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# How long does radioactivity last?

Years 9 and 10 Chemistry · Inside the atom

<!-- Speaker note: Students define half-life, work out how much of a sample is left after a number of half-lives, explain that decay is random for one nucleus but predictable for many, and link half-life to uses (AC9S9U06, node 4). About 27 minutes (Engage and Explore 9 min · Explain 11 min · Fluorine-18 4 min · Evaluate 3 min · Wider adds about 6 min). -->

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## Today

**We are learning to** each unstable nucleus decays at random, but a large sample halves in a fixed time: its half-life. After one half-life half is left, after two a quarter, after three an eighth. Half-lives range from minutes to billions of years, which decides what each isotope is used for.

- I can define half-life.
- I can work out how much of a sample is left after a number of half-lives.
- I can explain why an isotope's half-life suits a use.

<!-- Speaker note: Before class: A concept tutorial for introducing or revising the idea; it pairs well with the dice (or coin) simulation in class. Set the width with `?width=minimum`, `typical` (default) or `wider`. It builds on Isotopes and Alpha, beta and gamma (nodes 2 and 3). Not a hinge node, but its misconception is stubborn: students expect a sample to be gone after two half-lives, or each nucleus to decay at its half-life. The prediction tests the first; the "one nucleus" question tests the second. Board notes: the sample is simulated: in each tenth of a half-life every remaining nucleus decays with the same chance (about 6.7%), so the count halves on average each half-life but wobbles, more so with 100 nuclei than with 400. Each Start again is a new random sample. The dashed curve (exact halving) appears once a run has finished. Time is shown in the isotope's own unit. Teacher: In your own words: the sketch with one half-life marked and the 64-nuclei table are the evidence. -->

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## Why it matters

> Doctors give patients a radioactive drug in the morning that is almost gone by the next day. Yet some uranium in the rocks under you was made before the Earth formed, and about half of it is still there.

<!-- Speaker note: Unstable nuclei decay. This lesson asks how fast. -->

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## Engage: predict

**A sample has 80 iodine-131 nuclei. Half of any sample decays in 8 days. How many are left after 16 days?**

- 20
- 40
- 60
- 0: two halves make a whole

<!-- Speaker note: What happens: About 20. In the first 8 days half of the 80 go, leaving 40. In the next 8 days half of those 40 go, leaving 20. It halves each time; it never takes the same number twice. Take two or three predictions before anyone runs it. -->

<!-- Speaker note: Teacher: tally 20 / 0 / 40 / 60. The zeros are the misconception to work on. -->

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## Explore it

{{embed: https://studio.learningwaypoints.com/tutorials/_playground-board/index.html?id=deck%2Fscience%2Fchemistry-9-10%2Fhalf-life%2Fstep-2&code=widget%3A+atom%0Amode%3A+halflife%0Aisotope%3A+iodine-131%0Anuclei%3A+100%0A&fresh=1}}

[Open this step in the tutorial](https://studio.learningwaypoints.com/tutorials/science/chemistry-9-10/half-life/?full=step-2#step-2)

<!-- Speaker note:  -->

<!-- Speaker note: Teacher: after two runs, ask which nuclei decayed (different ones) and whether the graph changed much (not much). -->

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## What happened?

* About 20. In the first 8 days half of the 80 go, leaving 40. In the next 8 days half of those 40 go, leaving 20. It halves each time; it never takes the same number twice.

<!-- Speaker note: Reveal after running. Ask who predicted it, and what made them think so. -->

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## What half-life is

**What is the half-life of a radioactive isotope?**

- The time for half the nuclei in a sample to decay
- The time for one nucleus to decay halfway
- Half the time it takes the whole sample to decay

* Answer: The time for half the nuclei in a sample to decay

<!-- Speaker note: The half-life is the time for half the nuclei in a sample to decay. It is the same however big the sample is and however long it has been decaying. -->

<!-- Speaker note: Teacher: the two calculations and the definition are the success criteria; the 'one nucleus' question is the probabilistic idea. -->

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## Three half-lives

**A sample starts with 800 nuclei. How many are left after 3 half-lives?**

* Answer: 100

<!-- Speaker note: 800 → 400 → 200 → 100. After 3 half-lives, an eighth is left. -->

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## Carbon-14

**Carbon-14 has a half-life of 5730 years. How many years until a quarter of a sample is left?**

* Answer: 11460

<!-- Speaker note: A quarter is left after 2 half-lives: 2 × 5730 = 11 460 years. -->

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## One nucleus

**You watch one carbon-14 nucleus. When will it decay?**

- Within 5730 years for certain
- In exactly 5730 years
- No one can say: it could be in a second or in 50 000 years

* Answer: No one can say: it could be in a second or in 50 000 years

<!-- Speaker note: Decay is random for each nucleus. Only for a large sample can we say how many will go in a given time. -->

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## Nothing changes it

**A sample is heated, crushed and dissolved in acid. What happens to its half-life?**

- Nothing: half-life is the same whatever you do to the sample
- It gets shorter
- It gets longer

* Answer: Nothing: half-life is the same whatever you do to the sample

<!-- Speaker note: Half-life is a property of the nucleus. Temperature, pressure and chemical reactions change the electrons around it, not the nucleus. -->

