To solve this problem, we need to calculate the age of a rock sample based on the decay of a radioisotope X into a stable isotope Y. The ratio of the isotopes X and Y is given, and we are to find the age of the rock, given X's half-life. Here is the solution outlined clearly step-by-step:
1. Understand the given data:
2. Use the decay formula:
We know that the decay of a radioactive isotope follows the formula:
N_t = N_0 \left(\frac{1}{2}\right)^{t/T_{1/2}}
Where N_t is the remaining quantity of the radioisotope X after time t, and N_0 is the initial quantity of X.
3. Set up the equations:
The given ratio of X to Y is 1:7, meaning only 1 part of X is left to 7 parts formed as Y:
\frac{N_t}{Y} = \frac{1}{7}
Since Y equals the amount of X that has decayed, we have:
N_0 - N_t = 7N_t
This simplifies to N_0 = 8N_t.
4. Substitute and solve for time t:
Substitute N_0 = 8N_t into the decay formula:
N_t = 8N_t \left(\frac{1}{2}\right)^{t/T_{1/2}}
Cancel N_t:
1 = 8 \left(\frac{1}{2}\right)^{t/T_{1/2}}
\left(\frac{1}{2}\right)^{t/T_{1/2}} = \frac{1}{8}
Since \frac{1}{8} = \left(\frac{1}{2}\right)^3, we equate the exponents:
\frac{t}{T_{1/2}} = 3
t = 3 \times T_{1/2}
5. Substitute for T_{1/2}:
t = 3 \times 1.4 \times 10^9 years
t = 4.2 \times 10^9 years
The age of the rock is 4.20 \times 10^9 years.
The electric potential at the surface of an atomic nucleus \( (z = 50) \) of radius \( 9 \times 10^{-13} \) cm is \(\_\_\_\_\_\_\_ \)\(\times 10^{6} V\).
In a nuclear fission reaction of an isotope of mass \( M \), three similar daughter nuclei of the same mass are formed. The speed of a daughter nuclei in terms of mass defect \( \Delta M \) will be: