The process of heat transfer by convection involves the transportation of thermal energy within the fluids (liquids or gases) through molecular movement. It plays such an important part in our everyday life that we feel sensations, such as the warmth of a heater or the cool air from a ceiling fan, quite easily. Be it boiling water on a gas stove or movements of air in the atmosphere that creates climatic changes, convection is always in operation, making sure that energy is effectively spread around us.
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Convection is the process of heat transfer through a fluid (liquid or gas) caused by the movement of the fluid itself. It occurs when warmer, less dense portions of the fluid rise, and cooler, denser portions sink, creating a circulation pattern. This transfer of heat can happen naturally due to temperature differences (natural convection) or be forced by external means, such as a fan or pump (forced convection).
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Convection is the heat transfer due to the bulk movement of molecules within fluids such as gases and liquids. Convection is of two types -
If a fluid is forced(by means of a fan or draught or any external means) to move to take up heat from a hot body then the convection process is called forced convection. In this case, Newton's law of cooling holds good. According to which rate of loss of heat from a hot body due to moving fluid is directly proportional to the surface area of body and excess temperature of body over its surroundings.
Sea breeze: This phenomenon occurs during the day. The sun heats up both the sea surface and land. As the sea has a greater heating capacity, it absorbs much of the sun's energy but gets warmed up much slower than the land. As a result, the temperature above the land rises and heats the air in the atmosphere above it. Warm air is less dense, and hence, it expands, creating a low-pressure area over the land near the coast. Meanwhile, there is relatively high pressure over the sea. The difference in air pressure causes the air to flow from sea to land. The sudden gush of wind felt due to this is known as the sea breeze.
Land Breeze: This phenomenon occurs during the night when the situation reverses. As the sun sets, the land and sea start cooling down. The land quickly loses heat when compared to water due to the differences in heat capacity. Consequently, the temperature of the sea is relatively higher, which creates low air pressure there. This sets up a flow of cool breeze offshore, known as the land breeze.
Heat convection is the physical movement of a fluid (liquid, gas, or plasma) from one area to another to transfer thermal energy. In liquids and gases, heat convection is frequently the primary mechanism of energy transmission. Convection is one of three primary ways of heat transport, along with conduction and radiation.
Example 1: It is hotter for the same distance over the top of fire than it is on the side of it, mainly because
1) Air conducts heat upwards
2) Heat is radiated upwards
3) Conversion takes more heat upward.
4) Conversion, conduction and radiation all contribute significantly to transferring heat upwards.
Solution:
Convection: Mode of transfer of heat through migration of material particles of the medium.
Convection significantly transfers heat upwards. The top of a fire is hotter than its sides because hot air rises, creating a column of intense heat directly above the flames, while the heat is more dispersed on the sides.
Hence, the answer is the option (2).
Example 2: The layer of the atmosphere is heated through
1) Convection
2) Conduction
3) Radiation
4) 2 & 3 both
Solution:
Natural Convection
This arises due to the difference in densities at the two places.
wherein
The heating of the atmosphere is mainly because of natural convection.
Hence, the answer is the option (1).
Example 3: Heating of a room using a blower is an example of
1) Conduction
2) Natural convection
3) Forced convection
4) Radiation
Solution:
Forced Convection
If a fluid is forced to move to take up heat from a hot body.
wherein
So, heat transfer with the help of a blower is an example of heat transfer through forced convection.
Hence, the answer is the option (3).
Example 4: The rate of heat transfer in forced convection is
1) proportional to
2) proportional to
3) proportional to
4) proportional to
Solution:
Forced Convection
Where,
Hence, the answer is the option (1).
In solids, this is the most common mechanism of heat transport. Convection: If the medium is a fluid (i.e., anything that can flow), the medium particles can carry thermal energy and deliver it across. This mode has a bulk flow of medium particles.
Temperature variations between air parcels or heat transfer at surfaces cause natural convection (i.e. surface-to-air temperature difference). Natural convection becomes the sole way for air to mix inside confined spaces when forced convection is unavailable.
Yes, they are same.
Ice melting is an excellent illustration of convection. Because heat transfers from the air to the ice, it melts.
Convection is a type of thermal energy transmission that occurs in gases or liquids (whereas conduction occurs most often in solids) and is dependent on variations in heat.
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