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PC10 — Atomic & Nuclear Physics

📖 PC10  ·  CDS General Science — Physics 🎯 CDS Level : High Priority

Nuclear physics explores the innermost structure of matter — atoms, nuclei, and the immense energy locked within. CDS consistently tests atomic models, types of radioactive decay, half-life, and the distinction between nuclear fission and fusion. This chapter is scoring when studied systematically.

📌 CDS focuses on: Atomic models (Rutherford, Bohr); radioactivity — types (α, β, γ) and their properties; half-life concept; nuclear fission vs fusion; mass-energy equivalence E = mc²; applications (nuclear reactor, atomic bomb, hydrogen bomb, X-rays).

Topics at a Glance

① Atomic Models
Thomson, Rutherford, Bohr, quantum
② Radioactivity
α, β, γ decay — properties
③ Half-Life
Decay rate; amount remaining
④ Nuclear Fission
Heavy nucleus splits; chain reaction
⑤ Nuclear Fusion
Light nuclei combine; stars; H-bomb
⑥ X-rays & E=mc²
Properties; mass-energy equivalence

1. Atomic Models

1.1
Evolution of the Atomic Model
From plum pudding to quantum cloud — how our understanding evolved
Evolution of Atomic Models THOMSON (1897) "Plum Pudding" Electrons (●) embedded in diffuse +ve sphere ✗ Could not explain Rutherford's results RUTHERFORD (1911) Nuclear Model Nucleus (+ve) Tiny +ve nucleus; electrons orbit at large distances ✗ Could not explain atomic stability (e⁻ loses energy) BOHR (1913) Quantised Orbits Electrons in fixed orbits (shells) — no energy loss ✓ Explained hydrogen spectrum successfully
Fig. 1 — Three landmark atomic models. Bohr's model (1913) was the first to successfully explain the hydrogen emission spectrum using quantised (fixed-energy) electron orbits.
Bohr's Postulates (key for CDS):
1. Electrons revolve in fixed circular orbits (shells) — specific allowed radii only.
2. While in these orbits, electrons do NOT emit radiation (no energy loss — stable orbits).
3. When an electron jumps from a higher orbit to a lower orbit, it emits a photon of energy = difference in energy levels: E = hf.
4. When a photon is absorbed, the electron jumps to a higher orbit.

2. Radioactivity

2.1
Alpha, Beta & Gamma Radiation — Properties & Penetration
Three very different forms of radiation from unstable nuclei
Penetrating Power of Radioactive Radiations Radio- active Source α (Alpha) Paper β (Beta) Al (3mm) γ (Gamma) Lead (many cm) partially absorbed Penetrating power: γ >> β > α  |  Ionising power: α >> β > γ  |  α stopped by paper; β by Al; γ by thick lead
Fig. 2 — Penetrating and ionising power of the three radiations are inversely related. Alpha is the most ionising but least penetrating; gamma is least ionising but most penetrating.
PropertyAlpha (α)Beta (β)Gamma (γ)
NatureHelium nucleus (2p + 2n; charge +2)Fast electron (charge −1)Electromagnetic radiation (no charge, no mass)
PenetrationLeast — stopped by paper or few cm airModerate — stopped by a few mm AlGreatest — needs several cm of lead/concrete
Ionising powerGreatest (most dangerous to nearby tissue)ModerateLeast (but penetrates deep into body)
Deflection in fieldDeflected toward negative plateDeflected toward positive plate (opposite to α)Not deflected (no charge)
Speed~0.1c (slowest)Up to 0.9cSpeed of light c (fastest)

3. Half-Life

3.1
Radioactive Decay Rate
⚡ Half-Life Calculations
Half-life (T½): Time in which half the atoms in a radioactive sample decay. After n half-lives: Remaining amount = N₀ × (1/2)ⁿ = N₀ / 2ⁿ Examples: Initial amount: 80 g; T½ = 10 years After 10 yr: 40 g (n=1); After 20 yr: 20 g (n=2); After 30 yr: 10 g (n=3) If T½ = 5 years and initial amount = 160 g: After 20 years (= 4 half-lives): remaining = 160/2⁴ = 160/16 = 10 g Carbon dating: Carbon-14 has T½ ≈ 5730 years → used to date archaeological specimens up to ~50,000 years old.

4. Nuclear Fission vs Fusion

4.1
Two Ways to Release Nuclear Energy

⚡ Nuclear Fission

  • A heavy nucleus (e.g. Uranium-235 or Plutonium-239) splits into smaller nuclei when struck by a neutron
  • Produces 2-3 more neutrons → chain reaction possible
  • Releases enormous energy (from mass-energy conversion)
  • Atomic bomb (A-bomb): uncontrolled fission chain reaction
  • Nuclear reactor: controlled fission; used to generate electricity
  • Moderator (heavy water/graphite) slows neutrons; Control rods (cadmium) absorb neutrons

