Comprehensive Study Notes on Radioactivity

Radioactivity

Marie Curie's Life and Work

  • Marie Curie and Pierre Curie's marriage in 1895:

    • Marked the beginning of a partnership that led to significant discoveries.

  • Henri Becquerel's discovery in 1896:

    • Discovered radioactivity in uranium, which Marie Curie investigated further.

    • Marie Curie found radioactivity in thorium as well.

  • Nobel Prizes:

    • 1903 Nobel Prize in Physics: Awarded to Marie Curie, Pierre Curie, and Henri Becquerel.

    • 1911 Nobel Prize in Chemistry: Awarded solely to Marie Curie.

    • Marie Curie was the first woman to win a Nobel Prize.

  • Marie Curie's Early Life:

    • Exceptional memory from childhood.

    • Won a gold medal at the age of 16.

  • Marie Curie's Achievements:

    • Understood the importance of accumulating intense radioactive sources.

    • For treating illnesses and maintaining research supplies.

    • The Radium Institute in Paris had a stock of 1.5.

Radioactive Decay

  • Definition: Radioactive decay is the process where an unstable nucleus transforms into a more stable nucleus by emitting radiation (energy).

  • Nature of the Process:

    • Random: It is impossible to predict which specific nucleus will decay next.

    • Spontaneous: The process is not influenced by external conditions like temperature and pressure.

  • Radioisotopes:

    • Many elements have radioactive isotopes (radioisotopes) due to unstable nuclei.

    • Instability is often caused by a large number of nucleons, particularly an excess of neutrons.

    • Examples: cesium, cobalt, iodine, plutonium, radon, strontium, thorium, uranium.

Nuclear Stability

  • Nuclear Instability:

    • In large nuclei, nucleons are not held together as tightly due to the short effective range of the strong nuclear force, leading to instability.

    • Adding or subtracting neutrons can influence nuclear stability.

Types of Nuclear Emission

  • Emission Types:

    • Radioactive substances emit alpha particles, beta particles, or gamma rays.

    • Emission may also include energy in the form of rays.

  • Transformation of Elements:

    • The atom transforms into an atom of another element due to changes in the number of protons in the nucleus.

  • Outcomes of Emission:

    • Increased stability of the nucleus.

    • Reduction in excess neutrons.

Characteristics of Alpha, Beta, and Gamma Radiation

  • Alpha Particles:

    • Symbol: α

    • Composition: 2 protons + 2 neutrons

    • Mass: Approximately 4 times the mass of a proton, (4×mass of proton)(\approx 4 \times \text{mass of proton})

    • Speed: About 3×1073 \times 10^7 m/s

    • Charge: +2e

  • Beta Particles:

    • Symbol:

    • Composition: An electron

    • Mass: Approximately (mass of proton/1840)(\text{mass of proton} / 1840)

    • Speed: About 2.9×1082.9 \times 10^8 m/s

    • Charge: -1e

  • Gamma Rays:

    • Symbol: γ

    • Composition: Electromagnetic radiation

    • Mass: 0

    • Speed: 3×1083 \times 10^8 m/s

    • Charge: 0

  • Origin of Beta Particles:

    • Beta particles originate from inside the nucleus, where a neutron decays into a proton and an electron.

    • Equation: 01n11p+10e_{0}^{1}n \rightarrow _{1}^{1}p + _{-1}^{0}e

Ionizing Power

  • Depends on kinetic energy and charge.

  • Alpha Particles:

    • Most ionizing due to large mass and kinetic energy.

    • Interact heavily with surrounding material, pulling electrons off atoms.

  • Beta Particles:

    • Less ionizing than alpha particles.

  • Gamma Radiation:

    • Least ionizing.

  • Alpha particles are more harmful when inhaled or ingested.

    • Example: radon and thoron gases.

Penetrating Power

  • Alpha Particles:

    • Easily absorbed.

    • Travel about 5 cm in air before being absorbed.

    • Cannot penetrate a thin sheet of paper or skin.

  • Beta Particles:

    • Travel fairly easily through air or paper.

    • Absorbed by a few millimeters of metal, such as aluminum.

  • Gamma Radiation:

    • Most penetrating.

    • Requires several centimeters of dense metal (e.g., lead) or several meters of concrete to absorb most of the radiation.

Deflecting Radiation

  • Diagram illustrating the deflection of alpha, beta, and gamma radiation in a magnetic field.

