Title: Dating a meteorite
1Dating a meteorite (make sure you bring it back
by midnight)
2Hi! Im a Rubidium 87 atom
3I have 37 protons and 50 neutrons
4Im a slightly unstable individual. Theres a
slight chance that one of my neutrons could
change into a proton and an electron a process
called beta decay.
5Then I would turn into a very stable Strontium
87 atom
6There is a fifty-fifty chance that Ill do that
in the next 48.8 billion years.
7Nothing you can do will speed up the
process. Beat me up, heat me itll have no
effect.
8Youll just have to be patient.
9Does anyone know any jokes?
1030 billion years later
11Sr 87
Oooh a change came over me. I feel like a new
atom!
12In a pinhead of Rubidium 87 there are about
100,000,000,000 billion atoms. So at this rate
how many of them will turn into Strontium 87
every day?
13At this rate of decay, nearly three million of us
will turn into Strontium 87 every day.
14A pinhead of Rubidium 87 is just like a clock
ticking at the rate of 3 million ticks a day.
After 48.8 billion years half of the Rb 87 will
have transformed into Sr 87.
15- On 15 July 1878 at 1.45 in the afternoon, this
25kg lump of rock thudded to the ground in
Moravia, Czech Republic. - It was named the Tieschitz meteorite
16- This piece of the Tieschitz meteorite includes
mineral crystals that contained Rubidium 87 when
it formed. - The meteorite also contained Strontium when it
was formed. Some of this was Sr 86 and some of
it was Sr 87.
17- As the Rb87 decayed, the Sr87 increased in
quantity. However the amount of Sr86 would have
stayed the same.
18- By finding out the ratios of these three isotopes
it is possible to work out how old a piece of
rock is.
19Here are 6 isotopes analyses of the Tiechitz. The
first four are from different mineral crystals
and the last two are from mixed samples. Use
this data to clot a graph that will let you find
out how old Tieschitz is.
20Plot of daughter/reference ratios v
parent/reference ratios of Rb-Sr87 decay system
in the Tieschitz meteorite
0.7.30
0.720
daughter/reference ratio Sr 87/Sr86
0.710
0.700
0.690
0.4
0.2
0.3
0.1
0
Parent/Reference ratio Rb87/Sr86
21(No Transcript)
22- As the meteorite gets older, the amount of Rb87
reduces and the amount of Sr87 increases making
the line steeper. - Just for interest, you can also tell the original
ratio of the two strontium isotopes. This is
where there was no original rubidium where the
line crosses the y axis. - Next you need to find out how steep the line is -
the gradient.
23(No Transcript)
24Now you can work out how old the meteorite is
- First work out the slope
- Slope y/x 0.0245/0.380
- 0.645
- Now use the slope and the Decay constant for
Rb/Sr decay ( 1.42x 10-11 yr-1 ) - Age 0.0645/ 1.42x 10-11 yr-1
25- The Tieschitz meteorite is
- 4.54 billion years old!