Transformations of Unit Vectors and Integration in Various Coordinate Systems, Exams of Abnormal Psychology

The relationships between unit vectors in different coordinate systems, including cylindrical and spherical coordinates, and discusses the rules for integrating vector fields in these systems. It covers line, area, and volume integrals, providing examples and explanations for each type.

Typology: Exams

2015/2016

Uploaded on 04/08/2016

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RELATIONS BETWEEN UNIT VECTORS
Cylindrical Cartesian:
ˆs = cos φˆx + sin φˆy
ˆ
φ=sin φˆx + cos φˆy
ˆz =ˆz
Spherical Cartesian:
ˆr = sin θcos φˆx + sin θsin φˆy + cos θˆz
ˆ
θ= cos θcos φˆx + cos θsin φˆy sin θˆz
ˆ
φ=sin φˆx + cos φˆy
Spherical Cylindrical:
ˆr = sin θˆs + cos θˆz
ˆ
θ= cos θˆs sin θˆz
ˆ
φ=ˆ
φ
INTEGRATION IN VARIOUS COORDINATE SYSTEMS
Line Integration Element:
dl=
ˆx dx+ˆy dy+ˆz dzCartesian
ˆs ds+ˆ
φsdφ+ˆz dzCylindrical
ˆr dr+ˆ
θrdθ+ˆ
φrsin θdφSpherical
1-Dimensional (Line) Integrals
Rules: Use dlas is, for integrals of the form Rv·dl, where vis some
vector field. Choose one nonconstant variable to be the integration variable.
Write down the (two) restrictions which define the line forming the integration
path, and use these to substitute out all other variables besides the integration
variable. Take the implicit differential (d) of both restriction equations, and
use these to substitute out any differentials of variables besides the integration
variable, if necessary.
Example: to integrate along the line specified by the two restriction equations
y= 3x+ 2 and z= 5, one would choose either xor yas the integration variable
(since zis constant, it isn’t suitable to be integrated over.) Assume in the
following that we decide to integrate over x. Then whenever yappears in the
integrand, we would replace it by 3x+ 2. Whenever zappears, we replace it by
5. Taking the differentials of the restrictions tells us that if dyappears in the
integrand, we are to replace it by 3dx, and if dzappears, we replace it by 0.
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RELATIONS BETWEEN UNIT VECTORS

Cylindrical ↔ Cartesian: ˆs = cos φ ˆx + sin φ yˆ φˆ = − sin φ ˆx + cos φ ˆy ˆz = ˆz

Spherical ↔ Cartesian: ˆr = sin θ cos φ xˆ + sin θ sin φ ˆy + cos θ ˆz θˆ = cos θ cos φ xˆ + cos θ sin φ ˆy − sin θ ˆz φˆ = − sin φ ˆx + cos φ ˆy

Spherical ↔ Cylindrical: ˆr = sin θ ˆs + cos θ ˆz θˆ = cos θ ˆs − sin θ ˆz φˆ = φˆ

INTEGRATION IN VARIOUS COORDINATE SYSTEMS

Line Integration Element:

dl =

ˆx dx + yˆ dy + ˆz dz Cartesian ˆs ds + φˆ s dφ + ˆz dz Cylindrical ˆr dr + θˆ r dθ + φˆ r sin θ dφ Spherical

1-Dimensional (Line) Integrals Rules: Use dl as is, for integrals of the form

v · dl, where v is some vector field. Choose one nonconstant variable to be the integration variable. Write down the (two) restrictions which define the line forming the integration path, and use these to substitute out all other variables besides the integration variable. Take the implicit differential (d) of both restriction equations, and use these to substitute out any differentials of variables besides the integration variable, if necessary. Example: to integrate along the line specified by the two restriction equations y = 3x + 2 and z = 5, one would choose either x or y as the integration variable (since z is constant, it isn’t suitable to be integrated over.) Assume in the following that we decide to integrate over x. Then whenever y appears in the integrand, we would replace it by 3x + 2. Whenever z appears, we replace it by

  1. Taking the differentials of the restrictions tells us that if dy appears in the integrand, we are to replace it by 3dx, and if dz appears, we replace it by 0.

2-Dimensional (Area) Integrals Rules: Find the normal nˆ to the integration surface (nˆ needs to be the outward normal, if the surface is closed, in Gauss’ Law and the divergence theorem). For flux integrals (those of the form

v · nˆ da, where v is some vector field), construct da = d^2 (r) by multiplying together the two components of dl which are perpendicular to ˆn. Substitute out the nonintegration variable using the restriction equation which defines the surface. For non-flux integrals, the rules to construct da are exactly the same, only ˆn is only used to find the perpendicular components of dl (and not used in any dot product). Example: The familiar expression for area of a sphere comes from choosing the surface of constant radius (r = R) in spherical coordinates. The outward unit normal vector is nˆ = ˆr, so the differential area element is da = r^2 sin θ dθ dφ. Since r = R is constant, we take it outside the integral and find that the area

of the sphere is

da = R^2

∫ (^) π

0

sin θ dθ

∫ (^2) π

0

dφ = 4πR^2. It is often convenient

to use the substitution

∫ (^) π 0 sin^ θ^ dθ^ =^

− 1 du, where^ u^ = cos^ θ.

3-Dimensional (Volume) Integrals Rule: Use all 3 components of dl multiplied together to construct dτ.

dτ = d^3 (r) =

dx dy dz Cartesian s ds dφ dz Cylindrical r^2 sin θ dr dθ dφ Spherical

Notes:

  • The overall length, area, or volume of an integrated region always comes from the limits of the integrals, and never from any alteration of dl, da, or dτ.
  • If the limits of a two- or three-dimensional region are not formed by surfaces where one coordinate is constant, then the ‘inner’ integral(s) (those integrated first) will have limits which depend upon the variables in the ‘outer’ integral(s) (those integrated later). Special Note on VECTOR integrands:
  • If integrating a vector field to get a vector answer out (for example: total (vector) force on a surface F =

(f /area) da, with no dot product on f to make it a scalar), express the vectors only in Cartesian components (even when using other coordinate systems to perform the integration)! (Otherwise, the vector components being ‘integrated’ together really belong pointing in different directions; Cartesian unit vectors are special because they always point the same direction). This need not be a concern in flux integrals, however; taking the ‘dot product’ of a vector integrand with ˆn turns it into a scalar integrand, and scalars have no direction and thus may be integrated with reckless abandon.