The p-block elements occupy the right side of the periodic table, starting from Group 13 to Group 18. These elements have their valence electrons filling up the p-orbitals. Their electron configurations can be expressed as ns2 np1-6, with the 'n' indicating the period and '1-6' the varying number of electrons in the p-orbitals.
The p-block encompasses a diverse range of elements, including metals, nonmetals, and metalloids, thus showing a wide variety of properties. For example, carbon (C), a Group 14 element, has an electron configuration of 2s2 2p2 and is fundamental to all known life, while oxygen (O), with an electron configuration of 2s2 2p4 in Group 16, is essential for respiration.
Their capacity to form diverse types of compounds, from simple diatomic molecules to large polymers, makes p-block elements crucial in both organic and inorganic chemistry. Their chemistry is governed by the trends in electronegativity and electron affinity, alongside the octet rule—where atoms tend to gain, lose, or share electrons to achieve eight in their valence shell—a guideline of stability for many elements in this block.