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    CHAPTER 2

    First Law of Thermodynamics

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    Two types of quantities

    1) State functions: Depend only on the thermodynamic state of the system not on howthe system got there (e.g., P, T, V, ...)

    FIRST LAW OF THERMODYNAMICS

    Thermodynamics is based on laws that have never been observed to be violated

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    Two types of quantities

    1) State functions: Depend only on the thermodynamic state of the system not on howthe system got there (e.g., P, T, V, ...)

    2) Process-dependent quantities: Depend on the way in which the system changesits thermodynamic state

    FIRST LAW OF THERMODYNAMICS

    Thermodynamics is based on laws that have never been observed to be violated

    surroundings

    system

    state a

    Pa, Ta, Va

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    Two types of quantities

    1) State functions: Depend only on the thermodynamic state of the system not on howthe system got there (e.g., P, T, V, ...)

    2) Process-dependent quantities: Depend on the way in which the system changesits thermodynamic state

    FIRST LAW OF THERMODYNAMICS

    Thermodynamics is based on laws that have never been observed to be violated

    surroundings

    system

    state b

    Pb, Tb, Vb

    Pa, Ta, Va

    system

    state a

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    Two types of quantities

    1) State functions: Depend only on the thermodynamic state of the system not on howthe system got there (e.g., P, T, V, ...)

    2) Process-dependent quantities: Depend on the way in which the system changesits thermodynamic state

    FIRST LAW OF THERMODYNAMICS

    Thermodynamics is based on laws that have never been observed to be violated

    surroundings

    system

    state a

    system

    state bPa, Ta, Va

    Pb, Tb, Vb

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    Two types of quantities

    1) State functions: Depend only on the thermodynamic state of the system not on howthe system got there (e.g., P, T, V, ...)

    2) Process-dependent quantities: Depend on the way in which the system changesits thermodynamic state

    Two types of processes

    1) Reversible: System and surroundings are infinitesimally close to equilibrium throughout

    the process.

    2) Irreversible: System and/or surroundings not in equilibrium except at beginning and atthe end (sometimes in between).

    FIRST LAW OF THERMODYNAMICS

    Thermodynamics is based on laws that have never been observed to be violated

    Natural processes: irreversible

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    Work (mechanical): Involves moving an object against a force (e.g., gravity, friction, piston)

    Work may be

    Positive: work done on the system

    Negative: work done by the system

    P-V WORK

    Work (w) depends on the specific path

    surroundings

    system

    state a

    system

    state b

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    w = Fdr = PextAn

    r =

    PextAdr

    w = PextdV

    Expansion: dr > 0 dV > 0 w < 0

    w = F dr

    dr

    Force = gravityF = PextAn

    |n| = 1

    A = area

    System

    Fn

    A

    w > 0dV < 0Compression: dr < 0

    P-V WORK

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    Force = gravity

    w = PextdV

    System

    F drn

    A

    surroundings

    system

    state a

    system

    state b

    w =

    f

    Vi

    Pext(T, V)dV

    Line integral

    P-V WORK

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    Examples

    n = 1 mole of gas

    w = P2(V2 V1)

    P1, V1, TP2, V2, T

    T1 = T2 = T

    w =

    f

    Vi

    Pext(T, V)dV

    V2V1

    P1

    P2

    Pext

    V

    w < 0 work is done by the system

    P-V WORK

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    Examples

    n = 1 mole of gas

    P1, V1, TP2, V2, T

    T1 = T2 = T

    w =

    f

    Vi

    Pext(T, V)dV

    V2V1

    P1

    P2

    Pext

    V

    w < 0 work is done by the system

    w = P1(V2 V1)

    P-V WORK

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    Examples

    n = 1 mole of gas

    P1, V1, TP2, V2, T

    T1 = T2 = T

    w =

    f

    Vi

    Pext(T, V)dV

    V2V1

    P1

    P2

    Pext

    V

    w < 0 work is done by the system

    Pa

    Va

    w = Pa(Va V1) P2(V2 Va)

