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Iron


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Atomic symbol: Fe
Atomic number: 26
Atomic weight: 55.847
Atomic volume: 7.1 cm3/mol
Density: 7.86 g/cm3
Period Number: 4
Group number: 8
Group name: Trans. Met.
Element classification: Metal


States


Phase at room temperature: Solid
Melting Point: 1808.2 K
Boiling point: 3023 K
Heat of fusion: 13.80 kJ/mol
Heat of vaporization: 349.60 kJ/mol


Energies


Ionization Energy: 7.902 eV
1st ionization energy: 759.3 kJ/mole
2nd ionization energy: 1561.1 kJ/mole
3rd ionization energy: 2957.3 kJ/mole
Electronegativity: 1.9
Electron affinity: 15.7 kJ/mole
Specific heat: 0.44 J/gK
Heat atomization: 418 kJ/mole atoms


Oxidation & Electrons


Shells: 2,8,14,2
Electron Shell Configuration: [Ar] 3d6 4s2
Minimum oxidation number: -2
Maximum oxidation number: 6
Minimum common oxidation number: 0
Maximum common oxidation no: 3


Appearance & Characteristics


Structure:: bcc: body-centered cubic
Color: gray
Hardness: 4.5 mohs
Toxicity: ?
Characteristics: fairly soft when pure
Uses: steel


Reactions


Reaction with air: mild, =>Fe3O4
Reaction with 6M HCl: mild, =>H2, FeCl2
Reaction with 15M HNO3: passivated
Reaction with 6M NaOH: ?


Other Forms


Number of isotopes: 4
Oxide(s): FeO Fe3O4 Fe2O3
Hydride(s): none
Chloride(s): FeCl2 FeCl3


Radius


Atomic Radius: 126 pm
Ionic radius (1- ion): pm
Ionic radius (1+ ion): pm
Ionic radius (2- ion): pm
Ionic radius (2+ ion): 83.5 pm
Ionic radius (3+ ion): 73.8 pm


Conductivity


Thermal conductivity: 72.8 J/m-sec-deg
Electrical conductivity: 102.987 1/mohm-cm
Polarizability: 8.4 A^3


Abundance


Source: Hematite,magnetite(oxide)
Relative abundance solar system: 5.954 log
Abundance earth's crust: 4.8 log
Estimated crustal abundance: 5.63×104 milligrams per kilogram
Estimated oceanic abundance: 2×10-3 milligrams per liter
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 


History


(Anglo-Saxon, iron; L. ferrum) Iron was used prehistorically:


  • Genesis mentions that Tubal-Cain, seven generations from Adam, was "an instructor of every artificer in brass and iron."

  • A remarkable iron pillar, dating to about A.D. 400, remains standing today in Delhi, India. This solid shaft of wrought iron is about 7 1/4 m high by 40 cm in diameter. Corrosion to the pillar has been minimal although it has been exposed to the weather since its creation.




Sources


Iron is a relatively abundant element in the universe. It is found in the sun and many types of stars in considerable quantity. Its nuclei are very stable. Iron is a principal component of a meteorite class known as siderites and is a minor constituent of the other two meteorite classes. The core of the earth -- 2150 miles in radius -- is thought to be largely composed of iron with about 10 percent occluded hydrogen. The metal is the fourth most abundant element, by weight that makes up the crust of the earth.

The most common ore is hematite, which is frequently seen as black sands along beaches and banks of streams.


Properties


The pure metal is very reactive chemically and rapidly corrodes, especially in moist air or at elevated temperatures. It has four allotropic forms or ferrites, known as alpha, beta, gamma, and omega, with transition points at 700, 928, and 1530C. The alpha form is magnetic, but when transformed into the beta form, the magnetism disappears although the lattice remains unchanged. The relations of these forms are peculiar. Pig iron is an alloy containing about 3 percent carbon with varying amounts of sulfur, silicon, manganese, and phosphorus.

Iron is hard, brittle, fairly fusible, and is used to produce other alloys, including steel. Wrought iron contains only a few tenths of a percent of carbon, is tough, malleable, less fusible, and usually has a "fibrous" structure.

Carbon steel is an alloy of iron with small amounts of Mn, S, P, and Si. Alloy steels are carbon steels with other additives such as nickel, chromium, vanadium, etc. Iron is a cheap, abundant, useful, and important metal.


Uses


Iron is a vital constituent of plant and animal life and works as an oxygen carrier in hemoglobin.

Taconite is becoming increasingly important as a commercial ore. The pure metal is not often encountered in commerce, but is usually alloyed with carbon or other metals.


Isotopes


Common iron is a mixture of four isotopes. Ten other isotopes are known to exist.

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