  • Magnetic field is directed into the page.

  • Alpha particles are deflected in one direction, beta particles in the opposite direction, and gamma rays are not deflected.

Activity and Half-Life

  • Geiger Counter:

    • Used to measure radiation.

    • Records the rate at which radiation is detected, known as the count rate.

    • Unit: counts per second (count/s) or counts per minute (count/min).

  • Activity of a Radioactive Source:

    • The rate at which nuclei decay.

  • Half-Life of a Radioactive Source:

    • The average time taken for half the atoms in a sample to decay.

Half-Life Equation

  • Equation: N=N<em>0×2t/T</em>1/2N = N<em>0 \times 2^{-t/T</em>{1/2}}

    • N0N_0: Initial number of undecayed atoms (at time t = 0).

    • NN: Number of undecayed atoms at time t.

    • T1/2T_{1/2}: Half-life of the substance.

  • Applies to calculating count rate/mass.

Examples of Half-Life Calculations

  • Example 1: Iodine-131

    • Initial atoms: 20,000,000

    • Half-life: 8 days

    • Time: 32 days

    • N=20,000,000×232/8=625,000N = 20,000,000 \times 2^{-32/8} = 625,000

    • Alternatively, 32 days = 4 half-lives. N=10,000,000/2/2/2/2N = 10,000,000 / 2 / 2 / 2 / 2

  • Example 2: Radium-224

    • Half-life: 3.6 days

    • Original mass: 10 grams

    • Time: 7.2 days

    • m=10×27.2/3.6=2.5m = 10 \times 2^{-7.2/3.6} = 2.5

    • Alternatively, 7.2 days = 2 half-lives. m=10/2/2=2.5 gm = 10 / 2 / 2 = 2.5 \text{ g}

  • Example 3:

    • Using a graph of activity vs. time to determine half-life.

  • Example 4:

    • A radioactive source has a half-life of 0.5 hours.

    • A detector near the source shows a reading of 6000 counts per second.

    • Background radiation can be ignored.

    • What is the reading on the detector 1.5 hours later?

Background Radiation and Corrected Count Rate

  • Background Radiation:

    • Radiation that is always present in the environment.

    • Mostly from natural sources.

  • Corrected Count Rate:

    • Corrected Count Rate=Observed Count RateBackground radiation\text{Corrected Count Rate} = \text{Observed Count Rate} - \text{Background radiation}

Background Radiation Example Calculation

  • Example 5:

    • Observed count rate = 542 (sample + background)

    • Background count rate = 30

    • Initial count rate of sample = 542 – 30 = 512

    • Later count rate = 94 (sample + background)

    • Count rate of sample = 94 – 30 = 64

    • Decay: 512 -> 64 (512 / 64 = 8)

    • Number of half-lives: 3 (2×2×2=82 \times 2 \times 2 = 8)

    • Half-life = 12 minutes / 3 = 4 hours

  • Another Example:

    • Initial corrected count rate = 180 – 20 = 160

    • After one half life 160/2 = 80

    • The count rate measured = 80 + 20 (background) = 100

  • Using a graph of emission rate vs. time to estimate half-life.

    • The rate of emission of a radioactive source is measured until the reading reaches the background rate of 20 counts per minute.

Applications and Safety Precautions

  • Safety Measures:

    • Reducing exposure time.

    • Increasing distance from the source.

    • Using shielding to absorb radiation.

  • Effects of Radiation:

    • Cell death.

    • Mutations.

    • Cancer.

Effects of Radioisotopes on Cells

  • High Dose of Radiation:

    • Causes significant ionization in cells, leading to cell death (radiation burns).

  • Damage to DNA:

    • Can disrupt cell control mechanisms, leading to uncontrolled cell division and tumor formation (cancer).

  • Effects on Gametes (Sperm or Egg Cells):

    • Damaged DNA can be passed to future generations, causing genetic mutations.

    • Mutations can be harmful, leading to developmental issues or genetic disorders.

Uses of Radioisotopes

  • Based on:

    • Penetrating power.

    • Damage to living cells.

    • Detectability.

    • Radioactive decay and half-life.

  • Fault Detection:

    • Gamma rays are used to detect faults in manufactured goods.

    • Rays escape through faults and are detected on photographic film.

  • Thickness Measurements:

    • Beta radiation is used to measure thickness.

    • Radiation is directed through a sheet, and a detector measures the amount of radiation that passes through.

