C4- Radiation Flashcards

(31 cards)

1
Q

Radioactivity

A

Radioactivity is defined as the spontaneous decay of a radioactive nucleus, whereby it emits one or more forms of nuclear radiation.

Its the name given to a stream of particles or electromagnetic rays emitted during nuclear decay.

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2
Q

Terrestrial Raditaion

A

FROM THE EARTH- This radiation is emitted by the large number of radioactive nuclei emitting radiation from the Earth’s crust and the atmosphere

it can be natrual or artificial

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3
Q

Cosmic Radiation

A

FROM SAPCE- The atmosphere and the Earth’s magnetic field protect us from most cosmic radiation.

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4
Q

Alpha Decay

A

Alpha Decay is a type of radioactive decay where an unstable atomic nucleus emits an alpha particle (α) to become more stable.

Change in Atomic Number: The atomic number decreases by 2 (because 2 protons are lost).

Change in Mass Number: The mass number decreases by 4 (because 2 protons and 2 neutrons are lost).

2 protons + 2 nuetrons = overall mass loss of 4

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5
Q

Alpha Decay- PROPERTIES

A

As alpha particles have a charge of +2, they tend to attract electrons from nearby atoms and cause these atoms to ionise readily.

  • Low penetrating power (stopped by paper or skin).
  • High ionizing power (can cause damage if ingested or inhaled).
  • Occurs in heavy elements (e.g., Uranium, Thorium).
  • Speed: ~5-7% of the speed of light. (slowest )
  • Dangerous when inhaled or ingested, not harmful externally.
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6
Q

Beta Decay

A

an unstable nucleus transforms by emitting a beta particle (a fast-moving electron or positron) and a neutrino or antineutrino. It occurs when a neutron in the nucleus changes into a proton and an electron, maintaining charge balance.

The electron (β⁻ particle) is emitted, while the proton remains in the nucleus, increasing the atomic number (Z) by 1, while the atomic mass remains unchanged.

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7
Q

Beta Decay- PROPERTIES

A
  • Emits a beta particle (electron, β⁻).
  • Increases atomic number by 1, mass number remains the same.
  • Moderate penetrating power (can pass through paper, blocked by thin metal).
  • Moderate ionizing power.
  • Occurs in unstable nuclei (e.g., Carbon-14, Strontium-90).
  • Speed: Close to the speed of light. (99%)
  • External exposure can be harmful, but less damaging than alpha radiation.
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8
Q

Gamma Decay

A

Gamma decay is a type of radioactive decay in which an unstable nucleus releases gamma radiation in the form of high-energy electromagnetic waves (gamma rays).

Gamma decay typically occurs after alpha or beta decay, as the nucleus moves from a high-energy state to a more stable, lower-energy state. Unlike alpha and beta decay, gamma decay does not change the number of protons or neutrons in the nucleus, so it does not alter the atomic number (Z) or atomic mass. Gamma rays have no charge and high penetrating power, making them more difficult to shield against compared to alpha and beta particles.

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9
Q

Gamma Decay-Properties

A
  • Emits gamma rays (high-energy electromagnetic waves).
  • No change in atomic or mass numbers.
  • High penetrating power (requires thick lead or concrete to block).
  • Low ionizing power.
  • Typically follows alpha or beta decay to release excess energy.
  • Speed: Speed of light.
  • External exposure can be harmful, especially at high doses.
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10
Q

What is meant by Ionising?

A
  • Ionising refers to the ability of radiation to remove electrons from atoms, creating charged particles (ions).
  • Ionising radiation includes alpha, beta, and gamma radiation.
  • It can cause damage to living cells, leading to mutations or cancer.
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11
Q

Radio Isotope

A

A radioisotope (radioactive isotope) is an atom with an unstable nucleus that emits radiation as it decays into a more stable form. These isotopes can release alpha, beta, or gamma radiation.

  • Examples of Radioisotopes and Their Uses:
    Carbon-14 – Used in carbon dating to determine the age of ancient objects.
      Iodine-131 – Used in medical treatments for thyroid disorders.
    
      Uranium-235 – Used as fuel in nuclear power plants.
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12
Q

Radioactive

A

emitting or relating to the emission of ionizing radiation or particles.

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13
Q

Half Life

A

half-life, in radioactivity, the interval of time required for one-half of the atomic nuclei of a radioactive sample to decay (change spontaneously into other nuclear species by emitting particles and energy), or, equivalently, the time interval required for the number of disintegrations per second of a radioactive material to decrease by one-half.

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14
Q

Applications of Alpha Radiation

A

Smoke detectors – Americium-241 ionises air to detect smoke.

Spacecraft power – Used in RTGs to generate electricity.

Cancer treatment – Alpha therapy targets and kills cancer cells.

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15
Q

Applications of Beta Radiation

A

Medical tracers – Used in PET scans to diagnose diseases.

Thickness control – Measures paper and metal thickness.

Radiotherapy – Treats certain cancers by destroying cells.

Carbon Dating:- The beta decay of carbon-14 (C-14) to nitrogen-14 (N-14) is used to determine the age of organic materials, such as artifacts, wood, and animal remains.

