Half-life formulas are a decent metric to calculate the half-life of radioactive elements. The need for this formula occurred when the slowed rate of decay was found during the years. When an element is reduced, its decay rate also decreases, which might be challenging to calculate after some point. In simple words, the half-life is the time of decaying to half.
It is the time required to decay a radioactive element to its half. It can be alpha, beta or gamma decay in nature.
Example: Uranium₂₃₈ has a half-life of 4.5 billion years.
The half-life of elements and kinetic order of reactions have some connection.
The half-life of zero-order kinetic and second-order kinetic reactions depends on the rate of reaction constant and initial concentration.
The half-life of a first-order kinetic reaction depends on the reaction rate constant only.
To know whether a radioactive object or place is safe.
To calculate the age of organic objects.
To calculate the age of old artefacts.
Various kinds of half-life formulas are present depending on the data provided or the nature of decay.
m= 1/2ⁿ x original mass.
Where m is the mass remaining and
n is the number of half-lives.
Example :
How much Np-240 will be remaining after 6 hours if there is 75g now? (Given that half-life of Np- 240 is one hour)
Answer: m= 1/2ⁿ x original mass.
=1/2⁶x 75
=1.1718
Suppose we know the half-life of an element and how much mass remains. To calculate the amount of time required to obtain the mentioned mass is,
How long it will take an element ‘x’ to decay to 12.5g from 100g (half-life is 1200 years)
An exponential decay can be calculated by
From the exponential decay formula, we obtain another equation as
if λ is 1.6, what is the half-life of the particular element?
Answer: t1/2 = 0.693/ λ
Conclusion
The half-life is the time required to decay a radioactive element to its half. It can be alpha, beta or gamma decay in nature. Half-life formulas are a decent metric to calculate the half-life of radioactive elements. The need for this formula occurs after we find the slowed rate of decay during the years.