Home
Class 12
PHYSICS
The present day abundances (in moles) of...

The present day abundances (in moles) of the isotopes `U^(238)andU^(235)` are in the atio of 128 : 1. They have half lives of `4.5xx10^(9)` years and `7xx10^(8)` years respectively. If age of earth in `(49X)/(76)xx10^(7)` years, then calculate X (Assume equal moles of each isotope existed at the time of formation of the earth)

Text Solution

AI Generated Solution

The correct Answer is:
To solve the problem, we will use the concept of radioactive decay and the relationship between the initial and present abundances of isotopes. ### Step-by-Step Solution: 1. **Understanding the Problem:** We have two isotopes of Uranium: \( U^{238} \) and \( U^{235} \). Their present-day abundances are in the ratio of 128:1. We are given their half-lives and need to find the value of \( X \) in the age of the Earth, given as \( \frac{49X}{76} \times 10^7 \) years. 2. **Define Variables:** Let: - \( N_0 \) = initial amount of \( U^{238} \) = initial amount of \( U^{235} \) (since they are equal at the time of formation) - \( N_{238} \) = present amount of \( U^{238} \) - \( N_{235} \) = present amount of \( U^{235} \) 3. **Decay Formula:** The amount of a radioactive substance remaining after time \( t \) is given by: \[ N = N_0 e^{-\lambda t} \] where \( \lambda = \frac{\ln(2)}{T_{1/2}} \) and \( T_{1/2} \) is the half-life. 4. **Calculate Decay Constants:** For \( U^{238} \): \[ \lambda_{238} = \frac{\ln(2)}{4.5 \times 10^9} \text{ years}^{-1} \] For \( U^{235} \): \[ \lambda_{235} = \frac{\ln(2)}{7 \times 10^8} \text{ years}^{-1} \] 5. **Present Amounts:** Using the decay formula: \[ N_{238} = N_0 e^{-\lambda_{238} t} \] \[ N_{235} = N_0 e^{-\lambda_{235} t} \] 6. **Ratio of Present Amounts:** Given the ratio \( \frac{N_{238}}{N_{235}} = 128 \): \[ \frac{N_0 e^{-\lambda_{238} t}}{N_0 e^{-\lambda_{235} t}} = 128 \] Simplifying gives: \[ e^{-(\lambda_{238} - \lambda_{235}) t} = 128 \] 7. **Taking Natural Logarithm:** Taking the natural logarithm of both sides: \[ -(\lambda_{238} - \lambda_{235}) t = \ln(128) \] 8. **Substituting Values:** Substitute the values of \( \lambda_{238} \) and \( \lambda_{235} \): \[ -\left(\frac{\ln(2)}{4.5 \times 10^9} - \frac{\ln(2)}{7 \times 10^8}\right) t = \ln(128) \] 9. **Calculating \( t \):** Rearranging gives: \[ t = \frac{\ln(128)}{\left(\frac{\ln(2)}{4.5 \times 10^9} - \frac{\ln(2)}{7 \times 10^8}\right)} \] 10. **Finding Age of Earth:** We know that the age of the Earth is given as \( \frac{49X}{76} \times 10^7 \). Set this equal to \( t \) and solve for \( X \). 11. **Final Calculation:** After calculating \( t \) and comparing it to \( \frac{49X}{76} \times 10^7 \), we can solve for \( X \).
Promotional Banner

Topper's Solved these Questions

  • NUCLEAR PHYSICS

    AAKASH SERIES|Exercise ADDITIONAL PRACTICE PRACTICE SHEET (ADVANCED) Matrix Matching Type Questions|1 Videos
  • MOVING CHARGES AND MAGNETISM

    AAKASH SERIES|Exercise EXERCISE-III|49 Videos
  • NUCLEI

    AAKASH SERIES|Exercise Practice Exercise|40 Videos

Similar Questions

Explore conceptually related problems

Calculate the specific activities of Na^(24) & U^(235) nuclides whose half lives are 15 hours and 7.1xx10^(8) years respectively.

Uranium ores on the earth at the present time typically have a composition consisting of 99.3% of the isotope _92U^238 and 0.7% of the isotope _92U^235 . The half-lives of these isotopes are 4.47xx10^9yr and 7.04xx10^8yr , respectively. If these isotopes were equally abundant when the earth was formed, estimate the age of the earth.

A sample of uranium mineral was found to contain Pb^(208) and U^(238) in the ratio of 0.008 : 1. Estimate the age of the mineral (half life of U^(238) is 4.51 xx 10^(9) years).

Uranium ores on the earth at the present time typically have a composition consisting of 99.3% of the isotope ._92U^238 and 0.7% of the isotope ._92U^235 . The half-lives of these isotopes are 4.47xx10^9yr and 7.04xx10^8yr , respectively. If these isotopes were equally abundant when the earth was formed, estimate the age of the earth.

In the chemical analysis of a rock the mass ratio of two radioactive isotopes is found to be 100:1 . The mean lives of the two isotopes are 4xx10^9 years and 2xx10^9 years, respectively. If it is assumed that at the time of formation the atoms of both the isotopes were in equal propotional, calculate the age of the rock. Ratio of the atomic weights of the two isotopes is 1.02:1 .

In the chemical analysis of a rock the mass ratio of two radioactive isotopes is found to be 100:1 . The mean lives of the two isotopes are 4xx10^9 years and 2xx10^9 years, respectively. If it is assumed that at the time of formation the atoms of both the isotopes were in equal propotional, calculate the age of the rock. Ratio of the atomic weights of the two isotopes is 1.02:1 .

Half lives of two isotopes X and Y of a material are known to be 2xx10^(9) years and 4xx10^(9) years respectively if a planet was formed with equal number of these isotopes, then the current age of planet, given that currently the material has 20% of X and 80% of Y by number, will be:

Natural uranium is a mixture of three isotopes _92^234U , _92^234U , _92^235U and _92^238U with mass percentage 0.01%, 0.71% and 99.28% respectively. The half-life of three isotopes are 2.5xx10^5yr , 7.1xx10^8yr and 4.5xx10^9yr respectively. Determine the share of radioactivity of each isotope into the total activity of the natural uranium.

The atomic ratio between the uranium isotopes .^(238)U and.^(234)U in a mineral sample is found to be 1.8xx10^(4) . The half life of .^(234)U is T_((1)/(2))(234)=2.5xx10^(5) years. The half - life of .^(238)U is -

In a smaple of rock, the ration .^(206)Pb to .^(238)U nulei is found to be 0.5. The age of the rock is (given half-life of U^(238) is 4.5 xx 10^(9) years).