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    CHAPTER 3The Second Law of Thermodynamics

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    Experimental observation: All spontaneous processes are irreversible Not all irreversible processes are spontaneous

    SECOND LAW OF THERMODYNAMICS

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    Experimental observation: All spontaneous processes are irreversible Not all irreversible processes are spontaneous

    SECOND LAW OF THERMODYNAMICS

    plug

    vacuum

    yes

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    Experimental observation: All spontaneous processes are irreversible Not all irreversible processes are spontaneous

    SECOND LAW OF THERMODYNAMICS

    vacuum

    no

    4

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    Experimental observation: All spontaneous processes are irreversible Not all irreversible processes are spontaneous

    SECOND LAW OF THERMODYNAMICS

    water freezing at -10 C

    water/ice at 0 C

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    Experimental observation: All spontaneous processes are irreversible Not all irreversible processes are spontaneous

    SECOND LAW OF THERMODYNAMICS

    ice melting at +10 C

    water/ice at 0 C

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    Experimental observation: All spontaneous processes are irreversible Not all irreversible processes are spontaneous

    Some spontaneous processes have U and H > 0 (e.g., melting of ice at 10 C)

    Some spontaneous processes have U and H < 0 (e.g., freezing of water at -10 C)

    Issue: First law treats heat (q) and work (w) on an equal footing

    In reality they are not interchangeable:there are restrictions on how much qcan be converted to w

    SECOND LAW OF THERMODYNAMICS

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    Equivalent statements:

    SECOND LAW OF THERMODYNAMICS

    (1) Kelvin: heat cannot, by a cyclic process, be taken from a reservoir and convertedinto work without simultaneously delivering heat from a higher to a lowertemperature reservoir.

    Hot reservoir, TH

    Heatengine

    qH

    -w

    It is not possible to build a cyclicmachine that converts heat intowork with 100% efficiency!

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    Equivalent statements:

    (2) Clausius: In a cyclic process, heat cannot flow from a lower to a higher temperaturereservoir without the expenditure of work on the system. Generalization: all naturalprocesses are irreversible.

    SECOND LAW OF THERMODYNAMICS

    (1) Kelvin: heat cannot, by a cyclic process, be taken from a reservoir and convertedinto work without simultaneously delivering heat from a higher to a lowertemperature reservoir.

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    Equivalent statements:

    SECOND LAW OF THERMODYNAMICS

    Energy of universe is constant, but increasingly unavailable for useful work

    (3) It is impossible to achieve perpetual motion of the second kind, that is, to construct amachine that will convert heat into work isothermally.

    (4) No heat engine operating between two temperatures can be more efficient than areversible heat engine operating between the same two temperatures.

    (2) Clausius: In a cyclic process, heat cannot flow from a lower to a higher temperaturereservoir without the expenditure of work on the system. Generalization: all naturalprocesses are irreversible.

    (1) Kelvin: heat cannot, by a cyclic process, be taken from a reservoir and convertedinto work without simultaneously delivering heat from a higher to a lowertemperature reservoir.

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    A heat engine is a device that operates cyclically to convert heat to useful work.

    HEAT ENGINES

    Heating

    Work

    (1) A substance (normally a gas) is in acontainer closed by a piston

    (2) The substance is heated and expands,

    causing a piston to move (work).

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    A heat engine is a device that operates cyclically to convert heat to useful work.

    HEAT ENGINES

    Cooling

    (1) A substance (normally a gas) is in acontainer closed by a piston

    (2) The substance is heated and expands,

    causing a piston to move (work).

    (3) The substance is then cooled down to theoriginal temperature and the pistonreturns to its original position.

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    A heat engine is a device that operates cyclically to convert heat to useful work.

    HEAT ENGINES

    (1) A substance (normally a gas) is in acontainer closed by a piston

    (2) The substance is heated and expands,

    causing a piston to move (work).

    (3) The substance is then cooled down to theoriginal temperature and the pistonreturns to its original position.

    (4) The cycle starts again.

    Heating

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    A heat engine is a device that operates cyclically to convert heat to useful work.

    HEAT ENGINES

    Cooling

    (1) A substance (normally a gas) is in acontainer closed by a piston

    (2) The substance is heated and expands,

    causing a piston to move (work).

    (3) The substance is then cooled down to theoriginal temperature and the pistonreturns to its original position.

