Half-Life Determining the Age of a Material. How to Determine the Age of Something.
Transcript of Half-Life Determining the Age of a Material. How to Determine the Age of Something.
Types of Dating Absolute (exact number) Relative (approximate by putting in
order; 1st, 2nd, 3rd, …)
Tree Rings (Dendrochronology) Layers of Earth (Stratigraphy) Radioisotope (Radiometric)
Radioisotope Dating (Radioactive Decay) Mass can (not) be created nor destroyed
Radioactive decay means that the substance is changing (smaller by giving stuff away)
Half-life is a measurement of change (it is an average, not exact amount)
Half-life means the time it takes for ½ of something to turn into something else (not disappear)
The Process of Change
BeforeParent
Reactant
AfterDaughterProduct
The percent or fraction of change over
time
Change Different
Decay BiggerSmaller
Common Isotope Pairs Decay is
predictable
Each parent will decay into a specific daughter
Can be 1 step or a series (many) of steps
Half-Life The half-life is an approximation. A statistical
average. It is how we measure the change in decay
Google map says it takes 42 minutes to drive from Vancouver to Surrey
The average Canadian home has 1.9 children and 2.25 vehicles
Canadian Life Expectancy is 80.93 years
The chance of flipping a coin 5 times and getting all heads (each time) is 1/32
One generation is approximately 30 years
Half-Life The half-life is the rate of radioactive
decay for a given isotope
It is equal to the time required for ½ of the nuclei to decay (change)
Rate graph curve or line (w/ slope) x-axis = time Y-axis = amount of material (percent or
fraction)
Rate = percentage of material / time
DEMONSTRATION
Radioisotope Dating (Age) Because the process of decay can be
predicted or timed we can determine the age of things
If it takes 2 minutes for 500 grams of ice to turn into 250 grams at 22° Celsius
Then what can we predict:
We can Predict: How much we used to have (past) How much we will have (future) How old is it (past) How long will it live for (future) How old is something (unknown) compared to
something else (known)
Assume the rates (half-life) to be constant Use the percentage or fraction of change (not the
whole number) over time
½ or 50% of the ice melts, not 2.5 grams
Carbon Dating When things are
alive the ratio of C-14 to C-12 are equal
But, after death C-14 decays.
Calculating the ratio will give you the age
Initial: =
After: >
Potassium Clock When rocks are
formed by lava, all gasses are freed no Argon gas
But, after the rock is formed (hardened or cooled) then potassium decays into argon gas
Gas in rock tells age
Initial: = 0
After: > 0
Limitations/Dangers The age is only as accurate as the range
of the isotope
Can not measure things that are older than the isotope or things that will be around longer than it.
Have to be careful with initial conditions
Therefore we have to be careful in choosing an appropriate isotope to use
Types of Isotopes (General) Carbon-14 (5730 years): for life cycles
(organism’s remains) Potassium-40 (1,300 million years): for
the age of the earth Uranium-238 (4,468.3 million years):
makes plutonium Uranium-235 (703.8 million years): for
reactors & Weapons