    • Thickness is adjusted based on the radiation detected.

  • Smoke Detectors:

    • Americium-241 is used (long half-life, about 430 years).

    • Alpha radiation falls on a detector, creating a current that keeps the alarm silent.

    • Smoke entering the gap absorbs alpha radiation, stopping the current and triggering the alarm.

Sterilization and Food Irradiation

  • Medical Products:

    • Sealed in plastic bags and exposed to gamma rays to kill microbes.

  • Food Irradiation:

    • Preserves food by killing microbes with intense gamma rays.

    • Results in sterile food, often used in space or hospitals.

    • Single-celled organisms are killed due to cell damage.

Cancer Treatment

  • Method:

    • A source of gamma rays (or X-rays) is directed at the tumor.

    • The source moves around the tumor to minimize radiation exposure to other tissues.

Radioactive Dating

  • Principle:

    • Radioactive substances decay at a known rate, allowing the determination of the age of objects and materials.

  • Radiocarbon Dating:

    • Measures the amount of carbon-14 in an object to determine when it was alive.

    • After death, carbon-14 decays.

    • Nuclear weapons testing in the 1950s and 1960s increased carbon-14 in the atmosphere, affecting the accuracy of dating living objects from that period.

  • Dating Rocks:

    • Potassium-40 and argon are used.

Engineering and Radioactive Tracing

  • Tracing Underground Water Flow:

    • Water containing a radioactive chemical is injected into the ground.

    • Detectors at ground level monitor its movement through underground cracks.

  • Medical Tracing:

    • A radioactive chemical (tracer), such as technetium-99 (short half-life, about 6 hours), is injected into the patient.

    • A scanner is used to trace the path of the chemical.

5.2 Radioactivity (Summary)

5.2.1 Detection of Radioactivity
  • Core:

    • Understand background radiation.

  • Supplement:

    • Sources of background radiation:

      • Radon gas (in the air).

      • Rocks and buildings.

      • Food and drink.

      • Cosmic rays.

    • Ionizing nuclear radiation measured using a detector connected to a counter.

    • Use count rate (counts/s or counts/minute).

    • Use background radiation measurements to determine corrected count rate.

5.2.2 The Three Types of Nuclear Emission
  • Core:

    • Emission of radiation from a nucleus is spontaneous and random.

    • Identify alpha (α), beta (β), and gamma (γ) emissions by:

      • Their nature.

      • Their relative ionizing effects.

      • Their relative penetrating abilities (ẞ* are not included).

  • Supplement:

    • Deflection of α-particles, ß-particles, and γ-radiation in electric and magnetic fields.

    • Explain relative ionizing effects with reference to:

      • Kinetic energy.

      • Electric charge.

5.2.3 Radioactive Decay
  • Core:

    • Radioactive decay is a change in an unstable nucleus that results in the emission of α-particles or ß-particles and/or γ-radiation.

    • These changes are spontaneous and random.

    • During α-decay or ß-decay, the nucleus changes to that of a different element.

  • Supplement:

    • Isotopes may be radioactive due to an excess of neutrons and/or the nucleus being too heavy.

    • Describe the effect of α-decay, ß-decay, and γ-emissions on the nucleus, including increased stability and a reduction in excess neutrons.

      • The following change in the nucleus occurs during ß-emission: neutronproton+electronneutron \rightarrow proton + electron

    • Use decay equations, using nuclide notation, to show the emission of α-particles, ß-particles, and γ-radiation.

5.2.4 Half-Life
  • Core:

    • Define half-life as the time taken for half the nuclei of an isotope in a sample to decay.

    • Recall and use this definition in simple calculations.

  • Supplement:

    • Calculate half-life from data or decay curves from which background radiation has not been subtracted.

    • Explain how the type of radiation emitted and the half-life of an isotope determine its use in various applications, including:

      • Household fire (smoke) alarms.

      • Irradiating food to kill bacteria.

      • Sterilization of equipment using gamma rays.

      • Measuring and controlling thicknesses of materials.

      • Diagnosis and treatment of cancer using gamma rays.

5.2.5 Safety Precautions
  • Core:

    • State the effects of ionizing nuclear radiations on living things, including cell death, mutations, and cancer.

  • Supplement:

    • Describe how radioactive materials are moved, used, and stored safely.

    • Explain safety precautions for ionizing radiation in terms of reducing exposure time, increasing distance, and using shielding to absorb radiation.