Cations are positively charged ions.
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And that was exactly the type of clay I was thinking about. I'm like how can something grow in a medium that dries so hard.Don't think of clay as what you dig out of a riverbank and use to make pottery. There are other montmorillonite clay products out there as well. They have all been chelated with humic acid.
a soil’s CEC can decrease with time as well, through e.g. natural or fertilizer-induced acidification and/or OM decomposition.
Here's how to test it ...
There's a nice explanatory passage ...
The cation exchange capacity (CEC) of a soil is a measure of the quantity of negatively charged sites on soil surfaces that can retain positively charged ions (cations) such as calcium (Ca2+), magnesium (Mg2+), and potassium (K+), by electrostatic forces. Cations retained electrostatically are easily exchangeable with cations in the soil solution so a soil with a higher CEC has a greater capacity to maintain adequate quantities of Ca2+, Mg2+ and K+ than a soil with a low CEC. A soil with a higher CEC may not necessarily be more fertile because a soil’s CEC can also be occupied by acid cations such as hydrogen (H+) and aluminum (Al3+). However, when combined with other measures of soil fertility, CEC is a good indicator of soil quality and productivity.
Cation exchange sites are found primarily on clay minerals and organic matter (OM) surfaces. Soil OM will develop a greater CEC at near-neutral pH than under acidic conditions (pH-dependent CEC). Thus, addition of an organic material will likely increase a soil's CEC over time. On the other hand, a soil’s CEC can decrease with time as well, through e.g. natural or fertilizer-induced acidification and/or OM decomposition.
I have not used that particular clay product, GF, but I imagine it's similar. You seem no more or less testy than usual.
I've been trying to wrap my head around soil CEC lately, and I barely get it, lol, but I think there lies the answer