7.2 Half-Life 7.2 Half-Life the time it takes for half of a radioactive sample to decay the time it...

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7.2 Half-Life 7.2 Half-Life the time it takes for half of a the time it takes for half of a radioactive sample to decay radioactive sample to decay is a constant rate (always the same half is a constant rate (always the same half life for each element) life for each element) Example Example : Strontium-90 has a half-life of 29 : Strontium-90 has a half-life of 29 years. If you have 10 g of strontium-90 years. If you have 10 g of strontium-90 today, there will be 5 g (half) remaining today, there will be 5 g (half) remaining in 29 years. in 29 years. Terminology: Terminology: Parent isotope Parent isotope : the original radioactive : the original radioactive material material Daughter isotope Daughter isotope : the stable product that : the stable product that remains remains after decay has happened after decay has happened

Transcript of 7.2 Half-Life 7.2 Half-Life the time it takes for half of a radioactive sample to decay the time it...

Page 1: 7.2 Half-Life 7.2 Half-Life the time it takes for half of a radioactive sample to decay the time it takes for half of a radioactive sample to decay –is.

7.2 Half-Life7.2 Half-Life the time it takes for half of a radioactive the time it takes for half of a radioactive

sample to decaysample to decay– is a constant rate (always the same half life is a constant rate (always the same half life

for each element)for each element)

ExampleExample: Strontium-90 has a half-life of 29 : Strontium-90 has a half-life of 29 years. If you have 10 g of strontium-90 today, years. If you have 10 g of strontium-90 today, there will be 5 g (half) remaining in 29 years.there will be 5 g (half) remaining in 29 years.

Terminology:Terminology:Parent isotopeParent isotope: the original radioactive material: the original radioactive materialDaughter isotopeDaughter isotope: the stable product that : the stable product that

remains remains after decay has after decay has happenedhappened

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Decay Curves:Decay Curves:

Show the rate of Show the rate of decay for radioactive decay for radioactive elementselements

show the relationship show the relationship between half-life and between half-life and percentage of original percentage of original substance remaining.substance remaining.

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Radioactive Dating:Radioactive Dating: a method to determine age of objects a method to determine age of objects compares amount of parent isotope to compares amount of parent isotope to

daughter isotope.daughter isotope.

Example: Carbon dating measure the Example: Carbon dating measure the ratio of carbon-12 and carbon-14.ratio of carbon-12 and carbon-14.– Stable carbon-12 and radioactive carbon-Stable carbon-12 and radioactive carbon-

14 exist naturally in a constant ratio.14 exist naturally in a constant ratio. In nature, carbon-12 appears 98.9% of the In nature, carbon-12 appears 98.9% of the

time, while carbon-14 is very rare.time, while carbon-14 is very rare.

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When an organism dies, carbon-14 stops When an organism dies, carbon-14 stops being taken in and continues to slowly being taken in and continues to slowly decay.decay.– Comparing the amounts of carbon-12 to Comparing the amounts of carbon-12 to

carbon-14 is called carbon-14 is called radiocarbon datingradiocarbon dating and and gives us an age for the object.gives us an age for the object.

– Radiocarbon dating only works for organisms Radiocarbon dating only works for organisms less than 50,000 years old because the half-life less than 50,000 years old because the half-life of carbon-14 is 5730 years. (after 50,000 of carbon-14 is 5730 years. (after 50,000 years, there isn’t enough C-14 left!)years, there isn’t enough C-14 left!)

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There are many radioisotopes There are many radioisotopes that can be used for datingthat can be used for dating

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some elements require one step to decay, some elements require one step to decay, while others decay over many steps while others decay over many steps before reaching a stable daughter isotope.before reaching a stable daughter isotope.– Carbon-14 decays into nitrogen-14 in one stepCarbon-14 decays into nitrogen-14 in one step– Uranium-235 decays into lead-207 in fifteen Uranium-235 decays into lead-207 in fifteen

steps.steps.– Thorium-235 decays into lead-208 in ten Thorium-235 decays into lead-208 in ten

steps.steps.

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The Potassium-40 ClockThe Potassium-40 Clock Radioisotopes with very long half-Radioisotopes with very long half-

lives can help determine the age of lives can help determine the age of very old things.very old things. The potassium-40/argon-The potassium-40/argon-40 clock has a half-life of 40 clock has a half-life of 1.3 billion years.1.3 billion years.

Argon-40 produced by the Argon-40 produced by the decay of potassium-40 decay of potassium-40 becomes trapped in rock.becomes trapped in rock.

Ratio of potassium-40 : Ratio of potassium-40 : argon-40 shows age of argon-40 shows age of rock.rock.

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Half-life ProblemsHalf-life Problems::

1. What mass of a 200g sample of 1. What mass of a 200g sample of carbon-14 remains after 22,920 carbon-14 remains after 22,920 years?years?

2. A rock has 420g of radioactive 2. A rock has 420g of radioactive isotope. What percentage would isotope. What percentage would remain after 5 half-lives?remain after 5 half-lives?