Radioactivity. Detection, shielding, dating and half-life
The online radioactivity simulations on this page will help you understand the basic principles of radioactivity and enlighten you on some of its most important associated concepts such as radioactive detection, radioactive shielding, radioactive dating and radioactive half-life.
This Thematic Unit is part of our Chemistry collection

STEM OnLine mini dictionary
Alpha Emission (α)
Type of decay where the nucleus emits a heavy particle composed of two protons and two neutrons (Helium-4 nucleus).
Beta Emission (β)
Nuclear process where a neutron transforms into a proton by emitting a high-energy electron or positron.
Gamma Radiation (γ)
Emission of high-frequency electromagnetic waves with high penetrating power that often accompanies alpha and beta processes.
Half-life
Time required for half of the nuclei in a radioactive sample to decay into a different element.
Natural Radioactivity
Phenomenon present in nature due to unstable isotopes existing in the Earth’s crust or produced by cosmic rays.
Nuclear Stability
Balance of forces within the nucleus that determines whether an atom will remain intact or undergo spontaneous decay.
Nuclide
Atomic species characterized by its number of protons and neutrons, and its nuclear energy state.
Radioactivity
Spontaneous process of decay of unstable atomic nuclei through the emission of particles and electromagnetic energy.
What Is radioactivity
Radioactivity is a physical and chemical phenomenon in which the nuclei of certain unstable atoms lose energy by spontaneously emitting radiation. These atoms are known as radioisotopes.
To understand why this happens, we must look inside the atom’s nucleus, where protons and neutrons coexist. In nature, most of the atoms around us are stable; their nuclei have a perfect balance of forces and remain unchanged over time. However, when a nucleus is too large or has a clear excess of protons or neutrons, it becomes unstable.
To release that internal tension and seek stability, the nucleus decays naturally. During this decay process, the atom “spits out” particles or bursts of pure energy. We refer to this entire set of emissions as radiation. This process continues spontaneously until the unstable atom transforms into a completely different and chemically stable element, such as uranium, which, after many decays, eventually becomes lead.
Types of ionizing radiation
Radiation emitted by unstable nuclei has ionizing effects. This means it has enough energy to knock electrons out of the atoms it collides with, altering the structure of matter. Depending on the nature of the emission, physicists classify this radiation into three broad categories.
Alpha (α) radiation: heavy particles
Alpha radiation occurs when an atom’s nucleus is too large and needs to lose mass quickly. The nucleus emits an alpha particle, which consists of two protons and two neutrons (equivalent to a helium nucleus). Because these particles are so large and heavy, they have a high positive electric charge and move at relatively slow speeds. Due to their large size, they have very little penetrating power: a single sheet of paper or the outer layer of our skin is enough to stop them completely.
Beta radiation (β): escaping electrons
Beta radiation occurs when the nucleus has an imbalance between its protons and neutrons. To correct this, a neutron transforms into a proton, and in the process, the nucleus ejects an electron at extremely high speed, known as a beta particle. Since they are thousands of times smaller than alpha particles, they have moderate penetrating power. They can pass through paper and travel a few meters through the air, but they can be easily stopped by a thin sheet of aluminum or a piece of wood.
Gamma rays (γ): pure energy
Unlike the previous types, gamma radiation does not involve the emission of material particles, but rather the emission of high-energy electromagnetic waves (photons). It occurs when the nucleus, following an alpha or beta decay, still has excess accumulated energy and needs to fully stabilize. Since they have no mass or electric charge, gamma rays travel at the speed of light and have extremely high penetrating power. They can pass through the human body and require very dense materials, such as thick concrete walls or lead plates, to be stopped.
Half-life. How long does radioactivity last?
The decay of an atom is a purely random event; it is impossible to predict exactly which millisecond a specific nucleus will decay. However, when we analyze a sample containing millions of unstable atoms, the behavior becomes predictable and follows a strict mathematical law.
To measure the rate at which an element’s radioactivity decays, we use the concept of half-life, a term you’ll also find in physics and chemistry textbooks referred to as the half-life period. Both concepts mean exactly the same thing: it is the time required for half of the radioactive nuclei in an initial sample to decay and transform into stable elements.
For example, if you have a sample of 100 grams of a radioisotope with a half-life of one year, after twelve months you will have 50 grams of radioactive material left. After another year, the amount will be reduced to half of what remained, that is, 25 grams, and so on.
This rate of decay varies drastically depending on the chemical element being measured:
– Uranium-238 has a half-life of about 4.5 billion years, nearly the age of the Earth.
– Carbon-14 has a half-life of 5,730 years, which allows archaeologists to date ancient organic remains.