    (4) The cycle starts again.

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    The engine:

    (1) Absorbs some amount of heat qH from ahot reservoir (a hot body such as a boiler)

    (2) Converts part of it to work (-w) done on thesurroundings by, e.g., pushing a piston

    (3) The difference qH - (-w) = -qC is released

    back to the surroundings (a cold bodysuch as a condenser ) as heat.

    HEAT ENGINES

    A heat engine is a device that operates cyclically to convert heat to useful work.

    Hot reservoir, TH

    Cold reservoir, TC

    Heatengine

    qH

    qC

    -w

    Important:The reservoirs are large so thattheir temperature is not affected

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    Efficiency: =work output per cycle

    energy input per cycle=

    w

    qH

    HEAT ENGINES

    For a cyclic process U = 0

    U= 0 = q+ w = qH+ qC+ w

    But...

    w = qH+ qC

    =qH+ qC

    qH

    = 1 +qC

    qH

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    super > revImagine:

    18

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    super > revImagine:

    Hot reservoir, TH

    Cold reservoir, TC

    Reversibleheat engine

    qH

    qC

    -w

    rev =w

    qH

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    super > revImagine:

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    -wSuper

    heat engine

    QH

    QC

    -WReversibleheat engine

    rev =w

    qH

    super =W

    QH

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    Imagine: QH = 1.3 qH

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    -wSuper

    heat engine

    QH

    QC

    -WReversibleheat engine

    rev =w

    qH

    super =W

    QH

    10 cycles of the super engine = 13 cycles of the reversible engine

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    Imagine: QH = 1.3 qH

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    w

    QH

    QC

    -WReversibleheat pump

    Superheat engine

    10 cycles of the super engine = 13 cycles of the reversible engine

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    Imagine: QH = 1.3 qH

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    QH

    QC

    Reversibleheat pump

    Superheat engine

    10 cycles of the super engine = 13 cycles of the reversible engine

    W

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    QH

    QC

    Reversibleheat pump

    qH = QHafter 10 cycles of the super engine: super > revbut

    |W| > |w|

    Superheat engine

    W

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    QH

    QC

    Reversibleheat pump

    qH = QHafter 10 cycles of the super engine: super > revbut

    |W| > |w|

    net work

    Superheat engine

    W

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    QH

    QC

    Reversibleheat pump

    net work

    U= 0 = q+ w = qH+ qC+ wnet work must come from some energy input

    qH = QHbut (in 10 cycles of the super-engine):

    Superheat engine

    W

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    Carnots principle:

    No heat engine can be more efficient than a reversible heat engine whenboth engines work between the same pair of temperatures TH and TC

    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    Superheat engine

    QH

    QC

    Reversibleheat pump

    net work

    U= 0 = q+ w = qH+ qC+ wnet work must come from some energy input

    the energy input must come from the cold reservoir...

    W

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    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    qH

    qC

    Superheat engine

    QH

    QC

    Reversibleheat pump

    net work

    U= 0 = q+ w = qH+ qC+ wnet work must come from some energy input

    the energy input must come from the cold reservoir...

    Heat cannot, by a cyclic process, be taken from a reservoir and converted into workwithout simultaneously delivering heat from a higher to a lower temperature reservoir.

    NOT POSSIBLE BECAUSE VIOLATES THE KELVIN STATEMENT

    W

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    HEAT ENGINES

    U= 0 = q+ w = qH+ qC+ wnet work must come from some energy input

    the energy input must come from the cold reservoir...

    NOT POSSIBLE BECAUSE VIOLATES THE KELVIN STATEMENT

    super > rev

    Heat cannot, by a cyclic process, be taken from a reservoir and converted into workwithout simultaneously delivering heat from a higher to a lower temperature reservoir.

