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Lanthanides
Actinides

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Element Categories (Click to Select Multiple)

Alkali Metals
Alkaline Earth Metals
Transition Metals
Post-transition Metals
Metalloids
Nonmetals
Halogens
Noble Gases
Lanthanides (f-block)
Actinides (f-block)

Understanding the Periodic Table

Groups (Columns)

Elements in the same group share similar chemical properties and have the same number of valence electrons. Groups are numbered 1-18.

  • Group 1: Alkali Metals (highly reactive)
  • Group 2: Alkaline Earth Metals
  • Groups 3-12: Transition Metals
  • Group 17: Halogens (very reactive nonmetals)
  • Group 18: Noble Gases (inert)

Periods (Rows)

Elements in the same period have the same number of electron shells. Period number = number of electron shells.

Blocks (s, p, d, f)

Blocks indicate which orbital is being filled with electrons:

  • s-block: Groups 1-2 (valence electrons in s orbital)
  • p-block: Groups 13-18 (filling p orbitals)
  • d-block: Groups 3-12 (transition metals, filling d orbitals)
  • f-block: Lanthanides & Actinides (filling f orbitals)

Electron Configuration

Shows how electrons are distributed in atomic orbitals. Format: [Noble Gas] orbitalelectrons

  • Example: Carbon = [He] 2sΒ² 2pΒ² (2 electrons in 2s, 2 in 2p)
  • Aufbau Principle: Electrons fill lowest energy orbitals first
  • Order: 1s, 2s, 2p, 3s, 3p, 4s, 3d, 4p, 5s, 4d, 5p, 6s, 4f, 5d, 6p, 7s, 5f, 6d, 7p
  • Orbital Capacity: s=2, p=6, d=10, f=14 electrons
  • Valence Electrons: Outermost shell electrons determine chemical properties

Oxidation States

The charge an atom would have if all bonds were ionic. Indicates electron loss/gain in compounds.

  • Positive (+): Metals lose electrons (e.g., Na⁺, Ca²⁺, Fe³⁺)
  • Negative (βˆ’): Nonmetals gain electrons (e.g., Cl⁻, O²⁻, N³⁻)
  • Multiple States: Transition metals can have several (e.g., Fe: +2, +3)
  • Group Patterns: Group 1=+1, Group 2=+2, Group 17=βˆ’1, Group 18=0
  • Variable States: Allow formation of different compounds (FeClβ‚‚ vs FeCl₃)

Periodic Trends

Electronegativity

Ability of an atom to attract electrons in a chemical bond (Pauling scale: 0.7-4.0).

  • Increases β†’: Left to right across periods (more protons attract electrons)
  • Decreases ↓: Top to bottom down groups (electrons farther from nucleus)
  • Highest: Fluorine (3.98) - most electronegative element
  • Lowest: Francium (0.7) - least electronegative
  • Predicts Bonding: Large difference = ionic, small = covalent

Ionization Energy

Energy required to remove an electron from a gaseous atom (measured in kJ/mol).

  • Increases β†’: Left to right across periods (stronger nuclear attraction)
  • Decreases ↓: Top to bottom down groups (electrons farther, easier to remove)
  • Highest: Helium (2372 kJ/mol) - hardest to ionize
  • Lowest: Francium (380 kJ/mol) - easiest to ionize
  • Noble Gases: Highest in each period (stable electron configuration)

Atomic Radius

Distance from nucleus to outermost electron shell (measured in picometers, pm).

  • Decreases β†’: Left to right across periods (more protons pull electrons closer)
  • Increases ↓: Top to bottom down groups (more electron shells added)
  • Largest: Francium/Cesium (~298 pm) - most electron shells
  • Smallest: Helium (31 pm) - only one electron shell
  • Cations: Smaller than parent atom (lost electrons)
  • Anions: Larger than parent atom (gained electrons)

Walter Russell's Spiral Periodic Table (1926-1953)

This revolutionary design shows elements arranged in 9 octaves following musical wave patterns, with noble gases at amplitude peaks and elements spiraling from hydrogen at the center outward.

Overhead Spiral View

Helical Side View - "Ten Octaves of Integrating Light"

Russell's Principles

Generative (Male +)
Radiative (Female -)
Inert (Noble Gases)
Balance (Carbon)

πŸ”¬ Electron Orbitals & Configuration

Understanding Electron Orbitals

Orbitals are regions where electrons are likely to be found. The periodic table is organized by which orbital is being filled:

s-block (Groups 1-2)

Spherical orbitals. Max 2 electrons. Filling s orbitals.

p-block (Groups 13-18)

Dumbbell-shaped. Max 6 electrons (3 orbitals Γ— 2). Filling p orbitals.

d-block (Groups 3-12)

Complex shapes. Max 10 electrons (5 orbitals Γ— 2). Transition metals.

f-block (Lanthanides/Actinides)

Very complex. Max 14 electrons (7 orbitals Γ— 2). Rare earths.

Orbital Filling Order (Aufbau Principle)

1s
2s2p
3s3p
4s3d4p
5s4d5p
6s4f5d6p
7s5f6d7p

Electrons fill lowest energy orbitals first. Note: 4s fills before 3d, 5s before 4d, etc.

Key Principles

  • Aufbau Principle: Electrons fill orbitals from lowest to highest energy
  • Pauli Exclusion: Maximum 2 electrons per orbital (opposite spins ↑↓)
  • Hund's Rule: Electrons fill degenerate orbitals singly before pairing

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