Thermodynamics
Thermodynamics is the study of thermal energy, also known as internal energy, within systems. Temperature is a fundamental concept in thermodynamics.
Temperature
Our perception of temperature is not always reliable. For example, metal and wood at the same temperature may feel different to the touch because metal conducts heat away from our fingers more quickly than wood.
The Zeroth Law of Thermodynamics
Every object possesses a property called temperature. When two objects are in thermal equilibrium, their temperatures are equal, and vice versa.
Thermal Equilibrium
Thermal equilibrium is achieved when two bodies in contact reach the same temperature.
Celsius and Fahrenheit Scales
Celsius Scale
The Celsius scale is defined as: Tc=T−273.150, where T is in Kelvin.
Key Temperatures
Kelvin Scale
Scientists use the Kelvin scale to measure temperature. Zero Kelvin is the lowest attainable temperature.
Relationship between Celsius and Kelvin
Heat
Heat is the energy transferred between a system and its environment due to a temperature difference.
Units of Heat
SI unit: joule (J)
Other units:
Work
Work is the energy transferred when a force causes a displacement.
Work Done by Gas
For a small change in volume, the work done by a gas is: dW=Fds=PAds=PdV, where P is pressure and V is volume.
Total Work
The total work done during a thermodynamic process is: W=∫<em>V</em>iV<em>fPdV, where V</em>i and Vf are the initial and final volumes, respectively.
Work as Area Under the Curve
In a P-V diagram, the work done by the system is the area under the curve.
Positive and Negative Work
Thermodynamic Cycles
Path Dependence of Work
Work depends on the path taken in a thermodynamic process.
Illustration
Process i to a: Constant pressure, increase temperature, heat flows into the system, W=area under the curve.
Process a to f: Constant volume, decrease temperature, heat flows out of the system, W=0.
Work done by the system and heat flow are path-dependent.
First Law of Thermodynamics
The change in internal energy of a system is given by: ΔEint=Q−W, where Q is the heat transferred to the system and W is the work done by the system.
ΔE<em>int=E</em>int,f−Eint,i
W and Q are path-dependent, but Q−W is independent of the path.
Conservation of Energy
The first law of thermodynamics is a statement of the conservation of energy. It assumes that changes in kinetic and potential energies of the system are negligible.
Special Cases of the First Law of Thermodynamics
Adiabatic Processes
No heat transferred: Q=0. This occurs when the system is well insulated or the process is rapid. Then, ΔEint=−W.
Constant-Volume Processes
W=∫<em>VVPdV=0. Thus, ΔE</em>int=Q.
Cyclical Processes
Final state = Initial state, so ΔEint=0 and Q=W.
Free Expansion Processes
Q=0, W=0, so ΔEint=0.
Free Expansions
System is insulated, thus Q=0.
W=∫<em>V</em>iV<em>fPdV=∫</em>V<em>iV</em>f0dV=0
Thus, ΔEint=0.
