Poisson Probability Guide
Poisson Counts in Experimental Physics
Many detectors produce integer counts: radioactive decays, photon arrivals, ion hits, and rare trigger events. When events are independent and occur at a roughly constant average rate, the Poisson model is a practical first description for the count distribution within a fixed exposure window.
Key Inputs: Rate and Exposure
This calculator separates the physical rate λ (events per unit) from the exposure t (time, area, length, or any scale that linearly accumulates opportunity). Their product μ = λt is the expected count. For example, λ = 20 counts/s and t = 0.10 s gives μ = 2 expected counts.
Interpreting μ, Mean, and Variance
A defining feature of the Poisson distribution is that the mean and variance are both μ. This matters for uncertainty: the standard deviation is √μ, so relative noise scales as √μ/μ = 1/√μ. Doubling μ improves relative precision by about 1/√2, a common rule of thumb in counting statistics.
Exact Probability for a Single Count
Use Exact: P(X = k) when you want the probability of observing one specific count. If μ = 2, the probabilities are P(0) = e−2 ≈ 0.1353 and P(2) = e−2 22/2! ≈ 0.2707. Exact probabilities are useful for validating simulations and checking discrete outcomes.
Cumulative and Tail Probabilities
Engineering and physics decisions often depend on thresholds. P(X ≤ k) answers “How likely is a low count?” while P(X ≥ k) answers “How surprising is a high count?” If μ = 6 and you observe k = 12, the tail probability P(X ≥ 12) can quantify how unusual that spike is under the assumed rate.
Interval Probabilities for Acceptance Windows
Interval mode computes P(k ≤ X ≤ k₂), useful for defining pass bands in quality control, coincidence windows, or expected background ranges. For μ = 4, the probability of falling between 2 and 6 counts summarizes the “typical” region more directly than a single exact value.
Practical Data Examples in the Lab
In photon counting, a calibrated source might yield λ = 500 s−1. With t = 2 ms, μ = 1.0, so P(X = 0) ≈ 0.3679 and P(X ≥ 1) ≈ 0.6321. In radiation monitoring, λ = 0.2 s−1 over t = 60 s gives μ = 12, where √μ ≈ 3.46 sets a natural scale for fluctuations.
Limits, Assumptions, and Good Practice
The model assumes independent events and a stable average rate across the exposure. Dead time, pileup, drifting sources, or correlated bursts can break these assumptions. When μ becomes very large, the Poisson distribution approaches a normal distribution with mean μ and variance μ, which this calculator may use for stable cumulative estimates.