0,"Nonspontaneous","Spontaneous"=
))
B10: (F$5*F6)+(G$5*G6)+(H$5*H6)-(B$5*B6)-(C$5*C6)-(D$5*D6)
B11: (F$5*F7)+(G$5*G7)+(H$5*H7)-(B$5*B7)-(C$5*C7)-(D$5*D7)
B12: (F$5*F8)+(G$5*G8)+(H$5*H8)-(B$5*B8)-(C$5*C8)-(D$5*D8)
Mineral dissolution reaction can be written in many forms with
Al(OH)2+, Al(OH)3=F8, etc written as the products. Changes in
product species leads to considerable changes in the spontaneity
of the reaction.
Please send replies to my email address:
dbiddle@waite.adelaide.edu.au
Regards,
Dean Biddle.
From: Dean Biddle
University of Adelaide
Soil Science Dept
Waite Agricultural Res. Institute
Private Mail Bag No.1
Glen Osmond, South Australia, 5064.
Phone: (08) 303 7247
FAX: (08) 303 6511
Home Phone: (08) 379 0671
Email: dbiddle@waite.adelaide.edu.au
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