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Calculate The Double Integral R

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Double integrals involving r are fundamental in physics and engineering for calculating quantities like mass, charge, or work over two-dimensional regions. This guide explains how to set up and evaluate these integrals, including common coordinate systems and practical applications.

Introduction to Double Integrals

A double integral extends the concept of single integration to two dimensions. For a function f(x,y) over a region R in the xy-plane, the double integral calculates the volume under the surface z = f(x,y) above R. When r appears in the integrand, it typically represents a radial distance in polar coordinates.

Double Integral Formula

∫∫R f(x,y) dA = limn→∞ Σ f(xi,yi) ΔAi

The integral can be evaluated using either Cartesian coordinates (x,y) or polar coordinates (r,θ). Polar coordinates are often more convenient when the problem has circular or radial symmetry.

Double Integrals in Polar Coordinates

In polar coordinates, the double integral becomes:

Polar Coordinate Integral

∫∫R f(r,θ) r dr dθ

The factor r accounts for the increasing area of circular rings as r increases. The limits of integration for θ are typically from α to β, and for r from g(θ) to h(θ).

Key Consideration

The r in the integrand is distinct from the radial coordinate r used in the limits. The integrand's r comes from the Jacobian determinant of the polar coordinate transformation.

Applications in Physics

Double integrals involving r appear in several physics contexts:

  • Calculating mass distributions in circular plates
  • Determining electric charge in circular regions
  • Computing work done by radial forces
  • Analyzing fluid flow in circular domains

For example, the mass of a circular plate with density function ρ(r,θ) would be calculated as:

Mass Calculation

M = ∫∫R ρ(r,θ) r dr dθ

Worked Examples

Example 1: Simple Polar Integral

Calculate ∫∫R r dA where R is the unit disk (0 ≤ r ≤ 1, 0 ≤ θ ≤ 2π).

Solution

001 r · r dr dθ = ∫001 r² dr dθ

= ∫0 [r³/3]01 dθ = ∫0 (1/3) dθ = (1/3)(2π) = 2π/3

Example 2: Physical Application

Find the mass of a circular plate with radius 2 and density ρ(r,θ) = r.

Solution

M = ∫002 r · r dr dθ = ∫002 r² dr dθ

= ∫0 [r³/3]02 dθ = ∫0 (8/3) dθ = (8/3)(2π) = 16π/3

Frequently Asked Questions

Why do we include r in the integrand for polar coordinates?

The r in the integrand comes from the Jacobian determinant of the polar coordinate transformation. It accounts for the increasing area of circular rings as r increases, ensuring the integral correctly represents quantities like mass or charge.

When should I use polar coordinates instead of Cartesian coordinates?

Use polar coordinates when the problem has circular symmetry, when the region of integration is naturally described by angles and radii, or when the integrand depends on radial distance r.

What's the difference between the r in the integrand and the r in the limits?

The r in the integrand represents the radial distance and comes from the coordinate transformation. The r in the limits defines the radial boundaries of the region of integration and is independent of the integrand's r.