Background radiation refers to the low-level ionizing radiation that is constantly present in the environment. This radiation is a natural part of our surroundings and is made up of various types of radiation from different sources. It’s always present, even in places that are far away from nuclear reactors or other human-made sources of radiation.
Different sources of background radiation:
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Cosmic Radiation:
- This radiation originates from outer space and is composed of high-energy particles, such as protons and atomic nuclei, which are constantly bombarding the Earth’s atmosphere. The intensity of cosmic radiation increases with altitude and latitude (i.e., higher elevations and closer to the poles receive more radiation).
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Terrestrial Radiation:
- This comes from naturally occurring radioactive materials (e.g., uranium, thorium, radon) found in rocks, soil, and water. Some of these materials emit gamma rays, alpha particles, or beta particles as they decay over time. Radon gas, in particular, is a significant source of terrestrial radiation in many homes.
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Internal Radiation:
- The human body contains trace amounts of radioactive isotopes like potassium-40 and carbon-14, which decay naturally over time, emitting radiation. This is known as internal radiation.
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Man-Made Sources:
- Though less significant compared to natural sources, human-made sources of radiation contribute to background radiation as well. These include medical procedures (like X-rays and certain cancer treatments), nuclear power plants (if they leak), and certain industrial activities.
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Airborne Radiation:
- Certain gases in the atmosphere, like radon, can accumulate and lead to exposure, especially in buildings or areas with poor ventilation.
Altogether, the level of background radiation varies depending on location, altitude, and local geology, but on average, it contributes to an annual dose of around 2-3 millisieverts (mSv) per person worldwide.