One way to determine the age of a rock is to measure the extent to which the 87Rb in the rock has decayed to 87Sr (a first order process.)
k = 1.42 x 10-11 year-1
What fraction of the original 87Rb would still remain in the rock after 1.0 x 1010 years?
Can I just rearrange this equation:
ln(Rt) = ln(Ro) - kt . where Rt is amount at any time & Ro is original amount?
ln(Rt)/ln(Ro) = -kt
?
this way I get 14%
Or do I need to use 1/2 life?