Definition: Calorimetry is the measurement of the quantity of heat, which is the form of energy that flows from a hot body to a cold body.
Internal Energy: The sum of potential and kinetic energy of molecules is termed internal energy, leading to the concept of thermal energy—the total internal energy of all molecules in a substance. A hotter body contains more internal energy than a cooler one.
SI Unit: Joule (J).
Calorie: The amount of heat required to raise the temperature of 1 gram of water by 1°C. 1 Calorie equals 4.2 Joules (1 Cal = 4.2 J).
Definition: Temperature is a measure of the degree of hotness or coldness of a body, indicating its thermal state and determining the direction of heat flow between two bodies in contact.
Units: The SI Unit is Kelvin (K), while a common unit is degrees Celsius (°C): (T_k = t°C + 273).
The quantity of heat energy absorbed to increase the temperature of a body depends on:
Mass of the Body: Directly proportional to the mass (Q ∝ m).
Increase in Temperature: Directly proportional to the temperature rise (Q ∝ Δt).
Material of the Body: The specific heat capacity (c) influences the amount of heat absorbed (Q = cmΔt).
Heat Capacity (C'): Amount of heat required to raise the temperature of a body by 1°C. Given by (C' = [ \frac{Q}{Δt} ]), with units J/K.
Specific Heat Capacity (C): Amount of heat required to raise the temperature of a unit mass of a body by 1°C, expressed as (C = [ \frac{Q}{m \times Δt} ]), with units J kg⁻¹ K⁻¹.
Relationship: Heat Capacity = mass × specific heat capacity.
Water's Specific Heat Capacity: 4200 J kg⁻¹ K⁻¹.
Definition: An instrument used to measure the heat gained or lost by a body.
Heat Exchange: The heat energy lost by a hot body is equal to the heat energy gained by a cold body, based on the law of conservation of energy.
Mathematical Expression: (m₁c₁Δt = m₂c₂Δt).
Moderate Climate: Coasts experience less extreme temperatures because of water's high specific heat capacity.
Hot Water Bottles: Used for fomentation as water retains heat longer.
Effective Coolant: Water removes heat from heated machine parts effectively due to its high specific heat capacity.
Heat Reservoir: Useful in cold climates to prevent freezing of beverages.
Frost Protection: Filling fields with water prevents freezing and protects crops during cold nights.
Biological Importance: All plants and animals contain 80-90% water, helping to stabilize their body temperatures across seasons.
Thick Cooking Pan Base: Retains and evenly distributes heat.
Electric Press: Thick base retains heat after switch-off.
Calorimeter Construction: Made from thin copper sheet to minimize heat absorption and ensure accurate readings.
Definition: The transition between states of matter at constant temperatures due to heat exchange.
Processes:
Melting: Solid to liquid (absorbs heat).
Freezing: Liquid to solid (rejects heat).
Vaporization: Liquid to gas (absorbs heat).
Condensation: Gas to liquid (rejects heat).
Sublimation: Solid to gas.
Solidification: Gas to solid.
Melting Point: Constant temperature where solids turn to liquids.
Freezing Point: Constant temperature where liquids turn to solids.
Expansion/Contraction: Most substances expand upon melting, except for ice, which contracts.
Heating Curve of Ice: Graph of temperature versus time shows different states and transitions—AB (liquid) and constant temperature during boiling at B.
Volume Change: Most substances expand upon heating; water becomes significantly larger in vapor form compared to liquid.
Pressure Effects: Increasing pressure can lower melting points of certain substances and raise points for others.
Impurity Effects: Adding impurities generally decreases melting points and increases boiling points.
Definition: Change from liquid to gas at a constant temperature; boiling point is the temperature at which this occurs.
Heating Curve for Water: Similar to that of ice, reflecting heat absorption and state changes.
Volume Change on Boiling: Expansion of liquids occurs, resulting in steam (1 cm³ water to 1760 cm³ steam).
Latent Heat: Heat absorbed or released during phase changes without temperature change.
Specific Latent Heat (L): Given by (L = [ \frac{Q}{m} ]), measured in J/kg.
Fusion of Ice: Heat required to melt ice at 0°C to water at the same temperature.
Slow Melting of Snow: Mountain snow melts gradually due to high latent heat.
Water Bodies: Do not freeze immediately due to heat retention.
Quick Cooling: Ice cools drinks faster than cold water.
Temperature Drops: Surrounding air cools when ice melts due to heat absorption for phase change.
Hail Storm Effects: Colder conditions after hail due to ice melting and absorbing heat.