Chapter 8 - Particles in the Nucleus

8.1 Atoms, Isotopes and Radioisotopes

  • Earth is naturally radioactive; we are constantly exposed to background radiation.

  • Human senses cannot detect radiation, but our bodies are adapted to low levels. High doses can be damaging.

  • Radioactive atoms (radioisotopes) have beneficial uses (e.g., medicine).


The Standard Model

  • All matter is composed of 12 fundamental particles (fermions): 6 quarks and 6 leptons.

  • These are not seen in everyday situations; produced in high-energy particle accelerators.

  • Quarks (make up hadrons like protons & neutrons): up (u), down (d), charm (c), strange (s), top (t), bottom (b).

  • Leptons: electron (e⁻), muon (μ⁻), tau (τ⁻), and their neutrinos (ν_e, ν_μ, ν_τ).

  • Hadrons = particles made of quarks (baryons = 3 quarks; mesons = quark + antiquark).

    • Proton = uud (2 up + 1 down).

    • Neutron = udd (1 up + 2 down).


Fermions Table (masses relative to proton):

  • Quarks: Fractional charges (+2/3 or –1/3).

  • Leptons: Electron, muon, tau have charge –1; neutrinos have charge 0.


Antiparticles:

  • Same mass, opposite charge (or opposite quantum numbers).

  • Example: positron (e⁺) is antiparticle of electron.


The Structure of Atoms

  • Atoms consist of a tiny, dense nucleus (protons + neutrons = nucleons) surrounded by an electron cloud.

  • Nucleus contains >99% of atom’s mass but is extremely small (~10⁻¹² of atom’s volume).

  • Atomic notation: AZX

    • Z (atomic number) = number of protons.

    • A (mass number) = protons + neutrons (nucleons).

    • Neutrons (N) = A – Z.

Electrically neutral atom: Number of electrons = number of protons (Z).


Isotopes

  • Atoms of the same element (same Z) but different number of neutrons (different A).

  • Same chemical properties, different physical properties (e.g., density, mass).

  • Nuclide: Refers to a specific nucleus.

  • Hydrogen isotopes:

    • Protium (¹H): 1 proton, 0 neutrons.

    • Deuterium (²H): 1 proton, 1 neutron.

    • Tritium (³H): 1 proton, 2 neutrons.

Worked Example Highlights:

  • For ¹⁹⁷₇₉Au: Z=79 (protons), A=197 (nucleons), N=118, electrons=79.

  • Isotopes have same Z, different N and A.


Radioisotopes

  • Unstable isotopes that undergo spontaneous transmutation (emit radiation/particles and change into different element/isotope).

  • Most atoms are stable; only certain combinations of protons & neutrons are stable.

  • Radioactive if nucleus is unstable (naturally occurring or artificial).

  • Symbol: Radiation warning trefoil (Figure 8.1.11).

  • Periodic table: All isotopes of elements with Z > 83 (bismuth) are radioactive; many lighter elements have radioactive isotopes (shaded yellow in Figure 8.1.12).


Artificial Transmutation: How Radioisotopes Are Manufactured

  • Most radioisotopes (~3000) are produced artificially (only ~270 occur naturally).

  • Common method: Neutron absorption in a nuclear reactor.

    • Stable isotope + neutron → radioactive isotope.

  • Example: Cobalt-59 (stable) + neutron → Cobalt-60 (radioactive, used in medicine).

  • Produced in facilities like ANSTO (Lucas Heights, Sydney) using nuclear reactors.


Stability of Nuclei and Why Radioactive Nuclei Are Unstable

  • Strong nuclear force (mediated by gluons) holds nucleus together — very strong but short-range.

  • Electrostatic repulsion between protons tries to break nucleus apart.

  • Line of stability (Figure 8.1.15): Stable nuclei cluster around a curved line (N ≈ Z for light elements; N > Z for heavier elements).

  • For stability, neutrons help “dilute” proton repulsion.

  • Unstable nuclei (away from line) emit radiation (α, β⁻, β⁺) to reach stability.

  • Bismuth-209 is the heaviest stable isotope; heavier nuclei are unstable.


Examples:

  • Small balanced nuclei (e.g., carbon-12) are stable.

