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 about the -axis. Probes have confirmed the existence of a very rare and precious mineral inside the mountain, distributed uniformly by parts per in volume.
If the density of said mineral is on average, what would be the mass (in kilograms) of the entire deposit, to decimal places?
Details and Assumptions:
The Mountain
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We can reduce the number of variables in the expression to one:
H 0 e − k r
The volume of this 'mountain' can be approached by using concentric cyclindrical 'shells', with 'height' H 0 e k r , 'width' 2 π r Δ r , and 'volume' 2 π H 0 r e − k r Δ r . As Δ r → ∞ , this becomes the integral:
2 π H 0 ∫ 0 ∞ r e − k r d r
Evaluate the antiderivative using integration by parts:
∫ r e − k r d r = − k 1 r e − k r − ∫ − k 1 e − k r d r = − k 1 r e − k r − k 2 1 e − k r
At r = 0 , this is simply − k 2 1 . At x → ∞ , it is
x → ∞ lim − k 1 r e − k r − k 2 1 e − k r
While the second term obviously approaches zero, the first one requires to be solved by l'Hopital's Rule:
x → ∞ lim − k e k r r = x → ∞ lim − k 2 e k r 1 = 0
Thus, the volume is 2 π H 0 ( 0 − ( − k 2 1 ) ) = k 2 2 π H 0 , and when our values of k and H 0 are inputted, we obtain ∼ 1 , 6 9 1 , 6 5 5 . 2 4 m 3 . The volume of the mineral deposit is the volume of the mountain multiplied by 1 , 0 0 0 , 0 0 0 7 9 , or 1 3 3 . 6 4 0 7 6 4 m 3 . Finally, we multiply by the density, 3 4 m 2 k g , to obtain our answer of
∼ 4 5 4 3 . 7 8 6