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Magnesium is a metallic element with atomic number 12 and chemical symbol Mg, belonging to the alkaline earth metals group in the periodic table. It is a silvery-white lightweight and highly reactive metal. It has important industrial and biological roles.
Magnesium is an alkaline earth metal located in group 2A (group 2) of the third period of the periodic table. Its electron configuration is [Ne]3s², containing two valence electrons in its outermost shell. It readily loses these electrons to form +2 ions (Mg²⁺) in its compounds. This behavior makes magnesium a chemically active metal and explains why it is rarely found in its pure form in nature. At room temperature it exists as a solid and is a good electrical conductor. Due to its light weight and strength, it is an important component in alloys.
Magnesium was first identified in 1755 by Joseph Black in England as a distinct “earth” (oxide) different from Epsom salts (magnesium sulfate). Metallic magnesium was first isolated in 1808 by Sir Humphry Davy through the electrolysis of a mixture of magnesium oxide and mercury oxide.

Magnesium (Generated by Artificial Intelligence.)
The name magnesium derives from Magnesia, an ancient region in Greece corresponding to present-day Manisa and its surroundings, where various magnesium minerals such as magnesite and dolomite were abundant.
Magnesium, with electron configuration [Ne]3s², has a density of 1.74 g/cm³, a melting point of 650 °C, and a boiling point of 1090 °C. With an atomic radius of 1.73 Å, its electron affinity is unstable, indicating a very low or even negative tendency to gain electrons.
With an electronegativity of 1.31 on the Pauling scale, magnesium is a solid at room temperature and has a shiny silvery-white appearance. As a highly reactive metal, it forms a thin layer of magnesium oxide on its surface when exposed to air, which passivates the metal and protects it from further corrosion. However, in thin ribbons or powder form, it ignites easily and burns with a bright white flame to produce magnesium oxide (MgO) and magnesium nitride (Mg₃N₂). It reacts with hot water more readily than with cold water. Magnesium also reacts readily with acids, releasing hydrogen gas.
Magnesium is the eighth most abundant element in the Earth’s crust, found primarily in minerals such as magnesite (MgCO₃), dolomite (CaMg(CO₃)₂), and carnallite (KMgCl₃·6H₂O), as well as dissolved in seawater.
Naturally occurring magnesium has three stable isotopes: ²⁴Mg (the most abundant), ²⁵Mg, and ²⁶Mg. ²⁴Mg is highlighted as a significant isotope. In addition, several artificial radioactive isotopes are known.
Magnesium and its alloys are used in various fields due to their light weight and strength:
Magnesium is a vital mineral for all living organisms, including humans, animals, and plants. In the human body, it acts as a cofactor for hundreds of enzymes involved in essential metabolic processes such as energy production, protein synthesis, muscle and nerve function, blood sugar regulation, and blood pressure control.
Magnesium is also crucial for bone health; it is a structural component of bone and closely interacts with calcium metabolism. In plants, magnesium is the central atom in chlorophyll, the molecule essential for photosynthesis. This magnesium atom gives plants their green color and enables the conversion of sunlight into chemical energy.
Magnesium plays a role in the transmission of nerve impulses and in muscle contraction and relaxation. It is also required for the synthesis and structural stability of DNA and RNA. Adequate magnesium intake is essential for overall health and good quality of life; deficiency can lead to various health problems such as muscle cramps, fatigue, and nervous system disorders.

Classification and Basic Properties
Discovery
Etimology
Physical and Chemical Properties
Natural Occurrence and Extraction
Applications
Biological Importance