  • Large nuclei with too many protons or neutrons become unstable.


8.2 Radiation

  • Early researchers (Marie Curie, Ernest Rutherford, Paul Villard) discovered three types of radiation: alpha (α), beta (β), and gamma (γ).

  • Alpha & beta are particles emitted from the nucleus.

  • Gamma is high-energy electromagnetic radiation.

  • Radioactive decay: Process where unstable nucleus emits particles/radiation.


Alpha (α) Decay

  • Occurs in heavy unstable nuclei.

  • Emits an alpha particle (⁴₂α or ⁴₂He²⁺): 2 protons + 2 neutrons (helium nucleus).

  • Nuclear equation example (Uranium-238): ²³⁸₉₂U → ²³⁴₉₀Th + ⁴₂α + energy

  • Parent nucleus → daughter nucleus (different element = nuclear transmutation).

  • Atomic number decreases by 2; mass number decreases by 4.

  • Energy released mostly as kinetic energy of the fast-moving alpha particle.

Conservation: Atomic number (Z) and mass number (A) are conserved in nuclear reactions.


Beta (β) Decay

Beta-Minus (β⁻) Decay

  • Occurs when nucleus has too many neutrons.

  • A neutron changes into a proton + electron (β⁻) + antielectron neutrino (ν̅_e).

  • Example (Carbon-14): ¹⁴₆C → ¹⁴₇N + ⁻¹₀β + ν̅_e + energy

  • Atomic number increases by 1; mass number unchanged.

  • Beta particle is a high-energy electron from the nucleus.


Beta-Plus (β⁺) Decay

  • Occurs when nucleus has too many protons.

  • A proton changes into a neutron + positron (β⁺) + electron neutrino (ν_e).

  • Example: ¹²₆C → ¹²₅B + ¹₀β⁺ + ν_e

  • Atomic number decreases by 1; mass number unchanged.

  • Positron (β⁺) is the antiparticle of the electron (positive charge).


Gamma (γ) Decay

  • High-energy electromagnetic radiation (no mass, no charge).

  • Emitted when daughter nucleus is in an excited state after α or β decay.

  • Releases excess energy; nucleus rearranges to more stable state.

  • Example (Iodine-131 decay sequence): Beta decay → excited Xenon-131 → stable Xenon-131 + γ

  • No change in atomic or mass number.

  • Travels at speed of light.


Conservation Laws in Nuclear Reactions

  • Mass-energy: Total energy (rest mass + kinetic) is conserved (E = mc²).

  • Charge: Total charge before = total charge after.

  • Momentum: Total momentum before = total after.

  • Atomic and mass numbers are always conserved.

Worked Example Insight: Energy differences in decays are calculated in MeV (mega-electron volts).





Range of Energies for Different Radiations

  • Alpha particles: 5–10 MeV (or MeV range).

  • Beta particles: Up to a few MeV.

  • Gamma rays: Typically < 1 MeV (e.g., up to 412 keV for gold-198).

Higher energy → greater speed/frequency (for gamma).


Detection of Radiation

  • Human senses cannot detect it.

  • Geiger Counter (Geiger-Müller tube):

    • Filled with argon gas.

    • High voltage between electrodes.

    • Radiation ionises gas → current pulse → audible click.

  • Used for mineral exploration, safety monitoring, medical/industrial checks.


Physics in Action: How Technetium-99m is Produced

  • Most widely used radioisotope in nuclear medicine (cancer diagnosis/treatment).

  • Produced from Molybdenum-99 (from Lucas Heights reactor) via beta-minus decay: ⁹⁹₄₂Mo → ⁹⁹ᵐ₄₃Tc + ⁻¹₀β + ν̅_e

  • Tc-99m then emits gamma ray: ⁹⁹ᵐ₄₃Tc → ⁹⁹₄₃Tc + ⁰₀γ

  • Short half-life → produced on-site in hospital generators (lead-shielded).


8.3 Properties of Alpha, Beta and Gamma Radiation

  • Early experiments (with radium) using a magnetic field showed three distinct types of radiation (Figure 8.3.1):

    • Alpha (α): Deflected one way (positively charged).

    • Beta (β): Deflected the opposite way (negatively charged).

    • Gamma (γ): Not deflected (no charge).

