Calculation of CEC
The CEC is the number of positive charges that a soil can contain. It is usually described as the amount of equivalents necessary to fill the soil capacity. In soil science, an equivalent is defined by the number of charges in terms of a given number of hydrogen ions. As hydrogen ions have only one positive charge (H+), this makes calculations relatively simple. An equivalent of Al3+ would have one third as many ions for the same amount of charges, and Ca2+ would have half as many ions.
Translation from meq/100g to an every day unit, like lb/acre of available nutrients, can be made via calculation, that considers the atomic weight, the ion's valence, and by estimating the soil depth and its density. Mengel gives the following correspondence for 1 meq/100g:
Calcium, 400 lb/acre
Magnesium, 240 lb/acre
Potassium, 780 lb/acre
Ammonium, 360 lb/acre
Read more about this topic: Cation-exchange Capacity
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“To my thinking boomed the Professor, begging the question as usual, the greatest triumph of the human mind was the calculation of Neptune from the observed vagaries of the orbit of Uranus.
And yours, said the P.B.”
—Samuel Beckett (19061989)