1. Historical Development of the Periodic Table

Scientist Year Contribution Limitation
Döbereiner 1829 Law of Triads — middle element's atomic mass is average of other two; e.g., Li-Na-K, Ca-Sr-Ba, Cl-Br-I Only worked for a few elements; failed for most
Newlands 1866 Law of Octaves — every 8th element has similar properties to the 1st (like musical octaves) Worked only up to calcium; failed for heavier elements; no room for new elements
Mendeleev 1869 Periodic Law — properties of elements are periodic functions of their atomic masses; predicted eka-boron, eka-aluminium (Ga), eka-silicon (Ge) Position of H anomalous; isotopes not accommodated; wrong position of some elements (e.g., Co and Ni)
Moseley 1913 Showed atomic number (not mass) is the fundamental property; νZ (Moseley's law)

Mendeleev's Achievements

  • Predicted properties of undiscovered elements — eka-aluminium (later found as Gallium, Ga) and eka-silicon (later found as Germanium, Ge) — with remarkable accuracy.
  • Left blank spaces in the table for undiscovered elements.
  • Arranged elements in order of increasing atomic mass in groups and periods.
  • Accommodated noble gases (discovered later) without disturbing the table.

2. Modern Periodic Law

Based on Moseley's discovery, the Modern Periodic Law states:

"The physical and chemical properties of elements are periodic functions of their atomic numbers."

This replaced Mendeleev's atomic mass with atomic number as the basis of classification. Atomic number (Z) = number of protons = fundamental identity of an element.

Why Atomic Number and Not Atomic Mass?

  • Isotopes (same Z, different mass) have the same chemical properties — confirming Z is fundamental.
  • Atomic mass ordering causes anomalies (Co–Ni, Ar–K, Te–I) that are corrected by using atomic number.
  • Electronic configuration (which determines properties) depends directly on Z.

3. Structure of the Modern Periodic Table

The modern long form periodic table (also called Bohr's table) has 118 elements arranged in 7 periods (horizontal rows) and 18 groups (vertical columns).

Periods — The Horizontal Rows

Period No. of Elements Shell being filled Elements
1 (Very short) 2 1s H, He
2 (Short) 8 2s, 2p Li to Ne
3 (Short) 8 3s, 3p Na to Ar
4 (Long) 18 4s, 3d, 4p K to Kr
5 (Long) 18 5s, 4d, 5p Rb to Xe
6 (Very long) 32 6s, 4f, 5d, 6p Cs to Rn
7 (Incomplete) 32 7s, 5f, 6d, 7p Fr to Og (element 118)

Period number = number of the outermost shell (principal quantum number n of the valence shell).

Groups — The Vertical Columns

Groups 1–18 (IUPAC). Elements in the same group have the same number of valence electrons and similar chemical properties.

  • Groups 1–2: s-block
  • Groups 3–12: d-block (transition metals)
  • Groups 13–18: p-block
  • Lanthanoids (58–71) and Actinoids (90–103): f-block

4. Classification of Elements — The Four Blocks

Block Orbital being filled Groups General valence config. Examples
s-block ns 1, 2 ns1 or ns2 Li, Na, K (Gr 1); Be, Mg, Ca (Gr 2)
p-block np 13–18 ns2np16 B, C, N, O, F, Ne and their analogues
d-block (n1)d 3–12 (n1)d110ns02 Sc to Zn, Y to Cd, La, Hf–Hg
f-block (n2)f — (inner transition) (n2)f114(n1)d01ns2 Ce–Lu (lanthanoids), Th–Lr (actinoids)

Determining Block, Period, and Group from Electronic Configuration

  • Block: Identified by the type of orbital in which the last electron enters.
  • Period: = Principal quantum number (n) of the outermost shell.
  • Group (s-block): = Number of valence electrons (1 or 2).
  • Group (p-block): = 10 + number of valence electrons (ns2npx → Group 10+2+x=12+x).
  • Group (d-block): = Number of (n1)d electrons + number of ns electrons.

Quick Example

Element with Z=35 (Bromine): [Ar]3d104s24p5
Last electron enters 4pp-block.
Outermost shell n=4Period 4.
Valence electrons = 4s24p5 = 7 → Group =10+7=17Group 17 (Halogens). ✓

5. Nomenclature of Elements with Z>100

IUPAC recommends a systematic nomenclature for elements with atomic number >100 using numerical roots:

Digit Root Digit Root
0 nil 5 pent
1 un 6 hex
2 bi 7 sept
3 tri 8 oct
4 quad 9 enn

Rules: Join roots for each digit + suffix -ium. Symbol = first letter of each root (capitalised).
Example: Z=118 → Un(1) + un(1) + oct(8) + ium = Ununoctium (Uuo) → officially named Oganesson (Og).
Z=113 → Ununtrium (Uut) → officially named Nihonium (Nh).

6. Metals, Nonmetals and Metalloids

Property Metals Nonmetals Metalloids
Lustre Shiny Dull (except iodine, graphite) Semiconductor-like
Conductivity Good conductors Poor conductors (except graphite) Intermediate
Oxide nature Basic Acidic Amphoteric
Examples Fe, Cu, Na, Al (~80% of elements) C, N, O, S, Cl, noble gases B, Si, Ge, As, Sb, Te
Position in table Left and centre Right side Staircase boundary (zigzag line)

Representative elements: s-block and p-block elements (Groups 1, 2, 13–18).
Transition elements: d-block (Groups 3–12).
Inner transition elements: f-block (lanthanoids and actinoids).
Noble gases (Group 18): have completely filled orbitals — extremely stable and largely unreactive.

7. Electron Gain Enthalpy and Electronegativity — Introduction

A brief overview here as context — detailed treatment is in the next topic (Periodic Trends).

Key Definitions

Property Definition Unit
Valence electrons Electrons in the outermost shell; determine chemical behaviour
Ionisation Enthalpy (IE) Energy required to remove an electron from a gaseous atom/ion kJ/mol
Electron Gain Enthalpy (EGE) Enthalpy change when an electron is added to a neutral gaseous atom kJ/mol
Electronegativity Tendency of a bonded atom to attract shared electrons towards itself Pauling units
Oxidation state Hypothetical charge on an atom if all bonds were ionic