
Originally Posted by
relttem
This can be answered by that balance I posted:
h*A*(T2-T1) this is the air side heat transfer. IF, the air flow rate is the same, then h is constant, A and (T2-T1) are both constant as you mentioned.
This has to be balanced by
mdot*Cp*(T2-T1), which is the water side heat transfer.
mdot is your mass flow rate. Cp is going to be pretty constant at these small temperature changes. So, as mdot slows (T2-T1) (larger temperature difference) has to go up to balance the equation..or the other way around...as mdot gets higher your (T2-T1) (smaller temp difference) gets smaller..
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