Beryllium was first identified as an oxide in the gemstones emerald and beryl. In 1798, the French chemist Louis-Nicolas Vauquelin (1763-1829) discovered a new element by analyzing emerald and beryl. He initially named this element glucinium (from the Greek glykys = sweet) because of the sweet taste of its salts. It was not until 1828 that the chemists Friedrich Wöhler (1800-1882) in Germany and Antoine Bussy (1794-1882) in France independently succeeded in isolating the pure metal by reducing beryllium chloride with potassium. The name beryllium (from the mineral beryl) eventually became internationally accepted, although the term glucinium remained in use in some countries until the mid-20th century.
Beryllium (symbol Be, atomic number 4) is the first alkaline earth metal in the periodic table, consisting of four protons, five neutrons (for the stable isotope), and four electrons. The only natural stable isotope is beryllium-9 \(\,^{9}\mathrm{Be}\) (100% natural abundance).
At room temperature, beryllium is a hard, steel-gray metal, remarkably light (density ≈ 1.85 g/cm³), making it one of the least dense structural metals. It has exceptional rigidity (high elastic modulus) and excellent thermal conductivity. Beryllium is relatively stable in air due to the formation of a protective layer of beryllium oxide (BeO). The temperature at which the liquid and solid states can coexist (melting point): 1560 K (1287 °C). The temperature at which it transitions from liquid to gas (boiling point): 2742 K (2469 °C).
| Isotope / Notation | Protons (Z) | Neutrons (N) | Atomic mass (u) | Natural abundance | Half-life / Stability | Decay / Remarks |
|---|---|---|---|---|---|---|
| Beryllium-7 — \(\,^{7}\mathrm{Be}\,\) | 4 | 3 | 7.016930 u | Cosmogenic | 53.22 days | Radioactive by electron capture to \(\,^{7}\mathrm{Li}\); produced by cosmic rays in the atmosphere. |
| Beryllium-8 — \(\,^{8}\mathrm{Be}\,\) | 4 | 4 | 8.005305 u | Unnatural | ≈ 8.19 × 10⁻¹⁷ s | Extremely unstable; immediately decays into two alpha particles (helium-4 nuclei). |
| Beryllium-9 — \(\,^{9}\mathrm{Be}\,\) | 4 | 5 | 9.012183 u | 100 % | Stable | Only stable isotope of beryllium; used in all industrial and scientific applications. |
| Beryllium-10 — \(\,^{10}\mathrm{Be}\,\) | 4 | 6 | 10.013534 u | Cosmogenic | 1.387 million years | Radioactive β\(^-\) decay to \(\,^{10}\mathrm{B}\); used in geological dating and climatology to trace erosion. |
| Beryllium-11 — \(\,^{11}\mathrm{Be}\,\) | 4 | 7 | 11.021658 u | Unnatural | 13.76 s | Radioactive β\(^-\); has a neutron halo; studied in nuclear physics. |
| Other isotopes — \(\,^{6}\mathrm{Be},\,^{12}\mathrm{Be},\,^{14}\mathrm{Be}\) | 4 | 2, 8, 10 | — (resonances) | Unnatural | \(10^{-21}\) — 0.02 s | Very unstable states observed in nuclear physics; decay by neutron or particle emission. |
N.B. :
Electron shells: How electrons organize around the nucleus.
Beryllium has 4 electrons distributed across two electron shells. Its full electronic configuration is: 1s² 2s², or simplified as: [He] 2s². This configuration can also be written as: K(2) L(2).
K Shell (n=1): Contains 2 electrons in the 1s sub-shell. This inner shell is complete and highly stable.
L Shell (n=2): Contains 2 electrons in the 2s sub-shell. The 2s orbitals are complete, while the 2p orbitals remain totally empty. Thus, 6 electrons are missing to reach the stable neon configuration with 8 electrons (octet).
The 2 electrons in the outer shell (2s²) are the valence electrons of beryllium. This configuration explains its chemical properties:
By losing its 2 electrons in the 2s sub-shell, beryllium forms the Be²⁺ ion (oxidation state +2), its unique and systematic oxidation state in all its compounds.
The Be²⁺ ion then adopts an electronic configuration identical to that of helium [He], which gives this ion great stability.
