Overview of key concepts:
Temperature
Absolute Zero
Heat
Quantity of Heat
Laws of Thermodynamics
Entropy
Specific Heat Capacity
Thermal Expansion
Expansion of Water
Definition: A measure corresponding to the warmth or coldness of an object, measured by a thermometer.
It is a per-particle property with no upper limit and a definite lower limit.
Kinetic Theory: Temperature correlates with the average translational kinetic energy per particle.
Gas: Speed of gas particles bouncing.
Liquid: Speed of particles sliding past one another.
Solid: Vibration of particles in place.
Function by the expansion or contraction of liquid (mercury colored alcohol).
Reading achieved upon reaching thermal equilibrium with the object.
Infrared Thermometers: Operate by sensing IR radiation.
Celsius: 0°C (freezing) to 100°C (boiling).
Fahrenheit: 32°F (freezing) to 212°F (boiling).
Kelvin: 273 K (freezing) to 373 K (boiling), absolute zero at -273°C.
Definition: Lowest possible temperature at -273°C, where atoms lose all available kinetic energy.
Effects: Volume of gases changes with temperature adjustments.
Described through a sparkler’s temperature of 2000°C, illustrating high temperature but limited energy due to a small number of molecules.
Definition: Flow of thermal energy due to temperature difference; naturally flows from higher to lower temperature substances.
Practical Example: 1L vs. 3L of water absorbing the same heat results in a threefold temperature rise in the smaller volume.
Measurement: Expressed in joules or calories.
Calorie: Heat needed to raise 1g of water by 1°C.
Relation: 4.19 joules = 1 calorie.
Kilocalorie: Used in food labeling, equivalent to raising 1kg of water by 1°C.
First Law: Heat added equals the increase in internal energy plus external work done; total energy is conserved.
Second Law: Heat flows naturally from hot to cold; cannot flow reverse without external work.
Third Law: Absolute zero cannot be reached.
Definition: A measure of disorder in a system; energy transformations tend to increase disorder.
Natural systems evolve toward states of higher entropy over time.
Definition: Amount of heat required to raise the temperature of 1 unit mass by 1 degree; indicates resistance to temperature change.
Example: Water’s high specific heat capacity affects climate, taking longer to heat and cool compared to land.
Cause: Rise in temperature leads to increased molecular motion, causing expansion.
Notable Examples: Railroad tracks buckling in heat; expansion joints in bridges.
Special Consideration: Telephone lines need to be strung with sag to account for thermal expansion.
Unique property: Water expands upon freezing, making ice less dense. Water between 0°C and 4°C contracts before starting to expand.
Implications: In winter, colder water sinks until the temperature of the entire pond reaches 4°C. Ice forms on top, insulating the lower water layers.