    (any engine) (reversible engine)

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    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    Reversibleheat engine

    qB,HReversibleheat pump

    Two reversible heat engines

    A = A

    qA,H

    B = B

    qB,H

    A B

    qB,CqA,C

    qA,H

    B A

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    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    Reversibleheat engine

    qB,HReversibleheat pump

    Two reversible heat engines

    A = A

    qA,H

    B = B

    qB,H

    B A

    qB,CqA,C

    qA,H

    A B

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    HEAT ENGINES

    Hot reservoir, TH

    Cold reservoir, TC

    Reversibleheat engine

    qB,HReversibleheat pump

    Two reversible heat engines

    A = A

    qA,H

    B = B

    qB,H

    B A

    qB,CqA,C

    qA,H

    A = B

    All reversible engines operating between two given temperaturesmust have the same efficiency

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    HEAT ENGINES

    (any engine) (reversible engine)

    irrev rev

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    HEAT ENGINES

    All reversible engines operating between two given temperaturesmust have the same efficiency

    rev = f(TH, TC)

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    CARNOT CYCLE

    Hot reservoir, TH

    Cold reservoir, TC

    qC

    qHisotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    qI = wI = RTH lnV2

    V1> 0

    heat adsorbed by the system from the reservoir = work done by the system

    1) Reversible, isothermal expansion

    UI = 0

    I

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    CARNOT CYCLE

    Hot reservoir, TH

    Cold reservoir, TC

    qC

    qH

    V2V1 V

    P1

    P2

    P

    1

    2

    V3V4

    isotherm, TC

    4 3

    heat is released by the system = work is done on the system

    UIII = 0

    3) Reversible, isothermal compression

    III

    qIII = wIII = RTC lnV4

    V3< 0

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    CARNOT CYCLE

    Hot reservoir, TH

    Cold reservoir, TC

    qC

    qH

    V2V1 V

    P1

    P2

    P

    1

    2

    4 3

    V3V4

    adiabat

    II

    2) Reversible adiabatic expansion

    qII = 0

    wII < 0 work done by the system

    UII = +wII = CV(TC TH)

    37

    C O C C

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    CARNOT CYCLE

    Hot reservoir, TH

    Cold reservoir, TC

    qC

    qH

    V2V1 V

    P1

    P2

    P

    1

    2

    4 3

    adiabatIV

    UIV = +wIV = CV(TH TC)

    work done on the systemwIV > 0

    qIV = 0

    4) Reversible adiabatic compression

    V3V4

    38

    CARNOT CYCLE

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    CARNOT CYCLE

    Hot reservoir, TH

    Cold reservoir, TC

    qC

    qHisotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    U around the cycle is zero

    IV

    IIIII

    V3V4

    I

    39

    CARNOT CYCLE

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    CARNOT CYCLE

    Hot reservoir, TH

    Cold reservoir, TC

    qC

    qHisotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    The net work is done by the gas on the surroundings

    IV

    IIIII

    V3V4

    w = (wI + wII + wIII + wIV) = RTH lnV2

    V1

    + RTC ln

    V4

    V3

    I

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    CARNOT CYCLE

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    CARNOT CYCLE

    Hot reservoir, TH

    Cold reservoir, TC

    qC

    qHisotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    V3V4

    isotherm, TC

    4 3

    adiabatadiabat

    The net work is done by the gas on the surroundings

    T2

    T1

    = V1V2R/CV

    adiabatic processfor a perfect gas THV

    R/CV2

    = TCVR/CV3

    THVR/CV1

    = TCVR/CV4

    IV

    IIIII

    w = (wI + wII + wIII + wIV) = RTH lnV2

    V1

    + RTC ln

    V4

    V3

    I

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    CARNOT CYCLE

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    CARNOT CYCLE

    isotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    The net work is done by the gas on the surroundings

    THVR/CV2

    = TCVR/CV3

    THVR/CV1

    = TCVR/CV4

    V2

    V1= V3

    V4

    w = RTH lnV2

    V1+RTC lnV2

    V1

    IV

    IIIII

    V3V4

    w = (wI + wII + wIII + wIV) = RTH lnV2

    V1

    + RTC ln

    V4

    V3

    I

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    CARNOT CYCLE

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    CARNOT CYCLE

    isotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    The net work is done by the gas on the surroundings

    THVR/CV2

    = TCVR/CV3

    THVR/CV1

    = TCVR/CV4

    V2

    V1= V3

    V4

    w = R(TH TC) lnV2

    V1

    IV

    IIIII

    V3V4

    w = (wI + wII + wIII + wIV) = RTH lnV2

    V1

    + RTC ln

    V4

    V3

    I

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    CARNOT CYCLE

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    CARNOT CYCLE

    isotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    =wqI

    = R(THTC) ln(V2/V1)

