The coupling of mass and heat balance

that they are coupled 'by the interface' Arrhenius equation. The (exothermal) reaction 'exhibits some conversion' depending on the rate constant. This produces 'heat of reaction' and a 'rise of the temperature' (in the reaction mass). The 'new' temperature produces a 'new' rate constant following the Arrhenius equation. The new rate constant produces the next conversion step .....and so on, in adiabatic reactors the solution of this process is comparably simple, cf. the following link (or the task on an adiabatic STR ). Here you see the numerical approach of the simultaneous solution of both balances. Another possibility is the graphical solution which 'derives' from the 1/r(U)-plot procedure, see an example, - of course finally the same matter!!.
The procedure can get even a bit more complicated for adiabatic TFRs, where the calculation 'ends' in the consecutive solution of both balances for a TFR in a cell compartment model (cf. book of Jens Hagen, Chemische Reaktionstechnik)

But: Exterior heat and mass transport effects (e.g. caused by convection or interchange /exchange processes in not adiabatic and/or continuous reactors) influence (disturb) the two coupled systems and make the problem even more complex, - e.g. in the case of the calculations for polytropical (or a bit less difficult: isothermal) process conduction modes, - or think of the gradients in TFRs with heterogeneous phase flows or thermostatting jackets with countercurrent or cocurrent flows of two phases or within the heat exchanging process !

see a blackbord sketch of the various possibilities for the 3 basic reactor types

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