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1. What are the different types of transport phenomena?
Ans. The different types of transport phenomena are conduction, convection, and radiation. Conduction refers to the transfer of heat or mass through a solid material, convection involves the transfer of heat or mass through a fluid medium, and radiation is the transfer of heat or mass through electromagnetic waves.
2. How does conduction differ from convection in transport phenomena?
Ans. Conduction and convection differ in the way heat or mass is transferred. In conduction, the transfer occurs through direct contact between particles, such as molecules in a solid material. In convection, on the other hand, the transfer occurs through the movement of a fluid medium, such as air or water.
3. What is the significance of transport phenomena in engineering?
Ans. Transport phenomena play a crucial role in various branches of engineering. They are essential for understanding heat transfer, mass transfer, and fluid flow, which are vital in fields such as chemical engineering, mechanical engineering, and environmental engineering. Transport phenomena principles are used to design and optimize processes and systems in these fields.
4. How is transport phenomena related to everyday life?
Ans. Transport phenomena are present in numerous aspects of everyday life. Examples include the transfer of heat from a hot stove to a pot, the cooling of a room through air conditioning, and the movement of air pollutants in the atmosphere. Understanding transport phenomena helps in improving energy efficiency, designing better appliances, and addressing environmental issues.
5. What are some common applications of transport phenomena?
Ans. Some common applications of transport phenomena include heat exchangers, chemical reactors, distillation columns, and air pollution control systems. Transport phenomena principles are also applied in the design of cooling systems for electronic devices, transportation of fluids in pipelines, and the study of natural phenomena such as ocean currents and atmospheric circulation.
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