Q: F8's Aragonite, Chem and Bacteria.. the whole 9 yards?
Posted: Tue Jun 14, 2011 7:26 pm
I'd like, if possible to contunie the discussion / education from viewtopic.php?f=2&t=27228 as there are still many many questions. The more I try to read, the more questions I ask... Isn't always the case?
From Pufferpedia:
Water Parameters: Low-end brackish water (SG = 1.005 - 1.008)
One thing that got my knickers in a knot was this document:
http://www.ncbi.nlm.nih.gov/pmc/article ... 622888.pdf
It does an excellent job of bacteria identification for both FW and Marine, but they didn't specify which bacteria reside and die off during the transition from FW to SW. The did say that SW bacteria MAY exist in FW but it is undetectable and one would infer that it is trivial. Without mentioning the SG during transition we don't know what bacteria develops at what stages. I know you mentioned in the past that there is a transition period where both co-exist, but for some reason, given the chemical reactions you mentioned, there must be a non trivial portion of SW bacteria in the tank, even at low brackish levels.
Opps ... hit the submit button instead of the preview button......
Pufferpedia states:
Minimum Tank Size: 15 US Gallons (50 liters)
Does that include a reverse flow, under gravel filter WITH aragonite?
If one is using aragonite and a RFUGF, does that change the tank requirements?
When mentioned that high bioload and low salinity systems are unique, I wonder how so? It brings me back to the original question about shared bacteria and that maybe we should be testing for more than ammonia, nitrite, nitrate, and start adding portions of a marine system as well (alk, calcium and magnesium) to satisfy both strains of bacteria.
Here is a quote on marine systems, which may or may not be applicable:
From Pufferpedia:
Water Parameters: Low-end brackish water (SG = 1.005 - 1.008)
"Marine mix at 1.003-1.005 specific gravity does not provide enough alkalinity to keep the tank stable with sufficient alkalinity."
They are also obviously referring to SW, not light/low BW, which is an entirely different biochemical system and has quite different upkeep requirements.
If this is the case and the depletion of alk, is much higher than in regular FW tanks, does that mean there is SW bacteria in there also? If not, why are we not seeing this phenomena in FW tanks? If SW bacteria is present can we neglect the Ca/ Mg and Alk triangle to aid in the stabilization of the tank?Here much (but not all?) of the bacterial component is identical to FW tanks, and nitrification is filter-based
One thing that got my knickers in a knot was this document:
http://www.ncbi.nlm.nih.gov/pmc/article ... 622888.pdf
It does an excellent job of bacteria identification for both FW and Marine, but they didn't specify which bacteria reside and die off during the transition from FW to SW. The did say that SW bacteria MAY exist in FW but it is undetectable and one would infer that it is trivial. Without mentioning the SG during transition we don't know what bacteria develops at what stages. I know you mentioned in the past that there is a transition period where both co-exist, but for some reason, given the chemical reactions you mentioned, there must be a non trivial portion of SW bacteria in the tank, even at low brackish levels.
Opps ... hit the submit button instead of the preview button......
Pufferpedia states:
Minimum Tank Size: 15 US Gallons (50 liters)
Does that include a reverse flow, under gravel filter WITH aragonite?
Assuming that one is not using aragonite and a reverse flow under gravel filter (as it is not mentioned in Pufferpedia), one would assume that an F8 would produce 2.85ppm (not sure if ppm is the right measurement to use) of Nitrite per day at 15 gallons, given a 50% water change weekly. That is a pretty big bioload, but I know that swimming space is also factored in there.This issue and its solution are unique to high bioload low salinity systems
If one is using aragonite and a RFUGF, does that change the tank requirements?
When mentioned that high bioload and low salinity systems are unique, I wonder how so? It brings me back to the original question about shared bacteria and that maybe we should be testing for more than ammonia, nitrite, nitrate, and start adding portions of a marine system as well (alk, calcium and magnesium) to satisfy both strains of bacteria.
Here is a quote on marine systems, which may or may not be applicable:
That goes back to my original "drop it in and forget about it" water management statement. There really is more we (as hobbyists) need to test for under these "unique" circumstances. Although aragonite stagnation is not new to SW enthusiasts, it is something that should be considered for new F8 owners. Possibly add this to the Pufferpedia care sheet along with recommended testing for Alk and how to adjust those levels?This a suggestion based in the knowledge that calcareous substrata can dissolve in sea water. Some people, proving that a little knowledge is a dangerous thing, propose to use that dissolution to help balance calcium and alkalinity levels.
First, sure, ANY calcareous substrate will dissolve in sea water. Provided the pH is less than 7. So, if one maintains their system so that its pH becomes acidic the calcium carbonate in it will dissolve into the water. So will the corals in it, but that's another story. Between a pH of 7 and about 7.9 a small amount of calcareous substrate will dissolve as the pH and temperatur fluctuate. This will, at times, add calcium ion to the water. At other times the calcium will precipitate out. In both nature and reef tanks this dissolution and reprecipation is small. It is not trivially insignificant, but it is not enough to add any appreciable calcium to a tank's water. Nor will it balance to any appreciable extent, alkalinity.
To get significant amounts of calcium dissolved in the water from the substrate takes an acid solution that is harmful to most reef animals. This sort of pH is, in fact, one of the major determental aspects of increased carbon dioxide accumulation in the atmosphere, and one of the factors that will result in the death of most coral reefs over the next century.
There are any number of reasonable and rational ways to maintain calcium and alkalinity, they typically involve determining calcium and alkalinity levels (both have to be determined) and then adjusting them with addition of an additive such as kalkwasser or some other product. Trying to maintain appropriate levels of calcium and alkalinity by the dissolution of sediment is imprecise, inefficient and very stressful on everything living the tank, other than that it works just fine.