– Iodine-131, used in medical treatments, has a half-life of just 8 days, ensuring that it does not remain in the body for very long.
Practical applications of radioisotopes
Despite the negative reputation that often surrounds nuclear energy, controlled radiation is an indispensable tool in modern society. By knowing the exact half-life of each radioisotope and the type of particle it emits, science has learned to use them for the benefit of health and technical progress.
Nuclear medicine and diagnostics
In hospitals, very short-lived radioisotopes are used for two main purposes: diagnosis and treatment. For diagnosis, small doses of radioactive substances are introduced into the patient’s body to act as tracers, allowing advanced scanners such as PET to obtain detailed images of the interior of organs. In the field of treatment, techniques such as radiation therapy use intense sources of gamma radiation directed with pinpoint accuracy to destroy cancer cells and slow tumor growth.
Nuclear energy and industry
In the industrial sector, radioisotopes are used as high-precision inspection tools. Gamma emissions enable industrial radiography to check the quality of welds in pipes or detect invisible cracks in aircraft structures without having to disassemble them. On the other hand, the best-known application is electricity generation in nuclear power plants, where the immense amount of thermal energy released during the fission of heavy nuclei such as uranium is harnessed.
Risks Associated with Radioactivity
Radioactivity can be dangerous to living organisms if there is excessive exposure or if radioactive materials are released into the environment in an uncontrolled manner. Prolonged exposure to ionizing radiation can have harmful health effects, such as cellular damage, genetic mutations, and an increased risk of developing cancer. Therefore, precautions must be taken and safety limits established to minimize exposure to radioactivity and protect people and the environment.
To work safely with radioactive materials, medical physics and engineering rely on three fundamental pillars of radiation protection:
Time
The accumulated radiation dose is directly proportional to the time spent near the source. Reducing handling time to the absolute minimum is the first line of defense.
Distance
The intensity of radiation decreases dramatically as we move away from the source. Doubling the distance reduces exposure to one-fourth.
Shielding
Placing adequate physical barriers between the source and people blocks the particles. As we saw when analyzing the types of radiation, aluminum sheets are used for beta particles, and thick walls of lead or concrete are used to contain gamma rays.
In the event of a nuclear or radiological incident, it is important to follow the instructions of the authorities and evacuate or take protective measures as necessary. Regulatory agencies and nuclear safety programs are responsible for overseeing and regulating the use of radioactive materials to ensure the protection of public health and the environment.

STEM OnLine mini dictionary
Alpha Emission (α)
Type of decay where the nucleus emits a heavy particle composed of two protons and two neutrons (Helium-4 nucleus).
Beta Emission (β)
Nuclear process where a neutron transforms into a proton by emitting a high-energy electron or positron.
Gamma Radiation (γ)
Emission of high-frequency electromagnetic waves with high penetrating power that often accompanies alpha and beta processes.
Half-life
Time required for half of the nuclei in a radioactive sample to decay into a different element.
Natural Radioactivity
Phenomenon present in nature due to unstable isotopes existing in the Earth’s crust or produced by cosmic rays.
Nuclear Stability
Balance of forces within the nucleus that determines whether an atom will remain intact or undergo spontaneous decay.
Nuclide
Atomic species characterized by its number of protons and neutrons, and its nuclear energy state.
Radioactivity
Spontaneous process of decay of unstable atomic nuclei through the emission of particles and electromagnetic energy.
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Radioactivity simulations
Half-Life I
In radioactivity, the half-life is the time interval required for half of the atomic nuclei in a radioactive sample to decay. If the half-life passes again, half of the remaining mass will remain (1/2, 1/4, 1/8, 1/16, 1/32, …) The mass gets smaller and smaller, but there is always a little bit left.
Radioactivity dating
This simulation explains the concept of half-life, including the random nature of half-life, in terms of single particles and larger samples. It describes decay processes, including how elements change and emit energy and/or particles. Explains how radiometric dating works and why different elements are used for dating different objects. Also identifies that 1/2 life is the average time for a radioactive substance to decay.
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“If I have seen further, it is by standing on the shoulders of giants”
Isaac Newton
Michael Faraday
–
Amedeo Avogadro
–
Become a giant
Quantum Mechanics of Molecular Structures
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Test your knowledge
What is radioactivity, and why is it a fundamental phenomenon for understanding the structure and stability of atomic nuclei?
How do the different types of radiation emitted during radioactive decay differ, and what does this imply for their interaction with matter?
Why are some elements radioactive while others are not? What makes a nucleus “decide” to break apart?
Is radioactivity always dangerous, or does it depend on the type and amount?
Why do radioactive materials take so long to stop emitting radiation? Shouldn’t they “run out” quickly?
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