In chemistry, iron(III) or ferric refers to the chemical element iron in its +3 oxidation number. Ferric chloride is an alternative name for iron(III) chloride (). The adjective ferrous is used instead for iron(II) salts, containing the cation Fe2+. The word is derived from the Latin word , meaning "iron".
Although often abbreviated as Fe3+, that naked ion does not exist except under extreme conditions. Iron(III) centres are found in many compounds and coordination complexes, where Fe(III) is bonded to several Ligand. A molecular ferric complex is the anion ferrioxalate, , with three bidentate oxalate ions surrounding the Fe core. Relative to lower oxidation states, ferric is less common in organoiron chemistry, but the ferrocenium cation is well known.
Iron(III) in biology
All known forms of life require iron, which usually exists in Fe(II) or Fe(III) oxidation states.
Many
in living beings contain iron(III) centers. Examples of such
include
oxyhemoglobin,
ferredoxin, and the
. Many organisms, from bacteria to humans, store iron as microscopic crystals (3 to 8 nm in diameter) of iron(III) oxide hydroxide, inside a shell of the protein
ferritin, from which it can be recovered as needed.
Insufficient iron in the human diet causes anemia. Animals and humans can obtain the necessary iron from foods that contain it in assimilable form, such as meat. Other organisms must obtain their iron from the environment. However, iron tends to form highly insoluble iron(III) oxides/hydroxides in aerobic () environment, especially in . Bacteria and graminaceae can thrive in such environments by secreting compounds called that form soluble complexes with iron(III), that can be reabsorbed into the cell. (The other plants instead encourage the growth around their roots of certain bacteria that redox iron(III) to the more soluble iron(II).)[H. Marschner and V. Römheld (1994): "Strategies of plants for acquisition of iron". Plant and Soil, volume 165, issue 2, pages 261–274. ]
The insolubility of iron(III) compounds is also responsible for the low levels of iron in seawater, which is often the limiting factor for the growth of the microscopic plants (phytoplankton) that are the basis of the marine food web.
Iron(III) salts and complexes
Typically iron(III) salts, like the "chloride" are
with the formulas . Iron(III) nitrate and iron(III) perchlorate are thought to initially dissolve in water to give ions. In these complexes, the protons are acidic. Eventually these complexes
hydrolysis producing iron(III) hydroxides that continue to react, in part via the process called
olation. These hydroxides
precipitate out of the solution or form colloids. These reactions liberate
hydrogen ions lowering the pH of its solutions. The equilibria are elaborate:
The aquo ligands on iron(III) complexes are labile. This behavior is visualized by the color change brought about by reaction with thiocyanate to give a deep red thiocyanate complex.
Iron(III) with organic ligands
In the presence
chelation ligands, the complex hydrolysis reactions are avoided. One of these ligands is
EDTA, which is often used to dissolve iron deposits or added to fertilizers to make iron in the soil available (soluble) to plants.
Citrate also solubilizes ferric ion at neutral pH, although its complexes are less stable than those of EDTA. Many chelating ligands - the
- are produced naturally to dissolve iron(III) oxides.
Iron(III) complexes with 2,2'-Bipyridine|1,10-phenanthrolinebipyridine] is soluble and can sustain reduction to it iron(II) derivative:
Iron(III) minerals and other solids
Iron(III) is found in many minerals and solids, e.g., oxide (hematite) and iron(III) oxide-hydroxide are extremely insoluble reflecting their
polymer structure.
Rust is a mixture of iron(III) oxide and oxide-hydroxide that usually forms when iron metal is exposed to
humidity air. Unlike the passivating oxide layers that are formed by other metals, like
chromium and
aluminum, rust flakes off, because it is bulkier than the metal that formed it. Therefore, unprotected iron objects will in time be completely turned into rust.
Bonding
Iron(III) is a d
5 center, meaning that the metal has five "valence" electrons in the 3d orbital shell. The number and type of ligands bound to iron(III) determine how these electrons arrange themselves. With so-called "strong field ligands" such as
cyanide, the five electrons pair up as best they can. Thus
ferricyanide ( has only one unpaired electron. It is low-spin. With so-called "weak field ligands" such as
water, the five electrons are unpaired. Thus
aquo complex ( has only five unpaired electrons. It is high-spin. With chloride, iron(III) forms tetrahedral complexes, e.g. (. Tetrahedral complexes are high spin. The magnetism of ferric complexes can show when they are high or low spin.
See also
-
(Iron(III) chloride)
-
(Iron(III) oxide)
-
(Iron(III) fluoride)
