A few chemical principles are important for you to fully understand
soil fertility and plant growth/nutrition. You should know the name, chemical
symbol, valence, and ion name of these elements.
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Terminology
Atoms of chemical elements are the fundamental units of all matter. Ions are atoms that carry an electrical charge. Positively charged ions are call cations, and negatively charged ions are called anions. The amount of this charge is determined by the number of electrons that an element has gained or lost, which indicates combining ability and is called valence. With two valence states, “ic” denotes the higher state (ferric, Fe3+) and “ous” the lower state (ferrous, Fe2+).
Atomic weight is the relative weight of atoms of various elements (C is 12.0000 g).
Soil cation exchange capacity is normally expressed as milliequivalents (meq) per 100 g soil (or cmol per kg soil). This expresses the amount of charge present. One equivalent of charge (mole of charge) is equal to 6.022 x 1023 charges, and a milliequivalent is equal to 1/1000 of an equivalent or 6.022 x 1020 charges (when dividing 6.022 x 1023 by 1000, one substrates the exponents--1023-103). Therefore, a soil that has 30 meq/100 g of cation exchange capacity has 180 x 1020 or 1.8 x 1022 negative exchange sites to which positively charged ions could be attracted (30 times 6.022 x 1020 = 180 x 1020).
Examples:
One mole of potassium ions
weighs 39 g and has 6.022 x 1023 ions, each with a single charge, or
represents 6.022 x 1023 charges.
The equivalent weight of K is 39 g.
One milliequivalent (1/1000 of an equivalent) of potassium ions weighs
39 mg (39 g/1000), and represents 6.022 x 1020 charges. Therefore, the milliequivalent weight of K
is 39 mg.
One mole of calcium weighs 40
g and has 6.022 x 1023 calcium ions, each with two positive charges.
Therefore, the equivalent weight of calcium ions is 40/2 or 20 g, which
represents 6.022 x 1023 charges. Thus, the milliequivalent weight of calcium
ions is 20 mg, which represents 6.022 x 1020 charges.
One milliequivalent of potassium
ions (39 mg) will occupy exactly the same number of negative exchange sites
in soil as one milliequivalent of calcium ions (20 mg); i.e, 6.022 x 1020
sites.
In general:
Milliequivalent weight =
atomic weight (in milligram)
(1) If a soil holds 400 mg
per 100 g of Ca ions on cation exchange sites, the soil has a CEC of 20 meq/100
g.
(2) If a soil has a CEC of 15
meq/100 g, it could hold 585 mg of K+, or 180 mg of Mg2+,
or 0.345 g of Na+.