    RTH ln(V2/V1)

    =

    TH TC

    TH

    IV

    IIIII

    V3V4

    w = R(TH TC) lnV2

    V1

    q= qI

    We know:

    =

    work output per cycle

    energy input per cycle=

    w

    qH

    I

    44

    CARNOT CYCLE

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    CARNOT CYCLE

    isotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    =wqI

    = R(THTC) ln(V2/V1)

    RTH ln(V2/V1)

    IV

    IIIII

    V3V4

    w = R(TH TC) lnV2

    V1

    q= qI

    We know:

    =

    work output per cycle

    energy input per cycle=

    w

    qH

    =TH TC

    TH< 1

    I

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    CARNOT CYCLE

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    CARNOT CYCLE

    isotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    IV

    IIIII

    Ucycle = 0

    qcycle = wcycle

    qcycle = qI+ qIII

    = TH

    TCTH

    =

    wqI

    = qI+

    qIIIqI

    qI+ qIII

    qI=

    TH TC

    TH

    V3V4

    We know:

    I

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    CARNOT CYCLE

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    CARNOT CYCLE

    isotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    IV

    IIIII

    = TH

    TCTH

    =

    wqI

    = qI+

    qIIIqI

    V3V4

    qIII

    TC+

    qI

    TH= 0

    qI+ qIII

    qI=

    TH TC

    TH

    Ucycle = 0

    qcycle = wcycle

    qcycle = qI+ qIII

    We know:

    I

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    CARNOT CYCLE

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    CARNOT CYCLE

    isotherm, TH

    V2V1 V

    P1

    P2

    P

    1

    2

    isotherm, TC

    4 3

    adiabatadiabat

    IV

    IIIII

    V3V4

    I

    qIII

    TC+

    qI

    TH= 0

    Carnots cycle

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    ENTROPY

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    ENTROPY

    49

    ENTROPY

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    ENTROPY

    ycle

    qrev

    T= 0

    Sum of Carnot cycles

    qrev

    T= 0

    In the limit of an infinite number ofCarnots cycles

    state functionqrev

    T=

    50

    ENTROPY

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    ENTROPY

    ycle

    qrev

    T= 0

    Sum of Carnot cycles

    qrev

    T= 0

    In the limit of an infinite number ofCarnots cycles

    dS=qrev

    TS=

    state 2

    state 1

    qrev

    T= S2 S1

    51

    ENTROPY

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    ENTROPY

    qrev is not an exact differential is not a state function

    qrev

    Tis an exact differential is a state function

    dS=qrev

    TS=

    state 2

    state 1

    qrev

    T= S2 S1

    52

    ENTROPY

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    Calculation of entropy change - Pure substance

    ENTROPY

    dU= q+ w

    q= dU+ Pext dV

    qrev = dU+ P dV S(V, T)

    dS= qrev

    T

    53

    ENTROPY

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    dS= qrev

    T

    ENTROPY

    dS=S

    T

    VdT+

    SV

    TdVS(V, T)

    dS=

    dU

    T +

    P

    T dVqrev = dU+ P dV

    Calculation of entropy change - Pure substance

    54

    ENTROPY

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    dS=

    dU

    T +

    P

    T dV

    ENTROPY

    dS=

    S

    T

    V

    dT+

    S

    V

    T

    dV

    Calculation of entropy change - Pure substance

    dU =

    U

    T

    V

    dT+

    U

    V

    T

    dV

    but...

    dS=1

    T

    U

    T

    V

    dT+1

    T

    U

    V

    T

    dV+P

    TdV

    55

    ENTROPY

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    ENTROPY

    dS=

    CV

    T dT+PT +

    1

    TU

    V

    T

    dV

    dS=1

    T

    U

    T

    V

    dT+1

    T

    U

    V

    T

    dV+P

    TdV

    Calculation of entropy change - Pure substance

    56

    ENTROPY

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    ENTROPY

    dS=CV

    TdT+

    P

    T+1

    T

    U

    V

    T

    dV

    dS=

    ST

    V

    dT+

    SV

    T

    dV

    S

    T

    V

    =

    CV

    T

    S

    V

    T

    =

    P

    T+1

    T

    U

    V

    T

    dV

    Calculation of entropy change - Pure substance

    57

    ENTROPY

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    ENTROPY

    S

    T

    V

    =

    CV

    T

    S

    V

    T

    =

    P

    T+1

    T

    U

    V

    T

    dV

    Calculation of entropy change - Pure substance

    2f(x, y)

