Aluminum is the chemical element with atomic number 13. It is a soft, greyish-white metal with an estimated hardness of 2.5 to 3 on the Mohs scale. It is the third most abundant element in the earth's crust, after Oxygen and Silicon.

Aluminum is highly reactive. It oxidizes rapidly in a humid environment to form a protective coating that prevents it from being attacked by Oxygen and humidity. It is very ductile and malleable and can be worked and formed into other products using industrial techniques such as casting, forging and extrusion. It easily combines with other elements to form alloys, which are used in many different products.

Aluminum is one of the most widely used metals due to its lightness and resistance to corrosion. It is used in many industrial applications, including building materials, food products, packaging, conveyors, electronic equipment, household appliances and vehicles. It is also used in many alloys, which are used for their corrosion resistance and ease of processing.

660.5°
2467°

26.9815385

1
3

[Ne] 3s2 3p1

2
8
3

1.61

5.9858

Synthetic

Radioactive

Liquid

Gaseous

Electronic configuration diagram

Characteristics

Name	Aluminum
Number	13
Atomic	26.9815385
Symbol	Al
Fusion	660.5
Boiling	2467
Density	2.698
Period	3
Group	13

Discovery	1827 Wshler
Abundance	82300
Radius	1.8
Electronegativity	1.61
Ionization	5.9858
Number of isotopes	8
Electronic configuration	[Ne] 3s2 3p1
Oxidation states	1,3
Electron by energy level	2,8,3

Minerals containing this element : 1314

Mineral	Hardness	Density
Abswurmbachite	6.50 / 6.50	4.96
Abuite
Actinolite	5.50 / 5.50	2.98
Acuminite	3.50 / 3.50	3.30
Adachiite
Addibischoffite
Adranosite
Adrianite
Aenigmatite	5.00 / 6.00	3.74
Aerinite	3.00 / 3.00	2.48
Afghanite	5.50 / 6.00	2.55
Afmite
Aheylite	5.00 / 6.00	2.85
Ajoite		2.96
Akatoreite	6.00 / 6.00	3.48
Akdalaite	7.00 / 7.00	3.68
Alarsite	3.00 / 3.00	3.32
Albite	7.00 / 7.00	2.61
Aldermanite	2.00 / 2.00	2.00
Alfredopetrovite	2.50 / 2.50	2.50
Aliettite	1.00 / 2.00
Allanite-(Ce)	5.50 / 5.50	3.30
Allanite-(La)	6.00 / 6.00	3.93
Allanite-(Nd)
Allanite-(Y)	5.50 / 5.50	3.30
Allanpringite	3.00 / 3.00	2.54
Allendeite		4.84
Allophane	3.00 / 3.00	1.90
Alloriite	5.00 / 5.00	2.35
Almandine	7.00 / 8.00	4.09
Almarudite	6.00 / 6.00	2.71
Alnaperbøeite-(Ce)
Althupite	3.50 / 4.00	3.90
Altisite	6.00 / 6.00	2.64
Alum-(K)	2.00 / 2.00	1.76
Alum-(Na)	3.00 / 3.00	1.67
Aluminite	1.00 / 1.00	1.66
Aluminium	2.00 / 3.50	2.00
Alumino-ferrobarroisite
Alumino-ferrohornblende
Alumino-ferrotschermakite
Alumino-ferrowinchite
Alumino-magnesiohornblende
Alumino-magnesiotaramite
Alumino-ottoliniite
Aluminobarroisite	5.00 / 6.00	2.94
Aluminoceladonite
Aluminocerite-(Ce)	5.00 / 5.00	4.68
Aluminocopiapite	2.50 / 3.00	2.00
Aluminocoquimbite		2.04
Aluminokatophorite	5.00 / 6.00
Aluminomagnesiohulsite	6.00 / 6.00	3.84
Aluminopyracmonite		2.14
Aluminotschermakite	5.00 / 6.00
Aluminowinchite
Alumoåkermanite	4.00 / 5.00	3.00
Alumohydrocalcite	2.50 / 2.50	2.23
Alumoklyuchevskite	2.00 / 2.00	3.10
Alumotantite	7.50 / 7.50	7.00
Alumotungstite
Alumovesuvianite
Alunite	3.50 / 4.00	2.59
Alunogen	1.50 / 2.00	1.65
Alvanite	3.00 / 3.50	2.41
Amazonite	6.00 / 6.50	2.56
Amblygonite	5.50 / 6.00	2.98
Amesite	2.50 / 3.00	2.77
Amicite	5.00 / 5.50	2.06
Ammonioalunite	2.00 / 3.00	2.40
Ammonioleucite	5.50 / 6.00	2.29
Ammoniomagnesiovoltaite
Amstallite	4.00 / 4.00	2.40
Analcime	5.00 / 5.00	2.30
Anandite	3.00 / 4.00	3.94
Andalusite	6.50 / 7.00	3.13
Andesine	7.00 / 7.00	2.66
Angastonite	2.00 / 2.00	2.47
Ankinovichite	2.50 / 3.00	2.48
Annite	2.50 / 3.00	3.17
Anorthite	6.00 / 6.00	2.72
Anorthoclase	6.00 / 6.00	2.57
Anthoinite	1.00 / 1.00	4.80
Apjohnite	1.50 / 2.00	1.80
Arakiite	3.00 / 4.00
Arangasite	1.00 / 2.00	2.00
Aravaipaite	2.00 / 2.00	6.00
Ardennite-(As)	6.00 / 7.00	3.62
Ardennite-(V)	6.00 / 7.00	3.55
Armbrusterite	3.50 / 3.50	2.78
Armenite	7.50 / 7.50	2.76
Arrojadite-(BaFe)		3.54
Arrojadite-(BaNa)
Arrojadite-(KFe)	5.00 / 5.00	3.50
Arrojadite-(KNa)
Arrojadite-(NaFe)
Arrojadite-(PbFe)	4.00 / 5.00
Arrojadite-(SrFe)
Arsenocrandallite	5.50 / 5.50	3.25
Arsenoflorencite-(Ce)	3.50 / 3.50	4.10