ThermoChapter24 210 - Judith...

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2.4, 2.10

Applications of the First Law to ideal gases

RTpv =

What we know

Equation of state

Internal energy is function only of temperature dTcdu v= dTcdh p=

Rcc vp =−Specific heats are related

pdvdw −="expansion work"

The fist law dwdqdu += vdpdqdh +=

pdvdqdTcv −=

vdpdqdTcp +=

dTcdu v= dTcdh p= Rcc vp =−

dwdqdu +=

vdpdqdh +=

pdvdw −=

The first law of thermodynamics for an ideal gas

Isothermal vs. Adiabatic

An isothermal process in one in which the initial and final temperatures are the same.

Isothermal processes are notnecessarily adiabatic.

An adiabatic process in one in which no heat is exchanged between the system and its surroundings.

0=dT

0=dq

Reversible Changes

• A reversible change is one that can be reversed by an infinitesimal modification of a variable.

gasenv pp =

• In a reversible expansion or compression

Lets consider an isothermal expansion 0=dT

dTcdu v=Because Internal energy is function only of temperature, the internal energy of the gas is unchanged

pdvdqdTcv −= pdvdq =

The first law of thermodynamics for an isothermal expansion

pdvdq =

isothermal expansion

If we want to integrate pdvdq =

pdvdw −=only expansion work" ∫ ≠ 0dw

What do we need???? Path!!!

v1 v2

AB

Lets consider the path of an isothermal reversible expansion

Equation of state is satisfied during all the stages of the expansion

RTpv =

isothermal expansion

pdvdq = RTpv =v

RTp =

vdvRTdq = ∫=Δ 2

1

v

v vdvRTq

⎟⎟⎠

⎞⎜⎜⎝

⎛=Δ

1

2lnvvRTq

pRTv = ⎟⎟

⎞⎜⎜⎝

⎛=Δ

2

1lnppRTq

⎟⎟⎠

⎞⎜⎜⎝

⎛=⎟⎟

⎞⎜⎜⎝

⎛=Δ

2

1

1

2 lnlnppRT

vvRTq

If we want to integrate

isothermal expansion

Constant volume process 0=dv

dwdqdu += pdvdqdu −=

dqdu =

( )12 TTcq v −=Δ

dTcdu v=

The amount of heat required to raise the temperature of the gas from T1 to T2 at constant volume

dTcdq v=

dTcdu v= dTcdh p= Rcc vp =− pdvdw −=

Constant volume

vdpdqdh +=

Constant pressure process 0=dp

dqdh =

dTcdh p= dTcdq p=

The amount of heat required to raise the temperature of the gas from T1 to T2 at constant pressure

( )12 TTcq p −=Δ

dTcdu v= dTcdh p= Rcc vp =− pdvdw −=

Constant pressure

Adiabatic process Process in which NO HEAT is exchange between the system and its environment

0=dq

dwdqdu +=

dwdu =Fist law for a reversible adiabatic process

An adiabatic compression increases the internal energy of the system

q

q

w

pdvdu −=

Adiabatic process

pdvdqdTcv −= vdpdqdTcp +=

Adiabatic process 0=dq

pdvdTcv −= vdpdTcp =

Fist law for adiabatic expansion

The first law of thermodynamics for an ideal gas

Adiabatic process

Poisson’s equations

pdvdTcv −= RTpv =v

RTp =

dvv

RTdTcv −=vdvR

TdTcv −=

Lets assume constant vc There is a final and initial state

Lets consider a reversible adiabatic EXPANSION for an ideal gas

0=dq

∫∫ −= 2

1

2

1

v

v

T

Tv vdvR

TdTc

⎟⎟⎠

⎞⎜⎜⎝

⎛−=⎟⎟

⎞⎜⎜⎝

1

2

1

2 lnlnvvR

TTcv

vcR

vv

TT

⎟⎟⎠

⎞⎜⎜⎝

⎛=⎟⎟

⎞⎜⎜⎝

2

1

1

2During an adiabatic expansion of a gas, the temperature decreases

∫∫ −= 2

1

2

1

v

v

T

Tv vdvR

TdTc

Poisson’s equations

Reverse process adiabatic Compression

Work is done on the gas and the temperature increases

vcR

vv

TT

⎟⎟⎠

⎞⎜⎜⎝

⎛=⎟⎟

⎞⎜⎜⎝

2

1

1

2

pcR

pp

TT

⎟⎟⎠

⎞⎜⎜⎝

⎛=⎟⎟

⎞⎜⎜⎝

1

2

1

2

vp

cc

vv

pp

⎟⎟⎠

⎞⎜⎜⎝

⎛=⎟⎟

⎞⎜⎜⎝

2

1

1

2

RTpv =

A given pressure decrease produces a smaller volume increase in the adiabatic case relative to the isothermal case

