Heat transfer between objects occurs through three main mechanisms:
1. Conduction: This involves the direct transfer of energy through physical contact between particles. Imagine holding a hot mug. The hot cup's particles vibrate faster due to their higher temperature, and when they collide with your hand's particles, they transfer some of this energy, making your hand warmer. Metals are good conductors, while materials like wood or plastic are poor conductors.
2. Convection: This occurs in fluids (liquids and gases) and involves the movement of the fluid itself to transfer heat. Hot fluid expands and becomes less dense, rising up. Cooler fluid flows in to replace it, creating a circular motion. This is why you see water boiling in a pot – the hot water at the bottom rises, while cooler water descends, carrying heat to the surface.
3. Radiation: This is the transfer of energy through electromagnetic waves, most notably infrared radiation. Unlike conduction and convection, radiation doesn't require physical contact or a medium. The sun warms Earth through radiation, and you can feel the heat from a fire without touching it.
Now, let's see how temperature and pressure affect the kinetic energy of particles:
Temperature: Temperature is directly proportional to the average kinetic energy of particles in a system. As temperature increases, particles move faster and collide more frequently, transferring more energy through conduction and convection. This is why hot objects lose heat faster than cold ones.
Pressure: In gases, increasing pressure generally increases the kinetic energy of particles due to the closer proximity and more frequent collisions. However, in liquids and solids, the effect of pressure on kinetic energy is more complex and depends on factors like material properties and temperature.
Here are some additional points to consider:
The rate of heat transfer depends on the temperature difference between objects, the area of contact in conduction, and the density and specific heat capacity of the materials involved.
Specific heat capacity is the amount of heat required to raise the temperature of a unit mass of a substance by one degree. Materials with low specific heat capacity heat up or cool down quickly, while those with high specific heat capacity require more heat to change their temperature.
Pressure can also affect specific heat capacity and thermal conductivity in certain materials.
In addition to the previous complete and right answer, the Fourier Law of Thermal Conduction helps to calculate the heat time rate between objects, and it depends on the temperature.