Radon detection tests are designed to identify radon gas in picocuries per litre of air (pCi/L). The picocurie is used to measure the magnitude of radiation in terms of fragmentations per min. One pCi, one trillionth of a Curie, converts to 2.2 fragmentations per minute. One of the most typical geologic resource of radon stems from the decay of uranium. Radon is frequently located at reduced levels in commonly spread crustal developments, soil, and also water examples.
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