Radioactive decay is random for one nucleus and remarkably regular for a large population. You cannot predict which atom will transform next, but you can predict the expected fraction of a parent nuclide that remains after a measured time. The single-parent decay law turns that distinction into a calculator: it connects the number of undecayed nuclei, the activity in becquerels, the decay constant, and the half-life.
N(t) = N0e−λt · A(t) = λN(t)Keep λ and t in reciprocal, matching time units; the exponent must be dimensionless.

What the symbols mean
N(t) counts the parent nuclide only; it does not count daughter nuclei created by decay. λ is the conditional probability rate for a surviving nucleus in the constant-hazard model. The product λt has no unit. If the half-life is entered in hours, use hours for t and h⁻¹ for λ, or convert both to seconds before calculating activity in Bq.
Deriving the exponential law from constant hazard
Assume that, over a short interval dt, each surviving nucleus has decay probability λdt plus smaller-order terms. The expected population loss is proportional to the population still present:
dN = −λN dtdN/N = −λ dtln(N/N0) = −λtN(t) = N0e−λt−dN/dt = λN(t)A(t) = λN(t) = A0e−λtThe smooth curve is an expectation for a population. Individual transformations are independent random events, and a small detector sample can fluctuate around the curve. The exponential is not a claim that an identical fraction decays in every short interval or that a single atom has a predictable deadline.
Half-life, decay constant, and mean lifetime
Set N(T1/2) = N0/2 in the law:
T1/2 = ln 2 / λλ = ln 2 / T1/2τ = 1/λ = T1/2/ln 2The mean lifetime τ is about 1.4427T1/2. After one mean lifetime, the remaining fraction is e⁻¹ ≈ 0.3679, not one-half. After n half-lives, both parent population and intrinsic activity have fallen by 2−n for a pure parent source.
Activity is not the same as a nucleus count
Activity is the expected transformation rate:
A(t) = −dN/dt = λN(t)A0 = λN01 Bq = 1 s⁻¹Use λ in s⁻¹ when reporting Bq. A curie is an older activity unit: 1 Ci = 3.7 × 1010 Bq. The named becquerel distinguishes activity from any other quantity with reciprocal-second dimensions. The activity of a pure parent source and its parent count have the same exponential fraction, but they are different quantities with different units and interpretations.

Rearrangements for a decay calculator
Define the dimensionless remaining fraction f = N/N0. For a pure parent source with comparable activity calibration, f = A/A0 as well:
f = e−λt = 2−t/T1/2t = −ln(f)/λ = T1/2ln(1/f)/ln2N0 = N eλtA0 = A eλtλ = ln(N0/N)/tT1/2 = t ln2 / ln(N0/N)The domain for a finite elapsed time is 0 < f ≤ 1. Form the ratio before taking a logarithm: ln(0.300 MBq) is not meaningful, while ln(A/A0) is dimensionless. An inferred half-life is meaningful only when the two measurements refer to the same parent population and the same activity definition.
Worked example 1: population and intrinsic activity
Given N0 = 8.00 × 1012 parent nuclei, T1/2 = 6.00 h, and t = 15.0 h, find N(t) and A(t).
λ = ln2/6.00 h = 0.115524530 h⁻¹n = 15.0/6.00 = 2.50f = 2⁻²·⁵⁰ = 0.176776695N = (8.00 × 1012)f = 1.41421 × 1012λ = 0.115524530/3600 = 3.20901472 × 10⁻⁵ s⁻¹A = λN = 4.53823 × 107 Bq = 45.3823 MBqChecks: N/N0 = 0.176776695 agrees with e−λt. The initial activity is A0 = λN0 = 2.56721 × 108 Bq, and A/A0 = 45.3823/256.721 = 0.1767767. The activity is not the count of nuclei; it is the expected number of transformations per second.
Worked example 2: infer elapsed time from activity
Suppose a single parent source starts at A0 = 2.40 MBq, has half-life 12.0 h, and later measures A = 0.300 MBq. Find the elapsed time.
f = A/A0 = 0.300/2.40 = 0.125000 = 1/8λ = ln2/12.0 h = 0.057762265 h⁻¹t = −ln(0.125000)/0.057762265 = 36.0 h0.125 = 2⁻³, so t = 3 × 12.0 h = 36.0 hA(36 h) = 2.40 × 2⁻³ = 0.300 MBq0 < A/A0 ≤ 1This is an inverse model calculation, not a detector calibration. If “0.300 MBq” is really a raw count rate, first correct for efficiency, geometry, emission probability, dead time, and background.
Measuring activity in the real world
Intrinsic activity A = λN is an expected physical transformation rate. An instrument usually reports counts per second or an inferred activity. The conversion depends on detector efficiency, source-to-detector geometry, emission probability for the selected radiation line, background, dead time, coincidence effects, and calibration uncertainty. Sparse counts also fluctuate: for an ideal Poisson count, the variance equals the mean.
Always attach a reference time to an activity value. A detector reading can be correct for its timestamp and still be misused in a decay calculation if the timestamp is omitted. Use Bq for the calibrated activity, not a count rate that has not been corrected. Report uncertainty when the measurement, rather than the decay law, is the limiting source of precision.
Decay chains and branching are different models
The one-parent law does not describe a mixture or a daughter chain automatically. A parent may have multiple decay branches; a daughter may itself be radioactive. In a chain, coupled balance equations (often called Bateman equations) determine daughter ingrowth and activity. At secular equilibrium, daughter and parent activities can become similar even though their decay constants differ. A graph that appears to have one smooth half-life can therefore be an effective summary of several nuclides, not a physical half-life of one parent.
For biological clearance, leakage, chemical separation, or another independent first-order removal process, an observed effective constant can sometimes be written λeff = λphysical + λremoval. Its effective half-life is not the nuclide’s physical half-life. State which constant the calculator is returning instead of hiding removal inside a generic “decay” field.

