Subsections

# Numerical Integration and Polar Coordinates

## Purpose

The purpose of this lab is to give you some experience with using the trapezoidal rule and Simpson's rule to approximate integrals.

## Getting Started

To assist you, there is a worksheet associated with this lab that contains examples and even solutions to some of the exercises. You can copy that worksheet to your home directory with the following command, which must be run in a terminal window, not in Maple.

cp /math/calclab/MA1023/NumInt_start.mws ~


You can copy the worksheet now, but you should read through the lab before you load it into Maple. Once you have read to the exercises, start up Maple, load the worksheet NumInt_start.mws, and go through it carefully. Then you can start working on the exercises.

## Background

In class we have talked about the trapezoidal rule and Simpson's rule for approximating the definite integral

Both methods start by dividing the interval into subintervals of equal length by choosing a partition

satisfying

where

is the length of each subinterval. For the trapezoidal rule, the integral over each subinterval is approximated by the area of a trapezoid. This gives the following approximation to the integral

For Simpson's rule, the function is approximated by a parabola over pairs of subintervals. When the areas under the parabolas are computed and summed up, the result is the following approximation.

There are many times in math, science, and engineering that coordinate systems other than the familiar one of Cartesian coordinates are convenient. In this lab, we consider one of the most common and useful such systems, that of polar coordinates.

### Graphs in Polar Coordinates

The main reason for using polar coordinates is that they can be used to simply describe regions in the plane that would be very difficult to describe using Cartesian coordinates. For example, graphing the circle in Cartesian coordinates requires two functions - one for the upper half and one for the lower half. In polar coordinates, the same circle has the very simple representation .

These are three types of well-known graphs in polar coordinates. The table below will allow you to identify the graphs in the exercises.

 Name Equation cardioid or limaçon or rose or

### Intersections of Curves in Polar Coordinates

Finding where two graphs in Cartesian coordinates intersect is straightforward. You just set the two functions equal and solve for the values of . In polar coordinates, the situation is more difficult. Most of the difficulties are due to the following considerations.
1. A point in the plane can have more than one representation in polar coordinates. For example, , is the same point as , . In general a point in the plane can have an infinite number of representations in polar coordinates, just by adding multiples of to . Even if you restrict a point in the plane can have several different representations.
2. The origin is determined by . The angle can have any value.
These considerations can make finding the intersections of two graphs in polar coordinates a difficult task. As the exercises demonstrate, it usually requires a combination of plots and solving equations to find all of the intersections.

## Exercises

1. For each of the definite integrals given below, find the exact value of the integral using the int command. Then find the minimum number of subintervals needed to approximate the integral using the trapezoidal rule and then again using Simpson's rule with and error no greater than 0.001. Which method is better and why?

2. Find all points of intersection for the pair of curves in polar coordinates given by the equations and for .
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