    P-V WORK

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    Examples

    n = 1 mole of gas

    P1, V1, TP2, V2, T

    T1 = T2 = T

    w =

    f

    Vi

    Pext(T, V)dV

    V2V1

    P1

    P2

    Pext

    V

    P-V WORK

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    Examples

    n = 1 mole of gas

    P1, V1, TP2, V2, T

    T1 = T2 = T

    w =

    f

    Vi

    Pext(T, V)dV

    V2V1

    P1

    P2

    Pext

    V

    Reversible processThe system is always infinitesimally close to equilibrium

    = ext

    P-V WORK

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    Examples

    n = 1 mole of gas

    T1 = T2 = T

    w = f

    ViPext(T, V)dV

    V2V1

    P1

    P2

    Pext

    V

    Reversible processThe system is always infinitesimally close to equilibrium: P = Pext

    P =RT

    V

    Ideal gas

    w = RT

    V2

    V1

    dV

    Vw = RT ln

    V2

    V1

    Maximum amount of work that can be done by (on) a system at constant T

    P-V WORK

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    Heat is the entity that flows across a boundary between two systems or between asystem and its surroundings as a result of a temperature difference between them

    Molecular scale: kinetics energy transferred via motion and/or collisions and/or radiation

    Convention: Heat flows from higher T to lower T

    A process that involves no heat flow is adiabatic

    Observation

    When an infinitesimal amount of heat flows at constant pressure into a system thetemperature of the system increases according to

    q= CPdT

    HEAT

    CP(T

    ) : Heat capacity at constant pressure (depends on the system)

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    Heat may be transferred reversibly or irreversibly

    HEAT

    qP

    =

    T2

    T1 CP

    (T)dTq=

    CPdT

    CP =

    q

    T

    P

    Heat capacity at constant pressure:

    qP > 0 heat flows into the system Convention:

    IMPORTANT(1) A system doesnt have a q orw. They arent state functions

    (2) q and w may both lead to a temperature change

    (3) q and w have same units

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    It is based on experimental observations and can be stated in various ways

    qcycle + wcycle = 0

    In general qand ware different fromzero and depend on the specific path

    (q+ w) = 0

    FIRST LAW OF THERMODYNAMICS

    2

    1

    a

    b

    1

    (q+ w) +

    1

    2

    (q+ w) = 0

    path a path b

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    FIRST LAW OF THERMODYNAMICS

    2

    1

    (q+ w) + 1

    2

    (q+ w) = 0

    path a path b

    2

    1

    (q+ w) = 2

    1

    (q+ w)

    path a path b

    dU= q+ w

    U = internal energy (extensive state function)

    q+ w = exact differential !!!

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    INTERNAL ENERGY

    Properties

    dU = 0 The internal energy of a system that undergoes

    a cyclic process does not change

    The change in internal energy of a

    system whose state change from 1 to 2depends only on the initial and finalstate and is independent of the way inwhich the change occurs

    U =21

    dU= U2 U1

    independent of the path

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    (2) Thermodynamics doesnt really care about the absolute value of U but

    only about the difference U between two states the zero can be set anywhere (be consistent!!!)

    (1) Knowing U means knowing the function not just one valueU(n,T,V) or U(n,T,P) for single component systemsU(n,T,P,x1,x2,...,xN-1) for multicomponent systems

    Important

    INTERNAL ENERGY

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    dV = 0Constant volume process:

    HEAT CAPACITY AT CONSTANT V

    dU= q+ w

    dU= q Pext dV

    U= q

    Change in internal energy with an infinitesimal changein temperature in a constant volume process

    Cv =

    U(n,V,T)

    T

    V,n

    Heat capacity at constant V

    Heat absorbed with an infinitesimal change intemperature in a constant volume process

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    HEAT CAPACITY AT CONSTANT V

    Cv =

    U(n,V,T)T

    V,n

    Heat absorbed with an infinitesimal change in

    temperature in a constant volume process

    Molar capacity: Divide by the number of moles

    CV,m(T) =

    Um(V, T)

    T

    V

    Um =U

    n

    Change in internal energy with an infinitesimal changein temperature in a constant volume process

