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Question: A radioactive isotope \(X\) with a half-life of \(1.4\times {{10}^{9}}\) years decays to \(Y\) which...

A radioactive isotope XX with a half-life of 1.4×1091.4\times {{10}^{9}} years decays to YY which is stable. A sample of the rock from a cake was found to contain XX and YY in the ratio 1:71:7. The age of the rock is
A) 1.96×106 yearsA)\text{ }1.96\times {{10}^{6}}\text{ years}
B) 3.92×109 yearsB)\text{ 3}.92\times {{10}^{9}}\text{ years}
C) 4.20×109 yearsC)\text{ }4.20\times {{10}^{9}}\text{ years}
D) 8.40×109 yearsD)\text{ 8}.40\times {{10}^{9}}\text{ years}

Explanation

Solution

Hint: This problem can be solved by using the formula for the quantity of the original radioactive isotope present in terms of the number of half lives passed. After getting the number of half lives passed, we can get the age of the rock by multiplying the number with the half life of the radioactive isotope.

Formula used:
A=A0(12)nA={{A}_{0}}{{\left( \dfrac{1}{2} \right)}^{n}}

Complete step by step answer:
We will find the number of half lives passed by using the information of the quantity of the original radioactive isotope left in the quantity of the rock.
The quantity AA of radioactive isotope left in a sample after nn half lives have passed is given by
A=A0(12)nA={{A}_{0}}{{\left( \dfrac{1}{2} \right)}^{n}} --(1)
Where A0{{A}_{0}} is the quantity of the radioactive isotope in the original sample of the rock at the starting of the time period.
Hence, let the original quantity of the radioactive sample be P0{{P}_{0}}. It is given that XX decays to stable YY. Let the amount of XX left in the sample bePP and the amount of YY be QQ.
Let the number of half lives passed be nn.
Now according to the question,
P:Q=1:7P:Q=1:7
PQ=17\therefore \dfrac{P}{Q}=\dfrac{1}{7}
Q=7P\therefore Q=7P --(2)
Now, since XX decays to stable YY, it is obvious that the original quantity of XX will be equal to the total quantity of XX and YY in the sample.
P0=P+Q\therefore {{P}_{0}}=P+Q
Using (2), we get,
P0=P+7P=8P{{P}_{0}}=P+7P=8P --(3)
Now, using (1), we get,
P=P0(12)nP={{P}_{0}}{{\left( \dfrac{1}{2} \right)}^{n}}
P=8P(12)n\Rightarrow P=8P{{\left( \dfrac{1}{2} \right)}^{n}} [Using (3)]
P8P=(12)n\Rightarrow \dfrac{P}{8P}={{\left( \dfrac{1}{2} \right)}^{n}}
18=(12)n\Rightarrow \dfrac{1}{8}={{\left( \dfrac{1}{2} \right)}^{n}}
1323=(12)n\Rightarrow \dfrac{{{1}^{3}}}{{{2}^{3}}}={{\left( \dfrac{1}{2} \right)}^{n}}
(12)3=(12)n\Rightarrow {{\left( \dfrac{1}{2} \right)}^{3}}={{\left( \dfrac{1}{2} \right)}^{n}}
n=3\Rightarrow n=3
Hence n=3n=3 half lives have passed for the sample of the rock.
Now it is given that the half life of the isotope is λ=1.4×109 years\lambda =1.4\times {{10}^{9}}\text{ years}.
Now, since, the sample is 3 half lives old, its age will be
Age = Number of half lives passed×Half life\text{Age = Number of half lives passed}\times \text{Half life}
Age = 1.4×109×3=4.2×109years\therefore \text{Age = }1.4\times {{10}^{9}}\times 3=4.2\times {{10}^{9}}\text{years}
Hence, the age of the rock is 4.2×109years4.2\times {{10}^{9}}\text{years}.
Therefore, the correct option is C) 4.20×109 yearsC)\text{ }4.20\times {{10}^{9}}\text{ years}.

Note: By solving this problem, students must have got a feel for how the ages of rock samples and fossils are determined For determining the age of fossils and trees, usually carbon dating is used in which the radioactive element is the radioactive isotope of carbon, C14C-14 or 614C_{6}^{14}C. This is a good choice for a radioactive element since it has a convenient half life and almost all living organisms contain some amount of this radioactive isotope within them.