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In a smaple of rock, the ration .^(206)...

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).

A

`2.25 xx 10^(9)year`

B

`4.5 x 10^(9)` ln 3 year

C

`4.5 x 10^(9) (ln(3)/(2))/(ln2) year`

D

`2.25 xx 10^(9) ln((3)/(2))` year

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To find the age of the rock based on the ratio of lead-206 to uranium-238 nuclei, we can follow these steps: ### Step 1: Understand the Ratio The ratio of lead-206 (Pb) to uranium-238 (U) is given as 0.5. This means that for every 1 nucleus of U, there are 0.5 nuclei of Pb. ### Step 2: Relate the Ratio to Decay Since uranium decays into lead, we can express the relationship between the initial amount of uranium and the amount that has decayed into lead. Let: - \( N_0 \) = initial number of uranium nuclei - \( N \) = current number of uranium nuclei - \( N_f \) = number of lead nuclei produced From the decay process, we know: \[ N_f = N_0 - N \] ### Step 3: Set Up the Ratio Given the ratio: \[ \frac{N_f}{N} = 0.5 \] We can substitute \( N_f \): \[ \frac{N_0 - N}{N} = 0.5 \] ### Step 4: Solve for \( N_0 \) and \( N \) Rearranging the equation gives: \[ N_0 - N = 0.5N \] \[ N_0 = 1.5N \] ### Step 5: Relate to Exponential Decay Using the exponential decay formula: \[ N = N_0 e^{-\lambda t} \] We can substitute \( N_0 \): \[ N = 1.5N e^{-\lambda t} \] Dividing both sides by \( N \): \[ 1 = 1.5 e^{-\lambda t} \] Thus: \[ e^{-\lambda t} = \frac{1}{1.5} = \frac{2}{3} \] ### Step 6: Take the Natural Logarithm Taking the natural logarithm of both sides: \[ -\lambda t = \ln\left(\frac{2}{3}\right) \] So: \[ t = -\frac{\ln\left(\frac{2}{3}\right)}{\lambda} \] ### Step 7: Find \( \lambda \) The decay constant \( \lambda \) is related to the half-life \( t_{1/2} \): \[ \lambda = \frac{\ln(2)}{t_{1/2}} \] Given the half-life of \( U^{238} \) is \( 4.5 \times 10^9 \) years: \[ \lambda = \frac{\ln(2)}{4.5 \times 10^9} \] ### Step 8: Substitute \( \lambda \) Back Substituting \( \lambda \) back into the equation for \( t \): \[ t = -\frac{\ln\left(\frac{2}{3}\right)}{\frac{\ln(2)}{4.5 \times 10^9}} \] This simplifies to: \[ t = 4.5 \times 10^9 \cdot \frac{\ln\left(\frac{2}{3}\right)}{\ln(2)} \] ### Step 9: Calculate the Age of the Rock Using the values of logarithms: \[ t \approx 4.5 \times 10^9 \cdot \frac{\ln(2/3)}{\ln(2)} \] ### Final Answer Calculating this gives the age of the rock.

To find the age of the rock based on the ratio of lead-206 to uranium-238 nuclei, we can follow these steps: ### Step 1: Understand the Ratio The ratio of lead-206 (Pb) to uranium-238 (U) is given as 0.5. This means that for every 1 nucleus of U, there are 0.5 nuclei of Pb. ### Step 2: Relate the Ratio to Decay Since uranium decays into lead, we can express the relationship between the initial amount of uranium and the amount that has decayed into lead. Let: - \( N_0 \) = initial number of uranium nuclei ...
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In an ore containing uranium, the ratio of ^238U to 206Pb nuclei is 3. Calculate the age of the ore, assuming that all the lead present in the ore is the final stable product of ^238U . Take the half-life of ^238U to be 4.5xx10^9 years.

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