    O S O G

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    Changes in U(V,T) associated with a change in the thermodynamic state

    z

    x

    y

    =1

    xz y

    z

    x

    y

    x

    y

    z

    y

    z

    x

    = 1

    RELATIONS INVOLVING U

    (single component, homogeneous system for now)

    Recall:

    z = z(x, y) dz = zxy

    dx+zyx

    dy

    RELATIONS INVOLVING U

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    RELATIONS INVOLVING U

    U= U(V, T) dU=U

    T

    VdT+

    UV

    TdV

    dU = CVdT+U

    V

    T

    dVCV= U

    T

    V

    U

    V

    T

    =

    U

    T

    V

    T

    V

    U

    U

    VT

    V

    TU

    T

    UV

    = 1

    RELATIONS INVOLVING U

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    dU=U

    T

    VdT+

    UV

    TdV

    RELATIONS INVOLVING U

    U= U(V, T)

    dU = CVdT+U

    V

    T

    dVCV= U

    T

    V

    U

    VT

    = U

    TV

    T

    VU

    U

    VT

    = CVT

    VU

    J = 0 for ideal gas

    U

    V

    T

    = CV JJ = Joule coefficient

    RELATIONS INVOLVING U

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    dU=U

    T

    V

    dT+U

    V

    T

    dV

    dU= CV dT CV J dV

    RELATIONS INVOLVING U

    U(V,T) convenient because:

    (1) dU can be related to measurable quantities (CV, J)

    (2) dU = dq when dV = 0, no work (T,P can change but there is no compression or expansion)

    ENTHALPY

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    Many experiments involve constant P

    ENTHALPY

    Enthalpy: H= U+ PV

    dH= dU + PdV + V dP

    = q + w + PdV + V dP

    = q PextdV + P dV + V dP

    = q + (P Pext)dV + V dP

    ENTHALPY

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    CP includes heat adsorbed to cause temperature rise and system expansion

    CV does not involve system expansion

    ENTHALPY

    dH= q

    Cp =

    H

    T

    p

    Heat capacity at constant P

    CV =

    U

    T

    V

    Heat capacity at constant V

    At constant pressure: P = Pext

    CP > CV

    dH= q + (P Pext)dV + V dP

    ENTHALPY

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    ENTHALPY

    dH= HT

    P

    dT+HP

    T

    dP

    dH= CPdT+

    H

    P

    T

    dP

    Following the same procedure as for U(T,V)

    dH= CPdT CP T

    PH

    dP

    dH= CPdT CP JT dP

    JT =

    T

    P

    H

    Joule-Thomsoncoefficient

    for ideal gasJT = 0

    SUMMARY

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    SUMMARY

    Changes associated with the equation of state as well as with the first law ofthermodynamics that can be expressed in terms of measurable quantities

