Pressure Changes Along Flow Experiencing Heat Transfer

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In airflow experiencing significant heat transfer, such as a temperature change of approximately 600 degrees Celsius, compressible effects are crucial. The pressure gradient along the flow differs notably between compressible and inviscid flow scenarios. To analyze these changes, the Rayleigh flow technique can be employed. This method allows for the calculation of both the change in flow rate and the exit temperature based on the rate of heat transfer and initial flow conditions. Understanding these principles is essential for accurate modeling of high-temperature airflow dynamics.
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For an airflow experiencing a large heat transfer, say a delta of ~600 degrees celsius, I assume compressible effects cannot be ignored. I am struggling however with some conceptual elements, such as how the pressure gradient changes along the flow when compared with compressible and inviscid flow. Is there a technique for calculating both the change in flow rate and temperature at the exit given the rate of heat transfer and entry conditions of the flow?
 
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