Proving the half-life of Potassium-40

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In summary, the conversation discusses the decay of K-40 by two radioactive processes, electron capture and β- emission. Using the given data of a sample containing 4.0x10^18 nuclei of K-40 emitting 68 β- particles and photons per second, the half life of K-40 is calculated to be 1.3x10^9 years. The calculation is done by converting the given data into the equation A=λN and then solving for the half-life using T1/2 = ln2/λ. Finally, the half-life is converted from seconds to years to show that it is indeed 1.3x10^9 years.
  • #1
GandhiReborn
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Homework Statement



"K-40... decays by two radioactive processes. It can decay by electron capture or β- emission.

It is found that a sample containing 4.0x10^18 nuclei of K-40 emits a total of 68 β- particles and photons each second. This shows the half life is 1.3x10^9 years."

Use the data in the passage to show that the half life is 1.3x10^9 years.

Homework Equations



I'm assuming...

T1/2 = ln2/λ; A=λN; A=A0e^(-λ)(t)

The Attempt at a Solution



Using A=λN --> A/N=λ --> (68)/(4*10^18) = 1.7^10-17
then ln2/(1.7^10-17) = 4.1*10^16 ->> waayy too big.

I then tried various other combinations of the above, but to no success.

Please help! I know I'm missing something VERY obvious.
 
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  • #2
You calculated (correctly) the half-life in seconds. Now convert to years.
 
  • #3
phyzguy said:
You calculated (correctly) the half-life in seconds. Now convert to years.

D'oh!

You legend, thank you :D
 

1. What is the half-life of Potassium-40?

The half-life of Potassium-40 is approximately 1.25 billion years.

2. How is the half-life of Potassium-40 determined?

The half-life of Potassium-40 is determined through a process called radiometric dating, which measures the rate of decay of radioactive isotopes in a sample of material.

3. What is the significance of knowing the half-life of Potassium-40?

Knowing the half-life of Potassium-40 is significant because it allows scientists to accurately date rocks and minerals, providing valuable information about the age of the Earth and the evolution of geological processes.

4. How do scientists use Potassium-40 to determine the age of rocks?

Scientists use the ratio of Potassium-40 to its decay product, Argon-40, to determine the age of rocks. As Potassium-40 decays, it gradually turns into Argon-40 at a known rate. By measuring the amount of Potassium-40 and Argon-40 in a rock sample, scientists can calculate how long it has been since the rock formed.

5. Is the half-life of Potassium-40 constant?

Yes, the half-life of Potassium-40 is a constant value and does not change over time. This makes it a reliable tool for dating rocks and understanding the Earth's geological history.

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