I think that people that think PO4 is not lowered by bacterial growth are 'incorrect' - in the experimental conditions you have set up - almost by default, PO4 will decrease if bacteria are growing.
But - IMHO - this is where there is a key difference. in your experiment - during 'a bloom' - during the logarithmic growth phase - PO4 will decrease - my GUESS is that in a tank - with all of the variables - additions of food, etc - the PO4 will not decline significantly.
I guess I look at it this way. Take a tank - that produces a stable amount of ammonia, nitrate, PO4/day. Start dosing xxx Carbon. At first - there will be a logarithmic increase in bacteria x,y,z......... Then - that extra 'carbon' is utilized. Then one of 2 things will happen - if you dont add more carbon the nutrients will be re-released into the tank - right? So - you repeatedly dose carbon - and eventually a new steady state will be accomplished - and in theory the nitrate after a month lets say - of carbon dosing will be lower than the start.
But - if you're merely maintaining a population of bacteria thats basically eating ammonia and or nitrate (heterotrophs - with carbon) - they are not going to be using as much PO4 once they are in the 'stable' phase - as compared to the active growth phase. Does that make sense?
By the way - if you read the article I provided - my GUESS is that when you increase heterotrophs using carbon, the reason nitrate falls is not that the bacteria are eating nitrate 'per se' - though some do - its because they are utilizing ammonia - thus less nitrate is produced. I.e. carbon increases heterotrophs --->. Heterotrophs utilize both carbon and ammonia ---> less nitrate.
Note these are merely my ramblings - perhaps
@Lasse has a comment - as he would have much more knowledge than I