Classification of Elements and Periodicity
This chapter explains the organization of elements into the modern periodic table. It begins with the historical attempts at classification, such as Döbereiner's Triads and Newlands' Law of Octaves, before focusing on Mendeleev's periodic table, which was based on atomic mass. The chapter then transitions to the modern periodic law, which correctly arranges elements by their atomic number, leading to the long form of the periodic table we use today. Students will learn to identify elements' positions (group, period, block) based on their electronic configurations.
The main goal is to understand and predict periodic trends in atomic and physical properties. This includes atomic radius, ionic radius, ionization enthalpy, electron gain enthalpy, and electronegativity. You will learn how these properties change across a period (left to right) and down a group. The chapter often becomes difficult when dealing with the exceptions to these general trends, which arise from factors like nuclear charge, shielding effect, and the stability of half-filled and fully-filled electron subshells. A strong grasp of electronic configurations from the 'Structure of Atom' chapter is essential for success here.
Formulas for Classification of Elements and Periodicity
- Effective Nuclear Charge
- Z is the atomic number and σ is the screening or shielding constant.
- Allred-Rochow Electronegativity
- r is the covalent radius in angstroms (Å).
- Mulliken Electronegativity
- I.E. is Ionization Enthalpy and E.A. is Electron Affinity, typically in eV.
- Dipole Moment
- q is the magnitude of charge separation and d is the distance between charges.
- Percentage Ionic Character from Dipole Moment
- Calculated dipole moment assumes 100% ionic character (q = charge of one electron).
- Hanny-Smith Equation
- Relates the electronegativity difference of two atoms (A and B) to the ionic character of the bond.
- Pauling Electronegativity Difference
- E represents bond dissociation energies in kJ/mol.