CHEM - Uranium isotope relative abundance at diff times

In summary, the relative abundances of uranium isotopes in today's Earth crustal material are 99.2745% 238U, 0.7196% 235U, and 0.0055% 234U. When the Earth was formed 4.6x109 years ago, the relative abundances were likely different and could be calculated using the half-lives and ratios of the isotopes. It is important to only post a question once to avoid repeating work and to receive the best help.
  • #1
thiev
2
0
1. Homework Statement

The relative abundance of uranium isotopes in today’s Earth crustal material is:
99.2745% 238U
0.7196% 235U
0.0055% 234U
What were the relative abundances when the Earth was formed 4.6x109 years ago?


2. Homework Equations

t = age = 1/lambda * ln(N/No)

N = No*e^lambda*t

3. The Attempt at a Solution

i don't know how to approch this...
 
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  • #2
Hey,

I agree with LowlyPion in the other post that you need to know the half-lives and then I think it will be a matter of ratios.

Just post a question the once for the future. This is so people helping you are seeing what everyone is saying and not repeating work that has already been done. We only want to help. :biggrin:

The Bob
 
  • #3


I would approach this problem by first understanding the concept of radioactive decay and how it affects the relative abundance of isotopes over time. Uranium-238 has a half-life of 4.5 billion years, while uranium-235 has a half-life of 700 million years. This means that over time, the amount of uranium-238 will decrease while the amount of uranium-235 will increase.

Using the equations provided, we can calculate the relative abundances of the uranium isotopes at the time of Earth's formation. Since we know the age of the Earth (4.6 billion years), we can plug that into the equation t = age = 1/lambda * ln(N/No) and solve for the initial amount (No) of each isotope.

For uranium-238, we would use the equation N = No*e^lambda*t, where lambda is the decay constant for uranium-238 (0.693/4.5 billion years). This would give us an initial amount (No) of 99.999% for uranium-238.

Similarly, for uranium-235, we would use the equation N = No*e^lambda*t, where lambda is the decay constant for uranium-235 (0.693/700 million years). This would give us an initial amount (No) of 0.001% for uranium-235.

For uranium-234, we can assume that it was not present at the time of Earth's formation, since its half-life is only 245,500 years. Therefore, the initial amount (No) for uranium-234 would be 0%.

In conclusion, the relative abundances of uranium isotopes at the time of Earth's formation would have been approximately 99.999% for uranium-238, 0.001% for uranium-235, and 0% for uranium-234. This is due to the natural process of radioactive decay, which has been occurring since the formation of the Earth.
 

1. What is the significance of uranium isotope relative abundance at different times in chemistry?

The relative abundance of uranium isotopes is important in the study of nuclear reactions and radioactive decay. It also plays a crucial role in the use of uranium as a fuel for nuclear power and in determining the age of rocks and fossils.

2. How does the relative abundance of uranium isotopes change over time?

The relative abundance of uranium isotopes changes over time due to natural processes such as radioactive decay and geological processes like erosion and sedimentation. These processes can lead to changes in the concentration of different uranium isotopes in the environment.

3. What is the most common uranium isotope found in nature?

The most common uranium isotope found in nature is uranium-238, which makes up about 99.3% of all naturally occurring uranium. The remaining 0.7% is mostly uranium-235, with very small amounts of other isotopes.

4. How is the relative abundance of uranium isotopes measured?

The relative abundance of uranium isotopes can be measured through various techniques such as mass spectrometry, which separates and analyzes the different isotopes based on their mass-to-charge ratio. This allows scientists to determine the relative concentrations of different isotopes in a sample.

5. Why is it important to understand the relative abundance of uranium isotopes at different times?

Understanding the relative abundance of uranium isotopes at different times is important for various applications such as nuclear energy production, environmental studies, and dating of geological materials. It also provides valuable insights into the natural processes that have shaped our planet over time.

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