@Waira I would LOVE to elaborate! (now I get to talk about solution chemistry and geology related to growing weed
)
You are correct on the post burn of the rice hulls.. the first step is to get rid of the organic matter but this unfortunately does not give a soluble SiO2. I put a pic of the reaction diagram for silica polymerization, the full peer reviewed article can be found here for reference
https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3334419/
I have drawn in the colors to make it easier to talk about the process.
In step 1 (red) you see a reversible equilibrium reaction of H2O + Si(OH)4 <->(H3O+) + Si(OH)3O-, where ortho silicic acid (OSA) donates a proton (H+) to a water molecule producing hydronium ion (H3O+) which is an acid, and the conjugate base form of OSA (Si(OH)3O-).
In step 2 (blue) you see a reaction where the negatively charged oxygen forms a bond to the central Si atom of another molecule of OSA while at the same time, one of the OH groups on the second OSA molecule breaks its bond to Si and pulls the proton away from H3O+ making 2 molecules of H2O. This last reaction is OH- + H3O+ -> 2H2O. At the end of step 2 you have a dimer form of silica and you can imagine how it goes from there.
I circled the hydronium ion #3 in purple because this is an extremely important part of the system. At a high pH the concentration of the acidic hydronium is kept very low which prevents this polymerization in concentrated silica supplements!!! Once the silica is mixed into your feedwater and diluted this reaction does not take place because the low concentration provides enough physical separation that they don't contact each other often enough.
From the same paper directly below figure 2, "
Many factors affect the process of silica condensation from the molecular level upwards including concentration, temperature, pressure, pH and the presence of other ions, small molecules and polymers [1 and many subsequent reviews, including 2, 7] but in all cases the materials that form are amorphous on the 1nm length scale and are built up from SiO4 tetrahedra with variable Si-O-Si bond angles and Si-O bond distances.
The materials contain hydroxyl groups (some will be present as Si-O-) and according to the reaction environment in which the mineral forms, silica from different organisms/ precipitation conditions can vary greatly with regard to density, hardness, solubility and composition [
8]. "
Now for a real world example, NOTE: this is why you never want to mix concentrated nutrients!!
I took ~3ml of Core A and diluted it to ~30ml with tap water and then added a few drops of Bio-Si. These pics were taken over a total 5 min period so you can see this is a fairly fast process. When exposed to the lower pH and Mg2+ the silica almost immediately polymerized forming a white gelatinous blob. I poured out the liquid and refilled the cup with water. As you can see this silica does not re-dissolve and has been taken out of your nutrient solution (literally).
This is why you should always add silica supplements to your reservoir first and make sure they are thoroughly mixed before adding other nutrients. When topping off a reservoir that already has nutrient solution its best to add your silica to some plain water before putting it in so it is pre-diluted and less likely to react.