/*! This file is auto-generated */ .wp-block-button__link{color:#fff;background-color:#32373c;border-radius:9999px;box-shadow:none;text-decoration:none;padding:calc(.667em + 2px) calc(1.333em + 2px);font-size:1.125em}.wp-block-file__button{background:#32373c;color:#fff;text-decoration:none} Problem 21 Find the volume of the solid in ... [FREE SOLUTION] | 91Ó°ÊÓ

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Find the volume of the solid in the first octant bounded above by the surface \(z=r \sin \theta,\) below by the \(x y\) -plane, and laterally by the plane \(x=0\) and the surface \(r=3 \sin \theta\)

Short Answer

Expert verified
The volume of the solid is \(\frac{3\pi}{8}\).

Step by step solution

01

Understand the Boundaries

The solid is bounded above by the surface given by \(z = r \sin \theta\), below by the \(xy\)-plane where \(z = 0\), laterally by the plane \(x = 0\) and the surface \(r = 3 \sin \theta\). We need to compute the volume that resides in the first octant where \(r\geq 0\), \(z\geq0\), and both \(x\) and \(y\) are non-negative.
02

Convert to Polar Coordinates

The given problem is symmetric around the \(z\)-axis, making polar coordinates a natural choice. The polar coordinate transformation is \(x = r \cos \theta\) and \(y = r \sin \theta\), which simplifies describing circular regions.
03

Determine Limits for \(r\) and \(\theta\)

In polar coordinates, the radius \(r\) varies from 0 to the boundary defined by \(r = 3 \sin \theta\). The angle \(\theta\) varies from 0 to \(\frac{\pi}{2}\) because we are in the first octant and \(x\) is non-negative.
04

Set Up the Double Integral

The volume \(V\) is calculated as: \[ V = \int_0^{\pi/2} \int_0^{3 \sin \theta} z \cdot r \, dr \, d\theta \]where \(z = r \sin \theta\). Substitute and rearrange the integral:
05

Compute the Inner Integral

Substituting \(z = r \sin \theta\), the inner integral becomes:\[ \int_0^{3 \sin \theta} r \sin \theta \cdot r \, dr = \int_0^{3 \sin \theta} r^2 \sin \theta \, dr \]Compute the inner integral with respect to \(r\):\[ \sin \theta \int_0^{3 \sin \theta} r^2 \, dr = \sin \theta \left[\frac{r^3}{3}\right]_0^{3 \sin \theta} = \sin \theta \cdot \frac{(3 \sin \theta)^3}{3} \]
06

Simplify Inner Integral Result

Substitute \((3 \sin \theta)^3 = 27 \sin^3 \theta\):\[ \frac{27 \sin^4 \theta}{3} = 9 \sin^4 \theta \]
07

Compute the Outer Integral

Substitute the result from Step 6 into the outer integral:\[ V = \int_0^{\pi/2} 9 \sin^4 \theta \, d\theta \]This is a standard integral that can be solved using trigonometric identities or a table of integrals.
08

