More calculus with parametric curves

07 Theory - Distance, speed

Theory 3

Distance function

The distance function returns the total distance traveled by the particle from a chosen starting time up to the (input) time :

We need the dummy variable so that the integration process does not conflict with in the upper bound.


Speed function

The speed of a moving particle is the rate of change of distance:

This formula can be explained in either of two ways:

  1. Apply the Fundamental Theorem of Calculus to the integral formula for .
  2. Consider for a small change : so the rate of change of arclength is , in other words .
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08 Illustration

Example - Speed, distance, displacement

Speed, distance, displacement

The parametric curve describes the position of a moving particle ( measuring seconds). (a) What is the speed function?

Suppose the particle travels for seconds starting at . (b) What is the total distance traveled? (c) What is the total displacement?

Solution

(a)

Compute derivatives:

Now compute the speed:


(b)

Distance traveled by using speed.

Compute total distance traveled function:

Substitute and . New bounds are and . Calculate:

The distance traveled up to is:


(c)

Displacement formula:

Now compute starting and ending points.

For starting point, insert :

For ending point, insert :

Insert and :

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09 Theory - Surface area of revolutions

Theory 4

Surface area of a surface of revolution: thin bands

Suppose a parametric curve is revolved around the -axis or the -axis.

The surface area is:

The radius should be the distance to the axis:

This formulas adds the areas of thin bands, but the bands are demarcated using parametric functions instead of input values of a graphed function.

The formula assumes that the curve is traversed one time as increases from to .

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10 Illustration

Example - Surface of revolution - parametric circle

Surface of revolution - parametric circle

By revolving the unit upper semicircle about the -axis, we can compute the surface area of the unit sphere.

Parametrization of the unit upper semicircle:


Therefore, the arc element:

Now for we choose because we are revolving about the -axis.


Plugging all this into the integral formula and evaluating gives:

Notice: This method is a little easier than the method using the graph .

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Example - Surface of revolution - parametric curve

Surface of revolution - parametric curve

Set up the integral which computes the surface area of the surface generated by revolving about the -axis the curve for .

Solution

For revolution about the -axis, we set .

Then compute :

Therefore the desired integral is:

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Polar curves

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Videos, Organic Chemistry Tutor

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01 Theory - Polar points, polar curves

Theory 1

Polar coordinates are pairs of numbers which identify points in the plane in terms of distance to origin and angle from -axis:

Converting


Polar coordinates have many redundancies: unlike Cartesian which are unique!

  • For example:
    • And therefore also (negative can happen)
  • For example: for every
  • For example: for any

Polar coordinates cannot be added: they are not vector components!

  • For example
  • Whereas Cartesian coordinates can be added:

The transition formulas require careful choice of .

  • The standard definition of sometimes gives wrong
    • This is because it uses the restricted domain ; the polar interpretation is: only points in Quadrant I and Quadrant IV (SAFE QUADRANTS)
  • Therefore: check signs of and to see which quadrant, maybe need -correction!
    • Quadrant I or IV: polar angle is
    • polar angle is


Equations (as well as points) can also be converted to polar.

For , look for cancellation from .

For , try to keep inside of trig functions.

  • For example:
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02 Illustration

Example - Converting to polar: -correction

Converting to polar: pi-correction

Compute the polar coordinates of and of .

Solution

For we observe first that it lies in Quadrant II.

Next compute:

This angle is in Quadrant IV. We add to get the polar angle in Quadrant II:

The radius is of course since this point lies on the unit circle. Therefore polar coordinates are .

For we observe first that it lies in Quadrant IV. (No extra needed.)

Next compute:

So the point in polar is .

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Example - Shifted circle in polar

Shifted circle in polar

For example, let’s convert a shifted circle to polar. Say we have the Cartesian equation:

Then to find the polar we substitute and and simplify:

So this shifted circle is the polar graph of the polar function .

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03 Theory - Polar limaçons

Theory 2

To draw the polar graph of some function, it can help to first draw the Cartesian graph of the function. (In other words, set and , and draw the usual graph.) By tracing through the points on the Cartesian graph, one can visualize the trajectory of the polar graph.

This Cartesian graph may be called a graphing tool for the polar graph.


A limaçon is the polar graph of .

The shape of a limaçon is determined by the value of . Any limaçon can be rescaled to have this form:

: Limaçon satisfying : unit circle.

: Limaçon satisfying : ‘outer loop’ circle with ‘flat spot’, not quite a ‘dimple’:

: Limaçon satisfying : ‘cardioid’ ‘outer loop’ circle with ‘dimple’ that creates a cusp:

: Limaçon satisfying : ‘dimple’ pushes past cusp to create ‘inner loop’:

: Limaçon satisfying : ‘inner loop’ only, no outer loop exists:

: Limaçon satisfying : ‘inner loop’ and ‘outer loop’ and rotated :


Transitions between limaçon types, :

Notice the transition points at and :

The flat spot occurs when

  • Smaller gives convex shape

The cusp occurs when

  • Smaller gives dimple (assuming )
  • Larger gives inner loop
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04 Theory - Polar roses

Theory 3

Roses are polar graphs of this form:

The pattern of petals:

  • (even): obtain petals
    • These petals traversed once
  • (odd): obtain petals
    • These petals traversed twice
  • Either way: total-petal-traversals: always
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05 Illustration

Example - Finding vertical tangents to a limaçon

Finding vertical tangents to a limaçon

Let us find the vertical tangents to the limaçon (the cardioid) given by .

Solution

(1) Convert to Cartesian parametric using and :


(2) Compute and :


(3) The vertical tangents occur when . We must double check that at these points.

Substitute and observe quadratic:

Solve:

Then find :


(4) Compute the points. In polar coordinates:

In Cartesian coordinates:

At :

At :

At :


(5) Correction: is a cusp!

The point at is on the cardioid, but the curve is not smooth there, this is a cusp.

Still, the left- and right-sided tangents exists and are equal, so in a certain sense we could say the curve has vertical tangent at .

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