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Journey Inside the Atom
Chapter 8 — Grade 9 Science
Prepared by K Sandeep Swamy (M.Sc, B.Ed)
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Everything Around Us Is
Made of Atoms
All Matter
Every living and non-living
thing is ultimately made of
atoms — the fundamental
building blocks of matter.
Incredibly Tiny
Atoms are so small they
cannot be seen with the
naked eye — even the most
powerful optical microscopes
struggle to observe them.
The Big Question
Is the atom truly the smallest unit of matter, or can it be divided
into even smaller particles?
CHAPTER 8.1
Roots of Atomic Theory
Where did the idea of the atom come from? Let's travel back
thousands of years to find out.
Ancient Ideas: Kanada,
Leucippus & Democritus
Acharya
Kanada (India)
Matter divided
repeatedly
reaches the
smallest
indivisible particle
— the parmanu,
recorded in the
Vaisesika Sutras.
Leucippus &
Democritus
(Greece)
Called these
particles atomos
— Greek for
"indivisible."
Philosophical
Origins
Both ideas arose
as philosophical
concepts, not from
experiments —
science had not
yet begun.
Dalton's Atomic Theory (1808)
First scientific description of atoms — based on experimental evidence,
not philosophy
Proposed: all matter is composed of indivisible particles called atoms
Became the starting point for understanding atomic structure
Raised new questions: What are atoms made of? What do they look like?
Dalton's theory was revolutionary — it moved the atom from
philosophy into science for the first time.
CHAPTER 8.2
A Journey Through Atomic
Models
From Dalton's solid sphere to Bohr's energy levels — scientists
gradually uncovered the true structure of the atom.
Discovery of the Electron — J.
J. Thomson (1897)
Studied electric current through gases at very low pressure using a
cathode ray tube
Observed rays moving from cathode (−) to anode (+) — called cathode
rays
Concluded: streams of negatively charged particles (electrons) with
mass much smaller than atoms
Charge of electron: −1.602 × 10⁻¹⁹ C (taken as −1 by convention)
Thomson's Plum Pudding
Model
Thomson proposed the first model of atomic structure to explain what was
inside the atom.
Atom = a sphere of positive charge with electrons distributed
throughout
Nicknamed the "plum pudding model" — like a watermelon: red pulp =
positive charge, seeds = electrons
First genuine attempt to explain how positive and negative charges stay
balanced
The Gold Foil Experiment (1911)
The Setup
Geiger & Marsden (under Rutherford) fired α-particles
at a thin gold foil
Expected
Particles pass straight through — consistent with
Thomson's spread-out model
Observed!
Most passed through, but some sharply deflected — a
few even bounced back!
Conclusion
Thomson's model could NOT explain these astonishing
results
Rutherford's Planetary Model
Positive charge is concentrated in a tiny, dense nucleus — not spread
out
Most of an atom is empty space — that's why most α-particles passed
through undeflected
Electrons revolve around the nucleus like planets around the Sun
Nucleus is ~10⁵ times smaller than the atom
Atom ≈ 10⁻¹⁰ m | Nucleus ≈ 10⁻¹⁵ m
Why Rutherford's Model
Failed
Energy Loss Problem
An accelerating electron
should continuously lose
energy and spiral inward
toward the nucleus.
Atom Collapse?
If electrons spiralled in, all
atoms would collapse — but
matter around us is clearly
stable!
A New Model Was Needed
Rutherford's model could not explain atomic stability. Science
needed a breakthrough…
Bohr's Model of the Atom (1913)
Fixed Shells
Electrons move in fixed circular
paths called shells / orbits /
energy levels (K, L, M, N… or n = 1,
2, 3, 4…)
No Energy Loss
While in a fixed shell, an electron
does not radiate or lose energy —
solving Rutherford's stability
problem
Energy Jumps
Electrons absorb or release
energy when jumping between
shells — energy increases farther
from the nucleus
Evolution of Atomic Models at a Glance
1
Dalton
Indivisible solid sphere
2
Thomson
Plum pudding model
3
Rutherford
Nuclear planetary model
4
Bohr
Fixed energy levels
5
Modern
Quantum mechanical model
Science advances step by step — each model improved on the last, revealing deeper truths about atomic structure.
CHAPTER 8.3
Subatomic Particles
If atoms can be broken apart, what are they made of? Meet the three
fundamental subatomic particles.
Discovery of the Proton & Neutron
Proton (Rutherford)
Positive charge in the nucleus; charge = +1; much
heavier than the electron.
Neutron (Chadwick, 1932)
Neutral particle in the nucleus; mass ≈ proton;
Chadwick won the Nobel Prize in 1935.
Why Neutrons Matter
Helium has 2 protons but 4× the mass of hydrogen
— because it also has 2 neutrons!
Particle Symbol Relative
Charge
Electron e⁻ −1
Proton p⁺ +1
Neutron n⁰ 0
CHAPTERS 8.4 – 8.6
Symbols, Atomic Number &
Mass Number
How do scientists label elements and count what's inside the
nucleus?
Symbols of Elements
01
Pictorial Symbols (Dalton,
1803)
Dalton introduced simple
pictures to represent different
elements — the first attempt at
standardisation.
02
Alphabetic Symbols
(Berzelius, 1813)
Berzelius proposed using letters
to represent elements — far
more practical and universal.
03
IUPAC Standards (Today)
Rules: first letter uppercase, second letter lowercase — e.g., Al, Co, Cl.
