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By Becquerels, which is one disintegration per second, or by curies, which is 3.3x1010 disintegrations per second.
It varies from one element to another. It is measured in terms of its half-life. A half-life is the length of time it takes for half the number of radioactive atoms of the element in a lump to decay.
Just like any other material, it gets warmer, most likely expands, and may transition from solid to liquid and/or from liquid to gas. If it's already in the gaseous state, then its pressure increases. Its rate of radioactive decay is not affected.
The rate cannot be changed.
The count rate observed by a Geiger counter is proportional to activity, not to half-life.
The half life of a radioisotope indicates the rate of decay for a radioactive sample
By Becquerels, which is one disintegration per second, or by curies, which is 3.3x1010 disintegrations per second.
It varies from one element to another. It is measured in terms of its half-life. A half-life is the length of time it takes for half the number of radioactive atoms of the element in a lump to decay.
It tells what fraction of a radioactive sample remains after a certain length of time.
The Geiger counter measures a percentage of the disintegrations that occur in a radioactive source. Assuming the geometry is calibrated, you can back calculate the countrate into the disintegration rate, and that is proportional to the activity.
Just like any other material, it gets warmer, most likely expands, and may transition from solid to liquid and/or from liquid to gas. If it's already in the gaseous state, then its pressure increases. Its rate of radioactive decay is not affected.
The ticking of a clock is constant, occurring at a steady rhythm/frequency. While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.
The ticking of a clock is constant, occurring at a steady rhythm/frequency. While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.
The ticking of a clock is constant, occurring at a steady rhythm/frequency. While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.
The rate cannot be changed.
The count rate observed by a Geiger counter is proportional to activity, not to half-life.
The ticking of a clock is constant, occurring at a steady rhythm/frequency. While the decay of radioactive elements cannot be determined at a particular point in time, they do decay at a fairly steady rate over time. This allows you to statistically determine the rate at which a mass of radioactive material will steadily decay. So, the decay rate is steady, predictable, and follows a sort of rhythm over time just like the ticking of a clock.