Question:

At depths of 2000 m in the sea, the pressure is about 200 times atmospheric pressure $(1 \textrm{ atm} = 1.0 \times 10^5 \textrm{ N/m}^2)$. By what percentage does the interior space of an iron bathysphere’s volume change at this depth?

Giancoli, Douglas C., Physics: Principles with Applications, 7th Ed., ©2014. Reprinted by permission of Pearson Education Inc., New York.

The question will be visible after logging in, as required by Pearson Education Inc.

Quick Answer:

$-2 \times 10^{-2} \%$

**Note:** The last step in the video incorrectly shows dividing by 100 when it should show **multiplying** by 100 to get the percentage. Thank you jsh2672 for spotting that mistake. The quick answer above is correct, whereas the video shows a mistaken result.

### Transcript for this Giancoli solution

This is Giancoli Answers with Mr. Dychko. We know the fractional change in volume will equal the negative of 1 over the bulk modulus of the iron times its change in pressure that it experiences. So the final pressure is at the bottom of the ocean: 200 times atmospheric pressure and we assume that it starts at atmospheric pressure. So that's 200*Pa*minus

*Pa*which is 199

*Pa*. So fractional change in volume is negative 199 times 1.0 times 10 to the 5 newtons per square meter— that's atmospheric pressure— divided by the bulk modulus of iron, 90 times 10 to the 9 newtons per square meter and times by 1 over 100 to turn it into a percent and that gives negative 2 times 10 to the negative 6 percent and the negative sign means the volume is gonna decrease by this much.

## Comments

Why are you multiplying by 1/100? Shouldn't you be multiplying by 100 to get the percentage?

Thank you very much jsh2672 for noticing that! I've corrected the quick answer to show the result after multiplying by 100, and put a note about the error in the video.

Best wishes,

Mr. Dychko