Question
Question: A radioactive isotope X with a half-life of \(6.93\times {{10}^{9}}\) years decays to Y which is sta...
A radioactive isotope X with a half-life of 6.93×109 years decays to Y which is stable. A sample of rock from the moon was found to contain both the elements X and Y which were in the ratio of 1:7. The age of the rock is.
(A) 2.079×1010years
(B) 1.94×1010years
(C) 1.33×1010years
(D) 1010years
Solution
Hint: To understand this question, we should note that X is producing Y which is stable. That means there is no further decay. And we should note that Y is producing only from X, so we can now find the answer by doing calculation.
Complete step by step answer:
In this question, it is given that there is a radioactive isotope X, which has a half-life of 6.93×109years.
X=t21=6.93×109years.
And, in this question it is given that Y is producing only from X.
X→Y→(Nofurtherdecay)
By radioactive decay law, we know that: Y=X(1−e−λt)
And, in the question it is given that X and Y are found in moon rock in the ratio 1:7.
YX=71
The above ratio states that initially we had X0 and from this some part got converted into Y and some part remained as X. then, we multiplied it by k.
X0→Y=7×k↓X=1×k
After multiplication by k, we find that total X0 was 8k.
Y=87X0X=81X0
From the above equation we can say that the final value of X that remains is only81X0. And this states that three half-lives are gone. Let us calculate this by calculating this after each half life:
X0onehalflife2X0Secondhalflife4X0Thirdhalflife8X0
So, three half-lives are gone. (3t21)
Now, we can easily solve our question.
3t213×(6.93×109)20.79×109years
Or 2.079×1010years
So, from calculation we can say that answer of this question option A.
Note:We should know the radioactive decay. It is the phenomenon that is performed by the nuclei of an atom as a result of nuclear instability or we can say that it is a process by which the nucleus of an unstable atom loses energy by emitting radiation.
And one more concept that is important that is Half-life (symbol t1⁄2). It is the time required for a quantity to reduce to half of its initial value. We use this term in nuclear physics to describe how quickly unstable atoms undergo, or how long stable atoms survive.