Peoples Physics Book Version-2

(Marvins-Underground-K-12) #1

24.3. Decay Equations http://www.ck12.org


24.3 Decay Equations


Nuclear decay is often measured in terms of half lives. During the span of one half life, the amount of a decaying
substance decreases by half. Therefore, afterkhalf lives, the amount of a substance starting atN 0 left is


N(k) =N 0 ×^12
k

If we need to know the amount left after some timet, we first need to see find many half lives transpired (this will
be given bytHt, then use the formula above:


N(t) =N 0 ×^12
tt
H

If on the other hand, we know how much of a substance is left and would like to find how much time has transpired,
we can solve the equation above fort(left to reader):


t=tH

lnNN 0
ln^12

This equation is used in radioactive dating:


Question: The half-life of^239 Pu is 24,119 years. You have 31.25 micrograms left, and the sample you are studying
started with 2000 micrograms. How long has this rock been decaying?


Answer: We will use the equation for time and simply plug in the known values.


t=tH

lnNN 0
ln^12

=24119y

ln^312000.^25 μμgg
ln^12

= 144 ,700years

Radioactive carbon datingis a technique that allows scientists to determine the era in which a sample of biological
material died. A small portion of the carbon we ingest every day is actually the radioactive isotope^14 C rather than
the usual^12 C. Since we ingest carbon every day until we die (we do this by eating plants; the plants do it through
photosynthesis), the amount of^14 C in us should begin to decrease from the moment we die. By analyzing the ratio
of the number of^14 C to^12 C atoms in dead carbon-based life forms (including cloth made from plants!) and using
the technique illustrated above, we can determine how long ago the life form died.

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