Represent the ground-state electron configuration of an atom of an element or its ions using the Aufbau principle.
An atom is a small, dense, positively charged nucleus of protons and neutrons surrounded by negatively charged electrons. Everything about chemical behavior comes from the electrostatic attraction between those two, which the CED insists you describe with Coulomb's law: the force between charges is proportional to the product of the charges and inversely proportional to the square of the separation.
Electrons occupy shells (energy levels, labeled n) and subshells (s, p, d, f). Electrons in the outermost shell are valence electrons; the rest are core electrons. Three rules generate the ground-state configuration:
Configurations can be written in full (1s²2s²2p⁶3s¹), in noble-gas shorthand ([Ne]3s¹), or as an orbital-box diagram with arrows.
For ions: add electrons to the next available orbital for anions; for cations, remove electrons from the shell with the highest n first — not simply the last orbital filled. Iron is [Ar]4s²3d⁶, so Fe²⁺ is [Ar]3d⁶ (the 4s electrons go first), and Fe³⁺ is [Ar]3d⁵.
Finally, EK 1.5.A.4 connects configuration to energy: how hard it is to pull an electron off depends on its distance from the nucleus and the effective nuclear charge it feels after shielding by inner electrons. That is the seed of both PES (1.6) and the periodic trends (1.7).
Write the ground-state electron configuration of (a) Br, (b) S²⁻, and (c) Fe³⁺.
(a) Br (Z = 35): [Ar] 4s² 3d¹⁰ 4p⁵ — 18 + 2 + 10 + 5 = 35 ✓
(b) S²⁻: S is [Ne] 3s² 3p⁴ (16 e⁻). Adding 2 electrons gives [Ne] 3s² 3p⁶, which is isoelectronic with argon.
(c) Fe³⁺: Fe is [Ar] 4s² 3d⁶. Remove the two 4s electrons first, then one 3d electron → [Ar] 3d⁵.