1 / 12

Chem 300 - Ch 26/#2 Today’s To Do List

Chem 300 - Ch 26/#2 Today’s To Do List. Calculating K P from Δ r G o Δ r G vs Δ r G o Reaction Direction van’t Hoff Equation Temperature &  r H o. Calculating K P.  r G o = - RT ln K P (T) N 2 (g) + 3H 2 (g)  2NH 3 (g) @ 298K

kert
Download Presentation

Chem 300 - Ch 26/#2 Today’s To Do List

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. Chem 300 - Ch 26/#2 Today’s To Do List • Calculating KP from ΔrGo • ΔrG vs ΔrGo • Reaction Direction • van’t Hoff Equation • Temperature & rHo

  2. Calculating KP • rGo = - RT ln KP(T) • N2(g) + 3H2(g)  2NH3(g) @ 298K • rGo = 2 fGo(NH3) – [fGo(N2) + 3 fGo(H2)] • rGo = 2 fGo(NH3) – [ 0 + 0 ] • rGo = 2 ( - 16.5 kJ/mol) = -33.0 kJ/mol • RT = (8.31 J/mol-K)(298 K) = 2.48 kJ/mol • ln KP = - (-33.0kJ/mol)/(2.48kJ/mol) = 13.3 • KP = 6.0 x 105Thermodynamically exact

  3. Degree of Dissociation (α) • H2O  H2 + ½ O2 @ 2300 K • rGo(2300K) = 118.1 kJ/mol • First Calculate KP-- • ln KP = - rGo/RT = - 118.1/(8.31x2300) • ln KP = - 6.17  KP = 2.08 x 10-3 • Calculate α

  4. H2O  H2 + ½ O2

  5. If ideal gases • KP = P(H2) P½(O2)/P(H2O) • Subst from prev. slide: • KP = α3/2 P1/2/(1- α)(2 + α)1/2 = 2.08 x 10-3 • Thus α is small: α << 1 • KP  α3/2 P1/2/ 21/2 Since P = 1 • α  0.0205 small dissociation

  6. Reaction Direction • rG(T) = rGo(T) + RT ln Q • rGo(T) = - RT ln KP • rG(T) = - RT ln KP + RT ln Q = RT ln (Q/KP) • If (Q/KP) < 1  rG(T) < 0 Rxn spontan. • If (Q/KP) > 1  rG(T) > 0 Not spontan. • If (Q/KP) = 1  rG(T) = 0 At equilibr.

  7. Example • 2 SO2 + O2 2 SO3 KP = 10 @ 900K • Initial Conditions: • P(SO2) = 0.20 bar • P(O2) = 0.20 bar • P(SO3) = 0.10 bar • Q = P2(SO3) / P2(SO2) P(O2) =(0.01)/(0.04)(0.20) = 1.25 < KP Spontan. • rG(T) = RT ln (Q/KP) = (8.31)(900) ln (1.25/10) • rG(T) = - 15.6 kJ

  8. KP, T, @ van’t Hoff • Recall Gibbs-Helmholtz: • [(rGo/T)/ T]P = - rHo/T2 • Subst rGo(T) = - RT ln KP(T) • [(ln KP/ T]P = rHo/RT2 • If rHo> 0  KP(T) increases with T • If rHo< 0  KP(T) decreases with T • Integrate: • ln (K2/K1) = - rHo(1/T2 – 1/T1)/R

  9. H2 + CO2 = CO + H2OEndothermic Rxn

  10. When rHo not constant3H2 + N2= 2NH3

  11. Le Chatelier’s Principle • If a chemical reaction at equilibrium is subjected to a disturbance, it responds in a way that tends to minimize the effect.

  12. Next Time

More Related