Iodate

Polyatomic anion (IO3) with charge -1


title: "Iodate" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["halates", "iodates"] description: "Polyatomic anion (IO3) with charge -1" topic_path: "general/halates" source: "https://en.wikipedia.org/wiki/Iodate" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Polyatomic anion (IO3) with charge -1 ::

|ImageFile=File:iodate anion.svg |ImageCaption=The iodate anion, |ImageFile1=iodate-3D-vdW.png |ImageCaption1=Space-filling model of the iodate anion |Section1={{Chembox Identifiers | CASNo = 15454-31-6 | ChEBI = 29226 | ChEBI1_Comment=(class of salts) | ChEBI1 = 24856 | ChemSpiderID = 76615 | Gmelin=1676 | PubChem = 84927 | UNII = 877S7T6EXV | StdInChI=1S/HIO3/c2-1(3)4/h(H,2,3,4)/p-1 | StdInChIKey = ICIWUVCWSCSTAQ-UHFFFAOYSA-M | SMILES = [O-]I(=O)=O |Section2={{Chembox Properties | I=1|O=3|Formula_Charge=− |Section8={{Chembox Related | OtherCompounds=Periodate, Fluoroiodate, Bromate, Chlorate

An iodate is the polyatomic anion with the formula . It is the most common form of iodine in nature, as it comprises the major iodine-containing ores. Iodate salts are often colorless. They are the salts of iodic acid.

Structure

Iodate is pyramidal in structure. The O–I–O angles range from 97° to 105°, somewhat smaller than the O–Cl–O angles in chlorate.

Reactions

Redox

Iodate is one of several oxyanions of iodine, and has an oxidation number of +5. It participates in several redox reactions, such as the iodine clock reaction. Iodate shows no tendency to disproportionate to periodate and iodide, in contrast to the situation for chlorate.

Iodate is reduced by sulfite: : Iodate oxidizes iodide in acidic conditions: : Similarly, chlorate oxidizes iodide to iodate: :

Iodate is also obtained by reducing a periodate with a sulfide. The byproduct of the reaction is a sulfoxide.

Acid-base

Iodate is unusual in that it forms a strong hydrogen bond with its parent acid: : The anion is referred to as biiodate.

Principal compounds

Natural occurrence

Minerals containing iodate are found in the caliche deposits of Chile. The most important iodate minerals are lautarite and brüggenite, but also copper-bearing iodates such as salesite are known.

Natural waters contain iodine in the form of iodide and iodate, their ratio being dependent on redox conditions and pH. Iodate is the second most abundant form in water. It is mostly associated with alkaline waters and oxidizing conditions.

References

References

  1. Lyday, Phyllis A.. (2005). "Iodine and Iodine Compounds".
  2. {{Greenwood&Earnshaw2nd
  3. Qiu, Chao. (2005). "Distribution of Thioethers in Hydrotreated Transformer Base Oil by Oxidation and ICP-AES Analysis". [[Industrial & Engineering Chemistry Research]].
  4. "Radiological Protection Institute of Ireland | | Media | Press releases | Radioactivity released from Wylfa nuclear power plant is extremely low and of no health significance".
  5. "Decision to Discontinue the Future Distribution of Iodine Tablets".
  6. (1956). "The stability of potassium iodate in crude table salt". [[Bulletin of the World Health Organization]].
  7. "Home".
  8. (13 December 2013). "Iodine (including PVP-iodine) Product types 1, 3, 4, 22 (EU 528/2012 assessment)".

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halatesiodates