Mike, sorry have been slow on some questions
This will be long with some new info, never mentioned on ZEO threads, or in this hobby, as far as I know
First, and for you, while doing a search for Reedman I ran into this article which has been brought up, which stared all the arguing. It is this article that is full of a lot of nonsense. My analogy to the watermelon and a Mac truck, with trailer. So if anyone wants to know why let me know
http://www.wetwebmedia.com/ca/cav1i3/zeovit/Zeolite_Filters/Zeolite_Filters.htm
ammoniated
It may help accelerate things in the beginning. Bacteria can do some amassing things to a point (see below). However, I still find this so called ionic exchange theory amusing. Lets assume there is nitrification and denitrification going on the zeolite like LR or SB and there was some ammonia in the zeolite do to ionic exchange from FRESH zeolite. Bacteria do their thing and do what, coat the zeolite. We now have PA, both nitro and dentiro going on. As I said in the other post the denitro's are going to be the inner layer and it is the outer layer, the nitro's, that need the ammonia, just like LR or SB.
One would have to suggest that the denitro's are some how pulling the ammonia off the ion site, replacing it with something and then passing the ammonia right through itself to the nitro's. Why, what for, when the nitro's have all the ammonia they need in the water column. Nitro's excrete NO3- to the denitro's but denitro's only excrete things like N2 gas or sulfides (which may get passed to the zeolite) to the water column. And for sure we do not want the OAB (Obligated Anerobic Bacteria) doing their thing to any degree, which can take place in a poor SB. You expose these guys to O2 and things in your tank will be dead.
But there is more than meets the eye here
You are always told that denitro's use NO3- and convert it to N2 gas ( you kinda see that above). This is not always the case. Some denitro's, as I alluded to in the other post can produce their own FAD environment. Such bacteria often do not need NO3- at all, the can use ammonia as their N source and excrete N2 gas
. Which means what, you do not always need a two layer system, some dentrio's can do it all :lol:
There is also indications that Mn++++ can oxidize ammonia to N2 and that NO3-can be reduced by Mn++ to N2. Then there are other bacteria that can reductively dissimilate NO3- to ammonia. So in short, ammonia can be altered by a number of processes and producing a variety of products. Bacterial biogeochemistry is a very complicate issue and fills pages in such books as;
Bacterial Biogeochemistry: The Ecophysiology of Mineral Cycling
Microbial Ecology of the Oceans
So where does that leave me ? There is not ionic exchange going on between the zeo and the bact's. And for the sake of argument, if there was how would the zeo recharge itself, when, it is still coated with bact's. The bact's would have to pull elements out of the water column and by magic put these ions back into the zeolite, only to pull them out by ion exchange,. Pretty much nonsense. The only alternative is that the bact's are dissolving the zeo and pulling things out. So what would those be, that they would need ?
Chemical comp of Clino's
(Na, K, Ca)2 - 3Al3(Al, Si)2Si13O36-12H2O, Hydrated Sodium Potassium Calcium Aluminum Silicate
What would the bact's possible assimilate out of that other than water. If you go to the index of my two books the elements, Na, K, Ca, Al, Si, are not even in the index, so what does that tell you ? Although bact's can process things with these in them, they have no need for them. Into the zeo for ionic exchange and for what and are they going to pull out ?
Reedman
No I do not have access to that, it is a PH.D thesis. However, there are one or two on line articles that discuss seawater and the use of zeo's in regards to ammonia uptake. Lets assume that ammoniated zeo's or zeo's that have a high affinity in seawater for ammonia, would benefit these bact's. So what it would be short lived and you would have to replace the zeo. It can not recharge itself and is nonsense for the bact's to be capable of recharging it only to pull those same ions right back out again. Neither of my two books even remotely make a remark that bact's do/can ionic exchange with a media. I think some people are trying to compare plants and bact's.
I see Mojo posted a link for you
I almost for got Invin
It is my theory that the concentration of NH4 will be stronger around the zeolite rocks since NH4 is strongly attracted around this area because of the "magnet" the zeolite has for NH4.
How could that ever take place when the rocks are covered/coated with bact's ? It would have to be a virgin site, like new zeo. Tumbling will not create that.NH4+ is a weak "magnet", compared to the likes of Ca++, Mg++, etc.