Skip to main content
Back

Thermodynamics: Latent Heat, Laws, and Heat Transfer Mechanisms

Study Guide - Smart Notes

Tailored notes based on your materials, expanded with key definitions, examples, and context.

Latent Heat and Phase Transitions

Latent Heat: Definition and Application

Latent heat refers to the energy required for a substance to change its phase (solid, liquid, gas) without a change in temperature. This energy is absorbed or released during phase transitions such as melting, freezing, vaporization, or condensation.

  • Latent Heat of Fusion (Lf): Energy required to change 1 kg of a substance from solid to liquid at constant temperature.

  • Latent Heat of Vaporization (Lv): Energy required to change 1 kg of a substance from liquid to gas at constant temperature.

  • Formula: where Q is the heat absorbed or released, m is the mass, and L is the latent heat.

  • Temperature remains constant during the phase change, even as heat is added or removed.

  • Example: Melting ice at 0°C requires energy input, but the temperature does not rise until all ice is melted.

Table: Latent Heats of Common Substances

The following table compares melting points, boiling points, and latent heats for various substances at 1 atm:

Substance

Melting Point (°C)

Heat of Fusion (kJ/kg)

Boiling Point (°C)

Heat of Vaporization (kJ/kg)

Oxygen

-218.8

14

-183

210

Nitrogen

-210.0

26

-195.8

199

Ethyl alcohol

-114.0

104

78.5

855

Ammonia

-77.8

332

-33.4

1370

Water

0

335

100

2260

Lead

327

23

1750

860

Silver

961

88

2212

2090

Iron

1538

289

2861

6340

Tungsten

3410

184

5900

4850

Heat During Phase Transitions

Calculating the energy required for phase changes involves a stepwise process:

  1. Cool the substance to the phase change temperature:

  2. Change the phase (e.g., freeze or melt):

  3. Adjust temperature of the new phase:

Example: To freeze 1.5 kg of water from 20°C to -12°C, calculate the heat removed in each step and sum the results.

Zeroth Law of Thermodynamics

Thermal Equilibrium and Heat Flow

The Zeroth Law of Thermodynamics establishes the concept of thermal equilibrium:

  • Heat is defined as the flow of energy due to a temperature difference.

  • Heat flows spontaneously from higher to lower temperature until equilibrium is reached.

  • When two objects reach the same temperature, they are in thermal equilibrium.

  • Once equilibrium is achieved, no net heat flows between the objects.

First Law of Thermodynamics

Internal Energy, Heat, and Work

The First Law of Thermodynamics relates changes in internal energy to heat and work:

  • Internal energy (U): The total energy of all molecules in a system. For an ideal gas:

  • First Law Equation: where is heat added to the system, is work done by the system.

  • Adding heat or doing work on the system increases its internal energy.

Work Done in a System

Work is done when a system changes volume under pressure:

  • Formula:

  • For expansion (), work is done by the system; for compression (), work is done on the system.

Thermodynamic Processes

Types of Thermodynamic Processes

Thermodynamic processes are classified by which state variable remains constant:

  • Isothermal: Temperature constant ()

  • Isobaric: Pressure constant ()

  • Isovolumetric (Isochoric): Volume constant ()

  • Adiabatic: No heat exchange ()

Summary Table: Thermodynamic Processes

Process

Constant

First Law Relation

Isothermal

,

Isobaric

Isovolumetric

,

Adiabatic

Process Details and Equations

  • Isothermal: , ,

  • Isobaric: ,

  • Isovolumetric: , ,

  • Adiabatic: , ,

Molar Specific Heat

Specific Heat for Gases

For gases, specific heat depends on the process:

  • At constant volume:

  • At constant pressure:

  • Relation: (where is the gas constant)

Heat Transfer Mechanisms

Conduction

Conduction is the transfer of heat through molecular collisions, typically in solids.

  • Formula: where is thermal conductivity, is area, is length, and are temperatures.

  • High means good conductor; low means good insulator.

  • Example: Metal spoon in hot liquid conducts heat from hot end to cold end.

Convection

Convection is heat transfer by bulk movement of fluid (liquid or gas).

  • Heat is carried by moving particles, creating currents and circulation.

  • Example: Hot water rises, cooler water descends, creating convection currents.

Radiation

Radiation is heat transfer by emission of electromagnetic waves, even through vacuum.

  • Formula (Stefan-Boltzmann Law): where is emissivity, is Stefan-Boltzmann constant, is area, is temperature.

  • Emissivity () ranges from 0 (perfect reflector) to 1 (perfect emitter).

  • At thermal equilibrium, net heat exchange is zero.

Adiabatic Expansion of a Gas

Adiabatic Process Equations

In adiabatic processes, no heat is exchanged ():

  • First Law:

  • Adiabatic Condition:

  • (gamma) is the heat capacity ratio: Monatomic gases: Diatomic gases:

Example: Rapid expansion of a gas in an insulated container.

Additional info: Some context and equations were expanded for clarity and completeness, including the summary tables and process details.

Pearson Logo

Study Prep