E3-1. Isotopes, Background Radiation, and Radioactive Particles
1. Isotopes and Isotopic Data
Definition of Isotopes
- Elements are defined by a fixed number of protons (Atomic Number, $Z$) in their atoms.
- However, atoms of the exact same element can possess different numbers of neutrons (Neutron Number, $N$).
- An isotope is formally defined as: Nuclei that have the same number of protons but different numbers of neutrons.
- Because they have different neutron counts, isotopes have a different Nucleon Number ($A = Z + N$), meaning they have different atomic masses.
Relative Atomic Mass and Abundance
- Some isotopes have an imbalance of protons and neutrons, making them unstable and prone to radioactive decay.
- The relative atomic mass displayed on the periodic table is a weighted average that takes into account the masses and natural percentage abundances of all naturally occurring isotopes of an element.
2. Background Radiation and the Random Nature of Decay
Spontaneous and Random Decay
- Radioactive decay is the spontaneous disintegration of a nucleus to form a more stable nucleus, resulting in the emission of an alpha, beta, or gamma particle.
- Spontaneous: The process cannot be influenced by environmental factors such as temperature, pressure, or chemical conditions.
- Random: The exact time of decay of a single nucleus cannot be predicted. However, an unstable nucleus has a constant probability of decaying in a given time, allowing for statistical predictions over large groups of nuclei.
Background Radiation Sources
- Background radiation is the ionising radiation constantly present in our environment.
- Natural Sources: Radon gas from rocks and buildings constitutes the largest proportion (approx. 50%), followed by rocks/building materials (15%), cosmic rays from space (10%), and food/drink like carbon-14 and potassium-40 (11%).
- Artificial Sources: Medical procedures like X-rays and CT scans (13%), nuclear fallout, and nuclear waste (<1%).
- When measuring activity in a lab, the corrected count rate must be calculated by subtracting the background count rate from the measured source count rate.
3. Types of Radioactive Particles
| Particle | Composition | Charge / Mass | Ionising & Penetrating Power |
|---|---|---|---|
| Alpha ($\alpha$) | Helium nucleus (2 protons, 2 neutrons) | $+2e$ / $4\text{ u}$ | Highly ionising. Very low penetration (stopped by a few cm of air or paper). |
| Beta Minus ($\beta^-$) | High-energy electron emitted from the nucleus. | $-1e$ / $\sim 0.0005\text{ u}$ | Moderately ionising. Moderate penetration (stopped by a few mm of aluminum). |
| Beta Plus ($\beta^+$) | High-energy positron (antimatter electron). | $+1e$ / $\sim 0.0005\text{ u}$ | Annihilates upon contact with an electron, creating gamma rays. |
| Gamma ($\gamma$) | High-frequency electromagnetic wave (photon). | $0$ / $0$ | Weakly ionising. Highly penetrating (requires thick lead or concrete to reduce intensity). |
4. Advanced HL Examples
Example 1: Deflection in a Uniform Magnetic Field (Classic IB Mechanics Bridge)
Problem: A radioactive source emits a mixed beam of alpha ($\alpha$), beta-minus ($\beta^-$), and gamma ($\gamma$) radiation. The beam passes through a velocity selector, so all particles enter a uniform magnetic field $B$ (directed into the page) at the exact same velocity $v$.
(a) Describe the direction of deflection for each of the three radiations.
(b) Analytically prove which particle ($\alpha$ or $\beta^-$) will travel in a circular path with the larger radius, and calculate the exact ratio of their radii ($r_{\alpha} / r_{\beta}$). Assume $m_{\alpha} \approx 4\text{ u}$ and $m_{\beta} \approx \frac{1}{1836}\text{ u}$.
Solution:
Part (a): Direction of Deflection:
Using Fleming's Left-Hand Rule (or Right-Hand Palm Rule):
• The $\alpha$ particle is positive. Current is in the direction of velocity. The magnetic force deflects it upwards.
• The $\beta^-$ particle is negative. Current is opposite to velocity. The magnetic force deflects it downwards.
• The $\gamma$ ray has no charge. It experiences no magnetic force and travels straight through undeflected.
Part (b): Radii of Curvature:
Equating magnetic force to centripetal force: $qvB = \frac{mv^2}{r} \implies r = \frac{mv}{qB}$.
Because $v$ and $B$ are constant for both, the radius is proportional to the mass-to-charge ratio ($m/q$).
• For Alpha: $q_{\alpha} = +2e$, $m_{\alpha} = 4\text{ u}$. Thus, $r_{\alpha} \propto \frac{4}{2} = 2$.
• For Beta: $q_{\beta} = -1e$, $m_{\beta} = \frac{1}{1836}\text{ u}$. Thus, $r_{\beta} \propto \frac{1/1836}{1} \approx 0.00054$.
To find the exact ratio:
$$\frac{r_{\alpha}}{r_{\beta}} = \frac{\frac{m_{\alpha} v}{q_{\alpha} B}}{\frac{m_{\beta} v}{q_{\beta} B}} = \left(\frac{m_{\alpha}}{m_{\beta}}\right) \left(\frac{q_{\beta}}{q_{\alpha}}\right) = \left(\frac{4}{1/1836}\right) \left(\frac{1}{2}\right) = (7344) \times (0.5) = \mathbf{3672}$$
The alpha particle's radius is $3672$ times larger than the beta particle's. The beta particle curves very tightly, while the massive alpha particle barely curves at all!
Example 2: University Bridge — Statistics of Random Decay
Problem: Because radioactive decay is a purely random, stochastic process, the number of counts $N$ detected by a GM tube in a given time interval follows a Poisson distribution. In Poisson statistics, the absolute uncertainty (standard deviation) of a count is given by $\sigma = \sqrt{N}$.
A student measures the background radiation for 10 minutes and records 250 counts. They then place a radioactive source near the detector and record 3400 counts in 5 minutes. Calculate the corrected count rate in counts per minute (cpm) and determine its absolute uncertainty.
Solution:
Step 1: Calculate the background rate ($R_b$) and its uncertainty. $$N_b = 250 \implies \sigma_b = \sqrt{250} \approx 15.8 \text{ counts}$$ $$R_b = \frac{250}{10} = 25.0 \text{ cpm}$$ The uncertainty in the rate is $\frac{15.8}{10} = 1.58 \text{ cpm}$. So, $R_b = 25.0 \pm 1.6 \text{ cpm}$.
Step 2: Calculate the total source rate ($R_{total}$) and its uncertainty. $$N_{total} = 3400 \implies \sigma_{total} = \sqrt{3400} \approx 58.3 \text{ counts}$$ $$R_{total} = \frac{3400}{5} = 680 \text{ cpm}$$ The uncertainty in the rate is $\frac{58.3}{5} = 11.66 \text{ cpm}$. So, $R_{total} = 680 \pm 12 \text{ cpm}$.
Step 3: Calculate the corrected count rate ($R_c$) and propagate the errors. $$R_c = R_{total} - R_b = 680 - 25 = \mathbf{655 \text{ cpm}}$$ When adding or subtracting quantities with independent random uncertainties, we add their absolute uncertainties in quadrature (Pythagorean addition): $$\sigma_c = \sqrt{(\sigma_{R\_total})^2 + (\sigma_{R\_b})^2} = \sqrt{(11.66)^2 + (1.58)^2} = \sqrt{135.95 + 2.50} = \sqrt{138.45} \approx \mathbf{11.8 \text{ cpm}}$$ The final corrected count rate is strictly reported as $655 \pm 12 \text{ cpm}$.