1 / 11

Reaction Feasibility

Reaction Feasibility. Will a specific reaction occur ?. How can we predict if a reaction is feasible ?. NaHCO 3 + HCl → NaCl + H 2 O + CO 2. Δ H is +ve (endothermic). Entropy increases. We know this reaction is feasible. How can we predict if a reaction is feasible ?.

joel-wood
Download Presentation

Reaction Feasibility

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. Reaction Feasibility Will a specific reaction occur ?

  2. How can we predict if a reaction is feasible ? NaHCO3 + HCl → NaCl + H2O + CO2 ΔH is +ve (endothermic) Entropy increases We know this reaction is feasible

  3. How can we predict if a reaction is feasible ? ΔG = ΔH - T ΔS ΔG = free energy ( kJmol-1) ΔH = enthalpy change ( kJmol-1) T = temperature (K) ΔS = entropy change ( kJK-1mol-1) ΔS must be converted from JK-1mol-1 (/1000)

  4. How can we predict if a reaction is feasible ? ΔG = ΔH - T ΔS A reaction is feasible if ΔG is negative ΔG < 0 A reaction becomes feasible when ΔG = 0

  5. Calculate ΔG for the formation of CO2 from graphite at 298K, givenΔHf = -393.5kJmol-1& ΔS is +3.3 JK-1mol-1 ΔG = ΔH - T ΔS (-393.5) – (298 x 3.3/1000) ΔG = -394.5 kJmol-1 Feasible reaction ΔG = -ve

  6. Is the decomposition of limestone spontaneous at standard temperature?ΔS = +165 JK-1mol-1 ΔH = +178 kJmol-1 ΔG = ΔH - T ΔS (+178) – (298 x 165/1000) ΔG = +128.83 kJmol-1 Not feasible ΔG = + ve

  7. Feasible  Spontaneous Thermodynamics tells us nothing about the speed a reaction happens It only tells us that it can happen C + O2 → CO2 ΔG = -394.5 kJmol-1 EA is large so reaction very slow at 298K

  8. Calculate ΔG for the rusting of Fe at 298K, givenΔHf = -825 kJmol-1& ΔS is -272 JK-1mol-1 2Fe(s) + 3/2O2(g) → Fe2O3 (s) ΔG = ΔH - T ΔS (-825) – (298 x (-272/1000) ΔG = -744 kJmol-1 Feasible reaction ΔG = -ve

  9. At what temperature does this reaction cease to be feasible?ΔHf = -825 kJmol-1 & ΔS is -272 JK-1mol-1 ΔG = ΔH - T ΔS Reaction becomes feasible when ΔG = 0 ΔH = T ΔS ΔH = T ΔS = 3033K T = -825/-0.272

  10. Free energy & Equilibrium ΔG = ΔH - T ΔS ΔG = 0 for a system at equilibrium Changes of state are systems at equilibria ΔS =ΔH T ΔH = T ΔS ΔH = T ΔS

  11. Calculate the entropy change when ice melts given thatΔHfusion (melting) = + 6.0 kJmol-1 ΔG = ΔH - T ΔS ΔG = 0 for a change of state ΔH = T ΔS ΔS =ΔH T ΔS = + 6/273 = 0.0219 kJK-1mol-1 = 0.0219 x 1000 JK-1mol-1 = 21.9 JK-1mol-1

More Related