Phosphorus is vital for life, mainly through phosphates in DNA, RNA, ATP, and cell membranes. Early sources included human urine and bone ash, while phosphate mines often contain fossils. Phosphorus is crucial for fertilisers and is found in minerals such as phosphate. It exists as highly reactive white and red phosphorus and is never found free. The Earth’s crust contains about one gram of phosphorus per kilogram.
Phosphorus, with an atomic number of 15, is in the p-block of Group 15 and Period 3 of the periodic table.
Phosphorus compounds are widespread and commonly found in phosphate rocks, minerals, bones, and teeth. Key phosphate minerals include calcium phosphate (Ca₃(PO₄)₂), apatite (Ca₅(PO₄)₃OH), fluoroapatite (Ca₅(PO₄)₃F), and chloroapatite (Ca₅(PO₄)₃Cl). Elemental phosphorus was first obtained by H. Brand, and its name, derived from Greek words meaning "light" and "I bear," reflects the phosphorescence of white phosphorus due to slow oxidation.
The table below clearly and concisely compares the allotropic forms of phosphorus, highlighting their fundamental properties, chemical behaviour, preparation methods, and appearance.
1. Phosphorus(V) Compounds
2. Phosphorus(III) Compounds
3. Phosphorus(I) and Phosphorus(II) Compounds
Phosphides and Phosphines
Learn more: Oxoacids of Phosphorus
Phosphorus primarily forms covalent bonds with five valence electrons (valence shell configuration 3s²3p³). Elemental phosphorus can be produced from any phosphate rock. The process involves:
Reaction of Crushed Phosphate Rocks and Sand:
2Ca3(PO4)2 + 6SiO2 → P4O10 + 6CaSiO3
Reduction by Carbon:
P4O10 + 10C → P4 + 10CO
White phosphorus forms waxy solids of molecular crystals consisting of P4\text{P}_4P4 molecules. These undergo spontaneous combustion in the air:
P4 + 5O2 → P4O10
The P4 structure is a distorted tetrahedron, explained by phosphorus’s electronic configuration. Sharing three electrons with other P atoms results in six P−P bonds, leaving a lone pair.
Reactions with Oxygen:
P4 + 3O2 → P4O6
In P4O6, Oxygen atoms are inserted into each P−P bond.
P4 + 5O2 → P4O10
An additional oxygen atom attaches directly to phosphorus.
Oxides of Phosphorus:
P4O10 dissolves in water to form phosphoric acid:
P4O10 + 6H2O → 4H3PO4
The phosphorous cycle involves the movement and recycling of phosphorus through rocks, water, soil, sediments, and organisms. This biogeochemical cycle includes several steps influenced by rock type, air, and water. Phosphorus is crucial for cell development and energy storage in the form of ATP (Adenosine Triphosphate). A deficiency of phosphorus in the soil can lead to poor crop yields.
Phosphorus exists in four common forms: white, black, red, and violet. It plays a crucial role in living organisms. Phosphorus is a key component of animal and plant matter found in bones, the brain, blood, and living cells. In industry, important phosphorus compounds include orthophosphoric acid and phosphatic fertilisers.
Phosphorus, commonly found as phosphates in the environment, is essential for human health, contributing to DNA and energy delivery. It is also present in plants and added to soils through phosphate-rich manure, detergents, and foods like cheese and processed meats.
Excessive phosphate levels can lead to health issues such as kidney damage and osteoporosis, while phosphate shortages pose health risks. White phosphorus, a highly toxic form of phosphorus, is dangerous and can be fatal if ingested or inhaled.
(Session 2025 - 26)