Chapter 18: Temperature, Heat, and the First Law of Thermodynamics Notes

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=T273.150T_c = T - 273.150, where T is in Kelvin.

  • The Celsius degree has the same magnitude as the Kelvin.

  • The zero point of the Celsius scale is shifted for convenience relative to absolute zero.

Key Temperatures
  • Absolute zero: 0 K or -273.15°C

  • Water freezing temperature: 273.15 K or 0°C

Kelvin Scale

Scientists use the Kelvin scale to measure temperature. Zero Kelvin is the lowest attainable temperature.

Relationship between Celsius and Kelvin
  • 1 C0=1 K1 \text{ } C^0 = 1 \text{ } K

  • 00C=273.15 K0^0C = 273.15 \text{ } K

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:

    • calorie (cal): 1 cal=4.1860 J1 \text{ cal} = 4.1860 \text{ J}

    • British thermal unit (Btu): 1 cal=3.969×103 Btu1 \text{ cal} = 3.969 × 10^{-3} \text{ Btu}

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=PdVdW = F ds = P A ds = P dV, 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>fPdVW = \int<em>{V</em>i}^{V<em>f} P dV, where V</em>iV</em>i and VfV_f 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
  • Positive work: The final volume is greater than the initial volume (expansion).

  • Negative work: The final volume is smaller than the initial volume (compression).

Thermodynamic Cycles
  • Work in a cycle is the area of the loop in a P-V diagram.

    • Positive loop area: Positive work.

    • Negative loop area: Negative work.

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 curveW = \text{area under the curve}.

  • Process a to f: Constant volume, decrease temperature, heat flows out of the system, W=0W = 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=QW\Delta E_{int} = 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,fEint,i\Delta E<em>{int} = E</em>{int,f} - E_{int,i}

  • W and Q are path-dependent, but QWQ - 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=0Q = 0. This occurs when the system is well insulated or the process is rapid. Then, ΔEint=W\Delta E_{int} = -W.

Constant-Volume Processes

W=<em>VVPdV=0W = \int<em>V^V P dV = 0. Thus, ΔE</em>int=Q\Delta E</em>{int} = Q.

Cyclical Processes

Final state = Initial state, so ΔEint=0\Delta E_{int} = 0 and Q=WQ = W.

Free Expansion Processes

Q=0Q = 0, W=0W = 0, so ΔEint=0\Delta E_{int} = 0.

Free Expansions

  • System is insulated, thus Q=0Q = 0.

  • W=<em>V</em>iV<em>fPdV=</em>V<em>iV</em>f0dV=0W = \int<em>{V</em>i}^{V<em>f} P dV = \int</em>{V<em>i}^{V</em>f} 0 dV = 0

  • Thus, ΔEint=0\Delta E_{int} = 0.

Examples

Example 1

Steam to Water:

  • Initial state: P<em>i=1 AtmP<em>i = 1 \text{ Atm}, V</em>i=1×103m3V</em>i = 1 × 10^{-3} m^3, Ti=100CT_i = 100^\circ C, m=1 kgm = 1 \text{ kg}

  • Final state: P<em>f=1 AtmP<em>f = 1 \text{ Atm}, V</em>f=1.671m3V</em>f = 1.671 m^3, Ti=100CT_i = 100^\circ C, m=1 kgm = 1 \text{ kg}

Calculations:

  • W=<em>V</em>iV<em>fPdv=P</em>V<em>iV</em>fdv=P(V<em>fV</em>i)=1.01×105Pa(1.671m31×103m3)=169 kJW = \int<em>{V</em>i}^{V<em>f} P dv = P \int</em>{V<em>i}^{V</em>f} dv = P(V<em>f - V</em>i) = 1.01 × 10^5 Pa (1.671 m^3 - 1 × 10^{-3} m^3) = 169 \text{ kJ}

  • Q=LVm=2256 kJ/kg×1 kg=2256 kJQ = L_V m = 2256 \text{ kJ/kg} × 1 \text{ kg} = 2256 \text{ kJ}

