DeeDeeK,
Measuring CO2 directly is pretty easy with a ph & kh test kit.
I found this
article on measuring O2 level in water, though it requires some additional stuff.
Absolutely! However, Anoxia and I both seem not to have access to the right test kits (my case is due to improper circulation of currency through the DSB I call my wallet(yes, there is mulm at the bottom of it)). Additionally, an measure of concentration alone will not tell us if the fish are receiving too much or too little O2 or CO2; the behavior of the fish can be correlated with the concentrations of those gasses or with conditions conducive to adequate, inadequate, or excessive levels of said gasses. Hence the examination of fish to see whether they're gasping or happy with various circulation scenarios.
I'd MUCH prefer to just use a couple of test kits! Thanks for the info and the links!
I have a question: one of the alleged benefits of a DSB (as I understand it) is reducing nitrogen compounds with anaerobic bacteria. In my simple mind, there is a paradox that I can't resolve with this scenario. First, it seems to me that the exchange of water through the DSB would seem to be non-existent deep in the bed. There is no real mechanism for that to happen. But, let's assume that there is some interface level where there is ample flow to feed in fresh supplies of nitrogen and other compounds needed, but deep enough to be anaerobic. Wouldn't the same flow that pulls the nitrogen compounds to the anaerobic interface also carry with it dissolved O2, which would, by definition, make it not anaerobic? Or is there some process by which O2 is pulled out at it descends through the sand bed and is mostly void of oxygen before getting to the interface?
H2O molecules will circulate only very little, if at all, in the sand bed because there is nothing driving it to move. However, if a compound such as NO3 or H2O is present in one area and less or non-present in another, both areas being within the same body of water (let's say a body with no circulation), molecules will tend to move into the area where they are absent or present in lesser concentration until there is an even concentration. So, water molecules will move within the sand bed in one direction while a solute moves in the opposite. There, a VERY simplistic but accurate description of my personal mis-understanding of diffusion, partial pressure, etc. Just think that all molecules of any one kind within any one medium (water or air for example) want to go everywhere in equal numbers relative to one another and exert pressure against any barrier holding them back from regions where there are fewer of their own kind so they'll spread evenly throughout. If there were much actual movement of water, flow through the sand bed, it would interfere with regions usefully segregated by oxygen concentration from establishing themselves with their various bacterial entourages.
I know what I'm saying has been more clearly put by Anorth_UK but sometimes it's useful to read it put differently in a different "voice," so I hope this posting is more helpful than the inaccuracies contained herein are harmful.
Here's a thought: In the upper region of the DSB, the sand is looser, with larger interstices and therefor easier infiltration by solids and more rapid diffusion than the deeper regions have. Through this aerobic zone, all organic matter, dissolved or solid, on its way down must pass, where it will decay aerobically. Add to that aerobic ammonia, nitrite, sulfide, methane, or hydrogen eating bacteria (many of them autotrophs). By definition, the aerobic region is that region where there is enough O2 for aerobic metabolism, so that zone will be as deep as needs contain enough aerobic activity to consume almost all the available O2.
If the sand is loose enough and shallow enough and the supply of organics and dissolved gasses low enough, no anaerobic or anoxic zones will form. You could make a titanic aquarium with a substrate of stones the size and shape of hen's eggs but sufficient depth that the bottom is completely anoxic so long as no current is driving fresh water down into it. You could make a biofilter-type substrate bed aquarium with clay or silt as a very shallow substrate and still have nice, gooey anoxic and anaerobic zones, as well as a very shallow (I hypothesize) aerobic zone.
(You wouldn't believe the surface area of clay! Incredible, plus the particles are generally polar so bacteria really like sticking to them! I'm a ceramist and I can tell you the difference between aged clay, where bacteria have formed a thorough and gooey biofilm over all the particles, and clay freshly mixed from dry constituents can be extreme in terms of plasticity and wet strength! Massive gooey biofilm! Clay can be an extremely effective biofilter medium, but that's for another thread.)
Anyhow, given a deep enough substrate of small enough interstitial space with sufficient influx of material for the resident bacteria to oxidize, there will be underlying the aerobic region an anaerobic and possibly an anoxic region. O2 will diffuse from area A to area B at a rate determined partly by temperature and by differential in concentration as well as by the distance it must travel and the volume that may travel through that distance (through the sand bed, around grains in the limited space in between them is a twisty, narrow path) and no faster so at some point consumption will overtake supply given a long enough (deep enough) path for the O2 to travel.
