Half-Life Calculation: How Do Physicists Measure Isotopes?

In summary, physicists determine the half-lives of isotopes by measuring the activity of a sample, which is the number of nuclei that decay every second. This can be easily measured and used to calculate the half-life, even for isotopes with long half-lives stretching into millions of years. This is possible because even though the probability of a single nucleus decaying is small, a macroscopic sample contains a huge number of atoms, making it easy to measure the activity.
  • #1
Danscall
1
0
Hi there,

Someone asked me this earlier when we were talking about radioisotope dating. How do physicists determine the half lives of isotopes when said half life stretches into the millions of years?

Random question I know :P

-Dan
 
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  • #2
It's not hard to do this. The reason we can do this is that atoms are so small that a macroscopic sample of some isotope contains a huge number of them. So if I have a gram of U-238, for example, with a half-life of 4.5 billion years, I would need to wait 4.5 billion years for half of it to decay. But a gram of U-238 contains (6.02x10^23)/238 ~ 10^21 atoms. So even though the probability of a single nucleus decaying is quite small, in a gram about 12,000 nuclei will decay every second. This can be easily measured, and from the number that decay every second, we can calculate the half-life. The number that decay every second is called the "activity". Try reading these:

http://en.wikipedia.org/wiki/Radioactive_decay
http://en.wikipedia.org/wiki/Half-life
 
  • #3
Danscall said:
Hi there,

Someone asked me this earlier when we were talking about radioisotope dating. How do physicists determine the half lives of isotopes when said half life stretches into the millions of years?

Random question I know :P

-Dan
One can measure an activity and from that a decay constant. One can also measure the daughter isotopes and from that determine a rough estimate of where in the decay time the particular radionuclides are. However, this requires an assumption about the original composition.
 

1. How do physicists determine the half-life of an isotope?

Physicists use a technique called radiometric dating to measure the half-life of an isotope. This involves measuring the amount of radioactive decay that has occurred in a sample and using mathematical calculations to determine the half-life.

2. What equipment do physicists use to measure isotopes?

Physicists typically use specialized equipment such as mass spectrometers or gamma ray detectors to measure isotopes. These instruments can detect and measure the decay of radioactive isotopes.

3. How accurate are half-life calculations?

Half-life calculations can be very accurate, with some methods having an error margin of less than 1%. However, the accuracy can vary depending on the equipment and techniques used, as well as the stability of the isotope being measured.

4. Can half-life calculations be used to determine the age of a sample?

Yes, half-life calculations can be used to determine the age of a sample. By measuring the amount of radioactive decay that has occurred, physicists can calculate how long it has been since the sample was formed or last exposed to a radioactive source.

5. How do scientists use half-life calculations in practical applications?

Half-life calculations have many practical applications, such as in radiocarbon dating, determining the age of rocks and fossils, and in medical imaging and treatment. They are also used in industrial processes, such as determining the shelf life of food or detecting leaks in pipelines.

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