Solve the Outer Integral

Use the identity \(\sin^4 \theta = \left(\frac{1 - \cos(2\theta)}{2}\right)^2\) to simplify and solve the integral, or integrate directly to get the final result:\[ V = \frac{3\pi}{8} \] after evaluating the integral.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Polar Coordinates
Polar coordinates are particularly useful for problems involving symmetry around a point, often the origin of our coordinate system.
Instead of using the usual x-y coordinate grid, polar coordinates describe a point in space using a distance from the origin, r, and an angle from a reference direction, \( \theta \). This makes it easier to represent circles and radial boundaries.
In this exercise, the surface equations are given in terms of r and \( \theta \), making polar coordinates a natural choice for simplifying the problem.
  • Polar coordinates express x and y in terms of r and \( \theta \):
  • \( x = r \cos \theta \)
  • \( y = r \sin \theta \)
Understanding these transformations helps in visualizing and setting boundaries for solids in three-dimensional space, like the task at hand.
Triple Integration
Triple integration is the method of integrating a function of three variables over a three-dimensional region.
It is an extension of double integration, which is used for area, to compute volume by adding a third variable for height. In this exercise, however, we determine the volume in the first octant using a double integral because the function is already simplified in polar coordinates.The integral is split into inner and outer integrals, with the inner integral often involving the radius r, and the outer concerning the angle \( \theta \). For this problem:
  • The inner integral computes the volume over varying \( r \): \( \int_0^{3 \sin \theta} r^2 \sin \theta \, dr \)
  • The outer integral sums these slices over all \( \theta \): \( \int_0^{\pi/2} 9 \sin^4 \theta \, d\theta \)
This method simplifies calculating volumes by breaking the problem into manageable parts. The calculations involve substituting expressions for z, in terms of polar coordinates, into the integral to properly define the region of interest.
First Octant
The first octant refers to the region in 3D space where all three coordinates, x, y, and z, are non-negative.
This confines the solid to one eighth of the entire space around the origin, where typically, geometrical figures are more easily analyzed.
For this problem, only points where \( r \geq 0 \), \( \theta \geq 0 \) and \( z \geq 0 \) are considered, simplifying the bounds of integration.In the first octant, \( \theta \) ranges from 0 to \( \frac{\pi}{2} \), which corresponds to one quarter of a full circle, effectively limiting the volume to the positive x and y coordinates.
  • Bound by \( x = 0 \) and \( y = 0 \)
  • Generally, also by \( z = 0 \) at the bottom and some surface on top
This spatial restriction helps to pinpoint exact volumes with fewer calculations, as the symmetry and positive axes limit possibilities.

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Most popular questions from this chapter

These exercises reference the Theorem of Pappus: If \(R\) is a bounded plane region and \(L\) is a line that lies in the plane of \(R\) such that \(R\) is entirely on one side of \(L,\) then the volume of the solid formed by revolving \(R\) about \(L\) is given by $$\text {volume}=(\text {area of } R) \cdot\left(\begin{array}{c}{\text {distance} \text {traveled}} \\ {\text {by the centroid}}\end{array}\right)$$ Use the Theorem of Pappus to find the volume of the solid that is generated when the region enclosed by \(y=x^{2}\) and \(y=8-x^{2}\) is revolved about the \(x\) -axis.

(a) Verify that $$ \left|\begin{array}{ll}{a_{1}} & {b_{1}} \\ {c_{1}} & {d_{1}}\end{array}\right|\left|\begin{array}{ll}{a_{2}} & {b_{2}} \\ {c_{2}} & {d_{2}}\end{array}\right|=\left|\begin{array}{ll}{a_{1} a_{2}+b_{1} c_{2}} & {a_{1} b_{2}+b_{1} d_{2}} \\ {c_{1} a_{2}+d_{1} c_{2}} & {c_{1} b_{2}+d_{1} d_{2}}\end{array}\right| $$ (b) If \(x=x(u, v), y=y(u, v)\) is a one-to-one transformation, then \(u=u(x, y), v=v(x, y) .\) Assuming the necessary differentiability, use the result in part (a) and the chain rule to show that $$ \frac{\partial(x, y)}{\partial(u, v)} \cdot \frac{\partial(u, v)}{\partial(x, y)}=1 $$

Writing An early popular approach to defining surface area was to take a limit of surface areas of inscribed polyhedra, but an example in which this approach fails was published in 1890 by H. A. Schwartz. Frieda Zames discusses Schwartz's example in her article "Surface Area and the Cylinder Area Paradox, "The Two-Year College Mathematics Journal, Vol. 8, No. 4, September 1977, pp. \(207-211 .\) Read the article and write a short summary.

Evaluate the iterated integral by converting to polar coordinates. $$ \int_{0}^{1} \int_{0}^{\sqrt{1-y^{2}}} \cos \left(x^{2}+y^{2}\right) d x d y $$

Find the center of gravity of the cube that is determined by the inequalities \(0 \leq x \leq 1,0 \leq y \leq 1,0 \leq z \leq 1\) if (a) the density is proportional to the square of the distance to the origin; (b) the density is proportional to the sum of the distances to the faces that lie in the coordinate planes.

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