Double triple integrals, Polar coordinates

Multidimensional Integration

In Vector Calculus, we have to worry about integrating over two or three variables: double integrals or triple integrals.

โˆฌA f(x,y) dxdy
โˆญV f(x, y, z) dxdydz

Double integral can be interpreted as a volume, like a single integral is the area under the curve. When the limits don’t depend on any variable, and we could do integrals separately.

Polar coordinates

Polar coordinates is the most widely used curvilinear coordinate system in two dimensions. Polar coordinates, uses vector r and angle it makes with x-axis ฮธ, instead of x and y. And the length of the vector is denoted by r. We have unit vectors associated with polar coordinates:

  • r^ in the direction of increasing r (the length of the vector).
  • ฮธ^ in the direction of increasing angle (the angle the vector makes with the x-axis).

They are just a rotation of the i j unit vectors through an angle theta:

r^ = cosฮธ i + sinฮธ j
ฮธ^ = -sinฮธ i + cosฮธ j

The main difference with these curvilinear coordinate systems with the Cartesian coordinate system, is that the unit vectors depend on the position of the vector (they’re a function of ฮธ). The derivatives of r^ and ฮธ^ with respect to ฮธ have interesting relations.

dr^/dฮธ = ฮธ^
dฮธ^/dฮธ = -r^

The del operator โˆ‡ in polar coordinates:

โˆ‡ = r^ โˆ‚/โˆ‚r + ฮธ^ (1/r) โˆ‚/โˆ‚ฮธ

Using the operator โˆ‡, we could further define divergence โˆ‡ โˆ™ u, curl โˆ‡ ร— u and Laplacian โˆ‡ โˆ™ โˆ‡ in polar coordinates.

Polar coordinates divergence curl Laplacian

Central force

Newton’s law is F = ma. A central force means that you define your coordinate system so that the force is basically pointing from the object to the origin of the coordinate system.

Center force, Change of variables.

Change of Variables

It is probable that doing integral is hard in Cartesian coordinates, but easy in Polar coordinates. So to do that, we need to change variables in the integral; from an integral in Cartesian coordinates to an integral in polar coordinates, in 3 steps:

  1. Substitute the integrand
  2. Transform the infinitesimal unit, e.g: dxdy
  3. Change the limits of integration, e.g.: inverse function

When changing variables for double integral, the main difficulty will be transforming infinitesimal unit. It is important to remember the “change of variables formula”:

โˆฌA f(x,y) dxdy
Let x = x(s,t), y = y(s, t)
dxdy = | det(J) | dsdt
J is Jacobian matrix โˆ‚(x, y) / โˆ‚(s, t)
Change of variable, Cylindrical coordinates, Spherical coordinates.

Cylindrical coordinates

Polar coordinates (r, ฮธ) can be extended to 3-dimensional cylindrical coordinates (ฯ, ฯ†, z) by adding a new parameter z, which is the vertical height above the x, y plane. The position vector is now wirtten as:

r = ฯ ฯ^ + z z ^

Spherical coordinates

Spherical coordinates (r, ฮธ, ฯ) is the geometry associated with a ball or sphere.

Spherical coordinates, unit vector, del operator, Laplacian, divergence, curl.

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