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Question: In an old rock, the ratio of nuclei of uranium and lead is \[1:1\]. Half of the life of Uranium is \...

In an old rock, the ratio of nuclei of uranium and lead is 1:11:1. Half of the life of Uranium is 45×109  yrs45 \times {10^9}\;{\text{yrs}}. Initially it contains only uranium nuclei. How old is the rock?

Explanation

Solution

In this question, the concept of the decay constant is used to calculate the constant ratio for the number of atoms of radio nuclei that convert in a given period of time. Calculate the value the value ofλ\lambda , where λ\lambda is the decay constant

Complete step by step answer:
Consider the given question, we have given the ratio of nuclei of the uranium and the ratio of nuclei of the lead in a old rock as
UraniumLead=11\Rightarrow \dfrac{{{\text{Uranium}}}}{{{\text{Lead}}}} = \dfrac{1}{1}

And let us represent the uranium by UU and represent the lead by PbPb.
UPb=11\Rightarrow \dfrac{U}{{Pb}} = \dfrac{1}{1}
We have also given the half life of the uranium as
U=4.5×109  yrsU = 4.5 \times {10^9}\;yrs

The old rock initially contains the uranium nuclei. Let us represent the time bytt, represent the initial uranium in the rock by U0{U_0}. And the uranium after the time tt represented by Ut{U_t} and let represent the lead after time tt byPbtP{b_t}.
As we know that the initial uranium present in the old rock can be written as,
U0=Ut+Pbt\Rightarrow {U_0} = {U_t} + P{b_t}

We have U0=2{U_0} = 2 that is the initial uranium form. and the uranium after timett,
Ut=(Ut+Pbt)eλt......(1){U_t} = \left( {{U_t} + P{b_t}} \right){e^{ - \lambda t}}......\left( 1 \right)

As we know that the constant ratio for the number of atoms of radio nuclei is used to convert in a given period of time. Whereλ\lambda is decay constant.
λ=0.693t1/2U\Rightarrow \lambda = \dfrac{{0.693}}{{{t_{1/2}}U}}

Now we substitute the values in the above expression and obtain
λ=0.1551×109  yrs1\Rightarrow \lambda = 0.1551 \times {10^{ - 9}}\;{\text{yr}}{{\text{s}}^{ - 1}}
Now we substitute the values in equation (1)\left( 1 \right) as
1=(1+1)e(0.1551×109)t\Rightarrow 1 = \left( {1 + 1} \right){e^{\left( { - 0.1551 \times {{10}^{ - 9}}} \right)t}}
Now we take the log both sides,
log(12)=log(e(0.1551×109).t)\Rightarrow \log \left( {\dfrac{1}{2}} \right) = \log \left( {{e^{\left( { - 0.1551 \times {{10}^{ - 9}}} \right).t}}} \right)
After simplification we get,
0.1551×109t=0.693\Rightarrow 0.1551 \times {10^{ - 9}}t = 0.693

Now we solve the equation further for tt.
t=4.46×109  yrs\therefore t = 4.46 \times {10^9}\;{\text{yrs}}

Therefore, the rock is old t=4.46×109  yrst = 4.46 \times {10^9}\;{\text{yrs}}.

Note: As we know that the half-life means that the time taken to decay the material to its half quantity. Generally, the decay of the radioactive material obtains the logarithmic way that is it is difficult to obtain the life of the material, so we calculate the half-life of these materials.