RTpv =

isothermal expansion Vs reversible adiabatic expansion

P, v diagram

Temperature also decreases during the adiabatic expansion

Dry Adiabatic Processes in the Atmosphere

For reversible adiabatic processes for an ideal gas

pcR

pp

TT

⎟⎟⎠

⎞⎜⎜⎝

⎛= 00

Orographic Lifting Frontal Lifting

Low-level convergence Vertical Mixing

Lifting Processes

p

T

0=dq

A dry adiabatic process as long CONDENSATION DOES NOT OCCUR!!

Lifting:

pcR

pp

T ⎟⎟⎠

⎞⎜⎜⎝

⎛= 0θ

If for mb 10000 =p the temperature is , θ

pcR

pp

TT

⎟⎟⎠

⎞⎜⎜⎝

⎛= 00

pcRWhere for dry air is 286.0

72

25

==+

=+

=RR

RRc

RcR

vp

θ Potential Temperature

Temperature a parcel of gas (e.g. dry air) would have if compressed (or expanded) in an reversible adiabatic process from a state, and , to a a pressure of mb 10000 =pp T

θ Also a state variable, invariant during a reversible adiabatic process: Conservative quantity!!!!

pcR

pp

T ⎟⎟⎠

⎞⎜⎜⎝

⎛= 0θ

-1km C6Ο=Γ

Consider a Temperature profile with

For mb 1000<p T>θ⇒ Adiabatic compression to lower the parcel

mb 1000>p T<θ⇒

mb 1000=p T=θ⇒

T2 T1

Adiabatic expansion to rise the parcel

dzdT

−=Γ

Lapse rate

pcR

pp

T ⎟⎟⎠

⎞⎜⎜⎝

⎛= 0θ

Considering Water vapor

( ) ( )vpdpvvpdvp qccqcqc 87.011 +≈+−=Specific heat for moist air

vq Specific humidityd For dry air v For water vapor

( )vd qRR 608.01+=

And knowing(from Ch. 1) ( )v

pd

d

v

v

pd

d

p

qcR

qq

cR

cR 26.01

87.01608.01

−≈⎟⎟⎠

⎞⎜⎜⎝

⎛++

=

pcR

?? Considering water vapor

( )pd

vdc

qR

pp

T26.01

0

⎟⎟⎠

⎞⎜⎜⎝

⎛=θ

Potential Temperature for Moist Air

The difference between dry-air and moist air potential temperature is generally

less than 0.1 degree.

Important: is not conserved if a change of

phase occurs

θ

Adiabatic expansion or compression of moisture air can be treated as if

it were dry air

Liquid to vapor

solid to Liquid

Virtual Potential Temperature

Virtual Temperaturethe temperature a parcel which contains no moisture would have to equal the density of a parcel at a specific temperature and humidity.

temperature a parcel at a specific pressure level and virtual temperature would have if it were lowered or raised to 1000 mb.

vT

pdd

cR

vv ppT ⎟⎟⎠

⎞⎜⎜⎝

⎛= 0θ

Virtual Potential Temperature

Neglect the dependence on water vapor from the exponent, and replace temperature by virtual temperature

( )pd

vdc

qR

pp

T26.01

0

⎟⎟⎠

⎞⎜⎜⎝

⎛=θ

dzdT

−=Γ 1-km C8.9 Ο≈=Γpd

d cg

( )vpd qcg

87.01+=Γ

Adiabatic Ascent of a Parcel

T θ

vdpdTc p =

gdzdTc p −=

constant

Rate of decrease of temperature with height (first law, enthalpy form)

If there are no large vertical accelerations (hydrostatic relation applies)

vdpgdz =−

Lapse rate for dry air

For moist air

First law for adiabatic process