L04 - Temp and Heat
Lecture Overview
Physics 1003 Lecture 4: Temperature and Heat
Instructor: Mr. Chan Chung Yuen (TA-in-charge) - Contact: cychandg@connect.ust.hk
Temperature and Temperature Scales
Definition: Temperature gauges how hot or cold an object is relative to a reference point.
Temperature Scales:
Celsius (°C): 0°C (freezing point of water) and 100°C (boiling point of water) at 1 standard atmosphere.
Fahrenheit (°F):
Kelvin (K): Absolute temperature; conversion: 𝑇𝐾 = 𝑇𝐶 + 273.15
Key Temperature Points
Absolute zero:
0 K = -273.15 °C = -459.67 °F
Ice melts:
273.15 K, 0 °C, 32 °F
Water boils:
373 K, 100 °C, 212 °F
Average human body temperature: 309.95 K, 36.8 °C, 98.24 °F
Highest recorded temperature on Earth: 331 K, 58 °C, 136.4 °F
Lowest recorded temperature: -89.2 °C (184 K) at Vostok Station, Antarctica.
Cold Fact Summary
Atmospheric pressure: N2 gas condenses at 77 K and freezes at 63 K.
Helium condenses at 4.2 K.
Oxygen's boiling point: 90.188 K.
CO2 sublimates directly to gas above -78.5 °C.
Absolute Zero:
The ultimate cold limit; 0 K where atoms cease motion.
Ideal Gas Description
Ideal Gas Characteristics:
Inert gas; molecules interact minimally except during elastic collisions.
Temperature reflects the average kinetic energy of gas molecules.
Avogadro's Number
Avogadro’s Number: NA = 6.02 × 10²³ - number of molecules in a mole.
Kinetic Theory and Gas Behavior
Kinetic theory links temperature to molecular motion, defining states of matter in terms of kinetic and potential energy.
Thermal Equilibrium and Energy Transfer
Objects of differing temperatures reach thermal equilibrium through heat transfer.
Heat flows from hot to cold objects until thermal equilibrium is attained.
Zeroth Law of Thermodynamics:
If A is in equilibrium with B, and B with C, then A and C are in equilibrium.
Heat and Internal Energy
Internal Energy (U):
Comprises Kinetic Energy (KE) + Potential Energy (PE) of the system's molecules.
KE reflects molecular movement; PE is the result of intermolecular interaction.
Degrees of Freedom in Gases
Monatomic Gas: 3 translational degrees of freedom (DOF)
Diatomic Gas: 5 DOF (3 translational + 2 rotational)
Internal energy for gases:
Monatomic: U = (3/2)NkT
Diatomic: U = (5/2)NkT
Effects of Temperature Increase
As temperature increases:
Solids absorb heat (kinetic energy) and transition to liquids.
Liquids boil into gases.
Sublimation (solid to gas) occurs in certain materials.
Heat Capacity
Definition: The energy required to increase the temperature of a substance by 1°C per mole.
Varies based on material composition and internal energy distribution.
Heat Transfer Mechanisms
Methods of Heat Transfer:
Conduction: Direct contact transfer (via electrons and lattice vibrations).
Convection: Fluid particle movement transfers heat.
Radiation: Emitted energy via electromagnetic radiation, requiring no medium.
Thermal Radiation
Objects emit thermal radiation based on their temperature.
Mechanism involves temperature-induced vibrations of charged particles resulting in electromagnetic waves.
Electromagnetic Radiation Basics
Wave Properties:
Frequency (f): Measured in Hertz (Hz).
Wavelength (λ): Measured in micrometers (µm) or nanometers (nm).
Relationship: c = λf (c = speed of light).
Spectra
Electromagnetic Spectrum:
Ranges from gamma rays to radio waves, with varying frequency and wavelength characteristics.
Black-Body Radiation:
Planck's theory explains energy emission in quantized form, highlighting particle-nature of light.
Particle-Wave Duality
Louis de Broglie: 1924, proposed matter behaves as both particle and wave, earning the Nobel Prize in Physics in 1929.
Energy-wavelength frequency relation: E = hf = hc/λ (h = Planck constant).
Summary Report on Heat Transfer and Internal Energy
Heat transfer is critical in thermodynamics, impacting physical states and energy dynamics within systems. Understanding these principles is essential for grasping larger physics concepts.