Chapter 13: Problem 38
A solid is described along with its density function. Find the center of mass of the solid using spherical coordinates. (Note: these are the same solids and density functions as found in Exercises 31 through \(34 .)\) The cone bounded above \(z=\sqrt{x^{2}+y^{2}}\) and below the plane \(z=1\) with density function \(\delta(x, y, z)=z\).
Short Answer
Step by step solution
Convert the Given Surfaces to Spherical Coordinates
Determine the Limits of Integration
Express the Density Function in Spherical Coordinates
Set Up the Triple Integral for Mass
Evaluate the Integral for Mass
Set Up and Evaluate Integrals for the Center of Mass Coordinates
Compute the Center of Mass
Unlock Step-by-Step Solutions & Ace Your Exams!
-
Full Textbook Solutions
Get detailed explanations and key concepts
-
Unlimited Al creation
Al flashcards, explanations, exams and more...
-
Ads-free access
To over 500 millions flashcards
-
Money-back guarantee
We refund you if you fail your exam.
Over 30 million students worldwide already upgrade their learning with Vaia!
Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Spherical Coordinates
- \( \rho \) - the radial distance from the origin to the point.
- \( \phi \) - the angle measured from the positive z-axis.
- \( \theta \) - the azimuthal angle in the xy-plane from the positive x-axis.
- \( x = \rho \sin \phi \cos \theta \)
- \( y = \rho \sin \phi \sin \theta \)
- \( z = \rho \cos \phi \)
Density Function
When translating this function into spherical coordinates, you replace \( z \) with \( \rho \cos \phi \). Therefore, the density function becomes \( \delta(\rho, \phi, \theta) = \rho \cos \phi \). This modification is crucial when setting up integrals, as it maintains the proportional relationship between mass and position within the solid.
Interfaces with density become essential, especially when calculating mass, centers of mass, and other integral-related measures.
Triple Integral
The triple integral of a density function over a region will yield the total mass of a solid:\[ M = \int \int \int \delta(\rho, \phi, \theta) \, dV \]In spherical coordinates, the volume element \( dV \) is expressed as:\[ dV = \rho^2 \sin \phi \, d\rho \, d\phi \, d\theta \]Thus, the integral for mass becomes:\[ M = \int_0^{2\pi} \int_{\pi/4}^{\pi/2} \int_{\sec \phi}^{1} \rho^3 \cos \phi \sin \phi \, d\rho \, d\phi \, d\theta \]Each part of this integrand accounts for different elements: \(\rho^3\) accounts for radial distance calculations, \(\cos \phi\) integrates the z-component of density, and \(\sin \phi\) adjusts the surface area measure akin to a Jacobian adjustment in a coordinate transformation. This step forms the backbone of physical calculations involving volume and mass.
Limits of Integration
- \( \theta \) ranges from \( 0 \) to \( 2\pi \), covering the entire circular range around the z-axis.
- \( \phi \) spans from \( \frac{\pi}{4} \) to \( \frac{\pi}{2} \), representing the angle of the cone intersecting a plane.
- \( \rho \) stretches from \( \sec \phi \) to 1, neatly specifying the radial starting and stopping points with respect to the surfaces that bound the solid.