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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 = - - -