  • ΔEint=QW=2256 kJ169 kJ=2090 kJ\Delta E_{int} = Q - W = 2256 \text{ kJ} - 169 \text{ kJ} = 2090 \text{ kJ}

Example 2

Ideal gas expanding at constant pressure:

  • Q=500 JQ = 500 \text{ J}

  • V<em>i=0.2m3V<em>i = 0.2 m^3, V</em>f=0.3m3V</em>f = 0.3 m^3, P=4.0×103PaP = 4.0 × 10^3 Pa

Calculations:

  • Isobaric expansion: W=<em>V</em>iV<em>fPdv=P</em>V<em>iV</em>fdv=PΔV=P(V<em>fV</em>i)=4.0×103Pa(0.3m30.2m3)=400 JW = \int<em>{V</em>i}^{V<em>f} P dv = P \int</em>{V<em>i}^{V</em>f} dv = P \Delta V = P(V<em>f - V</em>i) = 4.0 × 10^3 Pa (0.3 m^3 - 0.2 m^3) = 400 \text{ J}

  • ΔEint=QW=500 J400 J=100 J\Delta E_{int} = Q - W = 500 \text{ J} - 400 \text{ J} = 100 \text{ J}

Example 3

Calculate work done by expanding 1 mole of gas:

  • P<em>i=4.0×103PaP<em>i = 4.0 × 10^3 Pa, V</em>i=0.2m3V</em>i = 0.2 m^3, Ti=96.2KT_i = 96.2 K

Two processes:

  1. Isobaric expansion to 0.3m30.3 m^3, Tf=144.3KT_f = 144.3 K

  2. Isothermal expansion to 0.3m30.3 m^3

Calculations:

  1. Isobaric expansion:

  • W=<em>V</em>iV<em>fPdv=P</em>V<em>iV</em>fdv=PΔV=P(V<em>fV</em>i)=4.0×103Pa(0.3m30.2m3)=400 JW = \int<em>{V</em>i}^{V<em>f} P dv = P \int</em>{V<em>i}^{V</em>f} dv = P \Delta V = P(V<em>f - V</em>i) = 4.0 × 10^3 Pa (0.3 m^3 - 0.2 m^3) = 400 \text{ J}

  • T<em>fT</em>i=V<em>fV</em>i=32\frac{T<em>f}{T</em>i} = \frac{V<em>f}{V</em>i} = \frac{3}{2}

  1. Isothermal expansion:

  • W=nRTlnV<em>fV</em>i=P<em>iV</em>ilnV<em>fV</em>i=4.0×103Pa×0.2m3×ln0.3m30.2m3=324 JW = nRT \cdot \ln{\frac{V<em>f}{V</em>i}} = P<em>i V</em>i \cdot \ln{\frac{V<em>f}{V</em>i}} = 4.0 × 10^3 Pa × 0.2 m^3 × \ln{\frac{0.3 m^3}{0.2 m^3}} = 324 \text{ J}

  • p<em>fp</em>i=V<em>iV</em>f=23\frac{p<em>f}{p</em>i} = \frac{V<em>i}{V</em>f} = \frac{2}{3}

Example 4

Heat absorbed by 3 moles of helium during isothermal expansion:

  • V<em>i=10 LV<em>i = 10 \text{ L}, V</em>f=20 LV</em>f = 20 \text{ L}, T=350 KT = 350 \text{ K}

Calculations:

  • For an ideal gas, isothermal means ΔEint=0\Delta E_{int} = 0

  • pV=nRTpV = nRT

  • Q=WonQ = -W_{on}

  • W<em>on=nRTlnV</em>fViW<em>{on} = -nRT \cdot \ln{\frac{V</em>f}{V_i}}

  • p<em>i=nRTV</em>i=8.72×105Pap<em>i = \frac{nRT}{V</em>i} = 8.72 × 10^5 Pa

  • p<em>f=p</em>i2=4.36×105Pap<em>f = \frac{p</em>i}{2} = 4.36 × 10^5 Pa

  • V<em>fV</em>i=20 L10 L=2\frac{V<em>f}{V</em>i} = \frac{20 \text{ L}}{10 \text{ L}} = 2

  • Q=(6048 J)=6048 JQ = -(-6048 \text{ J}) = 6048 \text{ J}

Heat Transfer Mechanisms

  1. Conduction

  2. Convection

  3. Radiation

Conduction

Collisions between adjacent atoms transfer heat along the material.