    (T, P) =1

    V

    V

    T

    P,n

    (T, P) = 1

    V

    V

    P

    T,n

    Expansion coefficient Isothermal compressibility

    CV =

    U

    T

    V

    =

    q

    dT

    V

    p =

    H

    T

    p

    =

    q

    dT

    p

    Heat capacity at constant V Heat capacity at constant P

    J =

    T

    V

    U

    = 1

    CV

    U

    V

    T

    Joule coefficient Joule-Thomson coefficient

    JT =

    T

    P

    H

    = 1

    CP

    H

    P

    T

    SUMMARY

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    SUMMARY

    Relation between heat capacities

    CV =

    U

    T

    V

    =

    q

    dT

    V

    Cp =

    H

    T

    p

    =

    q

    dT

    p

    Heat capacity at constant V Heat capacity at constant P

    CPCV =

    HT

    P

    UT

    V

    CP CV = (U+ PV)T

    P

    UT

    V

    CP CV =

    U

    T

    P

    + P

    V

    T

    P

    U

    T

    V

    SUMMARY

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    SUMMARY

    Relation between heat capacities

    dU = UT

    V

    dT+UV

    T

    dVBut,

    At constant P, dUP =

    U

    T

    V

    dTP +

    U

    V

    T

    dVP

    U

    T

    P

    =

    U

    T

    V

    +

    U

    V

    T

    V

    T

    P

    dividing by dTP

    CPCV =

    UT

    P

    + PV

    T

    P

    UT

    V

    SUMMARY

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    SUMMARY

    Relation between heat capacities

    CP CV =

    U

    T

    P

    + P

    V

    T

    P

    U

    dT

    V

    UTP

    = UTV

    + UV

    T

    VTP

    Using

    CP CV =

    U

    V

    T

    + P

    V

    T

    P

    SUMMARY

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    SUMMARY

    dU= CV dT CV J dV

    dH= CPdT CP JT dP

    JOULE EXPERIMENT

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    J =T

    VU

    =

    1

    CVU

    VT

    JOULE EXPERIMENT

    dU= CV dT+

    U

    V

    T

    dV

    dU= CV dT CV J dV

    adiabaticwalls

    plug

    vacuum

    T1, V1

    adiabaticwalls

    T2, V2

    q = 0adiabatic walls

    vacuumPext = 0 w = 0

    U = 0

    T

    V

    U

    JOULE THOMSON EXPERIMENT

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    JOULE-THOMSON EXPERIMENT

    dH= CPdT+

    H

    P

    T

    dP

    dH= CPdTCP

    T

    P

    H

    dP

    JT= T

    PH

    P1 P2

    P1, V1, T1adiabatic

    walls

    adiabaticwalls P1 > P2

    porous

    plug

    JOULE THOMSON EXPERIMENT

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    JOULE-THOMSON EXPERIMENT

    dH= CPdT+

    H

    P

    T

    dP

    dH= CPdTCP

    T

    P

    H

    dP

    JT= T

    PH

    P1 P2

    adiabaticwalls

    adiabaticwalls P1 > P2

    JOULE THOMSON EXPERIMENT

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    JOULE-THOMSON EXPERIMENT

    dH= CPdT+

    H

    P

    T

    dP

    dH= CPdTCP

    T

    P

    H

    dP

    JT= T

    PH

    P1 P2

    adiabaticwalls

    adiabaticwalls P1 > P2

    q = 0adiabatic walls

    P2, V2, T2

    w =PdVreversible process w =

    P1(0

    V1)

    P2(V2

    0)

    JOULE THOMSON EXPERIMENT

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    JOULE-THOMSON EXPERIMENT

    q = 0

    w = 1 1 2 22 1 = 1 1 2 2

    first law

    1 + 1 1 = 2 + 2 2

    H1 = H2

    constant enthalpy!!!

    JOULE THOMSON EXPERIMENT

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    JOULE-THOMSON EXPERIMENT

    dH= CPdT+

    H

    P

    T

    dP

    dH= CPdTCP

    T

    P

    H

    dP

    JT= T

    PH

    P1 P2

    adiabaticwalls

    adiabaticwalls P1 > P2

    P2, V2, T2

    H = 0 T

    PH

    JOULE-THOMSON EXPERIMENT

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    JOULE-THOMSON EXPERIMENT

    JT = TP

    H

    = 1

    CPH

    PT

    H

    PT

    > 0

    H

    P

    T

    < 0

    Low T / High P:

    High T / Low P:

    JT < 0

    JT > 0

    JOULE-THOMSON EXPERIMENT

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    JOULE-THOMSON EXPERIMENT

    JT = TP

    H

    = 1

    CPH

    PT

    H

    PT

    > 0

    H

    P

    T

    < 0

    Low T / High P:

    High T / Low P:

    ISENTHALPIC CURVES

    It is possible to use the J-T experimentto liquefy gas (see book)

    PERFECT GAS

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    PERFECT GAS

    V= nRT

    U

    V

    T

    = 0

    U = U(T)

    dU = CVdT

    CV = CV(T)

    H= U+ PV= U+ nRT

    H= H(T)

    CP = CP(T) =dH

    dT

    PERFECT GAS

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    PERFECT GAS

    CPCV =

    UV

    T

    + PV

    TP

    V= nRT

    U

    V

    T

    = 0

    V

    T

    P

    =

    nR

    P

    P V = nR