The element cobalt has one stable isotope: $^{59}$Co.
Chemists can construct several different isotopes of this
element with varying numbers of neutrons. All are unstable; the
five most stable are given in the following table (y=years,
d=days, m=minutes)
| Isotope |
Half life |
| $^{60}$Co |
5.2714 y |
| $^{57}$Co |
271.79 d |
| $^{56}$Co |
77.27 d |
| $^{58}$Co |
70.86 d |
| $^{55}$Co |
17.53 h |
I have a lump of pure cobalt, called sample $X$. I know that
sample X is uniformly composed of differing quantities of the
various isotopes of cobalt (including, possibly, some of the
more unstable isotopes not listed in the table above) in nice
ratios.
I take a piece of sample $X$ of weight $100$ g and leave it
to decay.
After exactly $10$ days $68.402$g of cobalt remains in the
sample. What information does this give you about the
possible initial composition of the sample? For example, are
there any isotopes which you can work out must be, or cannot
be, present in the sample? Use your common sense and simple
calculations before attempting a numerically detailed
analysis!
After $90$ days in total $58.283$g of cobalt remains. After
$360$ days $48.359$g of cobalt remains.
How accurately can you determine the composition of the
original sample? What would you expect the mass of cobalt to
reduce to in the long run?