Examples
Example 1
Steam to Water:
Initial state: P<em>i=1 Atm, V</em>i=1×10−3m3, Ti=100∘C, m=1 kg
Final state: P<em>f=1 Atm, V</em>f=1.671m3, Ti=100∘C, m=1 kg
Calculations:
W=∫<em>V</em>iV<em>fPdv=P∫</em>V<em>iV</em>fdv=P(V<em>f−V</em>i)=1.01×105Pa(1.671m3−1×10−3m3)=169 kJ
Q=LVm=2256 kJ/kg×1 kg=2256 kJ
ΔEint=Q−W=2256 kJ−169 kJ=2090 kJ
Example 2
Ideal gas expanding at constant pressure:
Q=500 J
V<em>i=0.2m3, V</em>f=0.3m3, P=4.0×103Pa
Calculations:
Isobaric expansion: W=∫<em>V</em>iV<em>fPdv=P∫</em>V<em>iV</em>fdv=PΔV=P(V<em>f−V</em>i)=4.0×103Pa(0.3m3−0.2m3)=400 J
ΔEint=Q−W=500 J−400 J=100 J
Example 3
Calculate work done by expanding 1 mole of gas:
Two processes:
Isobaric expansion to 0.3m3, Tf=144.3K
Isothermal expansion to 0.3m3
Calculations:
Isobaric expansion:
W=∫<em>V</em>iV<em>fPdv=P∫</em>V<em>iV</em>fdv=PΔV=P(V<em>f−V</em>i)=4.0×103Pa(0.3m3−0.2m3)=400 J
T</em>iT<em>f=V</em>iV<em>f=23
Isothermal expansion:
W=nRT⋅lnV</em>iV<em>f=P<em>iV</em>i⋅lnV</em>iV<em>f=4.0×103Pa×0.2m3×ln0.2m30.3m3=324 J
p</em>ip<em>f=V</em>fV<em>i=32
Example 4
Heat absorbed by 3 moles of helium during isothermal expansion:
Calculations:
For an ideal gas, isothermal means ΔEint=0
pV=nRT
Q=−Won
W<em>on=−nRT⋅lnViV</em>f
p<em>i=V</em>inRT=8.72×105Pa
p<em>f=2p</em>i=4.36×105Pa
V</em>iV<em>f=10 L20 L=2
Q=−(−6048 J)=6048 J
Heat Transfer Mechanisms
Conduction
Convection
Radiation
Conduction
Collisions between adjacent atoms transfer heat along the material.
Formula - Single Slab
Conduction rate: P<em>con=tQ=kALT</em>H−T<em>C, where k is thermal conductivity, A is the face area, T</em>H is the hot reservoir temperature, TC is the cold reservoir temperature, and L is the thickness.
Thermal Resistance (R-Value)
R=kL. A high R-value indicates a good thermal insulator.
Thermal Conductivity
A material with low thermal conductivity is a good thermal insulator.
Formula - Two Slabs
P<em>con=Lk</em>1A(T<em>H−T</em>X)=Lk<em>2A(T</em>X−TC)
P<em>con=Ak<em>1L</em>1+k<em>2L</em>2T</em>H−T<em>C=AR</em>1+R2T</em>H−T<em>C
Formula - Many Slabs
P<em>con=Ak<em>1L</em>1+k<em>2L</em>2+⋯+knL</em>nT</em>H−T<em>C
Checkpoint 4 Solution
In steady state, conduction rates through slabs are equal. kΔT is constant for slabs with the same length and cross-sectional area. Smaller temperature difference corresponds to greater thermal conductivity.
Convection
Expansion of fluid when heated leads to lower density, and buoyant forces cause it to rise.
Radiation
Thermal radiation consists of electromagnetic waves that do not require a medium for transfer (travel through vacuum).
Formula
Rate of thermal radiation emission: Prad=σεAT4, where σ is the Stefan-Boltzmann constant (5.67×10−8W/m2⋅K4), ε is emissivity, A is surface area, and T is temperature in Kelvins.
Rate of thermal radiation absorption: P<em>abs=σεAT</em>env4, where Tenv is the environment temperature in Kelvins.
Net rate of energy exchange: P<em>net=P</em>abs−P<em>rad=σεA(T</em>env4−T4)
Emissivity
Value from 0 to 1
Depends on the composition of the surface
Black body radiator (ideal): ε=1
White Shiny: ε=0
Example 5
Four-Layer Wall
Steady state: conduction rates through all layers are the same
k<em>d=5k</em>a
L<em>d=2L</em>a
T<em>1=25∘C, T</em>2=20∘C, T5=−100∘C
Solution:
L</em>ak<em>aA(T</em>1−T<em>2)=L</em>dk<em>dA(T</em>4−T<em>5)
P<em>a=P</em>d
L</em>ak<em>aA(T</em>1−T<em>2)=2L</em>a5k<em>aA(T</em>4−T<em>5)
T<em>1−T</em>2=25(T<em>4−T</em>5)
25∘C−20∘C=25(T4−(−10∘C))
T4=−8∘C