Iron Corrosion Products

Only iron and steel rust. Other metals corrode. Rusting is an oxidation process. What we normally call rust is a flaky red-brown solid which is largely hydrated iron.The primary corrosion product of iron is Fe(OH)2 (or more likely FeO.nH₂O), but the action of oxygen and water can yield other products having different colors:

1. Fe₂O₃.H₂O (hydrous ferrous oxide, sometimes written as Fe(OH)₃) is the principal component of red-brown rust. It can form a mineral called hematite.

2. Fe₃O₄.H₂O ("hydrated magnetite" or ferrous ferrite, Fe₂O₃.FeO) is most often green but can be deep blue in the presence of organic complexants as shown here.

3. Fe₃O₄ ("magnetite") is black

Red-brown flaky rust	Black magnetite	Blue/green unstable rust

So, you are wondering, how did we make these experiments.

1. For the first experiment we put a 5 cm finishing nail brushed with steel wool in a test tube containing 8 mL of tap water. The picture was taken three days later.

2. The second experiment was carried out with an acidic solution containing 12% acetic acid. The second picture was taken an hour after the start of the experiment. You can produce a similar reaction with vinegar which typically contains 3% acetic acid in water. However, you will have to be more patient than we were.

3. In the third experiment a pellet of sodium hydroxide (caustic 'Drano') was dropped in the test tube of the second experiment. The test tube was capped to prevent air to react with the solution. After three hours blue rust precipitates had more or less settled out as you can see in this picture.

If you have some questions please send them to our ...and do not be surprised if we post your questions right here.

Formula	Color	Oxidation State	Structure / comments
Fe2O3.H2O or Fe(OH)3	red brown	Fe3+	a-form Hematite, b-form used in recording tapes
Fe3O4	black	Fe2+/3+	magnetite/lodestone
Fe(OH)2	blue/green	Fe2+	soluble, the color going from yellow to green and blue by changing the pH of the solution from acidic to very basic
FeO	black	Fe2+	pyrophoric

See also:Equilibrium reactions of iron in water, Iron corrosion products, Iron species and their thermodynamic data, Pourbaix diagram of iron, Rust chemistry, Rust converters, Steel corrosion

• Hematite Rose is a circular arrangement of bladed crystals giving the appearance of the flower of a rose.
• Tiger Iron is a sedimentary deposit of approximately 2.2 billion years old that consists of alternating layers of silver gray hematite and red jasper, chert or even tiger eye quartz.
• Kidney Ore is the massive botryoidal form and gives the appearance of lumpy kidney-like masses.
• Oolitic Hematite is a sedimentary formation that has a reddish brown color and an earthy luster and is composed of small rounded grains.
• Specularite is a micaceous or flaky stone that is sparkling silver gray and sometimes used as an ornamental stone.

PHYSICAL CHARACTERISTICS:

• Color is steel or silver gray to black in some forms and red to brown in earthy forms. Sometimes tarnished with irredescent colors when in a hydrated form (called Turgite).
• Luster is metallic or dull in earthy and oolitic forms.
• Transparency: Crystals are opaque.
• Crystal System is trigonal; bar 3 2/m
• Crystal Habits include tabular crystals of varying thickness sometimes twinned, micaceous (specular), botryoidal and massive. also earthy or oolitic.
• Cleavage is absent however there is a parting on two planes.
• Fracture is uneven.
• Hardness is 5 - 6
• Specific Gravity is 5.3 (slightly above average for metallic minerals)
• Streak is blood red to brownish red for earthy forms.
• Associated Minerals include jasper (a variety of quartz) in banded iron formations (BIF or Tiger Iron), dipyramidal quartz, rutile, and pyrite among others.
• Notable Occurrences especially nice specimens come from England, Mexico, Brazil, Australia and the Lake Superior region.
• Best Field Indicators are crystal habit, streak and hardness.

The Hematite Group is a more or less informal group of closely related trigonal oxides. Their relationship is linked through their similar structures. The general formula for this group is A ₂O₃. The A cations can be either iron, titanium, aluminum, chromium, vanadium, magnesium, antimony, sodium, zinc and/or manganese. (reference)

The structure is composed of alternating layers of cations and oxygens. The cations occupy spaces in layers between the oxygen layers and each are bonded to three oxygens in the above layer and three oxygens in the bottom layer. Not all of the sites for these cations are occupied as only two out of three are filled. If all the sites were filled then the formula would be AO in stead of A ₂O₃.

In the Ilmenite Subgroup, alternating layers of cations are occupied by only titanium or antimony and the other cation layers are occupied by a dissimilar cation. This lowers the symmetry of this subgroup (bar 3); from the other members of this group (bar 3 2/m). The other members are not similarly affected because their A cations are all the same and thus there is no asymmetry to their stacking sequence. The same symmetry phenomena occurs between the Calcite Group and the Dolomite Group of carbonates.

These are the members of the Hematite Group:

• Corundum (Aluminum Oxide)
• Eskolaite (Chromium Oxide)
• Hematite (Iron Oxide)
• The Ilmenite Subgroup
  • Brizziite (Sodium Antimony Oxide)
  • Ecandrewsite (Zinc Iron Manganese Titanium Oxide)
  • Geikielite (Magnesium Titanium Oxide)
  • Ilmenite (Iron Titanium Oxide)
  • Melanostibite (Manganese Antimony Oxide)
  • Pyrophanite (Manganese Titanium Oxide)
• Karelianite (Vanadium Oxide)