Originally Posted by tmz
					(Post 21610696)
				 
				 
 
 
It's certainly seems counter intuitive to dose nitrate or another nitrogen source  but it may make sense. 
 
The redfeild ratio is rather useless as a  guide other than to offer  perspective on the general en masse proportions of carbon(C)106:N) 16: 1 P   in ocean plankton. Organisms may approximate those levels but some  including some bacteria vary significantly . Even if food put in the  tank is close to those proportions, the activity in the tank may not use  them  in those proportions.  All in all, trying to use the redfield  ratio to obtain a generalized optimal N to P ratio seems convoluted.   Using tank levels of  N and P  vs natural seawater  levels seems smarter  and more direct. 
 
To  clarify the  idea  as to  why dosing N might be necessary, a brief  look at the  three major nutrients coming in and going out of the bio  available mix in the tank     may be  helpful 
 
Organic carbon coming in for the most part with foods  can be used for  energy  or sunk in refractory( non bio available) organics like humic and  fulvic acids ;some may also  be contributed by photosynthesis. So, the  amount coming into the tank is not really  the bio available  amount in  the tank. 
 In many tanks it seems there is a shortfall as N and P levels climb. If  there  was enough organic C,  the bacteria would use up the  N and P too  and tank levels would approximate nsw levels ( PO4 ca .005ppm and  NO3ca. 0.2ppm)  more often than they do. This imbalance  is the basis  for organic carbon dosing( vinegar, vodka, pellets, sugar, etc)   
Unfortunately, hobby level measurement of organic carbon is not  possible. Even high level analyses with $ 50 K  analyzers don't really  tell you what organics are present and whether they are bio available.  So, we use No3 and PO4 as sort of a surrogate measure for nutrients,  often ignoring organic carbon. 
 
The proportion of N in and N out varies vis a vie the proportion of P in  and P out too.  The bacteria , consume C,N and P  for food( ie, they  assimilate them) and in turn are exported primarily by skimming  . Even  if we assume they have a perfect 116C to16Nto1 P biomass and the food  into the tank also has these exact proportions,more N will be exported  than P.  
Anaerobic activity  where the  bacteria use NO3 for oxygen  when free  oxygen is used up  exports extra   N .  NO3 is reduced to N as the  oxygen is taken ;some of the N  which binds to other N forming N2 which  bubbles out  into the atmosphere. How much of this occurs  is variable  from tank to tank but it does deplete nitrogen in addition to the  nitrogen assimilated by the bacteria as biomass;there is no other such   exit for P . 
This is why many use gfo or other adsorbents and or precipitants  for PO4 along with organic carbon dosing.  
 
Sometimes, N levels at 0 may induce some coral paleness, perhaps from an  N deficiency for the zooxanthelae or the  coral itself. Some think  adding extra N via sodium nitrate  or calcium nitrate will remedy that  and also help the bacteria to reduce more P. Very plausible  positions,imo. Some ,including me prefer to add extra N via aspartic  acid and amino acid which also adds some organic carbon.                          
  
			
			 
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