    xy=

    2f(x, y)

    yx

    for a state function

    V

    S

    T

    V

    T

    =

    T

    S

    V

    T

    V

    58

    ENTROPY

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    ENTROPY

    S

    T

    V

    =CV

    T

    SV

    T

    =PT+ 1

    T

    UV

    T

    dV

    Calculation of entropy change - Pure substance

    V

    ST

    V

    T

    = T

    SV

    T

    V

    1

    T

    V

    U

    T

    V

    T

    =

    T

    P

    T+1

    T

    U

    V

    T

    V

    59

    ENTROPY

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    ENTROPY

    1

    T

    V

    U

    T

    V

    T

    =

    T

    P

    T+1

    T

    U

    V

    T

    V

    Calculation of entropy change - Pure substance

    1

    T

    2U

    VT=1

    T

    P

    T

    P

    T2

    1

    T2

    U

    V

    +1

    T

    2U

    TV

    1

    T

    P

    T+1

    T

    U

    V

    T

    =1

    T

    P

    T

    V

    60

    ENTROPY

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    ENTROPY

    S

    V

    T

    =

    P

    T+1

    T

    U

    V

    T

    dV

    S

    V

    T

    =

    P

    T

    V

    Calculation of entropy change - Pure substance

    1

    T

    P

    T+1

    T

    U

    V

    T

    =1

    T

    P

    T

    V

    61

    HOW TO CALCULATE ENTROPY CHANGES

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    S for an isothermal expansion of a perfect gas from V1 to V2 at temperature T

    HOW TO CALCULATE ENTROPY CHANGES

    dS=

    ST

    V

    dT+

    PT

    V

    dVdS=

    ST

    V

    dT+

    SV

    T

    dV

    dS=

    P

    T

    V

    dV

    PV= nRT

    Perfect gas P

    T

    V

    =

    nR

    V

    62

    HOW TO CALCULATE ENTROPY CHANGES

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    HOW TO CALCULATE ENTROPY CHANGES

    dS=

    ST

    V

    dT+

    PT

    V

    dVdS=

    ST

    V

    dT+

    SV

    T

    dV

    P

    T

    V

    =nR

    VS= nR

    V2

    V1

    dV

    V

    S= nR lnV2

    V1

    independent of the path

    S for an isothermal expansion of a perfect gas from V1 to V2 at temperature T

    63

    HOW TO CALCULATE ENTROPY CHANGES

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    S for a process occurring at constant volume

    HOW TO CALCULATE ENTROPY CHANGES

    dS=

    ST

    V

    dT+

    PT

    V

    dVdS=

    ST

    V

    dT+

    SV

    T

    dV

    dS=

    S

    T

    V

    dT

    S

    T

    V

    =

    CV

    T

    From last lecture...

    dS=

    S

    T

    V

    dT =CV

    TdT

    64

    HOW TO CALCULATE ENTROPY CHANGES

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    dS=

    ST

    V

    dT+

    PT

    V

    dVdS=

    ST

    V

    dT+

    SV

    T

    dV

    dS=

    S

    T

    V

    dT =CV

    TdT S=

    T2

    T1

    CVdT

    T

    S= CV lnT2

    T1

    (assuming the CV is independent of T)

    S for a process occurring at constant volume

    HOW TO CALCULATE ENTROPY CHANGES

    65

    FEW OTHER DEFINITIONS & RELATIONS

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    dS=dH

    T

    V dP

    T

    dS=dU

    T

    +P

    T

    dV

    dU= dH PdV V dP

    dS=dH

    T

    PdV

    T

    V dP

    T+PdV

    T

    FEW OTHER DEFINITIONS & RELATIONS

    dS=qrev

    T

    dH= dU+ PdV+ V dPH= U+ PV

    But...

    66

    FEW OTHER DEFINITIONS & RELATIONS

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    dS=dU

    T

    +P

    T

    dV

    dU= dH PdV V dP

    FEW OTHER DEFINITIONS & RELATIONS

    dS=qrev

    T

    H= U+ PV

    But...

    dH= dU+ PdV+ V dP

    dS=dH

    T

    V dP

    T

    67

    FEW OTHER DEFINITIONS & RELATIONS

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    dS=dH

    T

    V dP

    T

    CP =

    H

    T

    P

    &

    dH= HT

    P

    dT+ HP

    T

    dP

    But...