  • Differences in charge, mass, and speed.


Speed and Charge

Alpha (α) Particles (Figure 8.3.2)

  • Consist of 2 protons + 2 neutrons (helium nucleus, ⁴₂He²⁺).

  • Charge: +2.

  • Mass: Relatively heavy.

  • Speed: Slow — up to 20,000 km/s (about 0.1c or 10% speed of light).

Beta-Minus (β⁻) and Beta-Plus (β⁺) Particles (Figure 8.3.3)

  • β⁻: Fast-moving electrons (negative charge).

  • β⁺: Positrons (positive charge, antiparticle of electron).

  • Mass: Very light (much lighter than alpha).

  • Speed: Very fast — up to ~90% speed of light (0.9c).

Gamma (γ) Rays (Figure 8.3.5)

  • High-energy electromagnetic radiation (part of EM spectrum, Figure 8.3.4).

  • Charge: 0 (no charge).

  • Mass: None (no rest mass).

  • Speed: Speed of light (3.00 × 10⁸ m/s).


Penetration Ability and Ionisation

Alpha (α) Particles (Figure 8.3.6)

  • High ionising ability: Strongly interact with atoms, knock off electrons, create ions.

  • Low penetration: Travel only a few centimetres in air; stopped by paper, skin, or thin card.

  • Easily absorbed — become helium atoms after gaining electrons.

Beta (β) Particles (Figure 8.3.8)

  • Low ionising ability: Fewer interactions due to smaller charge and higher speed.

  • Moderate penetration: Travel a few metres in air; stopped by a few mm of aluminium or thin metal/plastic sheet.

  • Can pass through skin but stopped by thin metal.

Gamma (γ) Rays

  • Very low ionising ability: Weak interaction with matter (only ionise if direct collision).

  • High penetration: Travel long distances in air; penetrate through human body, aluminium sheets, and several cm of lead (thick lead or concrete needed to stop).


Summary Table 8.3.1: Comparison of Properties

Property

Alpha (α) Particle

Beta (β) Particles

Gamma (γ) Ray

Mass

Heavy

Light

None

Speed

~10% c (slow)

~90% c (very fast)

Speed of light (c)

Charge

+2

–1 or +1

0

Ionising Ability

Very high

Low

Very low

Range in Air

A few centimetres

1 or 2 metres

Many metres

Penetration in Matter

~10⁻² mm (paper/skin)

A few mm (thin aluminium)

High (thick lead/concrete)


Physics in Action: Applications

Monitoring Thickness of Sheet Metal (Figure 8.3.10)

  • Beta-minus particles used.

  • Source under sheet; detector above.

  • Fewer beta particles reach detector if sheet is thicker → adjusts rollers automatically.

Gamma Knife Therapy (Figure 8.3.11)

  • Focused gamma beams from many directions target bra


  • in tumours.

  • High dose at tumour; surrounding tissue receives low dose.

Smoke Detectors

  • Use alpha emitter (e.g., Americium-241) — alpha particles ionise air; smoke reduces current, triggers alarm.


8.4 Half-Life and Decay Series

  • Different radioisotopes decay at different rates.

  • Activity: Rate of radioactive decay (measured by Geiger counter as counts per second).

  • Example:

    • Polonium-218: High initial activity, drops rapidly (almost zero in ~30 minutes).

    • Uranium-235: Low activity, remains almost constant over decades (Figure 8.4.1).


Half-Life (t₁/₂)

  • Definition: Time taken for half of the radioactive nuclei in a sample to decay.

  • Half-life is constant for a given radioisotope and cannot be changed by chemical reactions, heat, etc.

  • Determined only by nuclear instability.

  • Example: Polonium-218 has t₁/₂ ≈ 3.10 minutes.

Mathematical Formula:

  • Number of nuclei remaining:

  • Number of half-lives:

Decay Curve: Exponential decay — activity halves

with each half-life.

Worked Example Insight:

  • After each half-life, activity and number of nuclei halve (100% → 50% → 25% → 12.5%, etc.).


Activity (A)

  • Activity (A): Number of disintegrations per second (measured in becquerels, Bq). 1 Bq = 1 disintegration/second.

  • Formula:

    ?

