Periodic Table Lab

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All 118 elements in a lab notebook. Hover a tile for the basics, click it for its 3D atom.

Iron (Fe), element 26

Iron (Fe) is element 26, a transition metal in group 8, period 4 of the d-block. Most-used metal; the core of steel and of Earth, and carries oxygen in hemoglobin.

Alkali metalAlkaline earthTransition metalPost-transition metalMetalloidReactive nonmetalHalogenNoble gasLanthanideActinide

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Iron at a glance

Atomic number
26
Symbol
Fe
Atomic mass
55.845 u
Category
Transition metal
Group / period
8 / 4
Electron configuration
[Ar] 3d 6 4s 2
State at 25 °C
Solid
Melting point
1538 °C
Boiling point
2861 °C
Density
7.874 g/cm³
Electronegativity
1.83
1st ionization energy
763 kJ/mol
Oxidation states
+2, +3
Discovered
Antiquity

Atomic structure

A neutral iron atom has 26 protons and 26 electrons, and its most common isotope carries about 30 neutrons. One atom weighs about 9.27 × 10⁻²⁶ kg, so a mole of iron (6.022 × 10²³ atoms) weighs 55.845 g. That nucleus holds 1.15 neutrons for every proton. Its symbol Fe comes from ferrum. The electrons fill 4 shells (K 2, L 8, M 14, N 2), which gives the configuration [Ar] 3d 6 4s 2. As a d-block element, both its outer s electrons and its inner d electrons can take part in bonding, which is why it shows more than one oxidation state. It has 4 stable isotopes: Fe-54, Fe-56, Fe-57 and Fe-58. No other element has a stable isotope with mass number 56, so Fe-56 has no stable isobars; its neighbours on that line decay into it or away from it.

Physical properties

At room temperature (25 °C) iron is a solid. It melts at 1538 °C and boils at 2861 °C, so it stays liquid across a 1323-degree range. It stays solid in a candle flame (about 1000 °C) but would melt in molten iron (1538 °C). Its density is 7.874 g/cm³, 7.87 times as dense as water. Its atoms have a radius of about 140 pm (Manganese next door is 140 pm). In the solid, its atoms pack into a body-centred cubic lattice.

Chemical behaviour

Its electronegativity is 1.83 on the Pauling scale. Pulling off its outermost electron takes 763 kJ/mol. A bond between iron and chlorine would be polar covalent, with an electronegativity difference of 1.3. It releases 15 kJ/mol when it gains an extra electron. Its common oxidation states are +2, +3, so in compounds you will usually meet it as Fe²⁺ and Fe³⁺. Group 8 also holds Ruthenium, Osmium and Hassium, which share its outer-shell pattern.

Where it comes from

It makes up 5.63 % of Earth's crust, the 4th most abundant element there. In the human body it accounts for about 0.006 % of body mass. It has been known since ancient times, one of only 11 elements people used before modern chemistry. When excited it glows at its own set of colours; its brightest visible lines are at 527.0 nm, 438.4 nm and 430.8 nm.

Related elements

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Values are standard reference figures at 1 atm: melting and boiling points in kelvin, density at room temperature, electronegativity on the Pauling scale. Properties of elements 104 to 118 and some past fermium are predicted or estimated. Neutron counts use the most common isotope, approximately. The shells, orbital clouds and lattices are schematic, not to scale. Ionization energies, electron affinities, abundances and hazards are rounded reference values; the isotope stability check and decay chains are simplified. Shortcuts: ← → step through elements (with a tile focused, arrows move around the table), / search, S switch 3D or scribbles, D pencil tool, Esc stop the quiz or pencil.

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