coralreefdoc said:
this isn't innovative/cutting edge, by any means
Indeed. After I very excitedly mooted the idea of a cyano scrubber on another forum last year, I discovered that the aquaculture industry has been hip to this for years -- you can even buy cyano to seed your system with nowadays. We're clearly well behind the curve, here.
Stuff like this is why marine biologists point at us and laugh.
elegance coral said:
There is a balance in nature between nitrogen fixing and denitrification. They can both be viewed as hard work, or energy consuming processes
EC, I find your reasoning vague and unconvincing.
As noted by Barjam and myself, fixing N2 is substantially harder work than denitrification, so cyano will avoid it if possible. If it didn't, it would be outcompeted by other algae using the NO3 that the cyano is inexplicably ignoring, and cyano blooms would be uncommon, if not vanishingly rare, outside of tanks where NO3 is zeroed out and fixing N2 is the only game in town. Moreover, if your analysis were correct and cyano pulled potentially dangerous amounts of nitrogen into our systems, cyano would routinely crash any system that lacked an extensive anaerobic zone and a robust population of denitrifying bacteria living there. Which pretty much means that a cyano bloom would put the average FW tank into a death spiral...
And in any event, the point of the exercise is to export the cyano, so even granting for the sake of argument that you're right and cyano poses a risk for eutrophication by bringing additional nitrogen into the system, all that nitrogen would go down the drain when the screen is cleaned. Problem solved.
elegance coral said:
When Cyanobacteria bloom in our systems, it is a symptom of a problem.
Excellent point. Let's look at this problem more closely. Here's a deconstruction of a cyano bloom that I posted on my local MAS forum a little over a year ago...
begin repost:
I suspect that cyano outbreaks in well-run tanks with extremely low or zero measurable macronutrients are tied to nutrient levels in the substrate rather than the water. Specifically, I suspect that phosphorus accumulation in the substrate is key.
Most hobbyists are aware that cyano can fix its own nitrogen and therefore has a major competitive advantage in low N conditions. But it's more complex than that (...ain't it always?). It's not simply low N but
a low N
ratio (less than 16:1) that is advantageous to cyano. There are two ways to drop the N

ratio: either reduce N or raise P. Most hobbyists want low-N environments for the good health of our livestock and do everything we can to that end, so that's half the problem right there... The other half is that cyano can raise P by extracting it from the substrate -- or, more accurately, by creating conditions which allow P to diffuse out of the substrate at night.
In anoxic (low oxygen) and anaerobic (zero oxygen) water, a
fundamental aspect of the water's chemistry changes, permitting nutrients that aren't normally soluble to become so. Under anoxic/anaerobic conditions in the water within the substrate (known as "pore water" or "interstitial water" because it occupies the spaces between the individual grains of sand and silt) the solubility of some nutrients can be such that their concentration can potentially reach hundreds or even
thousands of times that measured in the overlying water.*
This is the source of what is colloquially known in the hobby as "the deep sand bed nutrient time bomb": at some point, the concentration of nutrients in the substrate will max out, and it will stop absorbing them. When this nutrient sink suddenly stops working, what appeared to be a balanced system will begin to accumulate nutrients and crash. Calling it a "bomb" is fundamentally misleading: nutrients aren't expelled from the substrate; rather, the substrate simply stops absorbing them. Back In The Day, this was known as "
old tank syndrome" among hobbyists. It occurs when the substrate becomes saturated with phosphorus.
The depth below the surface of a tank's substrate (or a DSB) at which oxygen becomes depleted is directly related to the grain size of the substrate. Smaller grain sizes become anaerobic at shallower depths because the grains pack tighter and interstitial spaces are smaller, which restricts the diffusion of oxygen into the substrate, and the exposed surface area per unit volume is greater, so there's more space for bacteria to colonize, and it's bacterial respiration that's consuming the oxygen. At what depth in the substrate this change in water chemistry occurs is also highly dependent on
whether or not critters are turning over the sand or mud, but the trend toward finer sand in display tanks facilitates it even in shallow sand beds. (...FYI, that's also how "miracle mud" works. And it's worth noting that some nutrients, including phosphorus, can adhere directly to substrate particles when in soluble form, so substrates with a high surface-area-to-volume ratio -- ie, a small grain size, like fine sand and mud -- make the best nutrient sinks.)
The availability of this reservoir of soluble nutrients not far below the surface of the substrate makes it a biological hot spot. It's an interface between two different environments, analogous to the intertidal zone or the littoral zone of a lake. In the wild,
mats of algae and bacteria will often grow in both FW and SW just above the substrate. These communities thrive by maintaining a pocket of anoxic water underneath the mats, allowing nutrients to diffuse up out of the substrate -- though only at night because photosynthesis oxygenates the water, and oxygen makes the nutrients (most notably phosphorus and iron, for those of you playing along at home) insoluble again. FWIW, I suspect that some freshwater aquatic plants can pull off this trick, as well.
Cyano has been a prime mover in the creation of microbial mats for billions of years, and that seems to be what it wants to do in our fish tanks, as well. That's why it doesn't like high flow, and that's why it goes away if you wait it out -- it will eventually deplete the phosphorus in the substrate, lose its competitive advantage over the other algaes in the tank, and die back. And when some critical tipping point is reached as phosphorus accumulates and population density increases, you get another cyano bloom.
--
* What's really going on is that the change in redox potential in anoxic/anaerobic conditions changes what chemical reactions are "profitable" to bacteria -- that is, it changes what reactions bacteria can extract energy from in order to survive and multiply. The highly soluble nutrients that accumulate in the interstitial water are metabolic waste products of the bacteria:
"The prokaryotes (bacteria) comprise the bulk of the biomass and chemical activity in sediments. ... The characteristic
vertical nutrient (electron donor and electron acceptor) profiles seen in sediments are produced as a result of microbial activities, with each nutrient a product or reactant of one or more metabolic groups."
SEDIMENT BACTERIA: Who's There, What Are They Doing, and What's New?
Annual Review of Earth and Planetary Sciences
Vol. 25: 403-434 (Volume publication date May 1997)
DOI: 10.1146/annurev.earth.25.1.403
--
And we conclude tonight's lecture with the obvious Q: Okay, Mr. Smarty-Pants, if cyano likes low N

