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PhysicsGrade 7· Indiana Academic Standards (IDOE)
Aligned to:Indiana Academic Standards / NGSS-aligned

Thermal Energy and Temperature

Students investigate how matter type and mass influence temperature change and the transfer of thermal energy toward equilibrium.

Thermal Energy and Temperature

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Thermal Energy and Temperature

Temperature and thermal energy are related, but they are not the same. Temperature measures the average kinetic energy of the particles in a substance. Thermal energy is the total energy associated with the motion and interactions of all the particles in a sample. Energy transferred because of a temperature difference is called heat. Thermal energy moves from matter at a higher temperature to matter at a lower temperature. For example, when a metal spoon is placed in hot soup, energy transfers from the soup to the cooler spoon. The spoon’s particles move faster as its temperature rises, while the soup loses some thermal energy. The amount of temperature change depends on the energy transferred, the spoon’s mass, and the type of metal.

Average Particle Motion

All matter is made of particles that are constantly moving. In a solid, particles vibrate around fixed positions. In liquids and gases, particles can also move past one another. Temperature measures the average kinetic energy of these particles, so a higher temperature means greater average particle motion. Not every particle moves at exactly the same speed, which is why scientists use an average. Imagine two sealed containers holding equal amounts of water. In the 20°C water, particles move with a lower average speed. In the 60°C water, particles move with a higher average speed. If energy is transferred into the cooler water, its particles gain kinetic energy, their average motion increases, and the measured temperature rises.

Mass and Temperature Change

Mass affects how much a substance’s temperature changes when thermal energy is transferred. If equal amounts of energy are added to two samples of the same material, the smaller mass usually has the larger temperature increase. The larger sample contains more particles, so the transferred energy is shared among more particles. For example, suppose identical heaters transfer the same amount of energy to 100 grams and 200 grams of water for the same time. If both start at 20°C and little energy escapes, the 100-gram sample will warm about twice as much as the 200-gram sample. A fair investigation keeps the material, starting temperature, heater power, and heating time the same while changing only mass. Students can measure and compare each temperature change.

Material Differences

Different materials can have different temperature changes even when their masses and the energy transferred are equal. This property is related to a material’s specific heat capacity, which describes how much energy is needed to raise the temperature of a certain mass by one degree Celsius. Water has a higher specific heat capacity than many metals, so it takes more energy to produce the same temperature increase in water. For example, equal masses of water and aluminum can be heated with identical heaters for the same amount of time. If both begin at the same temperature and receive equal energy, the aluminum’s temperature usually rises more. To test the relationship fairly, students should keep mass, starting temperature, heating time, and heater power constant and change only the type of matter.

Thermal Equilibrium

When objects at different temperatures touch or can exchange energy, thermal energy transfers from the higher-temperature object to the lower-temperature object. The warmer object’s particles lose kinetic energy on average, while the cooler object’s particles gain kinetic energy on average. This transfer continues until both objects reach the same temperature. This condition is called thermal equilibrium. At equilibrium, there is no net thermal energy transfer between the objects, although their particles continue moving. For example, an ice cube placed in warm water gains energy and melts while the water loses energy and cools. If the surroundings do not add or remove much energy, the water and melted ice eventually reach the same temperature. Recording both temperatures over time shows them approaching one shared equilibrium temperature.