HomeBlogPhysics › Radioactivity Guide

RADIOACTIVITY & NUCLEAR DECAY Alpha, Beta, Gamma Rays & Half-Life Physics N(t) = N₀ e⁻ˡᵗ | T₁/₂ = 0.693/λ | 1 Ci = 3.7×10¹⁰ Bq

Radioactivity & Nuclear Decay in Physics: Alpha, Beta, Gamma Rays Guide

By RRBCONTENTS Nuclear Physics Desk Published: July 27, 2026 | Updated: 2026-07-27
Radioactivity Physics Radioactive Decay Law Half-Life T1/2=0.693/λ Alpha Beta Gamma Rays Carbon-14 Dating Nuclear Medicine Isotopes 4000+ Words Complete Guide

Discovered accidentally by French physicist Henri Becquerel in 1896 and pioneered by Marie Curie and Pierre Curie, **Radioactivity** is the spontaneous disintegration of unstable atomic nuclei accompanied by the emission of ionizing radiation.

This 4,000+ word comprehensive exam guide covers **Rutherford's Discovery**, **Radioactive Decay Law ($N(t) = N_0 e^{-\lambda t}$)**, **Half-Life ($T_{1/2} = \frac{0.693}{\lambda}$)**, **Mean Life ($\tau = 1/\lambda$)**, comparison of **Alpha ($\alpha$), Beta ($\beta$), and Gamma ($\gamma$) Radiation**, **Soddy-Fajans Displacement Laws**, **Units of Radioactivity (Becquerel, Curie, Rutherford)**, **Carbon-14 Radiocarbon Dating**, **Medical Radioisotopes**, and solved numerical problems for SSC CGL, RRB NTPC, and UPSC Prelims.

Table of Contents

  1. 1. Discovery of Radioactivity & Natural vs Artificial Radioactivity
  2. 2. Rutherford-Soddy Law of Radioactive Decay ($N(t) = N_0 e^{-\lambda t}$)
  3. 3. Half-Life ($T_{1/2}$) & Mean Life ($\tau$) Formulas
  4. 4. Comparison of Alpha ($\alpha$), Beta ($\beta$) & Gamma ($\gamma$) Rays
  5. 5. Soddy-Fajans Group Displacement Laws
  6. 6. SI Units of Radioactivity: Becquerel (Bq), Curie (Ci) & Rutherford
  7. 7. Radiocarbon Dating ($^{14}\text{C}$) & Uranium-Lead Geological Dating
  8. 8. Applications of Radioisotopes in Medicine & Industry
  9. 9. Solved Numerical Examples for Competitive Exams
  10. 10. Must Remember Points for Quick Revision
  11. 11. Frequently Asked Questions (FAQ)

Key Takeaways & Core Highlights

N(t) = N₀ e⁻ˡᵗ
Decay Law Equation
T₁/₂ = 0.693/λ
Half-Life Formula
1 Ci = 3.7×10¹⁰ Bq
Curie to Becquerel
5,730 Yrs
Carbon-14 Half-Life

1. Discovery of Radioactivity & Natural vs Artificial Radioactivity

2. Rutherford-Soddy Law of Radioactive Decay ($N(t) = N_0 e^{-\lambda t}$)

The rate of disintegration ($-\frac{dN}{dt}$) of a radioactive sample at any instant is directly proportional to the number of active nuclei ($N$) present at that instant:

$$-\frac{dN}{dt} = \lambda \cdot N \implies N(t) = N_0 \cdot e^{-\lambda t}$$

Where $\lambda$ is the **Decay Constant (Disintegration Constant)** ($\text{s}^{-1}$).

3. Half-Life ($T_{1/2}$) & Mean Life ($\tau$) Formulas

$$\text{Half-Life } T_{1/2} = \frac{\ln 2}{\lambda} = \frac{0.69315}{\lambda}$$ $$\text{Mean Life } \tau = \frac{1}{\lambda} = \frac{T_{1/2}}{0.693} \approx 1.443 \cdot T_{1/2}$$

4. Comparison of Alpha ($\alpha$), Beta ($\beta$) & Gamma ($\gamma$) Rays

Property Alpha ($\alpha$) Rays Beta ($\beta$) Rays Gamma ($\gamma$) Rays
NatureHelium nuclei ($^4_2\text{He}^{2+}$)Fast electrons ($e^-$) or positrons ($e^+$)High-frequency Electromagnetic Photons
Charge$+2 e$$-1 e$ (or $+1 e$)Neutral ($0$)
Rest Mass$4 \text{ amu}$ ($6.64 \times 10^{-27}\text{ kg}$)$1/1836 \text{ amu}$ ($9.1 \times 10^{-31}\text{ kg}$)Zero rest mass
Speed$\sim 10^7 \text{ m/s}$ ($5\text{--}10\% \text{ of } c$)Up to $99\% \text{ of } c$Speed of Light ($c = 3 \times 10^8\text{ m/s}$)
Ionizing PowerHighest ($10,000 \times \gamma$)Moderate ($100 \times \gamma$)Lowest ($1$)
Penetrating PowerLowest (Stopped by paper / skin)Moderate (Stopped by $5\text{ mm}$ Aluminum)Highest (Requires thick Lead / Concrete)

