The systematic classification of elements is essential to organize the vast amount of chemical knowledge. As the number of discovered elements grew from 31 in 1800 to over 114 today, individual study became impractical, necessitating a system to rationalize chemical facts and predict new elements.
Dmitri Mendeleev proposed that the properties of elements are a periodic function of their atomic weights. He arranged elements in horizontal rows (periods) and vertical columns (groups).
In 1913, Henry Moseley showed that atomic number ($Z$) is a more fundamental property than atomic mass, based on regularities in characteristic X-ray spectra ($\sqrt{\nu}$ vs $Z$). This led to the formulation of the Modern Periodic Law:
"The physical and chemical properties of the elements are periodic functions of their atomic numbers."
To resolve discovery disputes, IUPAC recommended a systematic nomenclature based directly on the atomic number digits:
Comprises Group 1 (alkali metals, $ns^1$) and Group 2 (alkaline earth metals, $ns^2$). They are highly reactive metals with low ionization enthalpies, forming $1+$ and $2+$ cations respectively.
Comprises Groups 13 to 18 ($ns^2 np^{1-6}$). Together with the s-block, they are known as Representative Elements. Group 17 elements are halogens, Group 16 are chalcogens, and Group 18 are noble gases.
Comprises Groups 3 to 12, characterized by the filling of inner d-orbitals with a general configuration of $(n-1)d^{1-10} ns^{0-2}$. They are all metals, typically forming colored ions, exhibiting variable oxidation states, and showing paramagnetism.
Consists of two series at the bottom of the table: Lanthanoids ($Z=58-71$) and Actinoids ($Z=90-103$), with outer configuration $(n-2)f^{1-14} (n-1)d^{0-1} ns^2$. They are all metals; actinoids are radioactive.
The energy required to remove an electron from an isolated gaseous atom in its ground state:
$$X(g) \rightarrow X^+(g) + e^-$$
The enthalpy change when an electron is added to a neutral gaseous atom:
$$X(g) + e^- \rightarrow X^-(g)$$
The qualitative measure of an atom's ability to attract shared electrons in a chemical compound. It increases across a period and decreases down a group. Fluorine is the most electronegative element (assigned 4.0 on the Pauling scale).
Valence is determined by the number of valence electrons. For representative elements, it is usually equal to the number of valence electrons or $8$ minus that number. Oxidation state represents the charge acquired by an atom based on electronegativity differences in a molecule.
The first element of each group (Lithium, Beryllium, Boron to Fluorine) differs significantly from heavier congeners due to:
Diagonal Relationship: Lithium resembles Magnesium, and Beryllium resembles Aluminium due to similar ionic sizes and charge/radius ratios.