Here is another link, talks about gluconate sources and amounts to mix etc. : viewtopic.php?f=11&t=9696&hilit=gluconate
Also with iron we understand that it is very quickly locked up by phosphate when it goes in the water. Hence high iron and phosphate = milky water.
because TPn+ has very low levels. Plus other acids .....
The overall message I am reading from Tom and others in these threads (and more I haven't linked to) is that they use a mixture of gluconate which has a very very weak bond and then different chelators. The gluconate is readily available almost instantly on entry to the water but then is locked up very quickly. However the plants get their fed. Then the other mixture of chelators break down at different rates. The overall effect is like a drip feed where the plants get multiple fixes from the one dose as each different chelator breaks down.
The cloudiness is caused by insoluble compounds (possibly the milkiness is calcium phosphate), and iron will both oxidise (with Fe3+ ions and precipitate as rust) and react with phosphate to give insoluble iron phosphate complexes. This is Fe availability against pH for a range of plant nutrients (it is in the soil so a more complex situation, but the same basic principle holds)The KH/Ph plays a part in the break down of the chelators so where you have a low KH the gluconate is usable for longer where when the KH is higher (for most of us) then the chelators are more useful.
dw1305 said:Hi all,
Neither elemental iron (iron fillings) or iron oxides "rust" will work effectively as an iron source. The only compounds that will work are ones which disassociate into Fe2+ (ferrous) or Fe3+ (ferric) ions in solution.
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