IMO, that is a wild and baseless claim.
you really think there is so much hydrogen sulfide present that it dominates nitrate export over processes such as denitrification involving oxidation of organics?
This is from one of my articles, describing the process:
In the absence of O2, and taking the nitrogen species completely to N2 (which may happen in several reaction steps), we have the following overall reaction:
organic + 124 NO3– + 124 H+ → 122 CO2 + 70 N2 + 208 H2O
You believe that reactions involving hydrogen sulfide dominate over that one?
I am claiming nothing, just explaining how things work, based on approved information, available for consultation.
The process you talk about takes place only in anoxic conditions.( <0.5 ppm O) In a normal nitrifying biofilm most nitrate is exported in the oxygen transition zones. The formula you use is about anaerobic remineralization of organics, using nitrate as an oxygen source. When no nitrate is available manganese, iron and sulfate is used, In a marine aquarium sulfate is always available.
In a healthy and balanced nitrifying biofilm little nitrate becomes available in anoxic zones because it is used up in the transition zones for oxidizing H2S produced by anaerobic remineralization. Sulfur Bacteria following an anaerobic pathway are active in oxygen transition zones, and are able to switch between an aerobic pathway and an anaerobic pathway, using up available oxygen oxidizing sulfur compounds aerobically, using up nitrate oxidizing H2S and produced S anaerobically, creating conditions suitable for anaerobic remineralization, a minor but essential process in a nitrifying biofilm. This way nature closes the cycles. if more nitrate is used up in transition zones, less nitrate becomes available for anaerobic remineralization producing more H2S. If more H2S is produced more nitrate is used to oxidize it and less nitrate will become available for heterotrophic denitrification. An equilibrium may be established in relation to the available nitrate. Hereby again emphasizing the importance of nitrate production.
OM + 59H2SO4 → 106CO2 + 16NH3 + H3PO4 + 59H2S + 62H2O. Ammonia is produced providing the nitrogen source for new autotrophic growth in the oxygen transition zones. You do believe heterotrophic denitrification is dominant over that one?
The same takes place in the aquarium in places with very little water exchange, oxygen is consumed, first nitrate and sulfate are used for anaerobic remineralisation of organics. Some H2S is produced and is oxidized using nitrate present in the oxygen transition zones. Less nitrate becomes available for anaerobic remineralisation, more sulfate is reduced and more ammonia becomes available for maintaining growth, autotrophic growth needed to oxidize produced H2S, producing sulfur. Nature keeps all processes going. This in normal conditions.
There is no reason to believe that anaerobic remineralization using nitrate is a dominant process for exporting nitrate in normal aquarium conditions. It has been shown in normal aquarium conditions a biofilm exports +- 16 % of in the biofilm produced nitrate. It has been shown adding some elemental sulfur does increase the natural nitrogen export rate. ( it may reach +80% using
BADES rolls at a supply of 100 mg/l NH4-N per day ) this in normal aquarium conditions.
Your opinion the natural nitrogen export is mainly based on heterotrophic denitrification?
Is it what reefers must believe? No elemental sulfur is produced in a marine aquarium because it is a minor process without any importance for reefers?