You have kind of a good point here. The problem though, is that the 'hair roots' that accomplish most of the adsorption of minerals and water are actually extensions of single cells (one of those little bubbles in this picSo, keeping that scale in mind, the root tip is about as wide as the entire DE picture (the small inset in my version) -- it seems unlikely to me that root hairs are going to be fitting into any of the "tube" structures in DE.
The thing is, we're not talking about the moment when the particle is fractured. Long before that, it is pierced by the root - it is like a marshmallow on a stick, perfectly intact, other than the root sticking through it. So, again, unlike our other inorganic components, the root is finding a pathway through the akadama long before it cleaves it.I'm betting that at some scale larger than 10 microns, akadama clay has weak cleavage bonds for some reason, so turgid root tips are able to apply sufficient wedge pressure (as opposed to say, needing huge iron wedges, as in the granite video).
Absolutely, and I hope you don't think I was condemning you. I was just reporting what I have learned and observed first hand. I find this whole discussion interesting.As viewers though we should engage in discussion to further the horticultural science and ultimately further the art of bonsai. Not blindly listen and condemn others when they say new or conflicting ideas.
I take it all with a 'grain-of-salt', as 'they say'. I think you should too.Again I am not doubting Ryan on his method or results.
@milehigh_7 any progress on getting the coarse, larger particle size of the DE from the supplier in your area?
When I started bonsai in the 1980's I didn't know about bonsai clubs so relied on books from the 60-70s. Back then the book mix was 1 part sand, 1 part peat moss, and one part loam/soil/leaf mould or what have you. But you know what, my trees lived and . By the time I found the bonsai club (San Francisco 1990-2006) the popular mix was aquarium sand, red lava, fine fir bark and a little soil. Over time we tried replacing various ingredients such as expanded shale, decomposed granite, pumice, for a while everyone was using black lava instead of red. Then came akadama. Someone could say it was better for a tangible, scientific reason. So we all started putting it in our mixes. By then the soil was dropped and fir bark stayed in for a while (I still put a bit in for my deciduous trees), then came the "Boon Mix". A much simpler mix that seems to work well for most. The point of all of this is we learn and change over decades. Right now diatomite rock/DE seems to be all the rage and again there seems to be some scientific evidence in favor of it. I just bought a bag and am going to try it. Akadama seems to be having a good run, like red lava, the longevity of these are much better, so I'm guessing they are pretty good media. We learn and improve and try new things. Someone is going to find that Mt. Hood akadama and blow us all away with how great it is. I can't wait to try it! The trees may like it. Still, I think Walter Pall has a point, "the trees don't care". I might add "that much."
Oeh, I like that suggestion.All this discussion is widely superfluous. The energy could be spent on discussing how to make more artistic bonsai.
Agreed, same here.
To discuss soils the way it's done here recently is like having a cooking forum and then 90% of the discussion is about the chemical and physical properties of certain food ingredients. All this discussion is widely superfluous. The energy could be spent on discussing how to make more artistic bonsai.
Holding the tree, by the trunk over a nutrient solution that is being vigorously airated. Close enough that thd mist from the bursting bubbles could wet the roots but not IN the solution. Not sure how you would fit a pot in that setup...My main thought is that maybe it would be great if we had a medium that could maintain a monolayer of water molecules on the surface of hair roots
The energy could be spent on discussing how to make more artistic bonsai.
SUPER!!!Yes, actually they are working on a new size right now. I am going to call tomorrow and get some specifics. The one I have samples of right now ranges from 3/16 to 5/16. I am hoping they can take that bottom screen size down one to 1/8" I will let you all know. Then the question will be how to get it out to everyone...
I know. BIG difference, but it confuses people. At least make 'diatomite rock."It's exactly the same just a different size.
Is it feasible the breakdown of Akadama is at least in part due to freeze / thaw expansion and contraction rather than root action? If those tunnels are full of water and it freezes then it surely would split the particle at that point. It would be so amazing if an in depth study of the various common substrates were done in relation to how roots interact with each.Thank you for those images, @sparklemotion. I am fairly certain the division and breaking of akadama pieces is NOT attributed to roots entering tiny tubes which are then expanded and fractured by growing roots. I agree with your hypothesis that there is some interaction at the macro level that allows the unfired akadama to split apart.
Those SEM images of akadama are terribly small and do not show anything. Looks like there's some networking and structure present but the scale bar is unreadable.
Another thing to clarify is that the SEM image of the diatomaceous earth is depicting a diatom. One diatom. One of many shapes diatoms come in. It just so happened that diatom has a cylindrical tube like structure but is not indicative of DE as a whole. Also diatoms are immensely small. Some down to 2 microns in size meaning those tubes and networking are even smaller.
Again I am not doubting Ryan on his method or results. I am confident it is how he says. Except he want to present his information in a scientific manner. He's big on explaining and showing why things work instead of just telling people this is the way and because I said it it's right. I respect Ryan for that. But if he's going to engage in a scientific discussion it means to share knowledge and test ideas. If he just wants to blindly preach I can't respect him for that but I don't think he's doing that. He explains things best to his knowledge and openly admits areas he lacks it in.
As viewers though we should engage in discussion to further the horticultural science and ultimately further the art of bonsai. Not blindly listen and condemn others when they say new or conflicting ideas. Discussion can be so valuable but all I see on the different Facebook groups is people parroting the same conventions and putting down anyone who says otherwise. Admittedly some new comers did not put in their research and are asking dumb questions they could of solved on their own. The bigger picture I'm getting at is the kind of attitude we want to foster to help grow and develop the bonsai community.
Also as someone who has been fairly involved in the scientific community the past few years and have seen people work their ass off with insane hours to test, prove, and share their ideas. If you're going to claim the title of science and start using for itself then you better respect how science is built and works. Doing otherwise is an affront to the whole scientific community.
I did find my SEM images of pumice. I am fairly certain akadama is a pumice derived material. Some geological process I don't have any knowledge in transformed it into akadama. Let's just assume though that akadama does bear a similar networked porous structure as pumice. You look at the images yourself and measure the tunnel size with the scale bar. Compare that to the root meristem @sparklemotion shared and you'll quickly realize that the roots are at best barely the size of the opening with most tunnels significantly smaller than the roots. I think there is too much emphasis on the tube structure Ryan mentioned and may be misguiding. It's good that we are looking into the interaction between roots and soil though. Good understanding of the fundamental science can bring out techniques that may help us with bonsai.
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I just finished with Ryan's Q&A stream from today and I was able to ask him a couple questions about his DE comments from his live stream last week. First, the name brand horticultural grade of DE he's currently testing is AXIS - https://epminerals.com/products/axis-soil-amendment I did a quick Google search and unfortunately I wasn't able to find a spot to purchase any to try.
I also asked Ryan about the differences between horticultural grade and products like NAPA 8822 or Optisorb. He said it was about particle size and having the correct size to maintain a proper level of water & oxygen. For Ryan the proper particle size is 1/4" to 1/2" for the bottom air layer/drainage layer, and 1/16" to 1/4" for the interior soil.