Defining a Thermodynamic Cycle
A thermodynamic cycle is a sequence of thermodynamic processes that brings a working fluid or system back to its initial state. This means all state variables, such as pressure, temperature, and volume, are identical at the beginning and end of the cycle.
Key Characteristics and Energy Changes
During a cycle, the system interacts with its surroundings by exchanging heat and work. Crucially, the net change in the internal energy of the system over one complete cycle is zero. This principle is fundamental to the operation of devices that convert heat into work (like engines) or use work to transfer heat (like refrigerators).
Example: The Brayton Cycle
The Brayton cycle, used in gas turbine engines and jet engines, is a practical example. It consists of four main processes: isentropic compression, isobaric heat addition, isentropic expansion, and isobaric heat rejection. After these processes, the gas returns to its initial thermodynamic state, ready for the next cycle.
Importance in Technology and Science
Thermodynamic cycles are crucial for understanding and designing various engineering systems, including power plants, internal combustion engines, and refrigeration systems. They set the theoretical limits for the efficiency of energy conversion, guiding advancements in energy technology.