ratios, will raising N make it go away?
A: Yes, it probably will. Hardcore saltwater hobbyists may not be aware of this, but there's a management method for FW planted tanks called estimative index dosing which calls for maintaining a low level of N because if you permit the plants to suck all the N out of the water, you open the door to a cyano bloom.
Of course, raising N in an aquarium that isn't densely planted opens the door to a bloom of green algae, so if you're the type who likes to mess with water chemistry, you might try concurrently raising dissolved silicon to encourage a diatom bloom, instead. They'll outcompete green algae for P at high Si

ratios, and pretty much all your friendly neighborhood algae eaters totally heart diatoms. Though on the other hand, diatoms colonize microbial mats and may have a symbiotic relationship with cyano, so this tactic could massively backfire...
Back to the drawing board, then.
I'm not a devotee of EI dosing, but I can't help but notice that the goal of that system is to maintain 20-30 ppm N and 1-3 ppm P, and 1-2 ppm P would be close to the magic N

ratio of 16:1 that's the break point between cyano and green algae. Get down below 10:1 and cyano has the edge; get much above 20:1 and green algae has a competitive advantage. But if you stay close to 16:1, neither group of algaes can get ahead of the other. Of course, allowable nutrient concentrations are much lower in a reef tank, but the magic ratio should be the same, as FW algaes are all descended from species that evolved in SW. And note that
16:1 is part of the Redfield ratio of C:N
-- 106:16:1.
Something to think about, at any rate.
NOTES FOR REEF CENTRAL REPOST: (1) Turns out that your friendly neighborhood algae eaters only heart diatoms if the Si:N ratio is around 1:1 (...the standard "recipe" marine biologists use to trigger diatom blooms for experiments in NSW is an Si:N
ratio of 16:16:1, or an Si:N ratio of 1:1). Given more Si, diatoms will grow thicker and spikier silica armor. Their demand for Si will be saturated at an Si:N ratio of 3:1 (48:16:1 Si:N
), and the resulting diatoms will be all but inedible to zooplankton. (2) Also, I think my analysis of EI dosing was wrong in my original post -- I found Mr. Algae's blog when I was Googling for stuff to support what I had written, and I didn't read it closely enough to pick up on the "Buddy Ratio"... Still works, though: EI recommends 5-30 ppm NO3 and 1-3 ppm PO4 to restrict algae growth in FW planted tanks, and the upper ends of those ranges perfectly correspond to the ideal Buddy Ratio of 10:1. Assuming "average" NO3 of 17.5 ppm and 2 ppm PO4, that's a Buddy Ratio of 8.75 -- well within the recommend range. (3) Just to be clear, I do NOT advocate dosing N to fix a cyano bloom in a reef tank, as messing with macronutrients is way too risky IMHO. To err is human, after all... (4) FWIW, I tried to post a detailed explanation of how and why PO4 accumulates in anaerobic sediments as part of an effort to tie together all the information about deep sand beds that's floating around out there, but my thread was immediately deleted without explanation. Shame -- there was some good information in there, and this seemed like the appropriate place to share it.
/repost
Note, however, that this model doesn't specifically address the OP's cyano bloom, which is in a new system, not a mature one. Here's how cyano blooms work in new reef tanks...
The porous anaerobic interior of LR is a potential PO4 sink, like any anaerobic zone. In the wild, PO4 doesn't accumulate because nutrient levels are normally very low. However, while being cured, the dieback of inverts releases phosphorus, some of which ends up sequestered within the LR as orthophosphate (PO4). When placed in a new system with freshly mixed water and virgin substrate that contains little or no phosphate, some PO4 will leach out of the LR to bring it into chemical equilibrium with the water column. As the tank cycles, bacterial growth will draw down PO4 from the water, which in turn leaches more from the LR to maintain equilibrium.
Because any anaerobic substrate is a potential P sink, cycling a tank will establish new places for phosphorus to hide -- and because nature abhors a vacuum, it very much wants to hide there... This means that the slow flux of PO4 out of the LR will continue even after demand by the bacterial community falls off when the tank is fully cycled. This is the nutrient flux that cyano is exploiting in new tanks.
dg3147, I suspect I can explain why your success with this tactic was so rapid -- that is, why the cyano didn't come back when you lifted it off the substrate by giving it somewhere else to grow -- but doing so would require making reference to information I previously posted in the thread on DSBs and phosphorous sequestration that was deleted. I'm afraid to share any of the information in that thread without the express written consent of the mods, as I have no idea why it was deleted...