Below the aerobic level, there are anaerobes which use NO3 to oxidize all sorts of things. There are heterotrophs, which use the Os they remove from NO3 to burn up sugars, proteins, oils, etc., and get their complex organic molecules from the same source as their fuel-mulm. THEN there are autotrophs, which build their own complex organic molecules from CO2, H2O, and mineral sources for the chemical elements they need like iron, sulfur, boron, etc., just as do plants except they don't use photosynthesis to power the process but use the energy they gain by oxidizing, in my favorite case, hydrogen sulfide!
So, H2S diffuses upwards from below, where sulfate reducing bacteria and bacteria anaerobically breaking down sulfur-containing organics like protein produce it. Nitrate diffuses down from the aerobic, nitrifying bacterial bed. CO2 is practically everywhere from everything in the aquarium, water is omnipresent there, and the mulm releases mineral nutrients in excess of what comes from the water and the sand. If all goes well, H2S never builds up excessively in the sand bed, nitrate is drawn down into the bed by a differential in concentration between the aerobic layer/water column and the anaerobic layer(s) and organics continue to be consumed such that the mulm becomes mineralized (and hopefully absorbed by plants) and the sand bed doesn't become clogged for a VERY LONG TIME, while becoming ever more fertile.
I must point out that the sand bed becomes more compressed as it gets deeper, so NO3 doesn't move as quickly into the anaerobic region to be consumed as, say, NH3/NH4 does into the aerobic region. A very easy balance to achieve in the freshwater DSB is one where NO3 production outstrips NO3 reduction. The more evenly meshed the sand (therefore having a smaller size range of grains) and the more spherical the sand's grains shapes are, the more resistant to compaction with depth it will be and the evener the rates of diffusion will be across depths. In other words, get pool filter sand or evenly meshed riverbed sand (rounded grains, y'know) or horse racing track sand (carefully compounded to resist compaction over repeated poundings by hooves and wheels) without needing to be constantly graded and raked). Use one of these good sands and you'll get a deeper aerobic region and excellent NH3/NH4 & NO2 removal, be less dependent on burrowing critters and plants (though I consider plants all but indispensable unless you have a DEEP DSB with really fluffy sand), and better NO3 reduction so long as the bed is deep enough.
There are theorists, I can't remember who clearly but I promise these are not "straw-men" I am knocking over, who have stated one would need either a ridiculously deep DSB or absurdly finely-grained sand to achieve nitrate reduction in a freshwater DSB. I've never found the actual source so I don't know the basis of their hypothesis but I've found casual reference to such assertions in my even more casual reading - sorry to be apocryphal with this. So I mean to say that somewhere out there, there are doubters who have presumably thought this idea through pretty well as well as many of us (and I was of this camp once) who accept as received wisdom that DSBs will not work in freshwater.
It's good to read from a person who has some clear objections/concerns and voices them so well. It provides an opportunity to rethink or think-about-in-the-first-place important basic concepts as well as their many corollaries when answering, rebutting, or even (gasp!) agreeing said objector/concerned party.
In short, thanks for the questions and objections! Great stimulus for the verbose and grandiose writer such as yours truly.
I'm thinking of making a spreadsheet with every element, concept, hypothesis, presumed fact/strong theory, or relationship between the prior items in this list in it. Why? So at least an electronic brain can hold the whole thing together and not forget what things are affected by what and how that those relationships work. I'd like to be able to see the broad picture and how it generally changes as variables are added, removed, or changed.
Please pardon the thinking "out loud," but when I'm triggered to write a bunch by what I read in a thread, I gotta do it right then! Otherwise I just fill my mind with thoughts like "what the hell is killing and eating my bumblebee shrimp and rcs shrimplets? Is it planaria? They seem to attack and sometimes kill blackworms...I wonder if there were enough of them in a bathtub and I got in ...fizzle, pop, click," or "should I reheat that beef brisket from last night for lunch today?" Oh, yes, true thought of mine.
I actually go back and cut 'n' paste my postings and my favorite postings of you, my aquariacentral friends, into long rambling documents which I refer to in further writings or other projects!