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Applied Geochemistry & Lab Ch.2 Thermodynamics of Solutions

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1 Applied Geochemistry & Lab Ch.2 Thermodynamics of Solutions
JYU

2 1. DEFINITIONS Solution: A single homogeneous phase resulted from the dissolution of two or more compositionally different phases (end members) . End members: The (real or imaginary) component phases to form a solution Exsolution: Separation (phenomenon) into two or more different phases from a solution

3 2. Generals Composition of a solution phase
𝑆= 𝑋 𝐴 𝐢 𝐴 + 𝑋 𝐡 𝐢 𝐡 + 𝑋 𝐢 𝐢 𝐢 +… = 𝑖 𝑋 𝑖 𝐢 𝑖 where X =mole fractions C=chemical compositions of the end members 𝑖 𝑋 𝑖 =1 𝑋 𝑖 = 𝑛 𝑖 𝑗 𝑛 𝑗

4 Gibbs free energy of a solution
Gibbs free energy of mechanically mixed phases Gibbs free energy of mixing (solution forming) 𝐺 π‘ π‘œπ‘™ = 𝐺 π‘šπ‘’π‘β„Ž 𝐺 π‘šπ‘–π‘₯ (Will be duscussed this in much more detail later)

5 3. Preliminary Knowledge
Do you know Roult’s law, Henry’s law, Partial molal properties, Fugacity, Activity, Gibbs-Duhem equation, and Standard state (in thermodynamics)?

6 5. Chemical Potential Definition: πœ‡ 𝑖 = πœ•πΊ πœ• 𝑛 𝑖 𝑇, 𝑃, 𝑛 𝑗
Example: For a system having two phses A & B, The Gibbs free energy of the system 𝐺 𝑠𝑦𝑠 = 𝑛 𝐴 πœ‡ 𝐴 + 𝑛 𝐡 πœ‡ 𝐡 𝑑𝐺 𝑠𝑦𝑠 = πœ‡ 𝐴 𝑑 𝑛 𝐴 + πœ‡ 𝐡 𝑑 𝑛 𝐡 For a closed system, 𝑑 𝑛 𝐴 =βˆ’π‘‘ 𝑛 𝐡 At an equilibrium state, 𝑑𝐺 𝑠𝑦𝑠 =0 Thus, πœ‡ 𝐴 = πœ‡ 𝐡


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