Research and learning

1937

Element 43: Activity versus Identity

Read Perrier and Segrè’s 1937 record, then compare an invented mixed signal with a single-component claim without confusing time behaviour and chemical identity.

Original learning illustration: Element 43: Activity versus Identity
43
Atomic number proposed in the record
200, 75, 31.25
Invented signal at 0, 2, 4 days

The short answer

A signal can be radioactive without telling the observer which element produced it. Follow the historical distinction first, then test whether a fictional time series behaves like one component.

Original record and worked interpretation

Two questions for one sample

Ask what kind of conclusion each piece of information supports.

The numerical series is entirely invented.
QuestionEvidence used hereConclusion permitted
One fixed halving ratio?Two equal-interval ratiosThe fictional sum fails that condition.
Which element?Chemical discrimination in the historical recordNot supplied by the invented time series.
Exact historical halving periods?No complete underlying dataset inspectedNo values reconstructed.

Chronology

A timeline of the turning points

  1. Identification records

    Chemical evidence distinguishes activities.

  2. Original exercise

    An invented mathematical mixture.

What separated activity from an assignment

Perrier and Segrè’s Nature abstract describes an irradiated molybdenum plate supplied by Lawrence. It reports more than one radioactive component and chemical exclusions of zirconium, niobium, molybdenum and ruthenium before proposing atomic number 43.

The reproduced JCP opening also identifies multiple activities. The historical investigation did more than notice a decaying signal: it combined that signal with chemical discrimination. No laboratory separation procedure is reproduced here.

Sources for this section: [1] · [2]

Define the invented time series

Let t be time in days. Define two fictional detector-signal components by A(t)=100×2^(−t) and B(t)=100×2^(−t/2), in arbitrary signal units. Thus A halves each day and B every two days. Assume the detector adds them linearly with no background or daughter contribution.

Find their sum at t=0, 2, 4. Does the combined signal lose the same fraction in each two-day interval? The stipulated signals are not numbers of atoms, and their halving intervals are not historical measurements from the paper.

Sources for this section: [1]

Reference answer: the changing ratio

At t=0 the sum is 200. At t=2 it is 25+50=75. At t=4 it is 6.25+25=31.25. The successive two-day ratios are 75/200=0.375 and 31.25/75=5/12≈0.416667. They differ.

Under this idealised, noiseless fixture, the sum is therefore not a single component with one fixed halving ratio over these intervals. A slower component accounts for a growing share of what remains. That diagnosis still does not assign an atomic number to either component.

Sources for this section: [1]

Keep the evidential tasks distinct

A time pattern can challenge a one-component model under its assumptions. Chemical identity is a different conclusion requiring different evidence. Conversely, failure of this simple two-component fixture would not by itself identify the missing cause: background, changing detection or a more complicated decay chain could also matter. The exercise establishes none of those alternatives as a fact about the historical sample.

Sources for this section: [1]

Continue the chronology

Biography context

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Connected biographies

The researcher behind the record

Quick answers

Common questions

Do the invented signals represent atom counts?
No. They are detector-signal components stipulated to add linearly.
Does a changing ratio reveal an atomic number?
No. It tests the stated time-series model, not an elemental identification.

Primary and institutional sources

How this history was checked

Historical claims use the selected records below. Invented inputs and worked interpretations are labelled; they are not reconstructed experiments. This article was reviewed on 31 October 2026.

  1. C. Perrier and E. Segrè / Nature 140, 193–194 (1937)Radioactive Isotopes of Element 43
  2. C. Perrier and E. Segrè / Journal of Chemical Physics 5 (1937); opening reproduced in CERN-hosted presentation, PDF16Some Chemical Properties of Element 43 (opening excerpt)