02.06.2013 Views

Untitled - Kelly Walsh High School

Untitled - Kelly Walsh High School

Untitled - Kelly Walsh High School

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

302 CHEMISTRY FOR THE UTTERLY CONFUSED<br />

The current decay rate of the 14 C in a sample is 4.82 disintegrations per minute<br />

per gram (d/ming). The 14 C activity of living organisms is 15.3 d/ming. The halflife<br />

of 14 C is 5730 years. How many years old is the sample?<br />

We can recopy and label the variables to get:<br />

N 0 15.3 d/ming N t 4.82 d/ming t 1/2 5730 y t ?<br />

There is no single equation containing these four variables. For this reason, we<br />

need to use the two equations: ln (N t/N 0) kt and t 1/2 (ln 2)/k. We will<br />

begin with the half-life equation t 1/2 (ln 2)/k. We need to rearrange this equation<br />

and enter the half-life to determine the decay constant:<br />

k (ln 2)/t 1/2 (ln 2)/5730 y 0.693/5730 y<br />

1.209424 10 4 y 1 (unrounded)<br />

Now that we have the value of the decay constant, we can now use the other<br />

equation. We rearrange this equation:<br />

ln a<br />

t <br />

Nt b<br />

N0 k<br />

We can now enter the values and calculate the time.<br />

t 9550.8 9.55 103 4.82 d /min·g<br />

ln a<br />

15.3 d/min·g<br />

<br />

y<br />

b<br />

1.209402 104 y1 Nuclear reactions involve the decay of an unstable isotope to a more stable one.<br />

The natural decay modes include alpha emission, beta emission, gamma emission,<br />

positron emission, and electron capture. By considering the ratio of neutrons<br />

to protons in a particular isotope, we may be able to predict whether a<br />

certain isotope is stable and its possible decay modes. The half-life (t 1/2) is the<br />

amount of time that it takes for one-half of a sample of a radioactive isotope to<br />

decay. This decay follows first-order kinetics. Using the equations derived for<br />

first-order kinetics allows us to calculate time, half-life or amount. Einstein’s<br />

equation allows us to calculate the amount of energy released when a certain<br />

amount of matter is converted to energy. Practical applications of nuclear decay<br />

include fission, the decay of a larger isotope into two or more smaller ones, and<br />

fusion, the combining of lighter isotopes into a heavier one. Fission is currently<br />

used in nuclear power generators and atomic bombs. Fusion may eventually<br />

provide an unlimited power source.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!