Atom Structure
Dalton’s Atomic Theory
Key ideas:
Matter is made of tiny, indivisible particles called atoms
Atoms of the same element are identical
Atoms combine in simple whole-number ratios
Atoms are rearranged, not created or destroyed, in reactions
Limitations:
Atoms are divisible (subatomic particles exist)
Atoms of the same element can differ (isotopes)
📌 Exam tip: Be able to state + critique Dalton’s theory.
2. Discovery of Subatomic Particles
Electron
Discovered by J.J. Thomson
Cathode ray tube experiment
Charge: –1
Very small mass (≈ 1/1836 of a proton)
Proton
Discovered by Rutherford
Charge: +1
Relative mass: 1
Neutron
Discovered by Chadwick
Charge: 0
Relative mass: 1
📊 Summary Table
Particle | Charge | Relative Mass | Location |
|---|---|---|---|
Proton | +1 | 1 | Nucleus |
Neutron | 0 | 1 | Nucleus |
Electron | –1 | 1/1836 | Outside nucleus |
3. Atomic Models (Very Exam-Heavy)
Thomson’s Model
“Plum pudding” model
Electrons embedded in a positive sphere
❌ Could not explain scattering results
Rutherford’s Nuclear Model
Gold foil experiment:
Most α-particles passed straight through
Some deflected
Few rebounded
Conclusions:
Atom is mostly empty space
Dense, positively charged nucleus
Limitations:
Could not explain atomic stability or line spectra
Bohr’s Model
Key ideas:
Electrons move in fixed energy levels (shells)
Energy is absorbed/emitted when electrons move between levels
Energy equation:
ΔE=hf\Delta E = hfΔE=hf
Limitations:
Works mainly for hydrogen
Fails for multi-electron atoms
📌 Exam tip: Know experiments, observations, conclusions, and limitations.
4. Atomic Number, Mass Number & Isotopes
Definitions
Atomic number (Z): Number of protons
Mass number (A): Protons + neutrons
Neutrons=A−Z\text{Neutrons} = A - ZNeutrons=A−Z
Isotopes
Same number of protons
Different number of neutrons
Same chemical properties, different physical properties
Examples:
Carbon-12, Carbon-13, Carbon-14
Uses:
Carbon-14 dating
Medical tracers
Nuclear energy
5. Relative Atomic Mass (Ar)
Definition
Weighted average mass of an element’s isotopes compared to 1/12 of carbon-12.
Calculation
Ar=∑(isotopic mass×abundance)100A_r = \frac{\sum (\text{isotopic mass} \times \text{abundance})}{100}Ar=100∑(isotopic mass×abundance)
📌 Exam tip: Expect full calculations with working and units.
6. Electromagnetic Radiation
Key Terms
Wavelength (λ)
Frequency (f)
Speed of light (c = 3.0 × 10⁸ m s⁻¹)
Relationship:
c=fλc = f\lambdac=fλ
Energy of radiation:
E=hfE = hfE=hf
Where:
h=6.63×10−34 J sh = 6.63 \times 10^{-34} \, \text{J s}h=6.63×10−34J s
7. Atomic Emission Spectra
Produced when excited electrons fall to lower energy levels
Each element has a unique line spectrum
Evidence for quantised energy levels
📌 Exam favourite: Link line spectra → Bohr model → energy levels.
8. Electron Arrangement
Shells & Sub-shells
Shells: n = 1, 2, 3, 4…
Sub-shells: s, p, d, f
Orbital Capacities
s: 2 electrons
p: 6 electrons
d: 10 electrons
f: 14 electrons
Filling Order
Aufbau principle:
1s → 2s → 2p → 3s → 3p → 4s → 3d → 4p …
Rules:
Pauli Exclusion Principle
Hund’s Rule
9. Ionisation Energy (Intro Link)
Definition:
Energy required to remove one mole of electrons from one mole of gaseous atoms to form 1+ ions
Trends (basic):
Increases across a period
Decreases down a group
Reasons:
Nuclear charge
Atomic radius
Shielding effect