Where do 35S and 32P come from?

  • Thread starter Mr.V.
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In summary, the conversation discusses the use of radiotracers in biology, specifically those derived from decaying uranium and plutonium. The main radiotracers commonly used include ^{35}S, ^{32}P, ^{123}I, and ^{125}I, with ^{32}P having a short half-life and needing to be made through neutron irradiation in a reactor. Some isotopes must be made on-site and injected directly into patients.
  • #1
Mr.V.
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Hi all,

I remember a long time ago in high school our bio teacher mentioned that radiotracers used in biology back in the 40s-50s came out of the Manhattan project.

But searching through google, i haven't really been able to find which radiotracers that we commonly use in biology come from decaying uranium/plutonium etc.

2 of the big radiotracers we use are [tex]^{35}S[/tex] and [tex]^{32}P[/tex]. Normally sulfur is used to label proteins and phosphorus is used to label DNA (although [tex]^{32}P[/tex] is useful for phosphorylation states of proteins too)

There are also others used such as [tex]^{123}I[/tex] and [tex]^{125}I[/tex].

Many of these (particularly [tex]^{32}P[/tex]) have incredibly short half-lives so I'd imagine if they weren't being made from something with a much longer 1/2 life they'd have burned out of the universe long ago. So where do they come from and how are they made?
 
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  • #2
They aren't made from heavy metal decay but from neutron irradiation of smaller atoms -
for which you need a reactor.
Today they are generally made in small specialised reactors or as a side product in a few powerstations.
Very short lived isotopes you have to make on-site in an accelarator and then inject them directly into the patient - often involving a frantic sprint across the hospital.
 
  • #3


Thank you for your question. ^{35}S and ^{32}P are both radioactive isotopes of naturally occurring elements sulfur and phosphorus, respectively. These isotopes are produced through the process of nuclear reactions, specifically neutron bombardment.

In the case of ^{35}S, it is produced by irradiating ^{34}S with neutrons in a nuclear reactor. This process converts some of the stable ^{34}S atoms into radioactive ^{35}S atoms. Similarly, ^{32}P is produced by irradiating ^{31}P with neutrons.

These radioactive isotopes have short half-lives because they are not naturally abundant in the environment and are constantly decaying into stable isotopes. This is why they need to be continuously produced in nuclear reactors in order to be used as radiotracers in biology.

I hope this helps to answer your question. Let me know if you have any further inquiries.
 

1. Where do 35S and 32P come from?

35S and 32P are both radioactive isotopes that occur naturally in the environment. 35S is produced through the decay of potassium-40, while 32P is produced through the decay of uranium and thorium. They are also produced through artificial means, such as nuclear reactions in nuclear power plants and research facilities.

2. How are 35S and 32P used in scientific research?

These isotopes have a variety of uses in scientific research. 35S is commonly used in biological studies, particularly in molecular biology and genetics, as it can be incorporated into molecules and tracked using specialized detection methods. 32P is often used in nuclear medicine and imaging techniques, as well as in biochemical studies of metabolism and energy production.

3. Are 35S and 32P safe to handle?

Both 35S and 32P are radioactive and can pose health risks if not handled properly. However, the risks can be minimized by following proper safety protocols and using appropriate protective equipment, such as gloves and lab coats. It is important to receive proper training and follow all safety guidelines when working with these isotopes.

4. How do scientists obtain 35S and 32P for their research?

35S and 32P can be purchased from commercial suppliers that specialize in radioactive materials. These suppliers must adhere to strict regulations and guidelines set by government agencies. Scientists can also produce these isotopes in their own laboratories through nuclear reactions or by isolating them from naturally occurring sources.

5. What is the half-life of 35S and 32P?

The half-life of 35S is approximately 87.1 days, meaning that it takes 87.1 days for half of the original amount of 35S to decay into a stable isotope. The half-life of 32P is much shorter at only 14.28 days. This means that after 14.28 days, only half of the original amount of 32P will remain, and so on.

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