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16
Q

Applications of Gamma Radiation

A

Cancer treatment – Kills cancer cells in radiotherapy.

Sterilising medical equipment – Eliminates bacteria for safety.

Food irradiation – Preserves food by killing bacteria and pests.

17
Q

Ionising Radiation

A

Alpha, Beta, and GAmma radiation are all typs of ionising radiation. They cause the removal of electrons which result in the formation of positive ions.

X + radiation → (X+) + (e-)

18
Q

Detecting Radiation

A

A Geiger-Muller tube detects radiation by ionising gas within the tube, creating a current pulse that’s amplified and counted, indicating the presence and intensity of radiation

19
Q

Bacquerel

A

A becquerel (Bq) is the SI unit of radioactivity, representing one radioactive decay per second.

20
Q

Ionising Radiation exmaples

A

onizing Radiation (High energy, can remove electrons from atoms)
- Alpha (α) Radiation – Heavy, positively charged particles; low penetration (stopped by paper or skin).

  • Beta (β) Radiation – Fast-moving electrons; medium penetration (stopped by plastic or aluminum).
  • Gamma (γ) Radiation – High-energy electromagnetic waves; highly penetrating (requires lead or concrete to stop).
  • Neutron Radiation – Neutral particles that penetrate deeply; found in nuclear reactors and explosions.
21
Q

Sievert

A

The sievert quantifies the amount of radiation exposure that could cause a certain level of biological damage, such as the risk of radiation-induced cancer or genetic damage.

22
Q

Effects of Ionising Radiation

A

Can cause:

→ Burns,
→ Destruction of cells,
→ and cancer

due to mutation of DNA. This can be used to kill microorganisms so that the objects are sterilised

23
Q

Non-Ionizing Radiation examples

A

Non-Ionizing Radiation (Low energy, does not ionize atoms)
- Radio Waves – Used in communication (radio, TV, Wi-Fi).

  • Microwaves – Used in cooking and mobile phones.
  • Infrared Radiation – Used in remote controls and thermal imaging.
  • Visible Light – The only type of radiation we can see.
  • Ultraviolet (UV) Radiation – Causes sunburn and is used in sterilization.
24
Q

Nuclear Fission

A

Nuclear fission is the process where a large atomic nucleus, such as uranium-235 or plutonium-239, splits into two smaller nuclei. This process releases a large amount of energy, along with extra neutrons that can trigger more fission reactions in a chain reaction. Fission is used in nuclear power plants to generate electricity and in atomic bombs for explosive energy.

25
Nuclear Fusion
Nuclear fusion occurs when two small atomic nuclei, usually hydrogen isotopes like deuterium and tritium, combine to form a larger nucleus, such as helium. This process releases even more energy than fission and is the reaction that powers the sun and stars. Unlike fission, fusion produces little to no radioactive waste and is being researched as a potential clean energy source for the future.
26
Why do Alpha particles ionize more than gamma and beta
Alpha particles ionize more than beta and gamma radiation due to their large mass, +2 charge, and high linear energy transfer (LET). Their strong positive charge allows them to interact intensely with electrons, stripping them from atoms and causing frequent ionization. In contrast, beta particles, being smaller and having a single charge, ionize less efficiently, while gamma rays, as uncharged electromagnetic waves, interact indirectly through processes like the photoelectric effect and Compton scattering. Because alpha particles deposit their energy over a shorter range, they cause dense ionization, making them far more effective at disrupting nearby atoms.
27
Background Radiation
Background radiation refers to the ionizing radiation that is always present in the environment, regardless of human activities. It originates from various natural and artificial sources. Here are the key components: Cosmic radiation Terrestrial radiation Radon Gas radiation
28
Half-life graphs
Half-life graphs visually represent the decay of a substance over time. In these graphs, the x-axis represents time, and the y-axis represents the amount of substance remaining. The graph typically shows an exponential decay curve, with the amount of the substance decreasing by half at each half-life interval.
29
Artificial (Man-Made) Terrestrial Radiation:
This is a subcategory of radiation that comes from human activities but occurs in the Earth's environment: - Nuclear power plants: While their radiation is controlled, it can still contribute to terrestrial radiation if there is an accident or release of radioactive materials. - Nuclear testing and accidents: Events such as nuclear tests or accidents (like the Chernobyl disaster) have contributed to terrestrial radiation in the past.
30
Natural Terrestrial Radiation:
his type of radiation is emitted by naturally occurring radioactive materials found in the soil, rocks, and air. These materials are primarily due to the decay of isotopes present in the Earth's crust. The major contributors to natural terrestrial radiation are: Uranium-238 Thorium-232 Radon-222:
31
Atomic Radius
Definition: The distance from the nucleus to the outermost electron shell. Trends in the Periodic Table: - Increases down a group: As more electron shells are added, the outer electrons are farther from the nucleus. - Decreases across a period: Increased nuclear charge pulls electrons closer, reducing the radius. Factors Affecting Atomic Radius: - Effective nuclear charge: Higher charge pulls electrons closer, reducing the radius. - Electron shielding: Electrons in inner shells shield outer electrons from the nucleus, affecting the size. Explanation: Larger atomic radii have weaker attraction between electrons and the nucleus, while smaller radii have stronger attraction.