5pacey
New member
I have not seen this discussed yet so I thought I'll bring it up. This occurred to me while reading the description of how Seachem's de*nitrate works. I do not use it but the product drew my interest, and it basically is very similar to small size live rock rubble.
Basically, we know that live rock is porous and it is the pores which provide surface are for nitrifying bacteria to live and to conduct their business of turning ammonia into nitrate via nitrite. This happens in the aerobic conditions, or IOW where oxygen is available. We also know that it is the anaerobic conditions which support the existence of bacteria which turn Nitrate into Nitrogen. There are various strains of those, some like sulphur, some like carbon to eat etc. But all of them require anaerobic conditions.
Seachem says that for de*nitrate to work you have to maintain very low flow, 50GPH or less, in order for the bacteria in the top layers of the pores to convert ammonia into nitrate with sufficient intensity as to consume all available oxygen, thus depriving the deeper dwelling bacteria of it and creating the anaerobic conditions conducive to the bacteria which convert Nitrate to Nitrogen. Thus causing the de-nitrification process.
So... given that de*nitrate essentially simulates a form of live rock... wouldn't the same principle apply to live rock as well? IOW, if we reduced the flow past a section w/live rock to say 50Gph or less, wouldn't it start functioning as a de-nitrifying filter the same way as de*nitrate is suppose to?
Spacey
Basically, we know that live rock is porous and it is the pores which provide surface are for nitrifying bacteria to live and to conduct their business of turning ammonia into nitrate via nitrite. This happens in the aerobic conditions, or IOW where oxygen is available. We also know that it is the anaerobic conditions which support the existence of bacteria which turn Nitrate into Nitrogen. There are various strains of those, some like sulphur, some like carbon to eat etc. But all of them require anaerobic conditions.
Seachem says that for de*nitrate to work you have to maintain very low flow, 50GPH or less, in order for the bacteria in the top layers of the pores to convert ammonia into nitrate with sufficient intensity as to consume all available oxygen, thus depriving the deeper dwelling bacteria of it and creating the anaerobic conditions conducive to the bacteria which convert Nitrate to Nitrogen. Thus causing the de-nitrification process.
So... given that de*nitrate essentially simulates a form of live rock... wouldn't the same principle apply to live rock as well? IOW, if we reduced the flow past a section w/live rock to say 50Gph or less, wouldn't it start functioning as a de-nitrifying filter the same way as de*nitrate is suppose to?
Spacey