1. History of the Periodic Table
• Dobereiner's Triads (1817):
o Grouped elements in sets of three based on similar
properties.
o The atomic mass of the middle element was
approximately the average of the other two.
o Example: Lithium (7), Sodium (23), Potassium (39).
• Newlands' Law of Octaves (1865):
o Arranged elements in increasing order of atomic masses.
o Every eighth element showed similar properties, like the
notes in music.
o Limitations:
▪ Worked only for elements up to Calcium.
▪ Did not leave space for undiscovered elements.
• Mendeleev's Periodic Table (1869):
o Arranged elements in increasing atomic masses.
o Left gaps for undiscovered elements, predicting their
properties.
o Grouped elements with similar properties together.
o Limitations:
▪ Could not explain isotopes.
▪ Some elements were placed out of order to fit into
groups.
• Modern Periodic Table (1913, Henry Moseley):
, o Based on atomic numbers (not masses).
o Resolved issues with Mendeleev’s arrangement.
2. Features of the Modern Periodic Table
• Structure:
o Groups: 18 vertical columns.
o Periods: 7 horizontal rows.
• Arrangement:
o Elements are arranged in increasing order of atomic
numbers.
o Elements in the same group have similar chemical
properties.
o Elements in the same period have the same number of
shells.
3. Periods and Their Characteristics
Periods:
1. Period 1 (Very Short Period):
o Contains 2 elements: Hydrogen (H) and Helium (He).
o Single shell (K-shell).
2. Period 2 (Short Period):
o Contains 8 elements: Lithium (Li) to Neon (Ne).
o Two shells (K and L).
3. Period 3 (Short Period):
o Contains 8 elements: Sodium (Na) to Argon (Ar).
o Three shells (K, L, and M).