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Additional Equations for Entropy

  • This equation is specifically for a reversible process:
ΔS=qrevT\Delta S=\frac{q_{rev}}{T}
  • For a reversible process
ΔSuniv=ΔSsys+ΔSsurr=0\Delta S_{univ}=\Delta S_{sys} +\Delta S_{surr} =0
  • For an irreversible (spontaneous) process
ΔSuniv=ΔSsys+ΔSsurr>0\Delta S_{univ} =\Delta S_{sys} +\Delta S_{surr} >0

  • Note: If no subscript is given on ΔS assume it is ΔSsys
  • Spontaneous (irreversible) process: A process which proceeds in one direction and may only proceed backwards if work is done. eg. Piston, electric current, natural processes
  • loss of usable work
  • are spontaneous reactions always fast?
    No!
  • think about diamonds->graphite
  • Non-spontaneous process: A process which only proceeds by the addition of work.
  • ex. of a non-spontaneous irreversible process is pushing a piston to force a gas into a smaller volume
  • spontaneous is natural whereas non spontaneous is unnatural (needs human intervention)
  • Reversible Process: A Process that is non-spontaneous in both directions

2nd Law: Applications The 6 cases

Case 1: Spontaneous Process in an isolated system
q=0Why ?q=0 \hspace{30pt} \text{Why ?}

ΔSsurr=0\Delta S_{surr} =0

ΔSuniv=ΔSsys+ΔSsurr>0\Delta S_{univ} =\Delta S_{sys} +\Delta S_{surr} >0

ΔSsys>0\Delta S_{sys} >0


Case 2: Isochoric or Isobaric Processes
deltaS=(n)Cv or p ln(T2(T1))deltaS=\left(n\right)Cv\ or\ p\ \ln\left(\frac{T2}{\left(T1\right)}\right)

Case 3: Isothermal Processes
ΔU=0Why ?\Delta U=0 \hspace{30pt} \text{Why ?}
q=wq=-w
ΔS=nRlnV2V1=nRlnp1p2\Delta S=nR \ln \frac{V_2}{V_1}=nR \ln \frac{p_1}{p_2}

Case 4: Adiabatic Reversible Process
q=0Why ?q=0 \hspace{30pt} \text{Why ?}
ΔS=qrevT=0\Delta S=\frac{q_{rev}}{T} =0
  • For a reversible adiabatic process: ΔS_system = 0, ΔS_universe = 0.
  • For an irreversible adiabatic process: ΔS_system > 0, ΔS_surroundings = 0, and thus ΔS_universe > 0.
Case 5: Reversible Phase Change (Phase change at the melting/boiling point)
ΔS=ΔHT\Delta S=\frac{\Delta H}{T}
Remember. If the phase Change is happening at a different temperature we can use Kirchoff’s Law to deal with that.

Case 6: Chemical Reactions
In the same way we can use standard heats of formation to calculate a reaction enthalpy at room temperature and pressure, we can use So
ΔrSo=iviSm,io(products)jvjSm,jo(reactants)\Delta_rS^o =\sum_iv_iS^o_{m,i}(products) -\sum _j v_j S^o _{m,j} (reactants)

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a. An open flask containing 5 moles of water is heated from 25oC to 30oC what is the change in entropy. Cp (H2O(l)) = 4.18 J g-1 K -1 . Give your answer in J/K

Isobaric Heating;
deltaS=n(Cv)ln (T2/T1)
ΔS=Cv=ln(T2T1)=4.18JgKln(303K298K)=0.0696JgK\Delta S=C_v=\ln \bigg(\cfrac{T_2}{T_1}\bigg)=4.18\cfrac{J}{gK}\ln \bigg(\cfrac{303K}{298K}\bigg)=0.0696\cfrac{J}{gK}
ΔS=0.0696JgK×5mols×18gmol=6.26JK\Delta S=0.0696\cfrac{J}{gK}\times 5mols\times 18\cfrac{g}{mol}=6.26\cfrac{J}{K}
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b. A sealed 5L glass ampule full of F2(g) at 1atm at 25oC is found in a laboratory at UBC. We know that this type of glass ampule can easily withstand pressures up to 5atm. What would the change in entropy be if the F2(g) ampule was heated until the pressure reached 5atm? You can assume ideal gas behaviour for F2 and that the glass ampule does not change in volume.
Isochoric Heating:
ΔS=nCvln(T2T1)=n32Rln(T2T1)\Delta S=nC_v\ln \bigg(\cfrac{T_2}{T_1}\bigg)=n\cfrac{3}{2}R\ln \bigg(\cfrac{T_2}{T_1}\bigg)
Ideal gas law for Initial moles
n=PVRT=(1atm)(5L)(0.08206LatmK1mol1(298K)=0.204moln=\cfrac{PV}{RT}=\cfrac{(1atm)(5L)}{(0.08206Latm K^{-1}mol^{-1}(298K)}=0.204mol
Ideal gas law for final temperature
T=PVnR=(5atm)(5L)(0.204mol)(0.08206LatmK1mol1=1493KT=\frac{PV}{nR}=\frac{(5atm)(5L)}{(0.204mol)(0.08206LatmK^{-1}mol^{-1}}=1493K

deltaS=nCvln(T2(T1))=0.204moles(32R)ln(1493K(298K))=4.1JKdeltaS=nCv\ln\left(\frac{T2}{\left(T1\right)}\right)=0.204moles\left(\frac{3}{2}R\right)\ln\left(\frac{1493K}{\left(298K\right)}\right)=\frac{4.1J}{K}