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## Elaborate: fluorine-18 in hospitals

{{embed: https://studio.learningwaypoints.com/tutorials/_playground-board/index.html?id=deck%2Fscience%2Fchemistry-9-10%2Fhalf-life%2Fstep-4&code=widget%3A+atom%0Amode%3A+halflife%0Aisotope%3A+fluorine-18%0Anuclei%3A+100%0A&fresh=1}}

[Open this step in the tutorial](https://studio.learningwaypoints.com/tutorials/science/chemistry-9-10/half-life/?full=step-4#step-4)

<!-- Speaker note: What this step is for: Matching a short half-life to medical imaging gives half-life a purpose: the isotope must last long enough to take the picture, then fade quickly. -->

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## After 330 minutes

**Fluorine-18 has a half-life of 110 minutes. What percentage of it is left 330 minutes after it is made?**

* Answer: 12.5

<!-- Speaker note: 330 minutes is 3 half-lives: 100% → 50% → 25% → 12.5%. -->

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## Why 2 hours

**Fluorine-18 is used in PET scans: it is made in the hospital, injected, and its radiation is detected outside the body. Why does a half-life of about 2 hours suit this?**

- Any half-life would do: it makes no difference
- So the patient stays radioactive for years, ready for the next scan
- Long enough to make, inject and scan, short enough that little is left in the body by the next day

* Answer: Long enough to make, inject and scan, short enough that little is left in the body by the next day

<!-- Speaker note: After a day (about 13 half-lives) less than a thousandth is left. Isotopes for dating rocks, by contrast, need half-lives of millions or billions of years. -->

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## Elaborate: dating the past

{{embed: https://studio.learningwaypoints.com/tutorials/_playground-board/index.html?id=deck%2Fscience%2Fchemistry-9-10%2Fhalf-life%2Fstep-5&code=widget%3A+atom%0Amode%3A+halflife%0Aisotope%3A+carbon-14%0Anuclei%3A+400%0A&fresh=1}}

[Open this step in the tutorial](https://studio.learningwaypoints.com/tutorials/science/chemistry-9-10/half-life/?full=step-5#step-5)

<!-- Speaker note: What this step is for: Radiocarbon dating uses half-life backwards; its limit (too little carbon-14 left after about 50 000 years) explains why the oldest dates for people in Australia come from other methods that agree with it. -->

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## An old fireplace

**Charcoal from an old fireplace has an eighth of the carbon-14 that living wood has. Carbon-14's half-life is 5730 years. About how old is it, in years?**

* Answer: 17190

<!-- Speaker note: An eighth is left after 3 half-lives: 3 × 5730 = 17 190 years. -->

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## The limit

**Radiocarbon dating works back to about 50 000 years. Why not further?**

- After about 9 half-lives less than a five-hundredth of the carbon-14 is left, too little to measure reliably
- Nothing older than 50 000 years contains carbon
- Carbon-14 stops decaying after 50 000 years

* Answer: After about 9 half-lives less than a five-hundredth of the carbon-14 is left, too little to measure reliably

<!-- Speaker note: Each half-life halves what is left: after 9 half-lives (about 52 000 years) less than 0.2% remains, and tiny traces of modern carbon would swamp it. -->

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## More than 60 000 years

**Sites in northern Australia show First Peoples were there more than 60 000 years ago. Radiocarbon dates the younger layers; older layers are dated by other methods, such as luminescence (when sand grains were last in sunlight). Why does using more than one method matter?**

- Radiocarbon is always wrong
- It doesn't: one method is enough
- Independent methods that agree make the dates much more trustworthy

* Answer: Independent methods that agree make the dates much more trustworthy

<!-- Speaker note: Where their ranges overlap the methods are checked against each other, and agreement between independent methods is strong evidence. Together with First Peoples' own knowledge of Country, they show people have lived in Australia for more than 60 000 years. -->

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## Evaluate: look back

Write one sentence: "At first I thought… Now I think… because…"

**Revision summary**

- Each unstable nucleus decays at random: no one can say which will go next, or when.
- A large sample decays in a predictable way: half of it goes in one **half-life**, half of what is left in the next, and so on (1/2, 1/4, 1/8 …).
- Half-life is a property of the isotope; heat, pressure and chemical reactions don't change it.
- Short half-lives suit medical imaging (fluorine-18, about 2 hours); long ones suit dating (carbon-14, 5730 years; uranium-238, 4.5 billion years).

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## Exit ticket

**Iodine-131 has a half-life of 8 days. A hospital receives 40 g. How much is left after 24 days?**

* 5 g (40 → 20 → 10 → 5: three half-lives).

<!-- Speaker note: Students answer on paper or a mini whiteboard before the reveal. Anyone who cannot answer needs the main idea again next lesson. Where this leads: Next: decay chains (node 5) are a class task: the decay board with `isotope: uranium-238` follows the chain to lead-206. Half-life links to geological time in Earth and space. In class: the dice simulation (each roll, remove every die showing a 6) and a class decay curve; compare with the board's. The Wider step on dating First Peoples' presence is general: radiocarbon dates the younger layers and other methods (luminescence) the older ones. For richer context, use local resources and community guidance, and First Peoples' own accounts of their history on Country. -->