Beryllium does not exhibit any other stable oxidation state; only the +2 degree is observed in chemistry.
The electronic configuration of beryllium, with 2 electrons in its valence shell, classifies it among the alkaline earth metals (group 2 of the periodic table), although it exhibits atypical chemical behavior for this group. This structure gives it particular characteristic properties: due to its very small size and high charge (+2), the Be²⁺ ion is extremely polarizing, which means that beryllium mainly forms covalent bonds rather than ionic bonds, unlike other alkaline earth metals. Beryllium tends to form compounds where it does not obey the octet rule, with only 4 electrons around the central atom in molecules like BeCl₂.
Elemental beryllium is a light metal (density of 1.85 g/cm³), steel-gray, relatively hard, and brittle. It forms a protective oxide layer of BeO in the air that protects it from further oxidation. Beryllium exhibits exceptional mechanical properties at high temperatures and excellent thermal conductivity.
The importance of beryllium lies in its specialized technological applications: copper-beryllium alloys combine high strength, electrical conductivity, and non-magnetism, used in aerospace, electronics, and non-sparking tools; pure beryllium is used as a neutron reflector and moderator in nuclear reactors; its transparency to X-rays makes beryllium a material of choice for X-ray tube windows; beryllium oxide BeO is an excellent electrical insulator with high thermal conductivity, used in power electronics. However, beryllium and its compounds are extremely toxic when inhaled, causing berylliosis (a chronic lung disease), which requires strict precautions during handling.
Beryllium has two valence electrons and mainly forms compounds in the +2 oxidation state. Unlike other alkaline earth metals, beryllium exhibits atypical chemical behavior due to its small atomic size and relatively high electronegativity (for a metal). It forms covalent bonds rather than ionic bonds in many compounds, which is unusual for an alkaline earth metal.
Metallic beryllium is protected from oxidation by a thin layer of beryllium oxide (BeO) that forms spontaneously in air. This protective layer is extremely stable and resists dilute acids. However, beryllium reacts with concentrated acids and strong bases. It forms halides (beryllium fluoride, chloride), hydrides, and organometallic compounds. Beryllium and its compounds are highly toxic, causing a serious lung disease called berylliosis when inhaled as dust or vapor.
Beryllium occupies a special position in nucleosynthesis because it was not produced in significant quantities during the Big Bang. The extreme instability of beryllium-8, which decays into two helium-4 nuclei in a fraction of a second, creates a "bottleneck" in primordial nucleosynthesis. This instability prevented the formation of elements heavier than helium during the first minutes of the universe, creating what is known as the "beryllium-8 gap".
The beryllium present in the current universe is mainly produced by two processes: cosmic spallation (fragmentation of heavier atoms such as carbon and oxygen by cosmic rays) and nuclear reactions in the atmospheres of massive stars during supernova explosions. Beryllium-9 and cosmogenic beryllium-10 serve as tracers to study the history of galactic cosmic rays and mixing processes in stars.
In stars, beryllium is rapidly destroyed at relatively low temperatures (about 3.5 million kelvin), making it an excellent indicator of temperature and convection processes in stellar interiors. Astronomers use the abundance of beryllium in old stars to constrain stellar structure models and understand the chemical evolution of the galaxy.
Beryllium also plays a crucial role in modern stellar nucleosynthesis. In evolved massive stars, the triple-alpha reaction (which forms carbon-12 from three helium-4 nuclei) must overcome the beryllium-8 gap. This reaction only works because an excited state of carbon-12, predicted by Fred Hoyle in 1953, allows the ephemeral beryllium-8 to capture a third helium nucleus before decaying. This remarkable coincidence, sometimes called the "weak anthropic principle," is one of the reasons why carbon, and therefore life as we know it, can exist in the universe.
N.B.:
Toxicity of Beryllium: Beryllium and its compounds are classified as carcinogenic and highly toxic substances. Inhalation of dust or vapors containing beryllium can cause berylliosis, a serious and sometimes fatal chronic lung disease. This disease can develop even after brief exposure to low concentrations. For this reason, handling beryllium and its compounds requires rigorous protective measures and strict control in industrial environments. Despite its exceptional properties, the use of beryllium is limited to applications where no acceptable substitute exists, due to the health risks it poses.
