1. Atomic Structure and Models:
The Atom: Atoms are the fundamental building blocks of matter, consisting of a central nucleus surrounded by orbiting electrons. "Atoms are the fundamental building blocks of matter, and understanding their structure is crucial in physics."
The nucleus contains positively charged protons and neutral neutrons. "The nucleus is the dense center of an atom, made up of protons and neutrons." The number of protons defines the element.
Electrons are negatively charged and orbit the nucleus in specific energy levels. Electrons "balances the positive charge of the nucleus, making the atom electrically neutral overall."
Proton Number (Atomic Number, Z): The number of protons in the nucleus, defining the element.
Nucleon Number (Mass Number, A): The total number of protons and neutrons in the nucleus. "The Nucleon Number (or Mass Number , A ) is the total number of protons and neutrons in the nucleus." The number of neutrons can be calculated as A - Z.
Nuclear Notation: A standardised way to represent an atom, showing the element symbol, proton number (Z), and nucleon number (A).
Rutherford's Alpha Scattering Experiment: This experiment disproved the plum pudding model and led to the nuclear model of the atom.
Alpha particles were directed at a thin gold foil.
Observations: Most particles passed through undeflected, some were deflected at large angles, and a few were repelled.
Conclusions: Atoms are mostly empty space with a small, dense, positively charged nucleus. "Most alpha particles passed through the gold foil without deflection. This showed that atoms are primarily empty space." "A small fraction of alpha particles were deflected at large angles. This indicated the presence of a dense region (the nucleus) at the center of the atom."
2. Isotopes and Ions:
Isotopes: Atoms of the same element with the same number of protons but different numbers of neutrons (different mass numbers). "Isotopes are atoms of the same element that have different numbers of neutrons but the same number of protons." They have similar chemical properties but different physical properties.
Ions: Atoms that have gained or lost electrons, resulting in a net charge. "Atoms can gain or lose electrons to form ions, which are charged particles". Positive ions (cations) lose electrons; negative ions (anions) gain electrons.
3. Radioactivity and Radioactive Decay:
Radioactive Isotopes: Unstable isotopes that emit radiation to become more stable. "Some isotopes are radioactive due to: Having too many neutrons , which makes the nucleus unstable. The nucleus being too heavy , meaning that there are too many protons and neutrons, causing instability."
Types of Radiation:Alpha (α) Particles: Helium nuclei (2 protons, 2 neutrons), positively charged, highly ionising, low penetration (stopped by paper). "Composed of 2 protons and 2 neutrons."
Beta (β) Particles: High-speed electrons, negatively charged, moderately ionising, moderate penetration (stopped by aluminium). "Beta-minus (β⁻) particles are electrons emitted from the nucleus when a neutron decays into a proton."
Gamma (γ) Rays: Electromagnetic radiation (photons), no charge, weakly ionising, high penetration (requires lead or concrete for shielding). "Electromagnetic wave with no mass and no charge. High-energy photons, similar to X-rays but even more energetic."
Radioactive Decay Equations: Use nuclide notation to represent changes during decay, showing the parent nucleus, daughter nucleus, and emitted particle.
Example Alpha Decay equation is given.
Example Beta Decay equation is given.
Background Radiation: The low level of ionising radiation present in the environment from natural (e.g., radon gas, cosmic rays, rocks, food) and man-made (e.g., medical procedures) sources. "Background radiation is the low level of ionising radiation that is always present in the environment."
Measuring Radiation: Ionising radiation can be measured using a radiation detector connected to a counter e.g. a Geiger-Muller tube. Count rate refers to the number of radioactive events detected per second or minute.
4. Half-Life:
Definition: The time taken for half the nuclei of a radioactive isotope in a sample to decay. "The half-life of a radioactive isotope is defined as: The time taken for half the nuclei of that isotope in any sample to decay."
Calculation: Half-life can be determined from data tables or decay curves (graphs showing the decline of radioactive material over time).
5. Nuclear Fission and Fusion:
Nuclear Fission: The splitting of a large nucleus into smaller nuclei, releasing energy and neutrons. "This is the splitting of a large nucleus into smaller nuclei. Fission releases a significant amount of energy and is the process used in nuclear reactors." Used in nuclear reactors.
Nuclear Fusion: The joining of two small nuclei to form a larger nucleus, releasing even more energy. "This is the joining of two small nuclei to form a larger nucleus. Fusion releases even more energy than fission and is the process that powers the Sun." Powers the Sun.
Both processes involve the conversion of mass into energy, according to E=mc².
6. Applications of Radioactive Isotopes:
Household: Americium-241 in smoke alarms (alpha particles).
Food Industry: Gamma irradiation to kill bacteria and extend shelf life.