Formula - Single Slab

Conduction rate: P<em>con=Qt=kAT</em>HT<em>CLP<em>{con} = \frac{Q}{t} = kA \frac{T</em>H - T<em>C}{L}, where k is thermal conductivity, A is the face area, T</em>HT</em>H is the hot reservoir temperature, TCT_C is the cold reservoir temperature, and L is the thickness.

Thermal Resistance (R-Value)

R=LkR = \frac{L}{k}. 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=k</em>1A(T<em>HT</em>X)L=k<em>2A(T</em>XTC)LP<em>{con} = \frac{k</em>1 A(T<em>H - T</em>X)}{L} = \frac{k<em>2 A(T</em>X - T_C)}{L}

P<em>con=AT</em>HT<em>CL</em>1k<em>1+L</em>2k<em>2=AT</em>HT<em>CR</em>1+R2P<em>{con} = A \frac{T</em>H - T<em>C}{\frac{L</em>1}{k<em>1} + \frac{L</em>2}{k<em>2}} = A \frac{T</em>H - T<em>C}{R</em>1 + R_2}

Formula - Many Slabs

P<em>con=AT</em>HT<em>CL</em>1k<em>1+L</em>2k<em>2++L</em>nknP<em>{con} = A \frac{T</em>H - T<em>C}{\frac{L</em>1}{k<em>1} + \frac{L</em>2}{k<em>2} + \cdots + \frac{L</em>n}{k_n}}

Checkpoint 4 Solution

In steady state, conduction rates through slabs are equal. kΔTk \Delta T 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=σεAT4P_{rad} = \sigma \varepsilon A T^4, where σ\sigma is the Stefan-Boltzmann constant (5.67×108W/m2K45.67 × 10^{-8} W/m^2 \cdot K^4), ε\varepsilon is emissivity, A is surface area, and T is temperature in Kelvins.

  • Rate of thermal radiation absorption: P<em>abs=σεAT</em>env4P<em>{abs} = \sigma \varepsilon A T</em>{env}^4, where TenvT_{env} is the environment temperature in Kelvins.

  • Net rate of energy exchange: P<em>net=P</em>absP<em>rad=σεA(T</em>env4T4)P<em>{net} = P</em>{abs} - P<em>{rad} = \sigma \varepsilon A (T</em>{env}^4 - T^4)

Emissivity
  • Value from 0 to 1

  • Depends on the composition of the surface

  • Black body radiator (ideal): ε=1\varepsilon = 1

  • White Shiny: ε=0\varepsilon = 0

Example 5

Four-Layer Wall

  • Steady state: conduction rates through all layers are the same

  • k<em>d=5k</em>ak<em>d = 5k</em>a

  • L<em>d=2L</em>aL<em>d = 2L</em>a

  • T<em>1=25CT<em>1 = 25^\circ C, T</em>2=20CT</em>2 = 20^\circ C, T5=100CT_5 = -100^\circ C

Solution:

k<em>aA(T</em>1T<em>2)L</em>a=k<em>dA(T</em>4T<em>5)L</em>d\frac{k<em>a A(T</em>1 - T<em>2)}{L</em>a} = \frac{k<em>d A(T</em>4 - T<em>5)}{L</em>d}

P<em>a=P</em>dP<em>a = P</em>d

k<em>aA(T</em>1T<em>2)L</em>a=5k<em>aA(T</em>4T<em>5)2L</em>a\frac{k<em>a A(T</em>1 - T<em>2)}{L</em>a} = \frac{5k<em>a A(T</em>4 - T<em>5)}{2L</em>a}

T<em>1T</em>2=52(T<em>4T</em>5)T<em>1 - T</em>2 = \frac{5}{2} (T<em>4 - T</em>5)

25C20C=52(T4(10C))25^\circ C - 20^\circ C = \frac{5}{2} (T_4 - (-10^\circ C))

T4=8CT_4 = -8^\circ C