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  • 7/27/2019 wresdfhsadf gsakdfh asj fhaskfhjasfjhakjs xhhgfsawrwe

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    Heat Capacities

    o Consider a homogeneous system of constant compositiono Write dU(dH) as a total differential of the independent

    variablesXand Y(for our purposes,Xand Ycould be any

    pair ofp, V, and T). Then

    o From the 1st Law, Q = dU+pdV, we can substitute to get

    whereXand Yare Tand V, respectively.

    ( ) ( )Y X

    dU U X dX U Y dY = +

    ( ) ( )V T

    Q U T dT p U V dV d = + +

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    Heat Capacities

    o From Q = dHVdp we can substitute fordHto get

    whereXand Yare Tandp, respectively.

    o For a process of heating at V= const we get

    or per unit mass we can write

    ( ) ( )p T

    Q H T dT H p V dpd = + -

    ( )v v Vc m C Q dT U T d= = =

    ( )vv

    c q dT u T d= =

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    Heat Capacities

    o For a process of heating atp = const we get

    or per unit mass we can write

    o Can also calculate heat of change ofVandp at T= const

    o Not very useful, but given for completeness

    ( )p p pc m C Q dT H T d= = =

    ( )p pc q dT h T d= =

    ( ) ( ), andT T

    Q dV U V p Q dp H p V d d= + = -

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    Calculation of Internal Energy and Enthalpy

    o Our equations forCVand Cp can be integrated directly forprocesses with V= const andp = const, respectively to

    find UandH, ifCVand Cp are known as functions ofT

    oCVand Cp, from experiment, are usually polynomials in Tandv pU C dT const H C dT const

    = + = +

    2C T Ta b g= + + + K

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    Calculation of Internal Energy and Enthalpy

    o Consider 2 rigid vessels linked by a connection with astopcock (pg. 34). One contains gas, the other evacuated.

    o Stopcock opened, gas in 1 expands to occupy both vessels.

    o Temperature measurements show that system exchanges

    no heat with environment no work done, Q = 0, W= 0,

    and U= 0.

    o Sincep changed during process, we have U= U(T) only

    and partial derivative used above are total derivatives.

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of ThermodynamicsCalculation of Internal Energy and Enthalpy

    o Notes on this experiment

    When experiment done carefully, small heat exchange was found(Joule-Thomson effect), which vanishes for ideal gas behavior

    As gas confined in vessel 1 expands into 2, work is done by someportions of gas against others while volumes change (as molecules enter2, they are effected by molecules following)

    These are internal transfers that are not included in W

    This shows the importance of defining system carefully and clearlywhen considering a thermodynamic process

    In this case, the system is all the gas contained in both vessels (initially

    one is empty), whose total volume (V1 + V2) does not change

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    More on Heat Capacities

    o As noted above, since U= U(T) we have CV= dU/dTandcv = du/dT

    o We can writeH= U+pV= U+ nR*T=H(T) leading to

    Cp = dH/dTand cp = dh/dT

    oSince we are only interested in differences in internal

    energy and enthalpy, we can set the integration

    constant to 0 giving: UCVT,HCpT, ucvT, and

    hcpT

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    More on Heat Capacities

    o Since we have CV= dU/dT, Cp = dH/dTandH= U+pV=U+ nR*T, we have

    leading to Cp

    CV

    = nR*cp

    cv

    =R recalling that

    n = m/M.

    oAs mentioned earlier, heat capacities for all gases can

    be measured and the coefficients for the polynomial

    expansion can be determined (C= + T+ T2+ )

    * *

    p VdH dT dU dT nR C C nR= + = +

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of ThermodynamicsMore on Heat Capacities

    o For simple gases like N2, O2, and Ar, the experimental data are

    nearly constant for all temperatures and pressures of interest, so the

    temperature variation is not considered.

    o From earlier we have, for monatomic gases, the total internal energy

    is U= (3/2)NkT, which leads to CV= (3/2)nR* and cv = (3/2)R.

    Similarly, Cp = (5/2)nR* and cp = (5/2)R.

    o For diatomic gases, where there are more degrees of freedom, so we

    get CV= (5/2)nR* and cv = (5/2)R. Similarly, Cp = (7/2)nR

    * and cp =

    (7/2)R. The ratios Cp/CV= cp/cv = .

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    More on Heat Capacities

    o Dry air is considered to be a diatomic gas, so the secondform applies.

    o The ratio, cp/cv = = 1.4.

    o We then attach the subscript, d, to the specific heats to

    indicate dry air.

    o This leads to cvd= 718 J kg-1 K-1 and cpd= 1005 J kg

    -1 K-1

    andRd= cpdcvd= 287(.05) J kg-1 K-1.

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 4

    1

    st

    Law ofThermodynamics

    More on Heat Capacities

    o The table below shows the values ofcpdfor varioustemperatures and pressures. Note the slight variation.

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    More Forms of the 1st Law

    o Using the above expressions for (specific) heat capacities,we get more useful forms of the 1st Law, two of which are

    particularly useful

    and

    , andv vQ C dT pdV q c dT pd d d a= + = +

    , andp pQ C dT Vdp q c dT dpd d a= - = -

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    Department of Atmospheric SciencesATM 404/504Thermodynamics

    Ch. 41st Law of Thermodynamics

    Special Cases

    o For an isothermal transformation

    o For an isochoric (constant volume) transformation

    o For an isobaric transformation

    *ln f iQ nR T V V =

    (V f iU Q C T T D = = -

    ( ) (

    ( ) ( )

    andp f i f i

    p f i f i

    Q C T T W p V V

    U C T T p V V

    = - = -

    D = - - -