    S=CP

    TdT+

    V

    T+1

    T

    H

    P

    T

    dP

    68

    FEW OTHER DEFINITIONS & RELATIONS

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    dS= S

    TP

    dT+ S

    PT

    dP

    S=

    CP

    T dT+

    V

    T +

    1

    TH

    P

    T

    dP

    S(T, P)

    69

    FEW OTHER DEFINITIONS & RELATIONS

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    dS= S

    TP

    dT+ S

    PT

    dP

    S=

    CP

    T dT+V

    T +

    1

    TH

    P

    T

    dP

    S

    P

    T

    = V

    T+1

    T

    H

    P

    T

    S

    TP

    =

    CP

    T

    70

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    FEW OTHER DEFINITIONS & RELATIONS

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    dS= S

    T

    P

    dT+ S

    P

    T

    dP

    S

    T

    P

    =

    CP

    T

    S

    P

    T

    = V

    T+1

    T

    H

    P

    T

    not measurable

    S

    P

    T

    =

    V

    T

    P

    = V

    =1

    V

    V

    T

    P

    thermal expansion

    72

    HOW TO CALCULATE ENTROPY CHANGES

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    dS=

    ST

    P

    dT+

    SP

    T

    dP

    S for an isothermal expansion of a perfect gas from V1 to V2 at temperature T

    PV= nRT

    Perfect gas

    dS=

    S

    P

    T

    dP =

    V

    T

    P

    dP

    V

    T

    P

    =

    nR

    P

    73

    HOW TO CALCULATE ENTROPY CHANGES

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    dS=

    ST

    P

    dT+

    SP

    T

    dP

    VT

    P

    =

    nR

    P

    S for an isothermal expansion of a perfect gas from V1 to V2 at temperature T

    S= nR

    RT/V2RT/V1

    dP

    P

    dS=

    nR

    dP

    P

    S= nR lnV2

    V1

    independent of the path

    74

    HOW TO CALCULATE ENTROPY CHANGES

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    S= CP lnT2

    T1

    dS=CP

    TdT

    dS=S

    T

    P

    dT+ S

    P

    T

    dP

    S for a process occurring at constant pressure

    dS=

    S

    T

    P

    dTS

    T

    P

    =

    CP

    T

    S=

    T2

    T1

    CPdT

    T

    75

    HOW TO CALCULATE ENTROPY CHANGES

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    We can use either S(T,V) or S(T,P)

    dS=

    S

    T

    V

    dT+

    S

    V

    T

    dV

    dS= CV

    TdT+

    PT

    V

    dV

    dS=CV

    T

    dT+nR

    V

    dV

    S for a perfect gas from (V1, T1, P1) to (V2, T2, P2)

    P

    TV

    =

    nR

    V

    S= CV lnT2

    T1+ nR ln

    V2

    V1

    76

    HOW TO CALCULATE ENTROPY CHANGES

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    q = qrev = 0

    S for an adiabatic reversible expansion of a gas

    Pext

    V

    T1

    T2

    P1, V1

    P2, V2

    S=?

    dS=qrev

    T

    S = 0

    77

    HOW TO CALCULATE ENTROPY CHANGES

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    S for an adiabatic irreversible expansion of a gas

    dS=qrev

    T

    Pext

    V

    T1

    T2

    P1, V1

    P2, V2

    S=?

    q = qirrev = 0

    S= 0

    S must be calculated over a reversible path that connects theinitial and final states of the irreversible adiabatic expansion

    78

    THERMODYNAMIC TEMPERATURE SCALE

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    Up to now, ideal gas temperature scale

    depends on the substance

    We should not have to rely on any particular substance or eq. of state to define atemperature

    Carnots cycle (independent of the substance)

    rev = 1 +qC

    qH= f(C, H)

    qC

    qH

    =C

    H

    Choose a reference temperature (triple point of water)

