Uranium and Thorium; the third element is Potassium, all responsible for radioactivity in the environment.
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Two key sources of background radiation on Earth are cosmic rays (high-energy particles from space) and terrestrial sources like radon gas, which can seep into buildings from the ground. Both cosmic rays and terrestrial radiation contribute to the natural background radiation levels that we are exposed to daily.
Background radiation from rocks and soil is primarily due to the presence of radioactive elements like uranium, thorium, and potassium in Earth's crust. These elements emit radiation as they decay over time. Cosmic rays, on the other hand, are high-energy particles that originate from sources outside our solar system, such as supernovae and black holes, and interact with Earth's atmosphere to produce radiation.
Background radiation can be detected using specialized instruments such as Geiger counters, scintillation detectors, or ionization chambers. These instruments are able to measure the levels of ionizing radiation present in the environment, including background radiation from sources like cosmic rays and radioactive elements in the earth's crust. The detectors convert the interactions of radiation with matter into electrical signals that can be measured and analyzed.
Background radiation originates from various sources such as cosmic rays from space, naturally occurring radioactive elements in the Earth's crust, and even human-made sources like medical imaging procedures and nuclear power plants. This radiation is constantly present in the environment at low levels and can be detected all around us.
Three natural sources of radiation are the sun (solar radiation), radioactive elements in rocks and soil (terrestrial radiation), and cosmic rays from outer space.
Radiation can be both natural and unnatural. Natural radiation comes from sources like the sun and radioactive elements in the earth, while unnatural radiation is generated by human activities like nuclear power plants, medical procedures, and industrial processes.