5. Soddy-Fajans Group Displacement Laws

8. Applications of Radioisotopes in Medicine & Industry

Radioisotope Primary Medical / Industrial Application
Cobalt-60 ($^{60}\text{Co}$)Radiotherapy for Cancer Tumor treatment
Iodine-131 ($^{131}\text{I}$)Diagnosis and treatment of Thyroid gland disorders
Sodium-24 ($^{24}\text{Na}$)Detecting blood clots and circulation blockages
Phosphorus-32 ($^{32}\text{P}$)Leukemia treatment and agricultural fertilizer tracking
Carbon-14 ($^{14}\text{C}$)Radiocarbon dating of organic fossils

9. Solved Numerical Examples for Competitive Exams

Numerical Problem 1 (Half-Life Decay Calculation):

Question: A radioactive element has a half-life of $10\text{ days}$. What percentage of the original sample remains undecayed after $30\text{ days}$?

Solution:

$$\text{Number of half-lives } n = \frac{\text{Total Time } t}{T_{1/2}} = \frac{30}{10} = 3$$ $$\text{Remaining fraction } \frac{N}{N_0} = \left(\frac{1}{2}\right)^n = \left(\frac{1}{2}\right)^3 = \frac{1}{8} = 0.125 = 12.5\%$$

Answer: $12.5\%$ of the original sample remains.

Numerical Problem 2 (Curie to Becquerel Conversion):

Question: Express an activity of $5\text{ Curies}$ in Becquerels.

Solution:

$$1\text{ Ci} = 3.7 \times 10^{10} \text{ Bq}$$ $$\text{Activity } A = 5 \times 3.7 \times 10^{10} \text{ Bq} = 1.85 \times 10^{11} \text{ Bq}$$

Answer: Activity is $1.85 \times 10^{11}\text{ Bq}$.

10. Must Remember Points for Quick Revision

Exam Revision Cheat Sheet:

  • Decay Law: $N(t) = N_0 e^{-\lambda t}$. Exponential disintegration.
  • Half-Life: $T_{1/2} = 0.693/\lambda$. $N = N_0 (1/2)^n$.
  • Ionizing Power: $\alpha > \beta > \gamma$.
  • Penetrating Power: $\gamma > \beta > \alpha$.
  • SI Unit: Becquerel ($\text{Bq}$). $1\text{ Ci} = 3.7 \times 10^{10}\text{ Bq}$.
  • Carbon-14 Dating: $T_{1/2} = 5,730\text{ years}$ (Organic fossils up to 50k years).
  • Cobalt-60: Cancer therapy. Iodine-131: Thyroid treatment.

11. Frequently Asked Questions (FAQ)

What is the difference between Alpha (α), Beta (β), and Gamma (γ) radiation?

Alpha particles are Helium nuclei (⁴₂He²⁺) with high ionizing power but low penetrating power (stopped by paper). Beta particles are fast electrons (e⁻) or positrons (e⁺) with moderate ionizing and penetrating power (stopped by aluminum). Gamma rays are high-energy photons (EM radiation) with very low ionizing power but extreme penetrating power (requires thick lead/concrete).

What is the Half-Life (T₁/₂) of a radioactive substance?

Half-life is the time required for half of the initial number of radioactive nuclei in a sample to decay: T₁/₂ = (ln 2)/λ ≈ 0.693/λ. After n half-lives, remaining amount N = N₀ (1/2)ⁿ.

How does Carbon-14 Radiocarbon Dating work?

Living organisms absorb Carbon-14 (half-life T₁/₂ = 5,730 years) from the atmosphere. Upon death, C-14 intake stops and its activity decays. By measuring the remaining ratio of C-14 to stable C-12, scientists accurately date organic artifacts up to ~50,000 years old.

Related Physics & Science Guides

Continue your exam preparation with our comprehensive, deep-dive physics modules:

Master General Science & Physics on RRBCONTENTS

Practice PYQs, read formulas cheat sheets, and explore complete exam study modules.

Solve Physics PYQs → Explore Science Notes →

Join our official Telegram channel: @rrbcontents

🌐 Language