1 / 7

Ch. 2. THERMODYNAMICS FOR AQUEOUS GEOCHEMISTRY

Ch. 2. THERMODYNAMICS FOR AQUEOUS GEOCHEMISTRY. 2-1. Definitions - A review of undergraduate level thermodynamics Systems : Open, Closed, Isolated, (Adiabatic) Paramters : extensive, intensive Functions : Path dependent & Independent (static) Phases, components, degree of freedom

farica
Télécharger la présentation

Ch. 2. THERMODYNAMICS FOR AQUEOUS GEOCHEMISTRY

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Ch. 2. THERMODYNAMICS FOR AQUEOUS GEOCHEMISTRY • 2-1. Definitions - A review of undergraduate level thermodynamics • Systems: Open, Closed, Isolated, (Adiabatic) • Paramters: extensive, intensive • Functions: Path dependent & Independent (static) • Phases, components, degree of freedom • Gibbs phase rule • F=C-P+2=C’-P+2-R (C’; no of species, R; no. of rxn) 2-1

  2. Ch. 2. • 2-1. • Reactions: • Homogeneous vs heterogeneous (rxn) • Reversible vs irreversible rxns • Congruent vs incongruent rxns • Internal energy (U) • Entropy (S) • Enthalpy (H) • Gibbs free energy (G) • Chemical potential (m) 2-2

  3. Ch. 2. • 2-1. • Fist Law • Second Law • Third Law • State of a system: Evolutionary (disequilibrium), steady, & equilibrium • How do you determine evolution direction?: spontaneity problem • What is the qualitative meaning of U, S, H?? 2-3

  4. Ch. 2. • 2-2. Equilibrium constant K • For a reaction aA + bB = cC + dD DGr = total G of prod. – total G of reactants = SniGi = cGC + dGD – aGA – bGB = DGro + RT ln {[C]c[D]d/[A]a[B]b} When equil., ln K = - DGro /RT (Read the text from p.10 to 19 for the solution models) 2-5

  5. Ch. 2. • 2-2. • Effects of T-P changes on K (Read text from p.19 to 32) Compare this with the T-P dependency calculation of Gibbs free energy than converting it to K 2-6

  6. Ch. 2. • 2-2. • Check the following terms • Concentrations • Solutions • Mathematical expressons of activity quotuent (Q) • Internal consistency of a dataset 2-7

  7. Ch. 2. • 2-2. • Assignments • P. 34 problems 1, 2 and 5 • P. 35 problems 8 2-8

More Related