  • Activity also follows:

Worked Example Insight:

  • Technetium-99m (short half-life) activity drops rapidly — useful for medical imaging.


Common Radioisotopes and Their Applications (Table 8.4.1)


Decay Series

  • Decay of a radioisotope often produces another radioactive daughter nucleus → continues until a stable isotope is reached.

  • Decay series: Sequence of decays (Figure 8.4.4 shows Uranium-238 series).

  • Uranium-238 series ends at stable Lead-206.

  • Earth is old enough (4.5 billion years) that only 4 natural decay series remain active (Uranium, Actinium, Thorium, Neptunium).

Applications:

  • Rock dating: Measure proportions of radioactive elements and daughters in rocks.


Extension: Radiocarbon Dating33

  • Uses Carbon-14 (t₁/₂ = 5730 years, β⁻ decay to Nitrogen-14).

  • Living organisms have constant C-14/C-12 ratio (from atmosphere).

  • After death, C-14 decays and is not replaced → ratio decreases.

  • Compare C-14/C-12 ratio to estimate age (accurate up to ~60,000 years).

  • Examples: Shroud of Turin (medieval), mammoth fossils.


8.5 Radiation Doses and Effects on Humans

  • We are constantly exposed to low-level background radiation (natural sources).

  • High exposure from α, β, γ sources (medicine, industry, nuclear power) can be harmful.

  • Monitoring is essential for workers (radiologists, nuclear plant staff) and patients (cancer treatment).

  • Dosimeters measure personal exposure


Ionising Radiation

  • Ionising radiation: High-energy EM radiation (frequency > 2.00 × 10¹⁶ Hz) that can remove electrons from atoms, creating ions (Figure 8.5.3).

    • Includes: Gamma rays, X-rays, and some UV.

  • Non-ionising radiation: Lower energy (radio waves, microwaves, visible light, infrared, UV-A) — generally harmless in everyday amounts (Figure 8.5.2).

Effects of Ionisation:

  • Breaks chemical bonds in molecules (e.g., water → ions).

  • Can damage cells, cause cancer, or lead to radiation sickness.


Measuring Radiation Exposure

Absorbed Dose (AD)

  • Energy absorbed per kilogram of tissue.

  • Formula:

  • Unit: Gray (Gy) → 1 Gy = 1 J/kg.

Dose Equivalent (DE)

  • Accounts for the type of radiation (different biological damage).

  • Formula: DE = AD × QF (QF = quality factor / weighting factor).

  • Unit: Sievert (Sv) or millisievert (mSv), microSievert (μSv).

Quality Factors (Table 8.5.1):

  • α particles: 20 (highly damaging due to high charge, mass, low speed).

  • Neutrons (10 keV): 10.

  • β particles, γ rays, X-rays: 1.


Background Radiation

  • Average annual exposure in Australia: ~1.5 mSv.

  • Sources (Figure 8.5.4 & 8.5.6):

    • Natural (~90%): Cosmic rays, rocks/soil, food/drink, radon gas, natural radioactivity in air.

    • Artificial: Medical (X-rays), nuclear power, etc.

  • Background radiation is low and generally not harmful.


Effect of Radiation Exposure on Humans

  • Symptoms: Nausea, fatigue, hair loss, reduced white blood cells, cancer risk.

  • Rapidly dividing cells (cancer, bone marrow) are most vulnerable.


Medical Applications of Radiation

  • Cancer treatment: Targeted radiation (e.g., cobalt-60) damages cancer cells more than healthy tissue (Figure 8.5.8).

  • Radioactive tracers (Table 8.5.5): Short half-life isotopes injected/ingested to image organs.

  • Scintigraphy: Gamma camera detects tracer emissions to create images (Figure 8.5.10).

Typical Medical Exposures (Table 8.5.4):

  • Chest X-ray: 30 μSv.

  • CT scan: 5000 μSv.

  • Radiotherapy course: Very high (targeted).


Physics in Action: Scintigraphy

  • Uses radioactive tracers with same chemical properties as stable isotopes.

  • Tracer emits gamma rays → detected to map organ function.

Dosimeters (Figure 8.5.5):

  • Thermoluminescent dosimeters (TLDs) used by workers for accurate monitoring.