Sulfur is a chemical element with the symbol S and atomic number
16. It is abundant, multivalent, and nonmetallic. Under normal
conditions, sulfur atoms form cyclic octatomic molecules with a
chemical formula S₈
- Major sulfur (S) inputs to soils originate from organic litter
deposition and animal droppings. Most of this deposited S is
organically bound (organo-S).this organic sulfur mineralised by
fungi and bacteria and made available for plant uptake in form of
sulfate.
- Sulfur mineralization is a microbial driven decomposition which
changes organic to inorganic forms.
- In acid soils sulfate adsorption essentially
involves the chemistry of Fe and Al. The hydrous
Fe and Al oxides tend to form
coordination complexes due to the donor properties of oxygen. The
amount of sulfates adsorbed depends on the number of
one-coordinated FeOH and AlOH sites,the surface area of
adsorbent,the pH of the system.
- sulphate occurs as a co-precipitated or co-crystallized
impurity in the calcium carbonate.Sulphate adsorption was found to
be negligible above pH 6.5 and adsorbed sulphate may be determined
by aqueous extraction after increasing the pH above this value by
addition of solid calcium carbonate.
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