Medical:Sterilisation of equipment using gamma rays (Cobalt-60).
Diagnosis and treatment of cancer using gamma rays (Cobalt-60 in radiotherapy).
Industry: Measuring and controlling thickness of materials using beta radiation.
7. Safety Precautions:
Effects of Ionising Radiation:Cell death (high doses).
Mutations in DNA.
Cancer (prolonged exposure). "Prolonged or high levels of radiation exposure can lead to cancer."
Safe Handling:Transportation in shielded containers (thick lead).
Usage with remote tools and in shielded environments.
Storage in secure lead-lined containers.
Principles of Radiation Safety:Minimise exposure time. "The less time you spend near a radioactive source, the lower your exposure will be."
Maximise distance from the source (inverse square law). "Distance plays an important role in radiation safety."
Use appropriate shielding (paper/gloves for alpha, aluminium for beta, lead/concrete for gamma). "Different types of radiation require different types of shielding"
Describe the key findings of the alpha particle scattering experiment and their impact on the atomic model.
The alpha particle scattering experiment demonstrated that most alpha particles passed through gold foil undeflected, revealing that atoms are mostly empty space; however, some particles were deflected at large angles, indicating a small, dense, positively charged nucleus at the centre. This experiment led to the rejection of the "plum pudding model" and acceptance of the nuclear model of the atom.
2. How does the half-life of a radioactive isotope influence its suitability for different applications?
A radioactive isotope’s half-life dictates how quickly it decays and the duration of its activity; for example, isotopes with long half-lives are suitable for smoke alarms, providing consistent radiation over long periods, while those with short half-lives are more appropriate for applications like medical diagnosis where quick decay is preferable.
3. What are the main sources of background radiation?
The main sources of background radiation include naturally occurring radon gas from the ground, cosmic rays from space, radioactive elements in rocks and building materials, and small amounts found in food and drink. These sources contribute to a low level of ionising radiation that is present in the environment at all times.
4. Explain how a Geiger-Müller tube is used to measure radiation.
A Geiger-Müller tube detects ionising radiation; when radiation enters the tube, it ionises the gas inside, creating a current that the counter then records. The count rate, measured in counts per second or minute, indicates the amount of radiation detected.
5. What are isotopes, and how do they differ from each other?
Isotopes are atoms of the same element that have the same number of protons but a different number of neutrons, resulting in varying mass numbers. While isotopes share chemical properties, they may differ in physical properties, such as radioactivity.
6. Describe the process of beta decay and its effect on the nucleus.
In beta decay, a neutron in the nucleus is converted into a proton and an electron, where the electron is emitted as a beta particle. This process increases the proton number of the atom, transforming it into a different element with one more proton and one less neutron.
7. What are the primary safety precautions to take when handling radioactive materials?
Primary safety precautions when handling radioactive materials include minimising exposure time, maximising distance from the source using remote tools, and using appropriate shielding such as lead for gamma radiation or paper for alpha radiation.
8. What are the key components of an atom, and what are their charges?
An atom is composed of a nucleus containing positively charged protons and neutral neutrons, orbited by negatively charged electrons. The number of protons determines the element’s identity, and the number of protons is equal to the number of electrons, making the atom electrically neutral.
9. Compare and contrast the penetrating abilities of alpha, beta, and gamma radiation.
Alpha radiation has low penetration, being stopped by paper or skin; beta radiation has moderate penetration, passing through skin but being stopped by aluminium; gamma radiation has high penetration, only stopped by thick lead or concrete.
10. Explain the difference between nuclear fission and nuclear fusion.
Nuclear fission is the splitting of a large nucleus into smaller nuclei, releasing energy and is used in nuclear reactors. Nuclear fusion, on the other hand, is the joining of two small nuclei to form a larger nucleus, releasing vast amounts of energy, as seen in the sun.
11. What are isotopes and ions, and how are they different?
Isotopes are atoms of the same element (same number of protons) that have different numbers of neutrons. Ions are atoms that have gained or lost electrons, resulting in a net electrical charge. Isotopes have the same chemical properties but may have different physical properties (e.g., radioactivity), while ions have different electrical properties.
12. What are the three main types of nuclear emission, and how do their properties differ?
The three main types of nuclear emission are alpha (α), beta (β), and gamma (γ) radiation. Alpha particles consist of 2 protons and 2 neutrons (a helium nucleus), have a high ionising ability, and low penetration power (stopped by paper). Beta particles are electrons, have moderate ionising ability and penetration power (stopped by aluminium). Gamma rays are electromagnetic waves, have weak ionising ability and high penetration power (stopped by thick lead or concrete).