Reading a decay curve without over-interpreting it
A straight line appears only after taking the natural logarithm of a correctly normalized parent fraction: ln(N/N0) = −λt. Its slope has reciprocal-time units and its intercept is zero only when the chosen reference really is t = 0 for the same population. If a graph uses detector counts, first correct for background and keep the efficiency and geometry constant; otherwise a change in the instrument can masquerade as a change in λ.
The ratio form is often more reliable than subtracting two large activity values. For example, if both measurements share a common calibration factor, that factor cancels in A/A0. It does not cancel if the source moved, the emission line changed, the detector dead time changed, or a daughter contribution grew between measurements. An apparently tidy half-life can therefore be a property of the measurement setup rather than of the nuclide.
Use guard digits for λ and the fraction in an inverse calculation. When f is close to one, a small absolute error in two nearly equal activity readings can cause a large relative error in −ln f. When f is very small, background subtraction and finite counting statistics become dominant. A calculator should expose the ratio, timestamp, and uncertainty inputs instead of presenting an age as if it were exact.
Activity, dose, and count rate are not interchangeable
Activity describes transformations per unit time. Absorbed dose describes energy deposited per unit mass, and equivalent or effective dose includes radiation weighting and tissue factors. A high activity does not by itself determine a dose rate: particle energy, emission spectrum, shielding, distance, geometry, exposure time, and biological context also matter. This article’s A = λN relation is therefore not a dose calculator.
Likewise, a detector count rate is a measurement signal. To infer activity, a calibration model maps counts through efficiency, branching or emission probability, geometry, dead-time correction, and background. If any of those terms changes with time, the simple activity ratio is invalid. Keep the names visible in a user interface so that “Bq,” “counts per second,” and “dose” cannot be entered into one unlabeled field.
Common errors and guardrails
| Error | Why it fails | Repair |
|---|---|---|
| Mix seconds and hours | The exponent gains an unintended factor of 3,600. | Use matching units for λ and t; use s⁻¹ for Bq. |
| Use T1/2 where λ belongs | Half-life and decay constant are related but not equal. | Convert with λ = ln2/T1/2. |
| Treat activity as a nucleus count | A has units of Bq; N is a count. | Use A = λN and state the unit. |
| Confuse τ with T1/2 | One mean lifetime leaves e⁻¹, not one-half. | Use τ = 1/λ = T1/2/ln2. |
| Subtract a fixed number per interval | Decay removes a fraction of survivors, not a fixed count. | Use the exponential law or half-life powers. |
| Use detector counts as Bq | Efficiency, background, and geometry are missing. | Apply a stated calibration and uncertainty model. |
| Force a chain into one half-life | Daughter ingrowth and branches change the signal. | Use coupled chain equations or label an effective fit. |
| Round λ too early | Inverse logarithms magnify small parameter errors. | Keep guard digits until the final display. |
Limits of the single-exponential model
The model assumes one identified parent, a constant decay constant, a fixed reference time, no external production or removal, and a large enough population that the expected curve is informative. It does not model detector response, daughter photons, self-absorption, changing chemistry, biological clearance, or a time-varying source. For a nuclide-specific half-life, use an evaluated nuclear-data record and report its reference and uncertainty; a generic calculator example is not a substitute for isotope identification.
Sources and further reading
- OpenStax University Physics Volume 3, “Radioactive Decay”
- IAEA Module I: Nuclear physics and reactor theory
- IAEA TECDOC-1363: Guidelines for radioelement analysis
- BIPM CGPM Resolution 8: SI unit of activity
- NIST SP 330, SI Brochure §2
- NIST SP 811, Appendix B.9
- NIST RPD-P-23 activity calibration procedure
- U.S. NRC, “Radioactive decay” glossary
- U.S. NRC, “Radiation Basics”
- IAEA Manual for the Use of Stable Isotopes in Hydrology
- IAEA Nuclear Data Services