Natural convection is a type of heat transfer that occurs without any external force. Instead, it relies on natural processes to initiate fluid movement. When a fluid, such as air or water, is heated, its density decreases, and this causes it to rise, while cooler, denser fluid moves down to replace it. This creates a continuous circulation pattern driven by buoyancy forces. These forces occur when there is a temperature gradient within the fluid, leading to differences in fluid density.
Natural convection can be seen in various real-world situations:
- Air circulating around a heated room, where warmer air rises near a radiator.
- Water heating in a pan on the stove, where warmer water rises away from the heat source.
The efficiency of natural convection depends on several factors including the temperature difference and the properties of the fluid. Generally, since it relies on milder movement, the heat transfer is not as efficient as in forced convection, resulting in a lower convection heat transfer coefficient.