    = tr |q|

    |qtr|

    T = 273.16K|q|

    |qtr| tr = 273.16

    79

    REVERSIBILITY & IRREVERSIBILITY

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    Suniv = Ssys +Ssurr

    Tsys = Tsurr

    Reversible processes

    system

    surroundings

    dSuniv = dSsys + dSsurr =qsys

    Tsys

    +qsurr

    Tsurr

    Suniv = 0

    =qrev

    Tsys+qrev

    Tsurr

    qrev

    80

    REVERSIBILITY & IRREVERSIBILITY

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    reversibleisotherm, T

    V

    P

    1

    2

    1 3

    reversibleadiabat

    2irreversible adiabat

    Irreversible adiabatic processes (closed system)

    81

    REVERSIBILITY & IRREVERSIBILITY

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    reversibleisotherm, T

    V

    P4

    3 reversibleadiabat

    1

    2irreversible adiabat

    reversibleadiabat

    S12 +S23 +S34 +S41 = 0

    S23 = S41 = 0

    reversible adiabats

    S12 = S34 = q34

    TdU =

    (q+ w) = q34 + w = 0

    q34 > 0

    Not possible!

    it violates the 2nd law of thermodynamics (Kelvins statement)

    w = q34

    Irreversible adiabatic processes (closed system)

    82

    REVERSIBILITY & IRREVERSIBILITY

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    reversibleisotherm, T

    V

    P4

    3 reversibleadiabat

    1

    2irreversible adiabat

    reversibleadiabat

    S12 +S23 +S34 +S41 = 0

    S23 = S41 = 0

    reversible adiabats

    S12 = S34 = q34

    T

    w = q34

    dU =

    (q+ w) = q34 + w = 0

    S12 0

    Irreversible adiabatic processes (closed system)

    83

    REVERSIBILITY & IRREVERSIBILITY

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    reversibleisotherm, T

    V

    P4

    3 reversibleadiabat

    1

    2irreversible adiabat

    reversibleadiabat

    S12 +S23 +S34 +S41 = 0

    S23 = S41 = 0

    reversible adiabats

    S12 = S34 = q34

    T

    w = q34

    dU =

    (q+ w) = q34 + w = 0

    S12 = 0 S12 > 0

    Irreversible adiabatic processes (closed system)

    84

    REVERSIBILITY & IRREVERSIBILITY

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    Irreversible adiabatic processes (closed system)

    S > 0

    Irreversible adiabatic processes (isolated system)

    S > 0

    The universe can be considered as an isolated system

    Suniv = Ssys +Ssurr > 0 irreversible process

    Suniv 0

    85

    MOLECULAR CONNECTION

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    molecular kinetic energyT

    all energies [kinetic, potential (electronic,vibrational, rotational, nuclear, ...)]

    U

    ?S ?dS=dqrev

    T

    Higher S more probable states

    86

    MOLECULAR CONNECTION

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    probability ?

    1/4

    probability ?

    1/4

    probability ?

    1/4

    probability ?

    1/4

    =

    1/2probability

    Higher S more probable states

    A more uniform distribution much more probable than a very uneven one

    87

    MOLECULAR CONNECTION

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    probability

    1/4

    probability

    1/4

    =1/2

    probability

    Higher S more probable states

    macroscopic states

    A macroscopic state is associated with many microscopic states

    88

    MOLECULAR CONNECTION

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    probability

    1/4

    probability

    1/4

    =1/2

    probability

    Higher S more probable states

    What is a microscopic state?

    Depends on the system

    For an ideal gas

    If you know at an instant of time where every molecule is and what its velocity is youhave the full microscopic state

    89

    MOLECULAR CONNECTION

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    Some macroscopic states have many more microscopic states consistent with it(e.g, same P, T, components)

    Let p = probability of a thermodynamic state

    p =num er o m crostates cons stent w t a g ven t ermo ynam c state

    total number of microstates

    k = Boltzmanns constant

    true for anything

    entropy is associated with themicroscopic states of highest probability

    S= k lnp

    90

    MOLECULAR CONNECTION

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    Some macroscopic states have many more microscopic states consistent with it(e.g, same P, T, components)

    S= k lnp

    order / disorderS

    more disorder more probable more microstates

    S= k ln p2

    p1S=

    21

    qrevT

    difficult !!!

    91

    MOLECULAR CONNECTION

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    Some macroscopic states have many more microscopic states consistent with it(e.g, same P, T, components)

    = lnp

    order / disorderS