Some symbols come from Latin/German: Fe (ferrum), Hg
(hydrargyros), W (wolfram).
Atomic Number (Z) & Mass
Number (A)
Atomic Number (Z)
= Number of protons in the
nucleus. Uniquely identifies an
element. Since atoms are
neutral: protons = electrons.
Mass Number (A)
= Total number of nucleons
(protons + neutrons) in the
nucleus.
Key Formula: A = p⁺ + n⁰
Therefore: Neutrons = A − Z
CHAPTER 8.7
Electron Distribution in
Energy Levels
How are electrons arranged inside an atom? The Bohr-Bury rules give
us a clear set of guidelines.
Rules for Filling Electron
Shells (Bohr-Bury Rules)
1 Maximum electrons per
shell = 2n²
K shell (n=1): max 2 electrons
| L shell (n=2): max 8 | M
shell (n=3): max 18
2 Outermost shell
maximum = 8
No matter which shell is
outermost, it can hold a
maximum of 8 electrons (K-
shell exception: max 2).
3 Shells fill in order: K → L → M → N
Inner shells must be filled completely before electrons occupy the
next shell.
Electronic Configuration: Examples
Hydrogen (Z = 1)
K = 1
Configuration: 1
Carbon (Z = 6)
K = 2, L = 4
Configuration: 2, 4
Sodium (Z = 11)
K = 2, L = 8, M = 1
Configuration: 2, 8, 1
Argon (Z = 18)
K = 2, L = 8, M = 8
Configuration: 2, 8, 8
Notice how Argon (Z=18) has a complete outermost shell (8 electrons) — making it an extremely stable,
unreactive noble gas!
CHAPTER 8.8
Valency — Combining
Capacity of an Atom
Why do some atoms bond with one partner while others bond with
four? Valency holds the answer.
Valence Electrons & Valency
The valence shell is the outermost shell, and its electrons
are called valence electrons. Atoms strive to achieve a
complete octet (8 electrons) or duplet (2 for He) for
stability.
Element Config. Valence
e⁻
Valency
Sodium
(Na)
2, 8, 1 1 1 (loses
1e⁻)
Oxygen
(O)
2, 6 6 2 (gains
2e⁻)
Carbon
(C)
2, 4 4 4 (shares
4e⁻)
Neon (Ne) 2, 8 8 0 (stable
octet)
Lose electrons
Metals like Na lose valence
electrons — valency = electrons
lost
Gain electrons
Non-metals like O gain electrons
— valency = electrons gained
Share electrons
Carbon shares electrons —
valency = electrons shared
CHAPTER 8.9
A Deeper Look: Isotopes,
Isobars & Average Atomic
Mass
Not all atoms of the same element are identical — and sometimes
atoms of different elements share the same mass number.
Isotopes — Same Element,
Different Mass
Isotopes are atoms of the same element with the same atomic number (Z)
but different mass numbers (A).
The three isotopes of hydrogen:
Isotopes have the same chemical properties (same valence
electrons) but different physical properties.
Protium ¹H
~99.98% — the most common
form
Deuterium ²H
~0.015% — used in heavy water
Tritium ³H
Trace amounts — radioactive
Applications of Isotopes
²³uU — Nuclear Energy
Fuel in nuclear reactors to generate electricity safely and
efficiently.
v⁰Co — Cancer Treatment
Radiation therapy for treating cancer tumours using
cobalt-60.
¹³¹I — Thyroid Treatment
Treatment of goitre and thyroid cancer — absorbed
selectively by the thyroid gland.
¹tC — Carbon Dating
Determines the age of ancient fossils and artefacts by
measuring radioactive decay.
Average Atomic Mass — The Chlorine Example
Why 35.5 u?
Chlorine has two naturally occurring isotopes with
different abundances in nature:
Isotope Mass Abundance
³⁵Cl 35 u 75%
³⁷Cl 37 u 25%
Simple average = (35 + 37) ÷ 2 = 36 u — this
ignores abundance and is inaccurate!
Weighted Average (Correct Method)
(35 × 75/100) + (37 × 25/100)
= 26.25 + 9.25
= 35.5 u
The weighted average accurately reflects the mass of
chlorine as it occurs in nature.
Isobars — Same Mass,
Different Elements
Isobars are atoms of different elements that share the same mass
number (A) but have different atomic numbers (Z).
Argon (Z = 18)
Mass Number = 40
18 protons + 22 neutrons
Potassium (Z = 19)
Mass Number = 40
19 protons + 21 neutrons
Calcium (Z = 20)
Mass Number = 40
20 protons + 20 neutrons
Unlike isotopes, isobars are completely different elements
with different chemical properties — the same mass number
is just a coincidence of nuclear composition.
Key Takeaways: Journey Inside the Atom
01
Three Subatomic Particles
Atoms are made of electrons (−1), protons (+1), and
neutrons (0) — each with a specific location and role.
02
Atomic Number & Mass Number
Z = protons (identifies the element); A = protons +
neutrons (total nucleons in nucleus).
03
Electron Shell Rules
Shells fill in order K→L→M; max in outermost shell = 8;
each shell holds 2n² electrons.
04
Valency
= Electrons gained, lost, or shared to complete the octet
and achieve stability.
05
Isotopes vs Isobars
Isotopes: same Z, different A | Isobars: same A, different
Z — two very different concepts!
06
Science Is Ongoing!
The quantum mechanical model awaits you in higher
grades — the atom still has secrets to reveal! 🔬