A Big, Weird Mountain

Calculus Level 4

Geologists living on an infinite Euclidean plane, Earth, have recently discovered that their world is not so plane, or plain , after all. In fact, there is a very tall mountain on their Earth, stretching out to infinity and exactly described by the solid of revolution formed by rotating the curve y = H 0 e k x y=H_0e^{-kx} about the y y -axis. Probes have confirmed the existence of a very rare and precious mineral inside the mountain, distributed uniformly by 79 79 parts per 1 , 000 , 000 1,000,000 in volume.

If the density of said mineral is 34 kg/m 3 34 \text{ kg/m}^3 on average, what would be the mass (in kilograms) of the entire deposit, to 3 3 decimal places?

Details and Assumptions:

  • All units are in meters and kilograms.
  • k = 0.034 k=\sqrt{0.034}
  • H 0 = 9154 H_0=9154

The Mountain The Mountain


The answer is 4543.786.

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1 solution

Andrei Li
Nov 11, 2018

We can reduce the number of variables in the expression to one:

H 0 e k r H_0e^{-kr}

The volume of this 'mountain' can be approached by using concentric cyclindrical 'shells', with 'height' H 0 e k r H_0e^{kr} , 'width' 2 π r Δ r 2\pi r \Delta r , and 'volume' 2 π H 0 r e k r Δ r 2\pi H_0re^{-kr}\Delta r . As Δ r \Delta r \to \infty , this becomes the integral:

2 π H 0 0 r e k r d r 2\pi H_0\int_0^{\infty} re^{-kr} dr

Evaluate the antiderivative using integration by parts:

r e k r d r = 1 k r e k r 1 k e k r d r = 1 k r e k r 1 k 2 e k r \int re^{-kr} dr = -\frac{1}{k}re^{-kr}-\int -\frac{1}{k}e^{-kr} dr =-\frac{1}{k}re^{-kr}-\frac{1}{k^2}e^{-kr}

At r = 0 r=0 , this is simply 1 k 2 -\frac{1}{k^2} . At x x\to\infty , it is

lim x 1 k r e k r 1 k 2 e k r \lim_{x\to\infty} -\frac{1}{k}re^{-kr}-\frac{1}{k^2}e^{-kr}

While the second term obviously approaches zero, the first one requires to be solved by l'Hopital's Rule:

lim x r k e k r = lim x 1 k 2 e k r = 0 \lim_{x\to\infty}-\frac{r}{ke^{kr}}=\lim_{x\to\infty}-\frac{1}{k^2e^{kr}}=0

Thus, the volume is 2 π H 0 ( 0 ( 1 k 2 ) ) = 2 π H 0 k 2 2\pi H_0(0-(-\frac{1}{k^2}))=\frac{2\pi H_0}{k^2} , and when our values of k k and H 0 H_0 are inputted, we obtain 1 , 691 , 655.24 m 3 \sim1,691,655.24 m^3 . The volume of the mineral deposit is the volume of the mountain multiplied by 79 1 , 000 , 000 \frac{79}{1,000,000} , or 133.640764 m 3 133.640764 m^3 . Finally, we multiply by the density, 34 k g m 2 34 \frac{kg}{m^2} , to obtain our answer of

4543.786 \large\sim4543.786

I noticed that your image come from Desmos. How, exactly, did you get that graph?

Blan Morrison - 2 years, 7 months ago

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The integration can be done simpler using u = kx and then the Gamma function.

Andre Bourque - 2 years, 6 months ago

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