13. What is radioactive decay, and how does it change the composition of the nucleus?
Radioactive decay is the process by which an unstable atomic nucleus emits radiation to become more stable. In alpha decay, the nucleus loses 2 protons and 2 neutrons, decreasing the nucleon number by 4 and the proton number by 2, transforming the element into a new element. In beta decay, a neutron is converted into a proton and an electron (beta particle), increasing the proton number by 1, also transforming the element into a new element. Gamma emission releases excess energy from the nucleus without changing the number of protons or neutrons.
14. What is half-life, and how is it used to understand radioactive decay?
Half-life is the time taken for half of the radioactive nuclei in a sample to decay. It is a measure of how quickly an isotope undergoes radioactive decay. It can be determined from data tables or decay curves and is used in calculations to determine the remaining amount of a radioactive substance after a certain period.
15. What are some practical applications of radioactive isotopes, and what properties make them suitable for these uses?
Radioactive isotopes have diverse applications based on their radiation type and half-life. Americium-241 (alpha emitter with long half-life) is used in smoke alarms. Gamma radiation (e.g., from Cobalt-60 with a suitable half-life) is used to irradiate food to kill bacteria and sterilise medical equipment. Beta radiation is used in industry to measure and control the thickness of materials. Gamma rays are also used in radiotherapy for cancer treatment.
16. What are the potential dangers of ionising radiation, and what safety precautions should be taken when working with radioactive materials?
Ionising radiation can cause cell death, mutations (including genetic defects), and cancer. Safety precautions include minimising exposure time, increasing distance from the source, and using shielding. Alpha radiation can be blocked by paper/gloves, beta by aluminium, and gamma by lead or concrete. Radioactive materials should be transported in shielded containers, handled with remote tools, and stored in secure lead-lined containers.
Alpha Particle (α): A positively charged particle consisting of two protons and two neutrons, equivalent to a helium nucleus. Emitted during alpha decay and has low penetration ability.
Atom: The basic unit of matter, consisting of a nucleus containing protons and neutrons, and electrons orbiting the nucleus.
Atomic Number (Z): The number of protons in the nucleus of an atom, which defines the element. Also known as proton number.
Background Radiation: The low-level ionising radiation present in the environment from both natural sources (e.g., radon, cosmic rays) and man-made sources.
Beta Particle (β): An electron or positron emitted during beta decay, possessing moderate penetrating power.
Count Rate: The number of radioactive events detected per unit time (e.g., counts per second or counts per minute), indicating the amount of radiation.
Corrected Count Rate: The count rate from a specific radioactive source after subtracting the count rate from background radiation, providing a more accurate measure of the source's activity.
Decay Curve: A graph that shows the decrease in radioactivity over time, used to determine the half-life of a radioactive isotope.
Electromagnetic Wave: A form of energy that travels through space at the speed of light, including gamma radiation.
Electron: A negatively charged particle that orbits the nucleus of an atom, with a small mass relative to protons and neutrons.
Gamma Radiation (γ): High-energy electromagnetic radiation emitted from the nucleus of an atom, with high penetration and low ionisation capability.
Geiger-Müller Tube: A device used to detect ionising radiation, containing a gas that becomes ionised when radiation passes through, producing a signal.
Half-life: The time taken for half of the radioactive nuclei in a sample to decay. It’s a measure of the rate of decay of a radioactive isotope.
Ion: An atom or molecule that has gained or lost electrons and therefore has a net electric charge.
Ionising Radiation: Radiation with enough energy to remove electrons from atoms, creating ions. Includes alpha, beta, and gamma radiation.
Isotopes: Atoms of the same element with the same number of protons but different numbers of neutrons, resulting in different mass numbers.
Mass Number (A): The total number of protons and neutrons in the nucleus of an atom. Also known as nucleon number.
Neutron: A neutral particle found in the nucleus of an atom, having no electric charge.
Nuclear Fission: The process of splitting a large atomic nucleus into smaller nuclei, releasing a large amount of energy.
Nuclear Fusion: The process of combining two light atomic nuclei to form a heavier nucleus, releasing a vast amount of energy.
Nuclear Model: The model of the atom where a tiny, dense, positively charged nucleus is surrounded by orbiting electrons.
Nucleon Number: The total number of protons and neutrons in the nucleus of an atom. Also known as mass number.
Nucleus: The central part of an atom, containing protons and neutrons and the bulk of the atom's mass.
Plum Pudding Model: An obsolete model of the atom that suggested electrons were embedded within a diffuse positive charge.
Proton: A positively charged particle found in the nucleus of an atom; the number of protons determines the element.
Radioactive Decay: The spontaneous process by which unstable atomic nuclei emit radiation, transforming into more stable nuclei.
Radioactive Isotope: An isotope with an unstable nucleus that emits radiation to become more stable.
Shielding: The use of materials like lead or concrete to reduce or block radiation.