⚡ Nuclear Fusion

  • Light nuclei (hydrogen isotopes — deuterium + tritium) combine to form heavier nucleus (helium) + energy
  • Releases MORE energy per unit mass than fission
  • Requires extremely high temperature (~10⁷ to 10⁸ K) — "thermonuclear reaction"
  • Hydrogen bomb (H-bomb): uncontrolled fusion (triggered by fission bomb)
  • Sun's energy source: hydrogen nuclei fusing into helium continuously
  • Controlled fusion (ITER project): future clean energy goal
⚡ Mass-Energy Equivalence (E = mc²)
Einstein's equation: E = mc² E = energy released (Joules) m = mass converted (kg) c = speed of light = 3 × 10⁸ m/s In nuclear reactions, a tiny loss of mass (mass defect) results in enormous energy release. Even 1 gram of mass = 9 × 10¹³ J of energy. Mass defect: actual mass of nucleus < sum of masses of protons + neutrons Binding energy: energy needed to break the nucleus apart into constituents. Higher binding energy per nucleon → more stable nucleus. Iron-56 has highest binding energy per nucleon (most stable element).
⚠ Fission vs Fusion Traps: (1) Atomic bomb = fission (U-235 or Pu-239); Hydrogen bomb = fusion (triggered by fission). (2) Sun works by fusion — NOT fission. (3) Nuclear power plants use fission — NOT fusion (controlled fusion is not yet commercial). (4) Fusion releases MORE energy per unit mass than fission. (5) Moderator slows neutrons; control rod absorbs neutrons — different functions.
📝 CDS PYQ
Atomic & Nuclear Physics
Q1. The half-life of a radioactive substance is 10 years. Starting with 80 g, how much remains after 30 years?
  • (a) 40 g
  • (b) 20 g
  • (c) 10 g
  • (d) 5 g
Answer: (c) 10 g
30 years = 3 half-lives (30÷10=3). Remaining = 80 × (1/2)³ = 80/8 = 10 g. After each half-life: 80→40→20→10 g. This is the most frequently tested half-life type in CDS — always divide the total time by T½ to find n, then apply N₀/2ⁿ.
Q2. The energy produced in the Sun comes from:
  • (a) Nuclear fission
  • (b) Chemical combustion
  • (c) Nuclear fusion
  • (d) Radioactive decay
Answer: (c) Nuclear fusion
The Sun produces energy by the thermonuclear fusion of hydrogen nuclei (protons) forming helium nuclei. The enormous gravitational pressure at the Sun's core maintains the extreme temperatures (~15 million K) needed for fusion. This converts ~4 million tonnes of mass to energy per second via E = mc². Nuclear power plants use fission — the Sun uses fusion.
Q3. Which radiation cannot be deflected by electric or magnetic fields?
  • (a) Alpha
  • (b) Beta
  • (c) Gamma
  • (d) Both alpha and beta
Answer: (c) Gamma
Gamma radiation consists of electromagnetic waves — it has no charge and no mass. Since electric and magnetic fields act on charged particles, gamma rays are not deflected. Alpha particles (charge +2) deflect toward the negative plate; beta particles (charge −1) deflect toward the positive plate. Gamma rays travel straight through both electric and magnetic fields.
Q4. In a nuclear reactor, the function of the moderator (heavy water) is to:
  • (a) Absorb all neutrons to stop the reaction
  • (b) Slow down fast neutrons to thermal speeds
  • (c) Reflect neutrons back into the core
  • (d) Cool the reactor
Answer: (b) Slow down fast neutrons to thermal speeds
The moderator (heavy water D₂O, ordinary water H₂O, or graphite) slows down fast neutrons produced in fission so they can be captured by U-235 atoms to sustain the chain reaction. Slow (thermal) neutrons are more easily absorbed by U-235 than fast neutrons. Control rods (cadmium or boron) absorb neutrons to control the reaction rate — different from the moderator's function.

📚 Formula Sheet — PC10

⚡ Radioactivity
  • α = helium nucleus; +2 charge
  • β = electron; −1 charge
  • γ = EM wave; no charge, no mass
  • Penetration: γ > β > α
  • Ionising: α > β > γ
⏳ Half-Life
  • Remaining = N₀ / 2ⁿ
  • n = total time / T½
  • C-14: T½ = 5730 yr (dating)
  • U-238: T½ = 4.5 billion yr
  • Each half-life: amount halves
⚡ Fission vs Fusion
  • Fission: U-235 splits; A-bomb; reactors
  • Fusion: H-isotopes join; H-bomb; Sun
  • E = mc²; c = 3×10⁸ m/s
  • Moderator slows neutrons
  • Control rods absorb neutrons
🔬 Atomic Models
  • Thomson: plum pudding
  • Rutherford: nuclear (tiny +ve nucleus)
  • Bohr: fixed quantised orbits
  • Bohr: explained H spectrum
  • Quantum: electron cloud (modern)

⚡ Quick Revision — PC10

⚡ Radiation Summary
  • α: heaviest, most ionising, least penetrating
  • γ: massless, least ionising, most penetrating
  • α deflects to −ve plate; β to +ve plate
  • γ: not deflected by fields
  • All three stopped by: α=paper; β=Al; γ=lead
⏳ Half-Life
  • n half-lives → N₀/2ⁿ remaining
  • C-14 dating: up to 50,000 years
  • Decay is random but predictable statistically
  • T½ unchanged by temp/pressure/chemical state
🚨 CDS Traps
  • Sun = fusion (not fission)
  • Nuclear reactor = controlled fission
  • A-bomb = fission; H-bomb = fusion
  • Moderator ≠ control rod
  • Fusion releases more energy per kg than fission

📝 Practice Exercise

E-01
The half-life of a radioactive element is 5 years. If you start with 64 g, how much remains after 20 years?
  • (a) 8 g
  • (b) 4 g
  • (c) 16 g
  • (d) 2 g
E-02
Nuclear fission involves:
  • (a) Combining two light nuclei
  • (b) Splitting a heavy nucleus into lighter nuclei
  • (c) Emission of gamma rays only
  • (d) Conversion of neutrons into protons only
E-03
Which atomic model successfully explained the line spectrum of hydrogen?
  • (a) Thomson model
  • (b) Rutherford model
  • (c) Bohr model
  • (d) Dalton model
Answers:  E-01: (b) 4 g [n = 20/5 = 4 half-lives; remaining = 64/2⁴ = 64/16 = 4 g]  |  E-02: (b) Splitting a heavy nucleus — fission; fusion combines light nuclei  |  E-03: (c) Bohr model — proposed quantised orbits, explaining H emission spectrum (Balmer series etc.)
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