Imagine rolling millions of dice all at once. You can never predict exactly which die will roll a six, or when it will happen, but you can confidently predict the overall average number of sixes on the first roll.
Understanding this constant probability explains why scientists use a statistical average, known as , to measure decay.
Understanding exactly how fast radiation fades explains why some medical isotopes are safe to inject, while nuclear waste must be buried for millennia.
Where:
A radioactive isotope used in hospitals has a of 6 hours. Calculate the in emission after 24 hours, expressing your answer as a .
Find the number of ():
Calculate the using the formula:
Express the as a of final to :
Why do graphs of radioactive decay never actually reach zero?
Students often forget to subtract the background count from their initial readings before calculating half-life—always check if the exam question gives you a background radiation value.
In 'Analyse' or 'Interpret' graph questions, examiners award specific marks for drawing clear construction lines (dashed lines) from the y-axis to the curve and down to the x-axis to physically show how you found the half-life.
When asked to 'Explain' half-life in terms of randomness, you must clearly state that while individual decays are completely unpredictable, the overall probability for a large group of nuclei remains constant.
When Higher Tier questions ask for net decline as a ratio, OCR mark schemes usually expect the final simplified ratio of the present activity to the initial activity (e.g., 1:16).
Random decay
A spontaneous process where the exact timing of an individual nucleus decaying cannot be predicted and occurs without any external influence.
Radioactive nuclei
Unstable atoms that will eventually emit radiation in order to become more stable.
Half-life
The average time taken for the number of radioactive nuclei in a sample to halve, or for its activity to fall to half its initial level.
Activity
The rate at which a source of unstable nuclei decays.
Becquerel (Bq)
The unit of radioactive activity, equal to one decay per second.
Count rate
The number of radioactive decays recorded each second by a detector, such as a Geiger-Müller tube.
Background count
The low-level radiation measured from the natural environment that must be subtracted from a source's total reading.
Net decline
The overall reduction in radioactive emission after a specific period of time, often expressed as a ratio or fraction.
Ratio
A mathematical expression comparing two values, such as the final activity compared to the initial activity.
Integral half-lives
Whole-number multiples of the half-life period (e.g., 1, 2, or 3).
Exponential decay curve
A graph showing a quantity that decreases at a rate proportional to its current value, resulting in a characteristic 'halving' shape.
Activity-time graph
A plot showing how the activity of a radioactive source (y-axis) changes over time (x-axis).
Initial activity
The activity of a radioactive sample at the very start of a measurement or observation (at time zero).
Background radiation
Ionizing radiation that is around us all the time from natural and man-made sources.
Fraction remaining
The proportion of radioactive nuclei that have not yet decayed after a given period of time.
Put your knowledge into practice — try past paper questions for Physics B
Random decay
A spontaneous process where the exact timing of an individual nucleus decaying cannot be predicted and occurs without any external influence.
Radioactive nuclei
Unstable atoms that will eventually emit radiation in order to become more stable.
Half-life
The average time taken for the number of radioactive nuclei in a sample to halve, or for its activity to fall to half its initial level.
Activity
The rate at which a source of unstable nuclei decays.
Becquerel (Bq)
The unit of radioactive activity, equal to one decay per second.
Count rate
The number of radioactive decays recorded each second by a detector, such as a Geiger-Müller tube.
Background count
The low-level radiation measured from the natural environment that must be subtracted from a source's total reading.
Net decline
The overall reduction in radioactive emission after a specific period of time, often expressed as a ratio or fraction.
Ratio
A mathematical expression comparing two values, such as the final activity compared to the initial activity.
Integral half-lives
Whole-number multiples of the half-life period (e.g., 1, 2, or 3).
Exponential decay curve
A graph showing a quantity that decreases at a rate proportional to its current value, resulting in a characteristic 'halving' shape.
Activity-time graph
A plot showing how the activity of a radioactive source (y-axis) changes over time (x-axis).
Initial activity
The activity of a radioactive sample at the very start of a measurement or observation (at time zero).
Background radiation
Ionizing radiation that is around us all the time from natural and man-made sources.
Fraction remaining
The proportion of radioactive nuclei that have not yet decayed after a given period of time.